重装系统后,怎么再次安装正版的卡巴斯基_百度知道
色情、暴力
我们会通过消息、邮箱等方式尽快将举报结果通知您。
重装系统后,怎么再次安装正版的卡巴斯基
我的是3年版的，有光盘。我重装系统后怎么安装卡巴斯基，那个激活码可以再次使用在本机上吗？找不到激活码怎么办？
　　方法：　　使用正版卡巴斯基杀毒软件需要激活码，一般购买正版的激活码可以使用大约3次左右，如果的激活码没有使用超过3次，那么还是可以继续使用的，方法就是在卡巴斯基的激活界面输入激活码即可！
专业电脑维护
激活程序的步骤也与之前一样，当初购买的时候应该会有产品密码!
激活码还在有效期内，在重装后是可以继续使用的。如果你的激活码找不到了你好
本回答被提问者采纳
不过你有光盘的话，光盘里面应该包括软件和激活码了，如果你的激活码没有再给其他人用的话应该可以再次使用在本机的所以不担心啊。如果激活码找不到就去百度搜“天诺时空”或者“卡巴人”这两个网站下载key文件激活，激活方法网站里面都有介绍的，只是时不时会被封到时又要自己去重新找key激活重装系统后电脑里面对于这些账号信息的保存会丢失了
激活码很重要，不能忘记。kaba365网站找回激活码。用光盘安装，或者卡巴365网站下载。
其他1条回答
为您推荐：
其他类似问题
您可能关注的内容
重装系统的相关知识
换一换
回答问题，赢新手礼包会freestyle吗？ - 歌单 - 网易云音乐
会freestyle吗？
会freestyle吗？嗯？
播放：64次
网易云音乐多端下载
同步歌单，随时畅听320k好音乐
网易公司版权所有(C)杭州乐读科技有限公司运营：Multiple-scale-facies-and-reservoir-quality-variations-within-a-dolomite-body-Outcrop-analog-study
来源：互联网
责任编辑：张小俊字体：
tradingmultiples是什么意思交易倍数Quotesmustbeinvolumesofonetradingunitorintegralmultiplesofthatamount.Noindividualquotemayexceedninetradingunitsinvolume.申报数量须为一交易单位...OrderinMultiplesof是什么意思订单须以......的倍数为单位例如,multiplesof10,即必须是10,20,30等等=Complete=MultiplesAllowed=Optional=PendingReview=...Complete完成MultiplesAllowed允许多项Optional自愿的PendingReview待定查看Incomplete未完成NotYetAvailable还不可以Multiple-scale-facies-and-reservoir-quality-variations-within-a-dolomite-body-Outcrop-analog-study(图4)Multiple-scale-facies-and-reservoir-quality-variations-within-a-dolomite-body-Outcrop-analog-study(图6)Multiple-scale-facies-and-reservoir-quality-variations-within-a-dolomite-body-Outcrop-analog-study(图8)Multiple-scale-facies-and-reservoir-quality-variations-within-a-dolomite-body-Outcrop-analog-study(图11)Multiple-scale-facies-and-reservoir-quality-variations-within-a-dolomite-body-Outcrop-analog-study(图13)Multiple-scale-facies-and-reservoir-quality-variations-within-a-dolomite-body-Outcrop-analog-study(图20)
MarineandPetroleumGeology27(tradingmultiples是什么意思交易连锁商店multiples[英]['mʌltɪplz][美]['mʌltɪplz]n.&数&防抓取，好心游戏网提供内容，请查看原文。ContentslistsavailableatScienceDirecteachlineitemsmustbeorderedinmultiplesof100pcs是什么意...multiplesof100pcs每个项目必须有序的倍数100双语对照例句:Thismustbe防抓取，好心游戏网提供内容，请查看原文。MarineandPetroleumGeology精彩内容，尽在百度攻略：findthesumofallmultiplesof7between200aa1=203,a14=294,s=(203+294)*14/2=3479防抓取，好心游戏网提供内容，请查看原文。journalhomepage:/locate/mmultiplesofrestingmetabolism是什么意思?多种静止新陈代泄防抓取，好心游戏网提供内容，请查看原文。arpetgeo精彩内容，尽在百度攻略：Howmany4-digitnumbersarecommonmultiplesof7and11?要四位数字是7和11的公倍数,那么也就是说,从1000----9999里面有多少个数字是7和11的公倍数防抓取，好心游戏网提供内容，请查看原文。Multiple-scalefaciesandreservoirqualityvariationswithinadolomitebodyCOutcropanalogstudyfromtheMiddleTriassic,SWGermanBasinWhatistheaverage(arithmeticmean)ofallthemultiplesoften...102030...190这些数字的平均数是多少(10+20+30+40....+190)/19防抓取，好心游戏网提供内容，请查看原文。BastianSimonKoehrer*,ChristianHeymann1,FrankProusa2,ThomasAignermulti是什么意思问：multi是什么意思答：multi-前缀pref.1.表示"种种","多","多方面的"防抓取，好心游戏网提供内容，请查看原文。InstituteofGeosciences,UniversityofTuebingen,Sigwartstra?e10,72076Tuebingen,Germany精彩内容，尽在百度攻略：摄像机multi是干嘛用的答：multi接口可以让摄像机的信号直接输出到电视机上。防抓取，好心游戏网提供内容，请查看原文。articleinfo什么是Multi答：思博伦的Multi-GNSS模拟器可以根据测试场景参数，为车辆和卫星运动、信号特征、大气和其它效应等Multi-GNSS接收机的实际导航条件建立模型，从而重现GNSS接收机在动态平防抓取，好心游戏网提供内容，请查看原文。Articlehistory:相机上的Multi是什么意思答：多重防抓取，好心游戏网提供内容，请查看原文。Received10April2009Receivedinrevisedform31August2009精彩内容，尽在百度攻略：multibuysavings什么意思？答：multibuysavings什么意思？multi是multiple的缩写，multibuy即multiplebuy即多买同一物件。multibuysavi防抓取，好心游戏网提供内容，请查看原文。Accepted18September2009笔记本光驱上写着dvdmultirecorder这是刻录光驱吗答：你好！很高兴解答你的提问！请你阅读如下提示，排除烦恼。谢谢！1，笔记本电脑光驱面板上铭刻着DVDMultiRecorder，这显示其身防抓取，好心游戏网提供内容，请查看原文。Availableonline30September2009Keywords:multi是什么颜色问：multi是什么颜色答：混合色防抓取，好心游戏网提供内容，请查看原文。Dolomitebody精彩内容，尽在百度攻略：multi-hopnetwork是什么意思答：多跳网络：在无线网络中，任何无线设备节点都可以同时作为AP和路由器，网络中的每个节点都可以发送和接收信号，每个节点都可以与一个或者多个对等节点进行直接通信防抓取，好心游戏网提供内容，请查看原文。OutcropanalogstudyDVD-SuperMulti与DVD±RW的区别？答：DVD-RAMDVD-RAM的全称为DVD-RandomAccessMemory(DVD随机存储器)，是由在DVD标准争夺战中处于优势的三家公司联防抓取，好心游戏网提供内容，请查看原文。High-resolutionsequencestratigraphyReservoirqualitydistribution3D-modelingMulti-Touch和Retina显示屏有什么区别答：Multi-Touch是多点触控的意思，你可以用2根或更多的手指在屏幕上操作。Retina是视网膜的意思，在近距离观看时，人眼已经无法分辨单个像防抓取，好心游戏网提供内容，请查看原文。abstract精彩内容，尽在百度攻略：防抓取，好心游戏网提供内容，请查看原文。Thisstudyfocusesonaporousdolomitebodyintheproximalpartofanepeiriccarbonateramp(TriassicMuschelkalk,SouthGermanBasin),analogoustohydrocarbon-bearingdolomitereservoirsintheMiddleEast(e.g.KhuffandArabFormations).1.饥荒饥荒主人公威尔逊是个实验失败的科学家，一次实验时打开了收音机，收音机却传给他禁忌的知识，他造出了时空穿越器，启动后却不小心被传到了饥荒的时代。每个地图都会随机生成一个麦斯威尔的传送门，通过十五关有小弥弥，这看似是个勇士打败恶龙却变成恶龙的故事，实际背后的故事很有意思，不过我是个新手活不过第一晚∏_∏2.贪吃蛇大作战这个游戏是操纵一条小小蛇杀死其他蛇变大大粗粗蛇的游戏，据说国外有个大神玩到了几千万米，菜鸟表示666。不过这个游戏告诉我们，长大的我们渐渐失去了横冲直撞的勇气，想想也是哈~3.皮卡堂过家家虽然你要手机游戏但我强烈推荐这个电脑游戏，我很喜欢，它吧，我认为没钱玩不下去，除了天天做防抓取，好心游戏网提供内容，请查看原文。Thedolomitebodyismadeupofshoal,lagoonalandperitidalfaciestypesandisbuiltbyathree-foldhierarchyofcycles(3rd-orderto5th-order).Thebestreservoirqualityoccursin?nelycrystallinelagoonaldolo-mudstones(mean:K?37.8mD;4?20.2%)withmicro-intercrystallineandvuggyporosity.Coarselycrystalline,shoal-relateddolo-grainstonesshowvariablereservoirpotential(mean:K?30.1mD;4?4.4%)duetolatediageneticmodi?cation.Reservoirqualitysigni?cantlydecreasesinthenon-dolomitizedforeshoalsection(mean:K?4.5mD;4?3.6%).Stratigraphically,themostporousdolomiteoccursintheupperregressiveportionofthe3rd-ordercycle.Reservoirqualityprogressivelydecreasestowardsthelimybottomofthesection.分谁，adc340移速出鞋才400，荆轲出门就400，还没等跑呢，已经输了。没有位移adc350。荆轲出鞋你想跑都跑不了。现在荆轲有的出那个脱离战斗加60移速那个鞋。没法玩。不是技术不行，是先天压制。荆轲一个大半血放俩技能adc死了，除非带闪现跑。兰陵王秒adc分分钟的事，秒马克意识好能逃跑也得残。这游戏就看队友吧。前几天看队友选个周瑜和扁鹊，不想打了，挂机6分钟送了四个人头，经济辣三四千，对面橘子超神了，我拿大小姐慢慢玩，居然赢了。有时你想好好打，还是输。好难玩。防抓取，好心游戏网提供内容，请查看原文。Outcropmappingshowedhighlateralcontinuityforthedistributionoffaciestypesandporopermvaluesonthescaleofseveral10sofmeters.Withincorrelated5th-ordercycles,considerablefaciesandporopermheterogeneityisalreadyobservedonthe100sofmeters-scale.Ona1000sofmeters-scale,thefaciesandlithologydistributioniscontrolledbythegeometryofagentlyinclinedcarbonateramp.Duringregression,aprogradationalpatternisrecognized,markedbyabasinwardmigrationofbackshoalfaciesandadown-dipdecreaseofdolomitebodythickness.精彩内容，尽在百度攻略：这是我十九连败之后第一场胜利，自己看吧，对面齐刷刷的7级，我保存了录像回看了一遍，对面五个人没有一个打野的，而且从不顿草丛，一次配合也没有，期间我们伙死了好几次都没算人头，仅7分钟结束战斗，结束之后我去看最近比赛的人，对面的一个在线的都没有，我怀疑都是人机，十九连败后我说这局再输我就卸游戏了，结果第二十场秒赢。防抓取，好心游戏网提供内容，请查看原文。Lithology,faciesandporopermdatafromoutcropsandcoreswereusedfor3D-modelingwiththesoftwarePetrel.Themodeledvariationsintheporopermdistributionareconsistentwiththedegreeofheterogeneityexpectedforacombinationoflaterallypersistentlithologyandhighlyvariablefacies.Resultsofthisstudymayhelptobetterunderstandthereservoirheterogeneityofinnerrampdolomitebodiesandcanbeappliedtoimprovecharacterizationandmodelingofsimilardolomitereservoirs.大学的时候，班级一共三十个人，能组两个队伍5vs5，各种讨论战术，各种谁都不服。现在登上游戏，满满一页好友只有两三个在游戏中加的不认识的人在线，久久不显示正在游戏中。以前去网吧，爆满的网吧里玩其他游戏的不超过十个人，剩下全都是英雄联盟的。现在去网吧，再也看不到那种盛大的场景了，感觉玩英雄联盟的人少了之后，连通宵的人都少了。最深刻的感受是，排位拍了好久好久，还是没排到人，那一刻感觉，一切都回不到从前了。防抓取，好心游戏网提供内容，请查看原文。ó2009ElsevierLtd.Allrightsreserved.一星期前处个王者荣耀cp，加了微信一看，还挺好看。两个人发展感情很快，每天早安晚安，后来一起玩了游戏，我惊奇的发现，这个姑娘是真能bb啊，要是说玩的不好说几句队友，很正常，她会把全部说话开开，一个劲嘲防抓取，好心游戏网提供内容，请查看原文。1.Introduction精彩内容，尽在百度攻略：致Minecraft有一种游戏，叫做Minecraft.....我忘不了第一次玩MC的时候，撸掉的第一块原木，挖到了第一块钻石，第一次被苦力怕炸死，第一次见到末影人，并且怀着好奇心去和他对视，第一次找防抓取，好心游戏网提供内容，请查看原文。Anunderstandingofthedepositionalenvironments,strati-graphicoccurrencesanddiageneticpatternsofdolomitesiscrucialforexploration-scalepredictionand?eld-scalecharacterizationofhydrocarbondolomitereservoirs.大司马――我的梦想是开一家真皮网咖，本名韩金龙，是斗鱼直播平台旗下的一名签约主播。主播的内容当然是英雄联盟。直播时间段固定在每天下午三点到晚上八点，周三固定休息。其他时间段没特殊情况一般都会播。你是李时珍的皮，一生之敌愣头青！非常喜欢马老师的直播，幽默。马老师的贴吧微博都可以关注一波，时不时会有些小福利哟~~防抓取，好心游戏网提供内容，请查看原文。TheUpperMuschelkalk(MiddleTriassic)‘‘Rottweil-Formation’’(formerlycalled‘‘Trigonodus-Dolomite’’Formation)oftheSouthGermanBasinisaclassicinnerrampdolomitereservoiranalogcomposedofsubtidalcarbonatesassociatedwithtidal?atsand谢谢小秘书邀请(????)王者荣耀玩猴子用什么名字？个人认为玩猴子不一定非要去用与猴子相关的名字，既然题主就是有这样的需要，我绞尽脑汁想到了几个我个人认为还不错的名字。吃我一棒放屁都暴击齐天如果感觉只有文字很单调的话可以适当添加一些符号????????????????????????ζ?????????????????ζ?????????????n?????????????⊙●○①◎Θ⊙¤I★☆♀　??-?　?????├┝┞┟┠┡┢┣┤┥┦┧┨┩┪┫┬┭┮┯┰┱┲┳┴┵┶┷┸┹┺┻??oo?¤???ぁあぃいぅうぇえぉおかがきぎくぐけげこごさざしじすずせぜそぞただちぢっつづてでとどなにぬねのは防抓取，好心游戏网提供内容，请查看原文。*Correspondingauthor.Tel.:t1/t(Mobile);fax:t.精彩内容，尽在百度攻略：一如果是在游戏里打架的话那肯定MC赢咯，MC就是不用MOD不用指令不开创造，仗着人多也能把迷你狗们打到喊爹吧，适合打架的MOD我看非无尽贪婪莫属，无尽套穿满后不会再受到任何伤害，剑的伤害是∞，也就是说什么玩意都可以一刀放倒，而且都是无尽耐久的。无尽贪婪犯规？那再向迷你狗们亮拔刀剑吧，攻击快富有多样性，还能把你削的飞起来。还有一大杀器，就是命令方块！命令方块可以用tp把迷你狗全体位移虚空，kill指防抓取，好心游戏网提供内容，请查看原文。E-mailaddress:bastian.(B.S.Koehrer).1首先，其他人的回答都没抓到点子上。我手上就有一台小米5s，我来告诉你为什么这么卡！其实这是因为小米的温控降频锁核阻碍了你愉快地玩王者荣耀，目前解决的办法主要有两点∶一、想办法把手机电池的温度降到40摄防抓取，好心游戏网提供内容，请查看原文。Presentaddress:GeologicalCPaleontologicalInstitute,UniversityofHamburg,Germany.2以前玩大话最早是在05年，现在十多年了，那时候开始还买点卡，后来自己能跑200后，一直自己跑200挣点卡钱，一直也没冲过什么钱，直到他妈的有一次端午节任务，说出来是好事，但是塞翁失马焉知非福，我得了一防抓取，好心游戏网提供内容，请查看原文。Presentaddress:NederlandseAardolieMaatschappijB.V.,Assen,The精彩内容，尽在百度攻略：首先王者荣耀是属于一个推塔游戏再到团战游戏，而不是各打各的。实事证明车队打排位上分比起单排上分容易2.5倍，车队的胜率也比单排多19%左右。今天聊一下很多玩家都会遇到的情况。如果团灭敌方之后，是集合推防抓取，好心游戏网提供内容，请查看原文。Netherlands.感谢邀请，本人先说明一下，我的世界创始于2009年，迷你创建于啥时候？2015年！说minecraft抄袭垃圾迷你的，咋TM想的你！要你这么说Notch从2009年穿越到2015年抄袭迷你，再跑回去，防抓取，好心游戏网提供内容，请查看原文。/$Cseefrontmatteró2009ElsevierLtd.Allrightsreserved.doi:10.1016/j.marpetgeo.精彩内容，尽在百度攻略：如果是前期对线的话能打赢他的ADC的确不多，女警，奥巴马和他有的一拼。女警超远射程可以有很好的消耗效果，而且清兵特快，一旦推进了你的塔内，在你方塔下放三角阵或者八字，一字型夹子，那你补兵都不好补，只有呼叫打野。再说说奥巴马，前期超强存在，无论是清兵能力还是前期对拼因为他的被动都非常强，当然拼不过还有E逃跑，对线德莱文真的不好打他。如果要打纯后期单挑，德莱文带Q的斧子甚至可以两刀砍死其他ADC，他也防抓取，好心游戏网提供内容，请查看原文。lagoons.ItissimilartopartsoftheMiddlePermiantoLowerTriassicKhuffFormation(e.g.Al-Jallal,1995)andtheUpperJurassicArab-Cand-DFormationoftheArabianPlatform(e.g.Wilson,1985).Previousstudiesmainlyinvestigatedlithostratigraphy,facies我最后悔的是李白。。。哈哈手残个人觉得这些英雄容易买了后悔王者荣耀的英雄很多，但是新手就那么几个，虽然各种活动看上去能领的福利不少，但是能换成英雄的并不多，不是土豪的话，基本上一个月也就能搞1,2个英雄，那么有哪些英雄买了就很容易后悔呢？我们来看看吧？TOP5周瑜羽扇纶巾，谈笑间，樯橹灰飞烟灭。苏轼的一首赤壁怀古把周瑜的形象塑造得非常完美，再加上王者荣耀中小乔的地位一直不低，两人又有非常搭配的情侣皮肤，相信也有一部分人是在女朋友的要求下买这个英雄的。不过尴尬的是，他和小乔都是法师很难同时上场，本身作为法师的能力也不突出，买的好多都扔仓库了，只能期待他的重做归来了。TOP4哪吒我不知道有多少小伙防抓取，好心游戏网提供内容，请查看原文。¨derlin,;anddiagenesisofthisdolomitebody(e.g.Bru一般都会删除存档，但是千万不要这样做，发现自己辛辛苦苦创造的世界没有，真的会受到很大的打击。之前我的存档就被朋友不小心给删了一次，当时真的眼泪都在眼眶里打转了，那段时间真的心情非常的糟糕……“我的世界防抓取，好心游戏网提供内容，请查看原文。Bachmann,1973;Alesi,1984;SchauerandAigner,1997;ZeehandGeng,2001).Thisoutcropanalogstudyfocusesonthecharacter-izationanddistributionofreservoirqualitydolomiteona10sto1000sofmeter-scale.精彩内容，尽在百度攻略：wot属于比较冷门的类型，但好制作比较精良，虽然根据游戏性的需求做了点妥协，但还是有一定的真实度的，但“黄金五九”之类的做法还是有点反胃。毕竟wot的题材和操作门槛没办法让绝大部分人适应（虽然已经很简单了），就没办法属于快餐游戏，所以wot最初的目标人群是很明确的：军迷、坦克迷、二战迷。而这群人最初开始玩wot大约是在2010年（修改），作为二战坦克迷的我也是那个时间看到宣传片就马上开始玩了，一直到现在。当然其间有一段时间对d系感到失望透顶，放弃了一年多。到现在也在这游戏上花了累计有2-3千，算比较少的，比起人家一台金59就3千多（刚出时的价），算是保守得太多了。这算是我玩得时间最长的游戏，比防抓取，好心游戏网提供内容，请查看原文。Themainobjectivesofthisstudyare:(1)Todescribethefaciesdistributionwithinahigh-resolution谢邀。首先说一下王者荣耀的评分系统，根据你的击杀数，被杀数，助攻数还有参团率等一系列因素给你的评分。首先这个分数在有些情况下是很不合理的。举个栗子，李元芳打野很强，抢大龙小龙很快，偷到主宰对团队的贡献防抓取，好心游戏网提供内容，请查看原文。sequencestratigraphicframeworkinawell-exposedstudyarea(30?15km)inSW-Germany(FaciesandSequenceAnalysis).(2)Tocharacterizeporosityandpermeabilityparametersandtheir在这个困的睁不开眼得中午，你把我拉了过来，算了，说正题。支持那个游戏，说实话，我支持最开始，国外的我的世界，被网易一代理，作为一名学生党，哪有钱买啊，别说我穷，我真的掏不出来这45块钱，所以说，支持最开始国外的我的世界，迷你没啥可说，把原代码直接搬走了，查的时候还还加密了，明显有见不得人的地方。另外，如果去掉什么抄袭不抄袭，就单看游戏质量，就不一样了，迷你最让人讨厌的应该就是充值系统了吧，家具，玻防抓取，好心游戏网提供内容，请查看原文。distributionwithspecialattentiononsuper-permeable‘‘high-kstreaks’’(PoroPermAnalysis).精彩内容，尽在百度攻略：应该是我的世界好玩，添加一些mod，光影材质，动态光影，add-ons，皮肤，披风之类的。迷你世界的mod，皮肤，披风，add-ons，光影材质，动态光影都没有，而且这些有些要钱，里面的物品还要等级解锁，真服了这些迷你玩家是怎么玩下去的，联机方便怎么了，即使我没有盒子，我的世界也有自带的联机，只需输入电脑上的ip地址就行，在创建个世界，开启局域网世界。虽然是国版，但是也不能这么抄袭别人吧，那些支持防抓取，好心游戏网提供内容，请查看原文。B.S.Koehreretal./MarineandPetroleumGeology27(3871、一个连补刀都不用的游戏！王者相对lol来说却是简单的多，甚至站在旁边死掉的兵都会给你加钱，所以lol的玩家就觉得这是一个弱智的游戏，但是玩游戏不是为了开心吗？又不要打职业，娱乐就好！2、嫉妒心理可防抓取，好心游戏网提供内容，请查看原文。Fig.1.(A)EquatorialwestviewoftheEarthduringMiddleTriassictimes(fromBlakey,2008)(B)MuschelkalkpaleogeographyofcentralEurope(modi?edfromZiegler,1990那我们就来谈谈王者荣耀1v1模式厉害的英雄????(?￣???￣??)1、不知火舞火舞一套技能几乎是可以直接秒人的，特别是二技CD短，伤害高，还会减速，而且六段位连跳，可以直接让人吐血，但到了后期，能量需求比较高2、露娜露娜技人挺厉害的，后期也很肉，如果是遇上会玩的露娜，她可以把你杀到怀疑人生3、橘右京橘右京吸血也是挺6的，再加上二技能眩晕，杠杠的，在钻石王者局现在也很多人用4、花木兰花木兰我到没防抓取，好心游戏网提供内容，请查看原文。精彩内容，尽在百度攻略：我玩过的手游挺多，有保卫萝卜，植物大战僵尸，剑侠情缘手游等等，真正让我着迷的只有皇室战争，这是2016年现象级的全球最佳手游，2017年第二季度依然是最具吸引力手游之一，位列全球手游收入榜第二，3分钟防抓取，好心游戏网提供内容，请查看原文。).(3)Toevaluatethediageneticimpactonreservoirquality(Diage-neticAnalysis).楼主没有看过lck，只知道lpl吧。我觉得最强的是s5夏季赛skt，上单marin，打野bengi，中单faker，下路wolf加bang。我是狗粉，首先说为什么ad不选uzi，如果uzi是韩国人，在防抓取，好心游戏网提供内容，请查看原文。(4)Togenerate2D-stratigraphiccross-sectionsofsedimentaryand精彩内容，尽在百度攻略：今天是全中国和全高考生的大日子，那就是高考。对于高考想必很多人都是紧张的，尤其是家长和考生，三年来的努力都在7、8、9三日里体现了，在此小编也祝各位能够取得一个好成绩，上自己理想的大学。对于考试紧张压防抓取，好心游戏网提供内容，请查看原文。poropermarchitectureinordertounderstandlateralfaciesandreservoirqualitychangesonmultiplescales(Reservoirarchi-tectureanalysis).首先得看你在哪里，比如:1你在亚洲中国等地那你最先思考的是应该躲在哪里，毕竟这里禁枪人口又太密集，好一点的刀具也没多少，况且咱们又不是啥主角什么的出门就能捡个三棱军刺的，但是菜刀之流的千万别要拿，那玩意砍人太钝又太短，所以长棍是不错的，如果有信心可以去派出所和城管局刷装备，枪啊防爆盾什么的都是有的，但是体力不好的话就穿一套防刺服就行了，长电棍可以找一找的没有也没关系警棍可以前期勉强凑合一下。2你在防抓取，好心游戏网提供内容，请查看原文。(5)Toregionallymodelthedistributionofreservoirqualitydolo-mite(3D-modeling).Thisstudywasdesignedtobetterunderstandtheverticalandlateralcompartmentalizationandporopermarchitectureofperi-tidaldolomitereservoirs.Theresultsmaybeappliedto九年老玩家了，中间也穿插着玩过codol，前段时间还买了csgo（本人现在在日本留学，所以没考虑csgo国服）发现并不是我想象中的cs了，遂放弃。cf一直没断过，当然钱也没有少花，既然每天都要玩游戏，那么游戏应该算我生活的一部分，花点钱改善生活也无可厚非吧（个人观点，不喜勿喷）不说废话了，聊聊原因吧。首先，我本人就是喜欢枪战类游戏，从跟室友cs1.5联机到使命召唤6-10，到战地，反正就是喜欢。反而对dota，LOL这种类型的游戏玩不来也不感兴趣。其次，CF里有战队的基友每天一起野战、战俘，把妹打枪，吹逼。这种感情怎么可能随便断了呢？至于cf为什么没落了，个人感觉英雄级武器只是很主观（注意，不防抓取，好心游戏网提供内容，请查看原文。精彩内容，尽在百度攻略：怎么说，第一次有想写长篇评论的冲动……也许是刚刚看完b站楚河的录播的缘故吧……昨天看楚河直播，说是双方水军一个劲的带节奏，能看出来，是想给自己和对方一个台阶下，不想事情越搞越大，伤害的都是双方。没成想防抓取，好心游戏网提供内容，请查看原文。improve当然是CSGO啊！CSGO多有趣！CSGO有数多种枪支，分别是P90、P90、P90、P90、P90、P90、P90、P90、P90、P90、P90、P90……有二十多个地图，分别是dustII、du防抓取，好心游戏网提供内容，请查看原文。Fig.2.ChronostratigraphicandsequencestratigraphiccontextoftheUpperMuschelkalk(modi?edfromAignerandBachmann,1992).说《诛仙》与《七界传说》齐名，估计你会被喷出个爆款??我是看过的，这本书一开始还是不错的，后来吗，个人感觉有几个问题，1.各界的塑造不够，人物略少，整体缺乏“界”的气势，直观感觉其实都和一个门派差不多。2.人物刻画不足，女人们基本都是男主的迷妹，男人们有特色的没记住什么，男主令人印象最深刻的是他的种马，竟然连他一个师傅都难逃魔迪奥，在武侠仙侠这种尊师重道的小说中，这种情节太过违和，传出去绝对被各路防抓取，好心游戏网提供内容，请查看原文。388B.S.Koehreretal./MarineandPetroleumGeology27(精彩内容，尽在百度攻略：必须英雄联盟难啊！不要把手游的难度和端游来做比较，没有任何可别性的！那些扯什么王者荣耀难的，别逗我笑了，本人长期混迹于LOL一区白银，打王者荣耀目前没有一个赛季不在钻石以上。别说什么王者荣耀用户基数大防抓取，好心游戏网提供内容，请查看原文。reservoircharacterization,predictionandstaticreservoirmodelingofsimilarmid-toinnerrampdolomitebodiesintheMiddleEastandworldwide.2.Geologicsetting丧尸危机末日即将来临，人类文明一夜消失。没有救援，没有希望，我们各国幸存的老百姓及军队能否在满是丧尸的世界中与自己的爱人重逢和战斗？幸存下来的各国老百姓，是否能战胜这场看似无穷无尽的灾难，重建自己的家园？属于人类的亲情、友情、爱情，一切人性中美好的事物将会在这里升华；背叛、贪婪、自私，人性中的丑恶永远也不会与美好分离。注：本文部分内容源自马克思?布鲁克斯（MaxBrooks）的《丧尸生存手册》，和防抓取，好心游戏网提供内容，请查看原文。TheGermanBasinwasestablishedafterthebreak-upofthePermiansupercontinentPangeaduetoextensionaltectonicsandtheformationofseveraltroughsandhighsinCentralEuropeduringtheTriassic(Ziegler,1990).ThisintracratonicbasinwasseparatedfromtheTethysOceanbytheBohemianMassiftotheSE(Fig.1).《迷你世界》抄袭《Minecraft》是事实，有买《Minecraft》的版权的话，为什么《迷你世界》官方至今没把版权证明拿出来？《迷你世界》的皮肤人设极渣，还收费！艹！那么渣的皮肤也收费！《迷你世界》的游戏平衡性极差，一个方块也要收费。《迷你世界》的玩家素质很差，经常发一些侮辱《Minecraft》的言论。（有图为证。《迷你世界》的玩家老是说《迷你世界》的联机功能比《Minecraft》好，但他们不知道《Minecraft》的大型服务器可以支持百人以上的玩家，甚至可以支持千人以上的玩家。结尾我告诉大家:只要像《迷你世界》这样的垃圾游戏也能赚钱，还能有很多粉丝的话。国产游戏是不可能强大的！防抓取，好心游戏网提供内容，请查看原文。TheUpperMuschelkalktransgressionintheuppermostAnisiantoearlyLadinianconnectedtheGermanBasinwiththeopenTethysrealm.FullymarineconditionscausedagentlyinclinedSECNWdippingcarbonateramptodevelopwhichwasprobablysimilartothepresentdayArabianGulf(Aigner,1985).DuringtheUpperMuschelkalk,theGermanepicontinentalbasinwassituatedbetween35and43??Nofpaleolatitudeandcharacterizedbyasubtropical,semi-aridclimateheavilyaffectedbyhurricanesandwinterstorms(MarsagliaandKlein,1983;Aigner,1985;Parrish,1993).Paleocurrent-indicatingsedimentstructuressuggestthatstrongwindsprevailedinNEdirection(e.g.Aigner,1985;Braun,2003;KosticandAigner,2004).精彩内容，尽在百度攻略：玩了5年的起凡，不知道有没有人知道这个游戏。当时我还是小学的时候就比较火了（我08年6年级）。初一才开始到这个游戏。那个时候全班的男生百分之50都玩起凡。每天下课就聚在一起聊游戏。什么昨天我拿了两个mvp啊，几个破敌啊。谁谁谁是名将12啊（那个时候名将12很少，就相当于英雄联盟的王者）。反正每天就聊些这个。一放学就往网吧跑，叫上几个同学打几把10v10才肯回家。我玩的最凶的时候，每天早上5点就起来学校，学校7.50上课。中途还要去网吧打几把。后面发展到每个星期都要去通宵，中考那天晚上还要出去通宵，本来我成绩是全班第一的，当然是普通班，这里真的不是吹逼。因为玩游戏入迷导致高中没考上，最后交了择校防抓取，好心游戏网提供内容，请查看原文。Ageneralfaciesdistributionacrossthecarbonaterampincludesfourmainfaciesbelts(Aigner,1985):(a)asandynearshore(coastal)faciesbeltrepresentingclasticinputfromtheBohemianM(b)adolomiticbackbankfaciesbeltrepresentingthelagoonal(c)ahigh-energyshallowrampshoalfaciesbeltconsistingmainlyofskeletal/oolitican(d)adeeperrampforeshoaltooffshoalfaciesbeltmade要想逼格高最重要的一点是：走别人没走过的路叔本华曾说过这样一句话：有才之人，能击中别人无法击中的目标；天才，能击中别人连看都看不到的目标。Talenthitsatargetnooneelsecanhit.Geniushitsatargetnooneelsecansee.苹果逼格够高吧？世界首款无键盘全触屏手机IPHONE，谁提出来的？乔帮主乔布斯啊，逼格界的如来佛祖。乔布斯就是这样一个天才，永远能洞察世界的下一步的走向，领先世界五百年看到这你就要说了，现在就连小学生都用苹果手机，烂大街的东西哪还有什么逼格可言OK，你这么说了我也不反对，想要更有逼格的东西请你再看这张图你又要说了，你他妈在逗我？防抓取，好心游戏网提供内容，请查看原文。upofgradedstormbeds,argillaceouslimestonesandbasinalmarlstones.今天我要说的是关于本人的一个故事，一个关于《魔兽世界》JJC的故事个人认为魔兽世界PVP做的算是非常平衡了，首先天赋百花齐放，百家争鸣。部落最良心的地方就是不会出现土豪吊打潘康恼庵智榭龀鱿郑灰闶址雷ト。眯挠蜗吠峁┠谌荩氩榭丛摹Overthelastcentury,theUpperMuschelkalkFormationinSW-Germanyhasbeensubdividedbyawellde?nedlitho-andbiostratigraphicframework(e.g.Wagner,1913;Vollrath,1955a,b,c;精彩内容，尽在百度攻略：早在去年，新年后不再破解游戏和转载破解资源，三大妈全面转型，要发展成为集卖正版，出攻略的综合性网站。此事件起因，是因一家日本公司发给三大妈的警告信（函）引起，具体过程是三大妈破解（转载）了《三国志13》这款所谓的3A大作，#(喷)#(滑稽)这破游戏谁玩谁知道，这里不是我为三大妈说话，只因为这破游戏国区390RMB？就是190，都不会有几个人买的烂游戏，不知道光荣哪来的勇气定价如此高，今后光荣游戏一防抓取，好心游戏网提供内容，请查看原文。¨derlin,;Stier,1985).ThelithostratigraphyPaul,1936;Bru怎么样才可以一次抽到王者水晶呢？小编觉得很简单啊，想要一次就抽到王者水晶，最重要的就是要看你的RP好不好了。在王者荣耀中，王者水晶现阶段只能通过幸运夺宝来获取。王者荣耀王者水晶确实不是那么好抽，说到抽防抓取，好心游戏网提供内容，请查看原文。isbasedonbioclasticmarkerbeds(e.g.‘‘Spiriferina-Bank’’or‘‘Cycloides-Bank’’)orthinmarlstonebeds(e.g.‘‘Tonhorizontd’’).Duetotheverylowinclinationoftheramp(&0.1??)(e.g.Aigner,1985)andlowtectonicactivity,individualmarkerbedsareregionallycontinuousandtraceableoftenoverhundredsofkm.Abiostrati-graphicframeworkbasedonceratites(e.g.UlrichsandMundlos,1990),conodontsandostracods(Kozur,1974)wasestablished.AninitialsequencestratigraphicframeworkoftheGermanTriassicwasproposedbyAignerandBachmann(1992).Accord-ingly,theUpperMuschelkalkformstheTSTandHSTofa3rd-oderdepositionalsequence(Fig.2).3.Materialsandmethods战局逆风不放弃逆风翻盘是一件多么痛快的事情，有过经验的玩家都应该了解，战局逆风不代表输赢，万一对面浪了呢？万一对面吵架了呢？万一对面五个人打团就460呢？万一对面五个人掉线了呢？王者荣耀即将来到了赛季末，本来最初计划是七月初更新S8赛季，但是目前看来最早也是七月初更新S8赛季。想冲段位的看过来了，小白狐要将毕生的装比功力都传授给你们。排位上分心态好心态是一个很重要的东西，心情不好，那就不要打排位，匹配尽情的去送吧。认真对待排位，选择自己熟悉且强势的英雄，例如：诸葛亮、张飞、高渐离、杨戬、马可波罗、虞姬，等等。和谐上分勿争吵排位最令人输的不心甘的就是队友在吵架，或者自己在跟队友吵架，本来要赢了的防抓取，好心游戏网提供内容，请查看原文。TheinvestigateddatasetincludesdetailedsedimentologicaldescriptionsoffouroutcropsandcoresfromtwowellsinanareasouthwestofStuttgartandeastoftheBlackForestinSW-Germany(Fig.3).Thestudyareabelongstothedolomiticbackbankfaciesbeltde?nedbyAigner(1985).Thesectionsloggedforthisstudycoverastratigraphicintervalfromthe‘‘Tonhorizontd’’,aregionallytraceableshalehorizon,totheMuschelkalkCKeuperFormationboundaryatthetopofthesection.Thisrepresentstheupperpartoftheregressive3rd-orderhemi-sequence(HST)oftheUpperMuschelkalk(Fig.2精彩内容，尽在百度攻略：).Fig.3.LocationofthestudyareainSW-GermanywithUTM-coordinatesofallquarriesandwellsassociatedwiththisproject.Bluebox?areausedforPetrelmodeling.(Forinterpretationofthereferencestocolorinthis?gurelegend,thereaderisreferredtothewebversionofthisarticle.)精彩内容，尽在百度攻略：B.S.Koehreretal./MarineandPetroleumGeology27(391精彩内容，尽在百度攻略：Thework?owusedtocharacterizethesectionfolloweda1D(facies-,sequenceandporopermanalysis)to2D(stratigraphiccorrelation)to3D(geologicmodeling)approachassuggestedbyKeransandTinker(1997)andAignerandSchauer(1998).Lithofaciesanalysiswascarriedoutbasedon350rocksamplescollectedfromoutcropsandcores.Handspecimenwascutintoslabsandpolishedinthelab.Allslabswereusedformacrofaciesanalysis(e.g.grainsize,sorting,compositionandtexture).Aportableoutcropgamma-ray(GR)scintillationcounterwasruninalloutcropsandquarriesapplyingaproceduredescribedinAigneretal.(1995).ForwellBetraanintegralGRlogwasprovidedbythe¨rttemberg.GeologicalSurveyofBaden-Wu精彩内容，尽在百度攻略：Faciessequences(5th-ordercycles)wereanalyzedandtheirstackingpatternswithinacyclehierarchywereinterpreted.SequenceanalysiswasbasedontheconceptofaccommodationversussedimentsupplysummarizedinCrossetal.(1993),CrossandLessenger(1998)andHomewoodetal.(2000).Forporopermanalysis,324plugsweredrilledfromtherocksamples.PorositywasdeterminedforallplugsusingaHe-drivenpycnometer.Permeabilitymeasurementsofplugswerecarriedoutusingagasminipermeameter.Twoorientationsweremeasuredoneachsample:fourparalleltobeddingandfourperpendiculartobedding.Thebulkpermeabilitywascalculatedforeachplug.Thinsectionswerepreparedfromtheplugsandstainedwithbluedyetohighlightporosity.Astandardtransmissionlightmicroscopewasusedformicrofaciescharacterization.PoretypesandcementmorphologywereanalyzedtounderstandporosityCpermeabilityrelationships.Thedolomiticthinsectionswereinvestigatedusingcathodoluminescence(CL)microscopytoiden-tifythesuccessionofcementgenerations.Additionally,blue-light?uorescencemicroscopywasappliedtomostofthedolomiticsamplestovisualizeprimaryfabricsandfossilsoverprintedby精彩内容，尽在百度攻略：dolomitization.Togetbettersampleresponses,thethinsectionswerebackedwithwhitepaperassuggestedbyDravis(1991).Alldataacquiredinoutcrop,coresandlaboratorywasinte-gratedincompositelogsusingthesoftwareWellCAD.Petrelwasusedtogenerate3D-modelsoflithology,facies,porosityandpermeability.4.FaciesanalysisPreviousfaciesstudiesoftheUpperMuschelkalkdolomiteswerecarriedoutmainlybyBachmann(1973),Alesi(1984)andSchauerandAigner(1997).Inthisstudy,theestablishedsedi-mentaryfaciesschemewasextendedandupdatedintoelevenlithofaciestypes(LFTs)(Table1).Thesefaciestypeswereinter-pretedasdepositsofagentlyinclinedcarbonateramp.4.1.Faciesassociations精彩内容，尽在百度攻略：Faciesweregroupedinto?vegeneticallyrelatedlithofaciesassociations(LFAs)ordepositionalsub-environments:offshoal,foreshoal,shoal,lagoonandtidal?at(Fig.4).4.1.1.OffshoalfaciesassociationThelow-energyoffshoalsub-environment(Fig.4)isdominatedbybioturbatedmudstones(LFT2)andargillaceous,laminatedmarlstones(LFT1)bothinterpretedassuspensiondepositsbelowstormwave-base(SWB).Thelow-energysettingisindicatedbyparalleltowavylaminationandthedominanceoflutiticcompo-nents.Pyritecrystalsanddarkcolorindicateoxygen-depleted,evenanaerobicconditionsindeeperoffshoalsettings.However,changingEh-conditionsarere?ectedbyichnofossilswhichpointtostrongvariationsbetweenwelloxygenateddeeperrampenviron-ments(e.g.Rhizocorallium)andweaklyoxygenatedbasinal精彩内容，尽在百度攻略：settingsFig.4.LithofaciestypesoftheUpperMuschelkalkepeiriccarbonateramp.The11lithofaciestypesde?nedinthisstudyarerelatedtoaspeci?cdepositionalenvironmentalonganidealcarbonateramppro?le(sabkhatooffshoal).Thedolomitebodyre?ectstheprotectedinnerramptocoastalenvironment.FWWB?Fair-weatherwave-SWB?stormwave-base.精彩内容，尽在百度攻略：392B.S.Koehreretal./MarineandPetroleumGeology27(Fig.5.Photodocumentationofshoal-associatedfaciestypes:(A)Outcropphotographofabioclasticlime-packtograinstone(LFT6)withtabularcross-bedding.Notelargeintraclastatbase.(B)Handspecimenofabioclasticdolo-pack-tograinstone(LFT6)withfaintlow-anglelamination.Theooid-dominatedgrainstoneportions(1)showasigni?cantamountofmoldicandintercrystallineporositywhilelayersofmediumgreydolomite(2)aretight.(C)Bioclasticdolo-packstonetodolo-grainstone(LFT6).Inthisthin-sectionphotographtheinternalstructureofooidsisoverprintedbydolomitizationpreservingthe(possiblylimonite)nucleiandrims.Coatedgrainsareoftenleachedandthen?lledagainwithcalciticcement.Onlythecoatingsareeitherpreservedorshowdolomitecrystalovergrowth.(D)Intercrystallineporosityandwell-connectedporespaceindolomitizedooliticgrainstone(LFT7)withplanar-edolomitefabric(thin-sectionphotograph).(E)Cross-beddedooliticdolo-grainstone(LFT7).OoidsandothercoatedgrainsbecomevisiblewithCL-microscopy.Notesigni?cantamountofintercrystallineporosity(black).(e.g.Chondrites).Thenodularbeddingstyleofsomeofthemudstonesisduetobioturbationortodiageneticoverprinting,representedbystyloliticseamsaroundthecontactsbetweenlimestonenodulesandmarldrapes.精彩内容，尽在百度攻略：4.1.2.ForeshoalfaciesassociationThemoderate-energyforeshoalsub-environmentisplacedbetweenfair-weatherwave-base(FWWB)andSWB(Fig.4).Scouredmud-towackestones(LFT3)andcoarselygrained,normallygradedskeletalwackestoneandpackstonesheets(LFTs4and5)interpretedastempestites(Aigner,1985)areinter-beddedwith?nelygrainedbioturbatedmudstonesandparalleltowavylaminatedmarlstonesindicatingcalmperiodsdominatedbysuspensionsettlingandbackgroundsedimentation.Hummockycross-strati?cation,low-anglelamination,dewater-ingstructures,monamalgam-ationpointstoslightlyreducedaccommodationspace.Therela-tivelackofooidsandmicriticenvelopesandtheabundanceofcrinoidalcolumnarplatesandossiclespointtoanopenmarineenvironment.精彩内容，尽在百度攻略：4.1.3.ShoalfaciesassociationThehigh-energyshoalsub-environment(Fig.5)includingtheshoalfringeischaracterizedbyseveraldm-thickbioclasticpack-tograinstones(LFT6)andcross-beddedooliticgrainstones(LFT7).Grainstonesarecommonlyverywellsortedandconsistofmicri-tizedooidsandroundedbioclasts(SchauerandAigner,1997精彩内容，尽在百度攻略：).B.S.Koehreretal./MarineandPetroleumGeology27(393Fig.6.Photodocumentationofbackshoal-andtidal?at-associatedfaciestypes:(A)Oncoliticdolo-wackestone(LFT8).OncoidsofthespeciesGirvanella(Peryt,1980)nucleatearoundpartlyleachedbioclasts(1).Layersofcoarselygraineddolomitecrystalsalternatewithsetsof?nelygraineddolomite.(B)Mottledpeloidaldolo-wacke-topackstone(LFT9)witha?nelycrystallinedolomitetextureshowingabundantblackpebbles(redarrow).(C,D)Microbiallylaminateddolo-mudstone(LFT11)withalternatinglayersofmicrobiallaminites(1)andpeloidalwashovers(2).(E)Burroweddolo-mud-towackestone(LFT10).Abundantvugsareinterpretedasremnantsofgypsum/anhydritenodulesarrangedinanearlychicken-wiretexture.(F)Burroweddolo-mudstone(LFT10)showingvuggyporosity.Vugsindolo-mudstoneare?lledwithwhitesaddledolomiteandshowblack,possiblylimonite,rims.Bluedyeindicatesporosity.(Forinterpretationofthereferencestocolorinthis?gurelegend,thereaderisreferredtothewebversionofthisarticle.)精彩内容，尽在百度攻略：Grainstoneswithsimilarfeatureshavebeendescribedfromseveralmodernenvironmentsandareproducedinshallow(&5m)waterordetachedshoalsettings(e.g.modernArabianGulf).Packstoneandgrainstonetexture,cross-beddingandtheappearanceofooidsandshellhashindicatesedimentationandreworkingduetofrequenthigh-energyhydrodynamicconditionsandlowaccom-modationspace.Thinpatchesofgrainstonesintercalatedwithmoremuddylagoonalsedimentsrepresentstorm-inducedspill-overlobesorchannelsands.4.1.4.Backshoalfaciesassociation精彩内容，尽在百度攻略：Thelow-energybackshoalenvironment(Fig.6ACB)consistsofoncoliticdolo-packstones(LFT8),laminateddolo-marlstones(LFT1)andburrowedpeloidaldolo-wackestonestodolo-packstones精彩内容，尽在百度攻略：394B.S.Koehreretal./MarineandPetroleumGeology27(Fig.7.Faciesmodelandcycletypes:Simpli?ed3D-faciesblockdiagrambasedonapaleoenvironmentalreconstructionoftheobservedlithofaciesassociationsoftheUpperMuschelkalkepeiriccarbonateramp.Dominantsedimentaryprocessesintheprotected(lowwave-andstorm-energy)backshoalenvironmentaremicrobialbinding(tidal?at)andbioturbation(lagoon).Notethattheclastichinterlandisnotpresentinthestudyareabutisobservedinthesubsurface.FWWB?Fair-weatherwave-SWB?stormwave-base(lowerpart).Theidealizedprogradingshallowing-upwardfaciessequenceinferredfromthefaciesmodelcanbeseparatedinto?vemainsmall-scale(5th-order)cycletypesdiagnosticofspeci?csub-environmentsontheramp.Notethicknessdecreaseofcycletowardsthelowaccommodationtidal-?atsetting(upperpart).(LFT9).Shallowshelteredwatercausedbythebaf?ingactionofbarrier-likeshoalsisindicatedbytheabundanceofpeloids(mostlyfecalpellets),intensebioturbationandoncoids.Oncoidsarecommonlybetween5and30mmindiameterandoftheGirvanella-type(Peryt,1980).精彩内容，尽在百度攻略：4.1.5.Tidal-?atfaciesassociationInthetransitionzonefromthesubtidalbackshoaltotheintertidalzone?nelygrained,burroweddolo-mudstonesanddolo-wackestones(LFT10)arecoveredbymicrobiallylaminateddolo-mudstones(LFT11).Thesebiogenicmatsshowdome-likeorwavystructures(Fig.6CCD)whichpointtoaformationwithinashallowsubtidalenvironment(Smithetal.,2004).Episodichigh-energystormeventswashedpeloidsontothetidal?at(peloidalgrainstones)andledtothereworkingofpartlylithi?edmicrobiallaminites(?at-pebbleconglomerate).Thevery?nelygrained,burroweddolo-mud-todolo-wacke-stones(LFT10)commonlyshowmm-tocm-sizedvugs(Fig.6ECF).Thesestrataboundvugsmostlikelyformedduetothedissolutionofpatchilydistributedevaporitenodules(chicken-wirefabric)andindicatesupratidaloverprinting(SchauerandAigner,1997).4.2.Conceptualfaciesmodel精彩内容，尽在百度攻略：Basedonthedetailedfaciesanalysisand1D-verticalstackingpatterns,thespatiallateraldistributionofthesefaciestypeswasinferredaccordingtoWALTHER’slaw.A2DfaciesmodeloftheUpperMuschelkalkepeiriccarbonaterampwithidealizedlateralfaciesrelationshipswasdeveloped.ItisbasedonaSWCNEtransectthroughthestudyareaparalleltothepaleo-diplineoftheUpperMuschelkalkcarbonaterampoveradistanceofsome10sofkm(Fig.4).Thestudieddolomitebodyrepresentsthelagoonaltotidal-?atenvironmentoftheramp.Itisseparatedfromtheopenmarine,outerrampsettingbyshore-parallel,ooliticCbioclasticshoalpatches(Aigner,1985).Aconceptual3DdepositionalmodelisshowninFig.7,inte-gratingtheregionalknowledgeofthefaciesdistribution.5.Sequenceanalysis精彩内容，尽在百度攻略：Cyclicfaciessequencesofdifferentscaleswereobservedintheinvestigatedareabyanalyzingverticalfaciessuccessions.Athree-foldhierarchyofcycleswasobserved:small-scale(5th-order),medium-scale(4th-order)andlarge-scale(3rd-order).5.1.Small-scalecycles(5th-order)ThesmallestscaleofcyclicityintheUpperMuschelkalkis0.2C5minthickness.Thesesedimentaryunitslikelyrecorda100,000yearMilankovitchsignalandareconsequentlyinterpretedas5th-ordercycles(Aigneretal.,1999).Them-thickcyclesarereadilyrecognizedincoresandoutcropsections.Ascyclesymmetryandfaciesstackingpatternofindividualcyclesvaryalongthedeposi-tionalgradientandbathymetryasafunctionoflateralshiftsinaccommodationspace(Crossetal.,1993),small-scalecyclescouldbefurthersubdividedintoseveralgroups.Whereastheundolo-mitizedpartoftheUpperMuschelkalkisbuiltupbysubtidalforeshoal,shoalmarginandshoalcycles(Aigner,1985;KosticandAigner,2004),thedolomitebodyitselfiscomposedof精彩内容，尽在百度攻略：shallowing-B.S.Koehreretal./MarineandPetroleumGeology27(395Fig.8.Outcropappearance,thin-sectionphotographsandsimpli?edfacieslogofonetypicalsubtidalshoalsmall-scalecycle(5th-order)observedinquarryFrommenhausen.精彩内容，尽在百度攻略：upwardsubtidalshoalandbackshoalcyclesinthelowerpartandperitidalbackshoalcyclesintheupperpart.Thispatternre?ectstheoverallshallowing-upwardtrendoftheuppermostMuschel-kalk(SchauerandAigner,1997)(Fig.2).5.1.1.SubtidalshoalcyclesThistypeofcycle(Fig.8)ishighlyasymmetricalandcanbefoundinthetransitionzonebetweenlimestoneanddolomite.Itsthicknessvariesbetween1.5and3m.Thelowerpartofthecycleismadeofmassivebioturbatedmudstones(LFT2)andlaminatedmarlstones(LFT1)intercalatedwithgradedskeletalwacke-topackstonesheets(LFT4)andmassiveamalgamated,poorlysortedpackstonebeds(LFT5).Towardsthetop,thecycleconsistsofdm-thickbioclasticoolitic(dolo-)pack-to(dolo-)grainstones(LFT6)andoolitic(dolo-)grainstones(LFT7).Thegrainstonescommonlydisplaycross-beddingandahighamountofmicriticenvelopes,coatedgrainsandooids.Thesearecappedbygradedskeletalwacke-topackstones(LFT4)thatareoftenamalgamated(LFT5)followedbybioturbatedmudstonesandlaminatedmarlstones.精彩内容，尽在百度攻略：Thiscycleisinterpretedasaprogradingshoal(Aigner,1985).Afaciesshiftfrombasinalmarl-andmudstonestogradedandamalgamatedforeshoaltempestitesand?nallytoshallowwatershoalfaciesofthemidrampsuggestsaregressivehemicycle.Thisregressivetrendisfurtherindicatedbyenhancedmicrobialactivity(e.g.micriticenvelopesandcoatedgrains).Theregressivemaximumoccursatthetopofthebioclasticooidalpack-tograinstonesthatrepresentthetimeofmaximumdepositionalenergy.Thethintransgressivepartisrepresentedbyouterrampfacies,beiteitherbioturbatedmudstonesorlaminatedmarlstones.5.1.2.SubtidalbackshoalcyclesThiscycletype(Fig.9)occursinthelowerandmiddlepartofthedolomitebodyandformsalmostsymmetriccycles0.5C2minthickness.Thelowerpartofthecyclesconsistseitherofoncoliticdolo-packstones(LFT8)orooliticgrainstones(LFT7).Theupperpartofthecycleismadeupofbioturbatedpeloidaldolo-wacke-stonetodolo-packstones(LFT9)thatareintercalatedwithlami-natedmarlstones(LFT1).Burrowingiscommonandprimarystrati?cationisfullyorlargelydestroyed.精彩内容，尽在百度攻略：High-energyfaciestypesmarkthetransgressivephaseofthiscycletype.Reworkedintraclastsanderosivebasesindicatetrans-gressivesurfaces.Onlydm-thickbedsofooliticsediments,probablyrepresentingstormspilloverevents,arefoundinthebasalpartofthecycles.Oncoliticpackstonesareinterpretedasshore-paralleleventsheetsbehindtheooliticshoals(SchauerandAigner,1997).Thesedepositsareoverlainbyburrowed,peloid-richlagoonalfaciesandlaminatedmarllayers,depositedinaverylow-energylagoonalsetting,mostlikelywithinthewaveshadowofshoalbodies.5.1.3.PeritidalbackshoalcyclesTheperitidalbackshoalcycletypeisthethinnestofallcyclesdistinguishedinthisstudyandreachesathicknessofonly0.2C0.5m(Fig.10).Thesestronglyasymmetricalcyclesoccuronlyintheupperpartofthedolomitebody.Atthebase,burroweddolo-mud-towackestones(LFT10)arefoundwhichareoverlainbymicro-biallylaminatedmudstones(LFT11)intheupperpart.Insomecases,thelaminitesandtheburroweddolo-mud-towackestonesshowaprominentvuggyappearance.Themicrobialmatsareinturnagainsharplyoverlainbyburrowedwackestones.Reworkingofmicrobialmatsiscommon,leadingtotheformationof?at-pebbleconglomerates.精彩内容，尽在百度攻略：Thiscycleisinterpretedasprogradingtidal?atmostlikelysimilartomodernexamplesfromtheTrucialCoast(Shinn,1983).Autocyclicorallocyclicchangesmayleadtothis‘‘lowaccommo-dation’’-peritidalcycletype.Atransitionfromburrowedlagoonal精彩内容，尽在百度攻略：396B.S.Koehreretal./MarineandPetroleumGeology27(Fig.9.Outcropappearance,thin-sectionexamplesandsimpli?edsedimentologicallogofsmall-scalesubtidalbackshoalcycles(5th-order)inthedolomitebodyofquarryFrommenhausen.Thetransgressivehemicycleisindicatedbyanerosivecontactatthebase,frequentreworkingandlargeoncoiddebris.Oncoliticdolo-wackestone(LFT8)orooliticgrainstones(LFT7)verticallygradeintolagoonalbioturbatedpeloidaldolo-wackestone(LFT9).depositstointertidalmicrobiallaminitesindicatesashallowing-upwardsequence.Thevugs,occuringinsomeoftheobservedcycles,areinterpretedasleachedevaporitenodulesformedaroundpeakregressionundersupratidal(sabkha)conditions.5.2.Medium-scalecycles(4th-order)精彩内容，尽在百度攻略：Stacksofupto5small-scalecycles(5th-order)formtrans-gressiveCregressivemedium-scalecycles,3C10minthickness.Thesecyclesetsareinterpretedas4th-ordercyclesandaremostlytraceableovertensofkm.Theyarelaterallyvariableinthickness,faciesmake-upandgeometry.Thestudieddolomitebodyiscomposedof3C4medium-scalecycles.Theseconsistofstackedsubtidalandperitidalbackshoalsmall-scalecycles(Fig.11).Thestackingpatternwithrapidverticalfacieschangesre?ectsalowaccommodationsettingduringthelatehighstandofthe3rd-orderMiddletoUpperMuschelkalkdepositionalsequence(Fig.2).Medium-scalecyclesdisplaythelateralshiftoffaciesbelts,re?ectingthemedium-termchangesofrelativesealevel.5.3.Large-scalecycle(3rd-order)TheentireUpperMuschelkalkwasdepositedduringa3rd-orderriseandfallofthelateAnisiantoearlyLadinianeustaticsealevel(Aigner,1985;AignerandBachmann,1992)(Fig.2).ThustheMiddleandUpperMuschelkalkisinterpretedasonealmostsymmetrical,transgressiveCregressive3rd-orderdepositionalsequence(large-scalecycle)whichistransgressivelycappedbythe‘‘Grenzbonebed’’oftheoverlying‘‘Lettenkeuper’’Formation.6.Diageneticanalysis精彩内容，尽在百度攻略：Intheframeworkofthisstudy,abasicdiageneticanalysisusingstandardpetrographyandCL-microscopywascarriedouttoeval-uatethediageneticimpactonreservoirquality.Nostableisotopeandtraceelementsanalyseswerecarriedout.6.1.PreviousdiageneticstudiesAlesi(1984)andDernai(1994)suggestedthatthedolomitiza-tiontookplaceaccordingtotheearlydiageneticevaporative¨andSiegenthaler(1969)andthemixingpumpingmodelofHsu精彩内容，尽在百度攻略：watermodelofBadiozamani(1973).SchauerandAigner(1997)distinguisheda?rstevaporativedolomitizationphasefollowedbytwoburialdolomitizationphasesanda?nalcementationphaseoflatediageneticsparrycalcite.ZeehandGeng(2001)assumeanearlyevaporativedolomitizationandtworecrystallizationeventsduringburialconditionsunderthein?uenceofmixedmarine/meteoricwatersandadeepburialsaddledolomitecementation.6.2.CementandporositytypesBasedonfaciesandtexture,differentdolomiteandporositytypescouldbedistinguished(Figs.12and13).Dolomitetextureisclassi?edinthisstudyafterSibleyandGregg(1987),porosityisde?nedafterChoquetteandPray(1970).6.2.1.Mud-dominatedstrata精彩内容，尽在百度攻略：Shallowsubtidaltointertidaldolo-mud-andwackestones(LFTs10C11)consistofa?nelycrystallinedolomite(crystalsize&30mm)精彩内容，尽在百度攻略：B.S.Koehreretal./MarineandPetroleumGeology27(397Fig.10.Exampleofperitidalbackshoalcycles:(Upperpart):Peritidalsmall-scalecycle(5th-order)withsupratidaloverprint.Vugsarepartly?lledwith(latediagenetic)saddledolomite.(Lowerpart):Peritidalsmall-scalecycle(5th-order)withoutsupratidaloverprint.Microbiallaminitesarereworkedatthebaseofthetransgressive精彩内容，尽在百度攻略：hemicycle.Fig.11.Stackingpatterndiagramshowingthevariationsofaccommodationspaceandtheevolutionofthesedimentaryenvironments(foreshoaltobackshoal)alongaverticalsectionofquarryFrommenhausen.Small-scalecycles(5th-order)correspondtosmall-scalecyclicfacieschangesandstacktoformmedium-scalecycles(4th-order).TheoverallregressivepatternofthelateHST(3rd-ordercycle)isindicatedbytheoveralldecreaseinaccommodationspace.Arrowscorrespondtomedium-scalecyclicity.ForfaciescolorcodingseeFig.6.精彩内容，尽在百度攻略：398B.S.Koehreretal./MarineandPetroleumGeology27(Fig.12.Cathodoluminescence(CL)investigationsondolomiticsamplesfromtheinvestigateddolomitebody:(A)Dulltonon-luminescentsaddledolomite(SD)partlyin?llinganhydrite-dissolutionvugofshallowsubtidaldolo-mudstone(LFT10).Noteplanar-stononplanardolomitefabric(generation1)displayingahomogeneousreddishluminescencewithoutzonation(1).(B)Peloidaldolo-wacke-topackstone(LFT9)displayingthreedolomitegenerationsfromrighttothecenterofthephoto:?nelycrystallinedolomites(generation1)withoutzonation(1),zonedmedium-crystallinedolomiterhombs(2)ofgeneration2thatbothshowreddishluminescenceandcoarselycrystallinedolomiterhombs(3)withdullluminescence(generation3).(C)CL-microscopyofooliticdolo-pack-tograinstonesample(LFT6)showstwogenerationsofdolomites:medium-crystallinezoned,planar-edolomiterhombs(generation2)overprintingooidsandbioclastsshowingreddishluminescence(2)andanon-luminescentgeneration3formingtheouterrimsofthecrystals(3).Residualintercrystallineporespaceisoccludedwithlatediagenetic(generation4)calcitespar(4)withalternatingbrightandnon-luminescentzoning.(D)Porespaceinthisooliticdolo-grainstone(LFT7)islargely?lledwithorange-toyellowishluminescentcalcitecement(generation5)withoutzonation(5).(E)CL-photographofooliticdolo-grainstone(LFT7)showingorange-luminescent,latecalcitecement(5)entirelyoccludingtheporespacebetweenplanar-e,dullluminescentdolomiterhombs(2).Noterelict,yellow-orange-luminescent,zonedsparrycalcite(4).(F)CL-photographofooliticdolo-grainstone(LFT7).Non-luminescentouterrims(3)ofplanar-edolomiterhombs(2)andbrightluminescentcalcitecement(4)arepartlyleachedawayindicatingmeteoricdissolution.Noteooidghoststructure(centerbottom).Porespaceingreen.(Forinterpretationofthereferencestocolorinthis?gurelegend,thereaderisreferredtothewebversionofthisarticle.)withaplanar-stononplanardolomitefabric.Theydisplayahomogeneousreddishluminescenceandnozonation(Fig.12A).Commonly,coarsesaddledolomiterhombswithdullluminescenceoccurinvuggyporespace.Themostcommonporetypeinthesefaciestypesismicro-intercrystallineporosity.Additionally,vuggyandfenestralporosityisobserved(Fig.13).精彩内容，尽在百度攻略：Dolo-wackestonesandmud-dominateddolo-packstones(LFTs8C9)arevariableindolomitetexturesandcrystalsizes(30C100mm),probablydependingonshellcontentandtheintensityofbioturbation.Theyshow?nelycrystallinedolomiteswithhomo-geneousreddishluminescence,medium-crystallinereddishdolo-miterhombsthatarezonedandcoarselycrystallinedolomiterhombswithdullluminescence(Fig.12B).Micro-intercrystalline(&20mm)andminorvuggyporosityismostcommon(Fig.13).6.2.2.Grain-dominatedstrataGrain-dominateddolo-packstonesanddolo-grainstones(LFTs6C7)showaplanar-stoplanar-edolomitefabricandcrystalsizesbetween50and200mm.Individualdolomitecrystalsarezonedinmostcasesanddisplayreddishtodullluminescence(Fig.12C).Puregrainstonesarecompletelydolomitizedbyzonedmedium-crystal-linedolomiterhombs.Theymostlyshowreddishluminescencewiththeouterzonesbeingnon-luminescent.Pack-tograinstonesmostcommonlyshowmacro-intercrystallineandmoldicporosity(Fig.13精彩内容，尽在百度攻略：).B.S.Koehreretal./MarineandPetroleumGeology27(399精彩内容，尽在百度攻略：Fig13.Idealizedfaciessuccessionofthedolomitebodyshowingrelationshipbetweentexture,lithofaciestype,poretypeandoverallporositydistribution.Themostcommonporositytypeisintercrystallineporosity.Dependingontheporesize(mmCmmscale),itwasreferredtoasmicro-ormacro-intercrystallineporosity.精彩内容，尽在百度攻略：6.3.DiageneticmodelThediageneticanalysissuggeststhefollowingdiagenetichistory(expandingonSchauerandAigner,1997)(Fig.14).6.3.1.InitialporespacecreationEvaporite-relatedearlydolomitizationoftheperitidalandmud-dominatedlagoonalfaciestypesresultedin?nelycrystallinedolomitepresentinLFTs8C11(dolomitegeneration1).精彩内容，尽在百度攻略：DisplaciveFig.14.Simpli?eddiagenetichistoryoftheinvestigateddolomitebody.1,2,3?dolomitegenerations1,2,3;SD?S4,5?calcitecementgenerations4,5(extendedfromSchauerandAigner,1997).精彩内容，尽在百度攻略：400B.S.Koehreretal./MarineandPetroleumGeology27(crystals(dolomitegeneration3).Similardolomitezonationwithredluminescentcoresandnon-luminescentrimsmayre?ectthequenchingeffectofincreasingFecontentonluminescence(Fair-child,1983)duringongoingburialdiagenesis(SchauerandAigner,1997).Deepburialdolomitizationisfurtherindicatedbytheemplacementofsaddledolomite(SD)(Fig.12A)observedinthevugsofperitidalfaciestypesinquarryFrommenhausen,oucropReustenandcoreBetra(Fig.3).ZeehandGeng(2001)estimateaformationtemperatureofsaddledolomiteofabout82C110??C.Theelevatedtemperaturesneededforsaddledolomiteformationareexplainedbyhydrothermaleventsrelatedtoriftinginthe‘‘Rheingraben’’.Withinthegrain-dominatedfaciestypes,porespaceispartlydiminishedbybrightluminescentmultiple-zoned,latesparrycalcitecement(generation4)(Fig.12C).Fig.15.Porosity/permeabilitycrossplotsbasedonmineralogyforalldolomiteandlimestonesamplesofallinvestigatedsections.Porosityisgenerallybetterin精彩内容，尽在百度攻略：dolomites.anhydritenodulesindicateperiodicsupratidalconditions(earlychicken-wirestructure).精彩内容，尽在百度攻略：Stabilizationofformerevaporativedolomitecrystalsduringshallowburialdiagenesisledtorecrystallizationandincreaseincrystalsizewithinthemud-dominatedstrata(LFTs8C11),andthedevelopmentofsigni?cantmicro-intercrystallineporosity(SchauerandAigner,1997).Withinthegrain-dominatedstrata(LFTs6C7),zoneddolomiterhombsarrangedinaplanar-efabric(dolomitegeneration2)wereformedleadingtomacro-intercrystallineporosity.6.3.2.PorespacecementationAdeepburialdolomitizationphasewithingrain-dominatedpackstonesandgrainstonesisindicatedbynon-luminescent(Fe-rich)rimsaroundredluminescentcoresofindividualdolomite6.3.3.Telogeneticmodi?cation精彩内容，尽在百度攻略：AstheMuschelkalkinSW-GermanywasupliftedandpartlyexposedtobecomeanimportantaquiferasaconsequenceofAlpinetectonics,telogenesisstronglymodi?edtheporenetwork(Fig.14).Leachingandcementationmostlikelyoccurredasmete-oricwaterscouldin?ltratethesectionalongfractures.Withinthegrainyshoal-associatedfaciestypes(LFTs6C7),thedissolutionoflatesparrycalcitecementandearlierdolomitegenerationsenhancedreservoirquality(Fig.12F).However,manypack-andgrainstonesareaffectedbyfurthercalcitecementationoccludingremainingporespace.Theseverylatecalcitematrixcements(generation5)showahomogeneousorangeluminescenceanddisplaynozonation(Fig.12DandE).Telogeneticmodi?cationwithinthemud-dominatedfaciestypes(LFTs8C11)islimitedtocommonfracturingandsolution-enlargementofchicken-wirevugs.Pronetometeoricalteration,theFe-richsaddledolomite精彩内容，尽在百度攻略：isFig.16.Porosity/permeabilitycrossplotsbasedonfaciesassociations.Theshoalfaciesassociationmadeupofpackstonesandgrainstonesshowsaveryvariablereservoirqualityduetoacomplexdiagenetichistorywithlatesparrycalcitecementationand/orleaching.B.S.Koehreretal./MarineandPetroleumGeology27(401精彩内容，尽在百度攻略：Fig.17.Porosity/permeabilitycrossplotbasedonporetype(classi?edafterLucia,1999)andthin-sectionphotographsofthemainporetypesobservedinthestudiedinterval.Thehighestporopermvaluesareobservedinsamplesshowingacombinationofinterparticale(IP),separatevug(SV)andtouchingvug(TV)porosity.(A)Burrowedpeloidaldolo-wacke-topackstone(LFT9)withfractureporosity(TV).(B)Solution-enlargedvugporosity(IPtSVtTV)inooliticdolo-grainstone(LFT7).(C)Isolatedandnot-connectedvuggyporespace(SV)inburroweddolo-wackestone(LFT10).(D)Intercrystallineporosity(IP)inaburrowedpeloidaldolo-packstone(LFT9).leachedasitisindicatedbydarklimoniterimsaroundtheedgesofthevugs(Fig.6F).7.PoropermanalysisThemostporoussamplesarepuredolomites(graindensi-ty&2820kg/m3).Theleastporoussamplesarepurelimestones(graindensity&2720kg/m3)(Fig.15).Inthedolomiticsamples,porosityrangesfrom0.1to32%(mean4:17.8%),permeabilityrangesfrom1.7to266mD(meanK:21.3mD).Inthelimestonesamples,porosityrangesfrom0.1to16%(mean4:3.6%)andpermeabilityrangesfrom0.4to213mD(meanK:4.5mD).Thebetterreservoirqualitywithinthedolomitesisexplainedbythenetworkofintercrystallineporosity,representingthemostcommonporositytypeinthedolomiticsamples.Thelimestonesshowinterparticleandminormoldicporosity.Onsetofdolomiti-zationineachofthesectionsisgradual,withanupto4m-thick精彩内容，尽在百度攻略：zoneofdolomiticlimestonebetweenthelowerlimyandupperdolomiticpart.Incontrasttothemorecompetentlimybottomoftheinvestigatedstratigraphicintervalthatislessjointedandfrac-tured,thelesscompetentdolomitebodyisoverprintedbyintensefracturing.Thesizeofthefracturesisextremelyvariable,rangingfromthemmtomscale.Intheinvestigateddolomitebody,porosityandpermeabilityarecontrolledbyseveralfactors:(1)Faciesanddepositionaltexture:Thehighestporopermvalues精彩内容，尽在百度攻略：areencounteredwithinthebackshoalLFA(mean:K?37.8mD;4?17.8%)andtidal-?atLFA(mean:K?29.8mD;4?20.2%)(Fig.16).TheseLFAscontainahighamountofmicro-inter-crystalline,vuggy,fenestralandminormoldicporosity(Fig.13).TheshoalLFA(LFTs6C7)generallyshowsfairreservoirquality(mean:K?30.1mD;4?4.4)duetothepresenceofmacro-intercrystallineporespace(Fig.16B).Pack-andgrainstonesin精彩内容，尽在百度攻略：402B.S.Koehreretal./MarineandPetroleumGeology27(¨tzingen.WallrunsECW(seemapofquarry).A)OutcropwallFig.18.MappingoffaciesandporopermdistributioninthedolomitebodyintheuppermostlevelofquarryMo精彩内容，尽在百度攻略：photograph.B)Wallpaneloffaciestypes.C)Wallpanelofporopermvalues.B.S.Koehreretal./MarineandPetroleumGeology27(403Fig.19.Localcross-sectionintheReustenareashowingthelateralfaciesdistributionalonganepeiricramptransectslightlyobliquetodipdirection.Notefaciesinter?ngeringwithinonesmall-scalecycle(5th-order)onthescaleofhundredsofmeters.精彩内容，尽在百度攻略：theoutcropsandcoresarestronglyaffectedbylatediagenesis(telogenesis),asmentionedabove.Thelimyoff-toforeshoalLFAs(LFTs1C5)showfairreservoirpotential(mean:K?21.6mD;4?9.7%).Forthesefaciestypeshowever,sampleswereonlytakenfromthe?eldorcorewhereporespacewasalreadyvisiblewiththenakedeye.Thusthecalculatedaveragevaluesdonotrepresentthebulkvolumeofthelimestonesectionasitiscommonlytightduetoearlycalcitecementationandthegeneralscarcityofporespace.(2)Differentialdiagenesis:Thegrain-dominateddolomitizedstrata(LFTs6C7)inthestudiedoutcropsandcoreshasaveryvariablereservoirqualitywithveryloworveryhighpermeabilities(1C135mD)dependentonthedegreeoftelo-geneticleaching(poroperm-generation)(Fig.16C)orcemen-tation(poroperm-destruction)(Fig.16A).Forthedolomitizedmud-dominatedintervals(LFTs8C11),itseemslikelythatearlydolomitizationisthedrivingfactorofporositycreation.Theytendtohavehighmicro-intercrystallineporosityandfairpermeability.精彩内容，尽在百度攻略：(3)Poretype:Poretype,classi?edafterLucia(1999),seemstobeanimportantcontrollingfactorforreservoirqualitydistribu-tion(Fig.17).Samplesbasedonpureseparatevug(SV)ortouchingvug(TV)porosityscatterinazoneofverylowtolowporosity(usually&10%)andpoortomoderate精彩内容，尽在百度攻略：permeability404B.S.Koehreretal./MarineandPetroleumGeology27(精彩内容，尽在百度攻略：Fig.20.Distributionofporosityandhigh-kstreaksinthedolomitebody.Reservoirqualityisgenerallybetterintheupperpartofthesection.Thecross-sectionisorientedslightlyobliquetothepaleo-dipdirectionoftheepeiriccarbonaterampinSSECNNWdirection.B.S.Koehreretal./MarineandPetroleumGeology27(405精彩内容，尽在百度攻略：406B.S.Koehreretal./MarineandPetroleumGeology27(Fig.22.Petrel-modelingresults:(A)3D-lithologymodelgeneratedbyadeterministic,interactivedrawingapproach.Dolomitethicknessdecreasesdown-dipfromSEtoNW.(B)3D-faciesmodelgeneratedbysequentialindicatorsimulationresultsinamosaic-likefaciesdistributionofalowaccommodation,backshoalsetting.(usually&20mD).Sampleswithinterparticle(IP)porosityshownocleartrendor?elds,incontrasttocombinationsofIPwithotherporetypes.PlugswithIPtSVporespacealsodisplayawidescatter.However,sampleswithIPtTVporositytendtoreachhigherpermeabilitiesthansampleswithIPtSV.Thehighestporosity(upto31%)andpermeability(upto266mD)valuesarereachedbysampleswithIPtSVtTVporespace.精彩内容，尽在百度攻略：(4)Stratigraphicposition:Porositygenerallyincreasestowardsthetopofthesectionwithinthelatestagesofregressionofthelarge-scale(3rd-order)cycle(Figs.20and21).There,theabundanceofmuddybackshoaltotidal-?atdeposits(LFTs9C11)andtheirearlydolomitizationappearscriticalforthedevelopmentofreservoirqualityporosity.Incontrast,porosityprogressivelydecreasestowardsthecalciticbottomofthesection.精彩内容，尽在百度攻略：Inconclusion,oursamplesrevealedthatthepetrophysicalpropertiesofthestudiedcarbonaterocksarecontrolledbyaninterplayofseveralparameters.Theinitialdistributionoffaciestypesandtheiroccurrencewithinindividualcyclesseemstohaveonlylimitedin?uenceonporosityCpermeabilityrelationshipsasdepositionaltexturesarestronglymodi?edbylatediageneticreductionorenhancementofporespace.精彩内容，尽在百度攻略：Fig.21.Regionalcross-sectionshowingmeasuredsectionswithgamma-ray(GR)logsandporopermdataforlocationsonacorrelationlinefromFrommenhausen(SE)toHaiterbach(NW)(seeFig.3).Othersectionswereprojectedontothecorrelationline.GRwasdirectlymeasuredintheoutcropswhileporopermvaluesweredeterminedthroughmeasurementofplugsinthelaboratory.Redlinescharacterizemedium-scale(4th-order)regressivecycletopsatthefall-to-riseturnarounds.Bluelinescharacterizethemedium-scale(4th-order)transgressivemaximarepresentedbythemaximum?oodingsurfaces(MFS)attherise-to-fallturnarounds.Notethatdolomitethicknessdecreasesdown-dipfromproximal(SE)todistal(NW)asthedolomitizationfront(dashedline)cross-cutsthecorrelatedmedium-scalehemicycleboundaries.ThedepthofthedolomitizationfrontintheReustenlogwasinferredfromFig.19(Reusten-Hail?ngensection).SeeFig.19forfaciescolorcoding.(Forinterpretationofthereferencestocolorinthis?gurelegend,thereaderisreferredtothewebversionofthisarticle.)B.S.Koehreretal./MarineandPetroleumGeology27(4078.Multi-scalereservoirarchitectureanalysis精彩内容，尽在百度攻略：Tounderstandthedistributionofreservoir-pronedolomiteandthelateralcontinuityoffaciesandporopermvalues,stratigraphiccross-sectionsonthefollowingscaleswereconstructed:1)tensofmeters,2)hundredsofmetersand3)severalkilometers.8.1.Tensofmeters-scaleMappingoftheupperpartofthedolomitebodyinquarry¨tzingen(Fig.3)showedhighlateralcontinuityofthedifferentMolithofaciestypesonthescaleof10sofm(Fig.18).Thereisvirtuallynochangeinlithologyalongthequarrywallsandonlyminorvariationsinsedimentarystructuresandcomponentsoccur.Lateralcontinuityalsoexistsfortheporopermvaluesin2Datthescaleofseveral10sofm.However,rapidverticalfaciesandporopermchangeswithinindividualsmall-scalecyclesonadm-scaleareobserved.精彩内容，尽在百度攻略：8.2.Hundredsofmeters-scaleSigni?cantporopermvariationswereobservedona100sofm-scale(Fig.20).Theverticalporositydistributiondoesnotshowthesameabsolutevaluesbutthesametendenciesforthethreesections.Itisgenerallybettertowardsthetopofthesectionsandcontinuouslydecreasestowardsthebottom.Three?eldscanbedistinguishedinallsections.The?rstwithaporosityof0C10%,thesecond?eldhasaporosityof10C20%andathird?eldthathasaporosityof20C30%(Fig.20).Lateralvariationsinporosityofupto20%withinseveralhundredsofmetersofdistanceareobservedwithinthedolomitebody(Fig.20),re?ectingthefaciesandporetypeheterogneitywithinalowaccommodationsetting.精彩内容，尽在百度攻略：Individual‘‘high-kstreaks’’occurwithindifferentfaciestypesandporosityzones.However,theyaremainlyconcentratedintheupperpartoftheinvestigatedsection.Theyseemtobeoflimitedlateralcontinuity,possiblywithamaximumarealextendofafewhundredsofmeters.Itmaybespeculatedthatthese‘‘high-kstreaks’’representintervalsexposedtoenhancedtelogeneticleaching,possiblyclosetooralongfractures.8.3.Thousandsofmeters-scaleThreeoutcropsectionsaroundthevillageofReusten,eachsome20mthick,werelogged(Fig.3).Astratigraphiccross-sectionwasconstructedonthescaleofaboutonekmbycorrelatingsmall-scale(3rd-order)andmedium-scale(4th-order)cycles(Figs.19and20).精彩内容，尽在百度攻略：Thelateralfaciesdistribution(Fig.19)showsthatthemarlstonebeds(LFT1)selectedasdatumhorizons(locallyknownas‘‘Ton-horizonte’’and‘‘Tonhorizontz’’)canbetracedcon?dentlyoverthisdistance.Someoncoliticdolo-packstones(LFT8)andbioclastic/ooliticpack-andgrainstones(LFTs6C7),however,wereonlytraceableoverafewhundredsofmeters.Theyshowalateraltransitionintolagoonalfaciestypes(LFT1,LFT9).Atthetopofthesection,microbiallylaminateddolo-mudstones(LFT11)andbur-roweddolo-mudstones(LFT10)showcommoninter?ngering.Thespatialdistributionoffaciesinthecross-sectionre?ectstheoverallregression(large-scaleregressivehemicycle)intheupperpartoftheUpperMuschelkalkwithabasinwardshiftofthetidal-?atfacies.Outcropandsubsurfacedatawerecorrelatedoveradistanceofsome20km(Fig.21).Thestratigraphiccorrelationisbasedonlaterallypersistentturnaroundsofmedium-scalecycles,peak-to-peakcorrelationofGRsignalsandmarkerbeds.Aprominentshalebedwaschosenasdatumforcorrelation(‘‘Tonhorizontd’’).Thisdatumhorizonre?ectstheinitialdepositionaltopographyofthecarbonaterampandiseasilyrecognizedbyadistinctivegamma-raypeak(Fig.21).Thecross-sectionrunsapproximatelyparalleltothepaleo-dipinSECNWdirection,perpendiculartopaleo-shoreline,fromthemostproximal,landwarddatapoint(quarryFrommen-hausen)tothemostdistal,basinwarddatapoint(wellHaiterbach).Theremainingdatapointsareprojectedonthecorrelationline.Itisevidentthatthethicknessofthedolomitereservoirbodydecreasesdown-dipfromproximal(SE)todistal(NW).Thedolo-mitizationfrontcross-cutsthecorrelatedtime-linesofmedium-scalecycleboundaries(Fig.21).Inproximalsections(e.g.精彩内容，尽在百度攻略：quarryFig.23.Upperthreemedium-scalecycles(4th-order)ofthefaciesmodel(viewfromNE).Lateralfacieschangesinthe3D-modelre?ectthecorrelationresultsondifferentscales(outcrop,localandregionalscale).精彩内容，尽在百度攻略：408B.S.Koehreretal./MarineandPetroleumGeology27(Frommenhausen),thedolomitereachesaverticalthicknessofupto20mwhereasindistalsections(e.g.wellHaiterbach)thedolomitedecreasestoabout8m.Thus,anoveralldolomitethicknessreductionofaround50%overadistanceof20kmisobserved.9.3D-geologicalmodelingTheintegrationofcoreandoutcropdataofsixdatapoints(Fig.3)wasusedtoconstructa3D-geocellularmodelofthelithology,faciesandporopermdistributionwithintheinvestigateddolomitebody(Figs.22C24).9.1.Modelconstruction精彩内容，尽在百度攻略：Themodelingwork?owusedisdescribedbyAigneretal.(2007)andPalermo(2007).Accordingly,lithology,faciesandpetrophysicaldatafromoutcropsandwells(ASCII-?les)wereloadedasverticalpseudo-wellsintoPetrel.Medium-scale(4th-order)hemicycleboundarieswerecorrelatedandpickedaswelltops(Fig.21).Aprom-inentshalebed(‘‘Tonhorizontd’’)waschosenasthelowerboundaryofthemodel.TheuppermodelboundaryistopMuschelkalk.Modeldimensionsare25?15km.Vertically8isochronoussurfacesweregeneratedfromthecorrelationpointsresultingin7zones.The3D-modelcomprises900,000gridcellswithalateraldimensionof250?250m.Eachofthezonesre?ectsthegeometryofonemedium-scale(4th-order)hemicycle.Themodelwasfurthersubdividedinto150layersenhancingtheverticalresolutionofthegridto20cmtoaccountfortheobservedrapidverticalfacieschangesonadm-scale.Lithologyandfacieswereupscaledusingthe‘‘most-of’’-algorithm.Porositywasupsc