桂西北晚古生代地层中的毗连不整合研究
|
摘要
桂西北右江地区广泛发育碳酸盐岩孤立台地,台地边缘发育大量沉积岩脉、角砾岩体、台地边缘同沉积正断层、及局部地层缺失造成的特殊界面,各要素之间的成因关系一直有争论。毗连不整合是指因同沉积断层作用使平坦地形变成强烈起伏的陡坡地形,粗碎屑物质快速沉积于地形凹处,新沉积的地层与早先坡下的较老基岩横向相接,因此造成新老地层之间的不整合,多形成于构造不稳定地区。国外地质学家最初将其识别为普通的角度不整合、陆架边缘不整合或者台地边缘不整合等等,国内地质学家也注意到了这类特殊界面,但在一些野外露头上观察其为断层面,而在另一些露头上观察其为侵蚀间断(不整合)面,由此产生争论:这类特殊界面是断层还是不整合?并产生很多名称:同构造沉积不整合、碳酸盐岩台地边缘围限断裂带、角度不整合接触带、陡崖式假不整合、事件沉积不整合、超覆不整合、构造窗和飞来峰等等,迄今为止没有统一。笔者等在研究广西晚古生代孤立碳酸盐岩台地边缘沉积岩脉和角砾岩体的过程中,发现特殊界面与沉积岩脉和角砾岩体关系密切,并发现如果将这些特殊界面归类于传统不整合面,均有与地质事实相矛盾的地方,因而认为其应重新归类。随着研究的深入:笔者等在凤山剖面的同一露头上观察到关键地质现象:特殊界面下部具断层特征,上部具溶蚀间断特征,因此认为其是遭受溶蚀的同沉积断层面。其成因是:同沉积构造十分活跃,使同沉积断层面上部来不及被新沉积物掩埋而遭受水下溶蚀,从而形成巨大地形起伏,造成新老地层横向相接,与Davis毗连不整合概念吻合,据此将这类特殊界面统一命名为毗连不整合。随即发现桂西北晚古生代地层内部广泛发育毗连不整合,并且发现晚古生代地层与下伏寒武系、及上覆三叠系之间也是毗连不整合接触,这是桂西北晚古生代地层及相关寒武系和三叠系的基本特色,由于毗连不整合代表区域地质构造活动强烈,表明桂西北地质构造从古生代到中生代一直处于活动状态,地层—构造活动记录与古特提斯域特征相似,属古特提斯洋的东沿部分。从而结束特殊界面是断层还是不整合的争论,为桂西北地层与构造的深入研究及其大地构造归属提供了新证据。
Objectives: Isolated carbonate platforms are widely observed in Youjiang River area,northwestern Guangxi.Many neptunian dykes,carbonate debris,synsedimentary normal faults,and special surfaces showing as local lost strata are observed in margins around those isolated carbonate platforms. There were different ideas about the relationships among these elements. Buttress unconformity refer to that megabreccia rapidly deposit in topographic low when synsedimentary normal faulting change flat terrain to steep topography,and cause the younger beds laterally abuts the older basement strata,and result in the unconformity between the younger beds and the older basement. Buttress unconformity generally formed in unstable structural regions. Until Davis(1984) named it as buttress unconformity,foreign geologists named it as angular unconformity,shelf-margin unconformity,platformmargin unconformity etc. Chinese geologists also observe those special surfaces of unconformity which shown as fault surface in some crops and shown as unconformity interface in some others,and named them as syntectonic sedimentary unconformity, carbonate-platform-margin limited fault zone, angular unconformity contact zone,escarpment-style pseudounconformity,event-sediment unconformity,unconformability of overlap,even tectonic window or klippe etc. Consequently cause argument for they are fault or unconformity,and for their different names.Methods: When study Late Palaeozoic isolated carbonate platform margin neptunian dyke and carbonatebreccia-body,author observes the paragenetic special surface and their difference from the sorts of known reported surfaces in Guangxi. Suppose to classify the special surface to the known reported sorts,there are competing between the names and the geologic crop facts. Special surface should belong to different type. In a key field crop of Fengshan of Guangxi,the special surface is in coexistence with the neptunian dyke and carbonate-breccia-body,and shows its lower part as normal fault surface and its upper part as solution unconformity interface. It is solution fault surface.Results: Due to the frequently large amplitude synsedimentary normal faulting,lower part of the fault plane could be hidden by present deposits,but the upper part of the fault plane could expose to be eroded and hidden by later deposits,cause steep topography and the younger beds laterally abuts the older basement strata in buttress unconformity,coincide with Davis' s concept of buttress unconformity.Conclusions: The special surface of Guangxi could be named buttress unconformity. The collected reports show the unconformity between the Late Palaeozoic strata and the subjacent Cambrian strata,as well as the overlaying Triassic strata,are buttress unconformity. Buttress unconformity could be observed widely in Late Palaeozoic strata of Guangxi and become its geologic feature,which means the frequent regional structural activity have being developed from Palaeozoic to Mesozoic in northwestern Guangxi. The characteristics of strata and tectonic activity record of Guangxi is similar to that of Tethys. Guangxi belongs to the part of east Tethys. Therefore,the argument about the special surface is ended,and approaching geologic materials could help to the study for the strata and the tectonic of northwestern Guangxi.
Objectives: Isolated carbonate platforms are widely observed in Youjiang River area,northwestern Guangxi.Many neptunian dykes,carbonate debris,synsedimentary normal faults,and special surfaces showing as local lost strata are observed in margins around those isolated carbonate platforms. There were different ideas about the relationships among these elements. Buttress unconformity refer to that megabreccia rapidly deposit in topographic low when synsedimentary normal faulting change flat terrain to steep topography,and cause the younger beds laterally abuts the older basement strata,and result in the unconformity between the younger beds and the older basement. Buttress unconformity generally formed in unstable structural regions. Until Davis(1984) named it as buttress unconformity,foreign geologists named it as angular unconformity,shelf-margin unconformity,platformmargin unconformity etc. Chinese geologists also observe those special surfaces of unconformity which shown as fault surface in some crops and shown as unconformity interface in some others,and named them as syntectonic sedimentary unconformity, carbonate-platform-margin limited fault zone, angular unconformity contact zone,escarpment-style pseudounconformity,event-sediment unconformity,unconformability of overlap,even tectonic window or klippe etc. Consequently cause argument for they are fault or unconformity,and for their different names.Methods: When study Late Palaeozoic isolated carbonate platform margin neptunian dyke and carbonatebreccia-body,author observes the paragenetic special surface and their difference from the sorts of known reported surfaces in Guangxi. Suppose to classify the special surface to the known reported sorts,there are competing between the names and the geologic crop facts. Special surface should belong to different type. In a key field crop of Fengshan of Guangxi,the special surface is in coexistence with the neptunian dyke and carbonate-breccia-body,and shows its lower part as normal fault surface and its upper part as solution unconformity interface. It is solution fault surface.Results: Due to the frequently large amplitude synsedimentary normal faulting,lower part of the fault plane could be hidden by present deposits,but the upper part of the fault plane could expose to be eroded and hidden by later deposits,cause steep topography and the younger beds laterally abuts the older basement strata in buttress unconformity,coincide with Davis' s concept of buttress unconformity.Conclusions: The special surface of Guangxi could be named buttress unconformity. The collected reports show the unconformity between the Late Palaeozoic strata and the subjacent Cambrian strata,as well as the overlaying Triassic strata,are buttress unconformity. Buttress unconformity could be observed widely in Late Palaeozoic strata of Guangxi and become its geologic feature,which means the frequent regional structural activity have being developed from Palaeozoic to Mesozoic in northwestern Guangxi. The characteristics of strata and tectonic activity record of Guangxi is similar to that of Tethys. Guangxi belongs to the part of east Tethys. Therefore,the argument about the special surface is ended,and approaching geologic materials could help to the study for the strata and the tectonic of northwestern Guangxi.
引文
陈开礼.2000.桂西古侵蚀沉积间断面型金矿床(Ⅰ).广西地质,13(4):19～22.
陈开礼.2001a.桂西古侵蚀沉积间断面型金矿床(Ⅱ).广西地质,14 (1):37～40.
陈开礼.2001b.桂西古侵蚀沉积间断面型金矿床(Ⅲ).广西地质,14(4):7～13.
杜远生,龚一鸣,吴诒,冯庆来,刘本培.1997.黔桂地区泥盆纪层序地层和台内裂陷槽的形成演化.沉积学报,15(4):11～17.
杜远生,黄虎,杨江海,黄宏伟,陶平,黄志强,胡丽沙,谢春霞.2013.晚古生代——中三叠世右江盆地的格局和转换.地质论评,59(1):1～10.
郜兆典.2000.海相热水沉积矿床问题探讨.广西地质,13(2):23～29.
葛孟春,冯庆来,江元生,谢德凡,马振东.1999.初论变异性不整合——以滇西北中甸地区为例.地球科学——中国地质大学学报,24(5):563～567.
广西壮族自治区地质局第八地质队、淮南煤炭学院.1974.广西凌云沉积灰岩脉和沉积灰岩体的发现及其在古构造研究上的意义.地质力学文集,2:32～38.
广西壮族自治区地质矿产局.1985.广西壮族自治区区域地质志.北京:地质出版社:658～659,680～681.
侯中健,陈洪德,田景春,覃建雄,彭军.2000.右江盆地海相泥盆系—中三叠统层序界面成因类型与盆地演化.沉积学报,18(2):205～209.
黄虎,杜远生,黄志强,杨江海,黄宏伟,黄志强,谢春霞,胡丽沙.2012.桂西晚古生代硅质岩地球化学特征及其对右江盆地构造演化的启示.中国科学,43(2):304～316.
黄志强.2003.右江盆地二叠纪孤立碳酸盐岩台地边缘海绵礁特征、时代及海绵礁相.南方国土资源,23～26.
贾大成,胡瑞忠.2001.滇黔桂地区卡林型金矿床成因探讨,矿床地质,20(4):378～384.
康云骥,张耿,蔡贺清.2003.右江盆地岩浆岩的地球化学特征.南方国土资源,24～27.
李文勇,夏斌,路文芳.2004.论同沉积、继承性控煤构造——禹州煤田虎头山断层.沉积学报,22(1):148～153.
李镇梁.2005.广西泥盆纪至早石炭世地层的平行不整合.南方国土资源,24～29.
李容森,陆刚,潘艺文,胡贵昂,彭阳.2008.桂西土湖锰矿区泥盆系中的陡崖式假不整合构造.桂林工学院学报,28 (4) :449～457.
林畅松,潘元林,肖建新,孔凡仙,刘景彦,郑和荣.2000.“构造坡折带”——断陷盆地层序分析和油气预测的重要概念.地球科学,25(3):260～266.
刘超,陆刚,张喜,周府生,黄祥林,杜远生.2014.桂西北天峨孤立碳酸盐岩台地晚古生代沉积特征与演化.地质论评,60(1):55～70.
刘东周,刘海波,王长春,陈成.2002.同生断层分段生长特征与油气关系.西南石油学学院学报,24(3):16～19.
刘秋生,李火车,何碧竹,张玉体,王亚红,王婧韫,姜小林.2001.“花窗结构,菱形中心”——断陷盆地的沉积规律.石油与天然气地质,22(3):210～220.
陆刚,胡贵昂,张能,张耿,潘艺文,彭阳.2006.右江盆地二叠纪生物礁时空分布和沉积构造演化新知.地质论评,52(2):190～197.
陆刚,韦文林,张能,胡贵昂,李文强.2002.桂西北天峨、乐业地区上二叠统及下三叠统顶部的古岩溶不整合.广西地质,15(4):5～8.
罗允义,唐宾,林崇献,李光造,李家镶.2004.桂西右江裂谷的伸展作用和伸展不整合.地质通报,23(2):160～168.
马杏垣.2004.解析构造学.北京:地质出版社:274～277.
牟传龙.1997.湖南泥盆纪沉积盆地的演化与层序地层沉积模式.特提斯地质,21:85～99.
彭阳,胡贵昂,陆刚,章雨旭,乔秀夫.2004.桂西北晚古生代地层中的沉积灰岩墙研究进展.地质论评,50(6):1～7.
彭阳,李岩,胡贵昂,陆刚,乔秀夫.2007.广西桂林庙头上泥盆统融县组中的灰岩脉和角砾灰岩体及其成因.地质论评,53(6):736～743.
彭阳,陆刚,胡贵昂,周敏,乔秀夫,章雨旭.2009a.广西凌云下甲二叠纪沉积灰岩墙和角砾灰岩体的成因及地质意义,地质论评,55(1):43～48.
彭阳.2009b.桂林—右江上古生界沉积灰岩脉—角砾灰岩体—同沉积断层与古地震记录.指导老师:白志强.北京大学博士论文.
彭阳,陆刚,胡贵昂.2013.广西桂林南边村上泥盆统沉积灰岩脉研究.地质论评,59(2):217～224.
彭阳,陆刚.2015.广西乐业泥盆系—石炭系沉积碳酸盐岩脉及地震事件沉积的新发现.地质论评,61(2):1～7.
彭阳,杨天南,乔秀夫,李典志,王国帧,杨中柱,杨小波.2001.大连上震旦统地震灾变事件研究.地质学报,75(2):221～227.
乔秀夫,彭阳,高林志.2002.桂北二叠纪灰岩墙(脉)的地震成因解释.地质通报,21(2):102～104.
任光明,王鹏,张林奎,张斌辉,戴婕.2011.滇东南弗拉斯期放射虫硅质岩地球化学特征及沉积环境探讨.地质论评,57(4):505～514.
任建业,陆永潮,张青林.2004.断陷盆地构造坡折带形成机制及其对层序发育样式的控制.地球科学,29(5):596～602.
孙冬胜.1995.重力同沉积断层的数值模拟.断块油气田,2 (4):1～3.
谭富文,潘桂棠,王剑.2001.滇西泥盆纪——三叠纪盆—山转换过程与特提斯构造演化.矿物岩石,21(3):179～185.
田景春,曾允孚.1995.中国南方二叠纪古海洋锶同位素演化.沉积学报,13(4):126～130.
王桂斌.1992.论广西高龙地区马平阶与茅口阶之间的特殊界面——种新的不整合类型.广西区域地质,1991～1992合刊:19～24.
王海舟.1997.桂西晚二叠世裂谷概述.广西地质,10(1):7～10.
王剑,宁浦功.1998.桂北桂中泥盆纪沉积盆地大地构造演化与铅锌矿成矿作用.广西地质,11(1):1～6.
王生海,强子同,文应初,卢卫平.1989.四川华莹市涧水沟上二叠统长兴组生物礁复合体中的水成岩墙及其意义.西南石油学院学报,11(3):16～22.
王新强,史晓颖.2008.桂西北晚古生代乐业孤立台地碳酸盐岩台地沉积特征与演化阶段.古地理学报,10(4):329～340.
王英民,金武弟,刘书会,邱桂强,李群,刘豪,辛仁臣,杨飞.2003.断陷湖盆多级坡折带的成因类型、展布及其勘探意义.石油与天然气地质,24(3):199～214.
王忠诚、吴浩若、邝国敦.1997.桂西晚古生代海相玄武岩的特征及其形成环境.岩石学报,13:260～265.
吴冲龙,汪新庆,刘刚,李绍虎,毛小平,李星.2001.抚顺盆地构造演化动力学研究.中国科学(D)辑,31(6):477～485.
吴根耀,吴浩若,钟大赉,邝国敦,季建清.2000.滇桂交界处古特提斯的洋岛和岛弧火山岩.现代地质,14(4):393～400.
吴浩若,邝国敦,王忠诚.1999.放射虫硅质岩对华南古地理的启示.古地理学报,1(2):28～35.
吴浩若,邝国敦,咸向阳,李曰俊,王忠诚.1994.桂南晚古生代放射虫硅质岩及广西古特提斯的初步探讨.科学通报,39(9):809～812
吴浩若.2000.广西加里东运动构造古地理问题.古地理学报,2(1):70～76.
吴浩若.2003.晚古生代—三叠纪南盘江海的构造古地理问题.古地理学报,5(1):63～76.
吴继远,孙忠.1981.桂西那坡混杂岩的特征及其形成机制.广西地质科技,24:29～37.
殷鸿福、吴顺宝、杜远生、彭元桥.1999.华南是特提斯多岛洋体系的一部分.地球科学-中国地质大学学报,24(1):1～12.
张旗、钱青、王焰.1999.扬子地块西南缘晚古生代基性岩浆岩的性质与古特提斯演化.岩石学报,15(4):576～583 .
张振贤.1998.桂南断裂构造和微粒型金矿的关系.广西地质,11(4):37～43.
周开华,陈春芳,陆刚,田青,李新华,汤新田.2011b.广西田东步兵石炭纪水下沉积灰岩脉及其地质意义.地质论评,57(6):900～905.
周开华,陆刚,陈春芳,田青,蒋亮,李新华,吴立河.2011a.广西古美测区1:5万区调主要成果.华南地质与矿产,27(4):342～351.
周永胜,王东坡,杨丙中,孙春岩,郭少斌.1993.伊舒地堑的构造—沉积演化及其聚油条件.岩相古地理,13(5):1～15.
Algouti A,Algouti Ah,Chbani B and Zaim M.2001.Sedimentation and syn-sedimentary volcanism of the infra-Cambrian Adoudounian Basal series interpreted from two areas in the Moroccan anti-atlas mountains.Journal of African Earth Science,32(4):541～556.
Alvarez W.1990.Pattern of extensional faulting in pelagic carbonates of the Umbria—Marche Apennines of central Italy.Geology,18:407～410.
Amy C G and Ann B K.2013.Strucural geology and geomorphology of the NW Coyote mountains,Elsinore fault zone,Southern California.Geological Society of America,45(7):548.
Bernoulli D,Jenkys H C.1974.Alpine,mediterranean and central Atlantic Mesozoic facies in relation to the early evolution of the Tethys.Modern and ancient geosynclinals sedimentation.Dott R H,Shaver R H (eds).SEPM Spec.Publ.,19:129～160.
Betzler C,Martin J M,Braga J C.2000.Non-tropical carbonates related to rocky submarine cliffs (Miocene,Almeria,southern Spain).Sediment.Geol.,131:51～65.
Bouillin J P,Dumont T,Mouterde J,Somma R,Hippolyte J C.1999.A Liassic to Eocene sub-marine scarp in the Peloritan Dorsale (Sicily,Italy).328:347～352.
Bourrouilh R,Bourque P A,Dansereau P,Bourrouilh-Le Jan F,Weyant P.1998.Synsedimentary tectonics,mud-mounds and sea-leavel changes on a Palaeozoic carbonate platform margin:a Devonian Montagne Noire example (France).Sedimentary Geology,118:95～118.
Catalano R,D’Argenio B.1982.Infraliassic strike-slip tectonics in Sicily and Southern Apennines.Rend Soc.Geol.Ital.,5:5～10.
Chen Kaili.2001a&.Palaeoerosion sedimentary discontinuity type golddeposit of Western GuangXi.Guangxi Geology,14(1):37～40
Chen Kaili.2001b&.Palaeoerosion sedimentary discontinuity type golddeposit of Western GuangXi.Guangxi Geology,14(4):7～14.
Chen Kaili.2000&.Palaeoerosion sedimentary discontinuity type golddeposit of Western GuangXi.Guangxi Geology,13(4):19～22.
Cox S J D,Scholz C H.1988.On the formation and growth of faults:an experimental study.Journal of Structural Geology,10(4):413～430.
Davis G H.1984.Structural Geology of Rocks and Regions,John Willey & Sons,Inc.
Di Stefano P,Galacz A,Mallarino G,Mindszenty A,Voros A.2002.Birth and early evolution of a Jurassic escarpment:Monte Kumeta,Western Sicily.Facies,46:273～298.
Di Stefano P,Mindszenty A.2000.Fe—Mn encrusted “Kamenitza” and associated features in the Jurassic of Monte Kumeta (Sicily):subaerial and /or submarine dissolution.Sediment Geol.,132:37～68.
Du Yuansheng,Gong Yiming,Wu Yi,Feng Qinglai,and Liu Benpei.1997&.Devonian sequence stratigraphy and formation and evolution of intraplatform rift trough in the Guangxi and Guizhou area,China.Acta Sedimentologica Sinica,15(4):11～17.
Du Yuansheng,Huanghu,Yang Jianghai,Huang Hongwei,Tao Ping,Huang Zhiqiang,Hu Lisha,Xie Chunxia.2013&.The basin translation from Late Paleozoic to Triassic of the Youjiang basin and its tectonic signification.Geological Review,59(1):1～10.
Eberli G.1988.The evolution of the southern continental margin of the Jurassic Tethys ocean as recorded in the Allgau Formation of the Austroalpine Nappes of Graubunden (Switzerland).Eclogae Geol.Helv.,81:175～214.
Fernandez-Mendiola P A and Garcia-Mondejar J.1995.Volcaniclastic sediments in the early Albian Manaria carbonate platform (northern Spain).Cretaceous Research,16 (4):451～463.
Gao Zhaodian.2000&.Discussion on marine hydrothermal sedimentary deposit.Guangxi Geology,13(2):23～29
Ge Mengchun,Feng Qinglai,Jiang Yuansheng,Xie Defan,Ma Zhendong.1999&.Variability unconformity in Zhongdian region,Northwestern Yunnan Province,China.Earth Science——Journal of China university of Geosciences,24(6):563～567
Gischler E.1996.Late Devonian—Early Carboniferous deep-water coral assemblages and sedimentation on a Devonian seamount:Iberg Reef,Harz Mts.,Germany.Palaeogeography,Palaeoclimatology,Palaeoecology,123:297～322.
Gullo M,Vitale F P.1986.The “Megabreccia event” in the Upper Cretaceous—Eocene “Scaglia” of Western Sicily.Rend.Soc.Geol.Ital.,9:195～202.
Hou Zhongjian,Chen Hongde,Tian Jiangchun,Qin jianxiong,Peng Jun.2000&.Genesis of sequence boundary and basin evolution in Youjiang basin during the Devonian to the middle Trassic.Acta Sedimentologica Sinica,18( 2):205～209.
Huang Hu,Du Yuansheng,Huang Zhiqiang,Yang Jianghai,Huang Hongwei,Huang Zhiqiang,Xie Chunxia,Hu Lisha.2013#.Depositional chemistry of chert during late Palaeozoic from western Guangxi and its implication for the tectonic evolution of the Youjiang Basin.Science China:Earth Science,56(2):479～493.
Huang Zhiqiang.2003#.The feature and age of sponge-reef and its facies rimmed the Permian isolated carbonate platform in Youjiang basin.South Land Resources,23～26.
Hunt D V,Fitchen W M,Kosa E.2002.Syndepositional deformation of the Permian Capitan reef carbonate platform,Guadalupe Mountains,New Mexico,USA.Sedimentary Geology,154 (3～4):89～126.
Jenkyns H C.1970a.Growth and disintegration of a carbonate platform.Neues Jb Geol Palaont Mh,6:325～344.
Jenkyns H C.1970b.The Jurassic of Western Sicily.In:Geology and History of Sicily.Petr.Expl.Soc.Libya.,245～254
Jenkyns H C.1980.Tethys:past and present.Proc.Geil.Assoc.,91:107～118
Jia Dacheng,Hu Ruizhong.2001&.Analysis of genesis of Carlin-type gold deposits in Yunnan—Guizhou—Guangxi triangle area.Mineral Deposits,20( 4):378～384.
Kang Yunji Zhang Geng,Cai Heqing.2003#.The geochemical signature of magmatic rocks in Youjiang basin.South Land Resources,24～27.
Li Wenyong,Xia Bin,Lu Wenfang.2004&.Discussion on syndepositional & inherited coal-controlling structure——Hutoushan fault in Yuzhou Coalfield.Geological Review,55(1):43～48.
Li Zhenliang.2005#.The parallel unconformities of Devonian—Early Carboniferous strata in Guangxi.South Land Sources,24～29.
Li Rongsen,Lu Gang,Pan Yiwen,Hu Guiang and Peng Yang.2008.Characteristics of escarpmentive pseudo-unconformity in Devonian Tuhu Manganese Deposit of western Guangxi.Journal of Guilin University of Technolog,28 (4) :449～457.
Lin Changsong,Pan Yuanlin,Xiao Jianxin,Kong Fanxian,Liu Jingyan,Zheng Herong.2000&.Structural slope break zone:key concept of stratigraphic sequence analysis and petroleum forecasting in fault subsidence basins.Earth Science——Journal of China University of Geosciences,25( 3):260～266.
Liu Chao,Lu Gang,Zhang Xi,Zhou Fusheng,Huang Xianglin,Du Yuansheng.2014&.Sedimentary characteristics and evolutionary stages in late Paleozoic of Tian’e isolated platform in northwestern Guangxi.Geological Review,60(1):55～70.
Liu Dongzhou,Liu Haibo,Wang Changchun,Chen Cheng.2002&.The relationship between the segmented growth feature of the syngenetic fault and the hydrocarbon.Journal of Southwest Petroleum Institute,24( 3):16～19.
Liu Qiusheng,Li Huoche,He Bizhu,Zhang Yuti,Wang Yahong,Wang Jingyun,Jiang Xiaolin.2001&.“Fenestral structure,rhombic center”——depositional regularity of faulted basins.Oil & Gas Geology,22( 3):210～220.
Lu Gang,Hu Guiang,Zhang Neng,Zhang Geng,Pan Yiwen,Peng Yang.2006&.Recent approach to space—time distribution and sedimentary structural evolution of Permian reef in Youjiang basin.Geological Review,52( 2):190～197.
Lu Gang,Wei Wenlin,Zhang Neng,Hu Guian,Li Wenqiang.2002&.Paleokarst unconformity of late Permian and early Triassic in northwestern Guangxi.Guangxi Geology,15( 4):5～8.
Luca Basilone,Maurizio Gasparo Morticelli,Gabriele Lena.2010.Mesozoic tectonics and volcanism of Tethyan rifted continental margins in western Silicy.Sedimentary Geology,226:54～70.
Luca Basilone.2009.Mesozoic tectono-sedimentary evolution of Rocca Busambra in Western Sicily.Facies,55:115～135.
Luo Yunyi,Tang Bin,Lin Chongxian,Li Guangzao,Li Jiaxiang.2004&.Extension and extensional unconformity of the Youjiang rift in western Guangxi.Geological Bulletin of China,23( 2):160～168.
Ma Xingyuan (legacy works).2004#.Analytical Tectonics.Beijing:Geological Publishing House:274～277.
Maurice E Tucker,V Paul Wright with a chapter by J A D Dichson.1990.Carbonate Sedimentology.Blackwell Scientific Publications:45～255.
Moretti and Colletta.1988.Fault-block tilting:the Gebel Zeit example,Gulf of Suez.Juornal of Structural Geology,10(1):9～19.
Mou Chuanlong.1997&.Devonian sedimentary basins in Hunan:evolution and sequence stratigraphic model.Tethyan Geology,21:85～99.
Peng Yang,Hu Guiang,Lu Gang,Zhang Yuxu,Qiao Xiufu.2004&.Progress in studying on limestone dykes in late Paleozoic strata in northwestern Guangxi.Geological Review,50( 6):1～7.
Peng Yang,Li Yan,Hu Guiang,Lu Gang,Qiao Xiufu.2007&.Limestone dykes and breccia limestone bodies in the upper Devonian Rongxian formation in Miaotou area,Guilin,Guangxi.Geological Review,53( 6):736～743.
Peng Yang,Lu Gang,Hu Guiang,Zhou Min,Qiao Xiufu,Zhang Yuxu.2009a&.Genesis of the Permian limestone neptunian dykes and limestone breccia talus in the Xiajia area,Lingyun county,Guangxi,and its geological significances.
Peng Yang,Lu Gang,Hu Guiang.2013&.Study on carbonate limestone dykes (neptunian dykes) of upper Devonian in Nanbiancun,Guilin,Guangxi.Geological Review,59(2):217～224.
Peng Yang,Lu Gang.2015&.New approach on Devonian—Carboniferous carbonate neptunian dykes and earthquake events in Leye,Guangxi.Geological Review,61(2):1～7.
Peng Yang,Yang Tiannan,Qiao Xiufu,Li Dianzhi,Wang Guozhen,Yang Zhongzhu,Yang Xiaobo.2001&.A study of seismic events in the late Sinian carbonates of Dalian,China.Acta Geological Sinica,75(2):221～227.
Peng Yang.2009b&.Late Palaeozoic Limestone Dyke-breccia Limestone Body——Synsedimentary Fault with Palaeoseismic Record,Guilin-Youjiang.Doctoral Supervisor:Bai Zhiqiang.Beijing:Peking University Ph.D.dissertation.
Qiao Xiufu,Peng Yang,Gao Linzhi.2002&.Interpretation of the seismic origin of Permian limestone dykes in northwestern Guangxi.Geological Bulletin of China,21(2):102～104.
Ren Guangming,Wang Peng,Zhang Linkui,Zhang Binhhui,Dai Jie.2011&.Discussion on geochemical charateristics and sedimentary environment of the Frasnian Radiolarian chert in southeastern Yunnan.Geological Review,57(4):505～514.
Ren Jianye,Lu Yongchao,Zhang Qinglin.2004&.Forming mechanism of structural slope-break and its control on sequence style in faulted basin.Earth Science——Journal of China University of Geoscience,29(5):596～602.
Santantonio M.1993.Facies associations and evolution of pelagic carbonate platform/basin systems:examples from the Italian Jurassic.Sedimentology,40:1039～1067.
Santantonio M.1994.Pelagic carbonate platforms in the geologic record:their classification,and sedimentary and paleotectonic evolution.AAPG Bull.,78:122～141.
Stefano P D,Mindszenty A.2000.Fe—Mn-encrusted “Kamenitza” and associated features in the Jurassic of Monte Kumeta (Sicily):subaerial and/or submarine dissolution.Sedimentary Geology,132:37～68.
Stephen Marshak,M.Scott Wilkerson,Joshua DeFrates.2016.Structural geology of the Baraboo District:an introduction.GSA Field Guides,43:13～36.
Sun Dongsheng.1995&.Numerical simulation of gravity synsedimentary fault.Fault-Block Oil & Gas Field,2(4):1～3.
Tan Fuwen,Pan Guitang,Wang Jian.2001&.Devonian—Triassic basin——range transformation and the tectonic evolution of Palaeo-Tethys in western Yunnan,China.Journal of Mineral Petrol,21(3):179～185.
Tanner L H and Hubert J F.1992.Depositional facies,paleogeography and palaeoclimatology of the Lower Jurassic McCoy Brook Formation,Fundy rift basin,Nova Scotia.Palaeogeography,Palaeoclimatology,Palaeoecology,96(3～4):261～280.
The Bureau of Geology and Mineral Resources of Guangxi Zhuang Autonomous Region.1985#.Regional Geology of Guangxi Zhuang Autonomous Region,People’s Republic of China.Beijing:Geological Publishing House:658～659,680～681.
The Eighth Geological Team,Guangxi Zhuang Autonomous Region and the Huainan Coal College,Anhui Province.1978#.On the discovery of early Permian sedimentary limestone dykes and limestone bodies in Lingyun county,Guangxi Zhuang Autonomous region,China,and their significance in the study of Palaeotectonics.In proceedings of the 25th International Geological Congress by Zhouzhian and in Geomechanics Corpus,(2):32～38.
Thomas W,Dibblee J R.1971.A great middle Tertiary buttress unconformity in the Newberry mountains,Mojave desert,California,and its paleogeologic inplications.GeoRef Record/GeoScienceWorld,3(2):110.
Tian Jingchun,Zeng Yunfu.1995&.The revolution of the isotopic composition of strontium in the Permian palaeo-ocean in south China.Acta Sedimentologica Sinica,13(4):125～130.
Vendeville B,Cobbold P R.1988.How normal faulting and sedimentation interact to produce listric fault profiles and stratigraphic wedges.Journal of Structural Geology,10(7):649～659.
Wang Guibin.1992#.On the special surfaces between Maping Stage—Maokou Stage in Gaolong area,Guangxi——a new type of unconformity.Guangxi Region Geology.Combined issue of 1991～1992:19～24.
Wang Haizhou.1997&.Rifts of late Permian epoch in western Guangxi.Guangxi Geology,10(1):7～10.
Wang Jian,Ning Pugong.1998&.Study on tectonic evolution of Devonian sedimentary basins and Lead—Zinc metallization of Guangxi.Guangxi Geology,11(1):1～6
Wang Shenghai,Qiangzitong,Wen Yingchu,Lu Weiping.1989&.Neptunian dykes and their significance of Jianshuigou upper Permian reef comples in Huaying mountains,Sichuan,China.Journal of Southwestern Petroleum Institute,11(3):16～22.
Wang Xinqiang,Shi Xiaoyin.2008&.Sedimentary characteristics and evolution of the late Paleozoic Leye isolated carbonate platform in northwest Guangxi.Journal of Palaeogeography,10(4):329～340.
Wang Yingmin,Jin Wudi,Liu Shuhui,Qiu Guiqiang,Li Qun,Liu Hao,Xin Renchen,Yang Fei.2003&.Genetic types,distribution and esploration significance of multistage slope breaks in rift lacustrine basin.Oil & Gas Geology,24(3):199～214.
Wang Zhongcheng,Wu Haoruo,Kuang Guodun.1997&.Characteristics of the late Paleozoic oceanic basalts and their eruptive environments in west Guangxi.Acta Petrologica Sinica,13(2):260～265.
Wendt J .1965.Synsedimentaire Bruchtektonik im Jura Westsiziliens.N Jb Geol Palaontol Mh,5:286～311.
Wendt J.1971.Genese and Fauna submariner sedimentaaarer Spaltenfullungen im mediterranen Jura.Palaeontographica A 136:122～192.In:Luca Basilone,Maurizio Gasparo Morticelli,Gabriele Lena.2010.Mesozoic tectonics and volcanism of Tethyan rifted continental margins in western Silicy.Sedimentary Geology,226:54～70.
Winterer E L,Metzler C V,Sarti M.1991.Neptunian dykes and associated breccias (Southern Alps,Italy and Switzerland):role of gravity sliding in open and closed systems.Sedimentology,38:381～404.
Winterer E L,Sarti M.1994.Neptunian dykes and associated features in southern Spain:mechanisms of formation and tectonic implication.Sedimentology,41:1109～1132.
Wu Chonglong,Wang Xinqing,Liu Gang,Li Shaohu,Mao Xiaoping,Li Xing.2001#.On kinetics of tectonic evolution of Fushun basin.Science in China (Series D),31(6):477～485.
Wu Genyao,Wu Haoruo,Zhong Dalai Kuang Guodun,Ji Jianqing.2000&.Volcanic rocks of palaeotethyan oceanic island and island-arc bordering Yunnan and Guangxi,China.Geoscience.Journal of Graduate School,China University of Geosciences,14(4):393～400.
Wu Haoruo,Kuang Guodun,Xian Xiangyang,Li Yuejun,Wang Zhongcheng.1994.On late Palaeozoic Radiolarian chert in south Guangxi and preliminary discuss on palaeotethyan in Guangxi.Chinest Science Bulletin,39( 9):809～812.
Wu Haoruo.1999&.Implications of Radiolarian chert for the palaeogeography of south China.Journal of Palaeogeography,1(2):28～35.
Wu Haoruo.2000&.A discussion on the tectonic palaeogeography related to the Caledonian movement in Guangxi.Journal of Palaeogeography,2(1):70～76.
Wu Haoruo.2003&.Discussion on tectonic palaeogeography of Nanpanjiang sea in the late Palaeozoic and Triassic.Journal of Palaeogeography,5(1):63～76.
Wu Jiyuan,Sun Zhong.1981.The characteristics of Napo mixtite and its formation mechanism.Guangxi Geological Science and Technology,24:29～37.
Yin Hongfu,Wu Shunbao,Du Yuansheng,Peng yuanqiao.1999&.South China defined as part of Tethyan archipelagic ocean system.Earth Science——Journal of China University of Geoscience,24(1):1～12.
Zhang Qi,Qian Qing,Wang Yan.1999&.Late Palaeozoic basic magmatism from SW Yangtze Massif and evolution of the Palaeo-Tethyan Ocean.Acta Petrologica Sinica,15(4):576～583.
Zhang Zhenxian.1998&.Relationship between fault and micrograined disseminated gold deposit southern Guangxi.Guangxi Geology,11(4):37～43.
Zhou Kaihua,Chen Chunfang,Lu Gang,Tian Qing,Li Xinhua,Tang Xintian.2011b&.Genesis of Carboniferous subaqueous limestone dykes in Buding area,Tiandong county,Guangxi.Geological Review,57(6):900～905.
Zhou Kaihua,Lu Gang,Chen Chunfang,Tian Qing,Jiang Liang,Li Xinhua,Wu Lihe.2011a&.New Progresses in 1:50000 regional geological survey in Gumei area,Guangxi.Geology and Mineral Resources of South China,27(4):342～351.
Zhou Yongsheng,Wang Dongpo,Yang Bingzhong,Sun Chunyan,Guo Shaobin.1993&.Tectono-sedimentary evolution and oil accumulation in the Yishu Graben,northeastern China.Lithofacies Palaeogeography (Journal of Palaeogeography),13(5):1～5.
(1) 广西地勘局.1992.定安幅—八渡圩幅1∶5万区域地质调查报告.Guangxi Geological Survey Bureau.1992.Regional Geological Exploration Reports on Ding’an Chart—Baduxu Chart of 1∶50000 Geological Map.
(2) 广西地勘局.1995.乐业幅1∶5万区域地质调查报告.Guangxi Geological Survey Bureau.1995.Regional Geological Exploration Reports on Leye Chart of 1∶50000 Geological Map.
(3) 广西地勘局.1992.金牙—凌云1∶5万区域地质调查报告.Guangxi Geological Survey Bureau.1992.Regional Geological Exploration Reports on Jinya Chart—Lingyun Chart of 1∶50000 Geological Map.
(4) 广西地勘局.2001.凤山—天峨幅1∶5万区域地质调查报告.Guangxi Geological Survey Bureau.2001.Regional Geological Exploration Reports on Fengshan Chart—Tian’e Chart of 1∶50000 Geological Map.
(5) 广西地勘局.2000.甘田镇—浪平幅1∶5万区域地质调查报告.Guangxi Geological Survey Bureau.2000.Regional Geological Exploration Reports on Gantianzhen Chart—Langping Chart of 1∶50000 Geological Map.
(6) 广西地勘局.2004.下雷—上映测区1∶5万区域地质调查报告.Guangxi Geological Survey Bureau.2004.Regional Geological Exploration Reports on Xialei Chart—Shangyin Chart of 1∶50000 Geological Map.
(7) 广西地勘局.1989.广西地质图(1∶250万)说明书.Guangxi Geological Survey Bureau.1989.Specification on 1∶2500000 Guangxi Geological Map.
陈开礼.2001a.桂西古侵蚀沉积间断面型金矿床(Ⅱ).广西地质,14 (1):37～40.
陈开礼.2001b.桂西古侵蚀沉积间断面型金矿床(Ⅲ).广西地质,14(4):7～13.
杜远生,龚一鸣,吴诒,冯庆来,刘本培.1997.黔桂地区泥盆纪层序地层和台内裂陷槽的形成演化.沉积学报,15(4):11～17.
杜远生,黄虎,杨江海,黄宏伟,陶平,黄志强,胡丽沙,谢春霞.2013.晚古生代——中三叠世右江盆地的格局和转换.地质论评,59(1):1～10.
郜兆典.2000.海相热水沉积矿床问题探讨.广西地质,13(2):23～29.
葛孟春,冯庆来,江元生,谢德凡,马振东.1999.初论变异性不整合——以滇西北中甸地区为例.地球科学——中国地质大学学报,24(5):563～567.
广西壮族自治区地质局第八地质队、淮南煤炭学院.1974.广西凌云沉积灰岩脉和沉积灰岩体的发现及其在古构造研究上的意义.地质力学文集,2:32～38.
广西壮族自治区地质矿产局.1985.广西壮族自治区区域地质志.北京:地质出版社:658～659,680～681.
侯中健,陈洪德,田景春,覃建雄,彭军.2000.右江盆地海相泥盆系—中三叠统层序界面成因类型与盆地演化.沉积学报,18(2):205～209.
黄虎,杜远生,黄志强,杨江海,黄宏伟,黄志强,谢春霞,胡丽沙.2012.桂西晚古生代硅质岩地球化学特征及其对右江盆地构造演化的启示.中国科学,43(2):304～316.
黄志强.2003.右江盆地二叠纪孤立碳酸盐岩台地边缘海绵礁特征、时代及海绵礁相.南方国土资源,23～26.
贾大成,胡瑞忠.2001.滇黔桂地区卡林型金矿床成因探讨,矿床地质,20(4):378～384.
康云骥,张耿,蔡贺清.2003.右江盆地岩浆岩的地球化学特征.南方国土资源,24～27.
李文勇,夏斌,路文芳.2004.论同沉积、继承性控煤构造——禹州煤田虎头山断层.沉积学报,22(1):148～153.
李镇梁.2005.广西泥盆纪至早石炭世地层的平行不整合.南方国土资源,24～29.
李容森,陆刚,潘艺文,胡贵昂,彭阳.2008.桂西土湖锰矿区泥盆系中的陡崖式假不整合构造.桂林工学院学报,28 (4) :449～457.
林畅松,潘元林,肖建新,孔凡仙,刘景彦,郑和荣.2000.“构造坡折带”——断陷盆地层序分析和油气预测的重要概念.地球科学,25(3):260～266.
刘超,陆刚,张喜,周府生,黄祥林,杜远生.2014.桂西北天峨孤立碳酸盐岩台地晚古生代沉积特征与演化.地质论评,60(1):55～70.
刘东周,刘海波,王长春,陈成.2002.同生断层分段生长特征与油气关系.西南石油学学院学报,24(3):16～19.
刘秋生,李火车,何碧竹,张玉体,王亚红,王婧韫,姜小林.2001.“花窗结构,菱形中心”——断陷盆地的沉积规律.石油与天然气地质,22(3):210～220.
陆刚,胡贵昂,张能,张耿,潘艺文,彭阳.2006.右江盆地二叠纪生物礁时空分布和沉积构造演化新知.地质论评,52(2):190～197.
陆刚,韦文林,张能,胡贵昂,李文强.2002.桂西北天峨、乐业地区上二叠统及下三叠统顶部的古岩溶不整合.广西地质,15(4):5～8.
罗允义,唐宾,林崇献,李光造,李家镶.2004.桂西右江裂谷的伸展作用和伸展不整合.地质通报,23(2):160～168.
马杏垣.2004.解析构造学.北京:地质出版社:274～277.
牟传龙.1997.湖南泥盆纪沉积盆地的演化与层序地层沉积模式.特提斯地质,21:85～99.
彭阳,胡贵昂,陆刚,章雨旭,乔秀夫.2004.桂西北晚古生代地层中的沉积灰岩墙研究进展.地质论评,50(6):1～7.
彭阳,李岩,胡贵昂,陆刚,乔秀夫.2007.广西桂林庙头上泥盆统融县组中的灰岩脉和角砾灰岩体及其成因.地质论评,53(6):736～743.
彭阳,陆刚,胡贵昂,周敏,乔秀夫,章雨旭.2009a.广西凌云下甲二叠纪沉积灰岩墙和角砾灰岩体的成因及地质意义,地质论评,55(1):43～48.
彭阳.2009b.桂林—右江上古生界沉积灰岩脉—角砾灰岩体—同沉积断层与古地震记录.指导老师:白志强.北京大学博士论文.
彭阳,陆刚,胡贵昂.2013.广西桂林南边村上泥盆统沉积灰岩脉研究.地质论评,59(2):217～224.
彭阳,陆刚.2015.广西乐业泥盆系—石炭系沉积碳酸盐岩脉及地震事件沉积的新发现.地质论评,61(2):1～7.
彭阳,杨天南,乔秀夫,李典志,王国帧,杨中柱,杨小波.2001.大连上震旦统地震灾变事件研究.地质学报,75(2):221～227.
乔秀夫,彭阳,高林志.2002.桂北二叠纪灰岩墙(脉)的地震成因解释.地质通报,21(2):102～104.
任光明,王鹏,张林奎,张斌辉,戴婕.2011.滇东南弗拉斯期放射虫硅质岩地球化学特征及沉积环境探讨.地质论评,57(4):505～514.
任建业,陆永潮,张青林.2004.断陷盆地构造坡折带形成机制及其对层序发育样式的控制.地球科学,29(5):596～602.
孙冬胜.1995.重力同沉积断层的数值模拟.断块油气田,2 (4):1～3.
谭富文,潘桂棠,王剑.2001.滇西泥盆纪——三叠纪盆—山转换过程与特提斯构造演化.矿物岩石,21(3):179～185.
田景春,曾允孚.1995.中国南方二叠纪古海洋锶同位素演化.沉积学报,13(4):126～130.
王桂斌.1992.论广西高龙地区马平阶与茅口阶之间的特殊界面——种新的不整合类型.广西区域地质,1991～1992合刊:19～24.
王海舟.1997.桂西晚二叠世裂谷概述.广西地质,10(1):7～10.
王剑,宁浦功.1998.桂北桂中泥盆纪沉积盆地大地构造演化与铅锌矿成矿作用.广西地质,11(1):1～6.
王生海,强子同,文应初,卢卫平.1989.四川华莹市涧水沟上二叠统长兴组生物礁复合体中的水成岩墙及其意义.西南石油学院学报,11(3):16～22.
王新强,史晓颖.2008.桂西北晚古生代乐业孤立台地碳酸盐岩台地沉积特征与演化阶段.古地理学报,10(4):329～340.
王英民,金武弟,刘书会,邱桂强,李群,刘豪,辛仁臣,杨飞.2003.断陷湖盆多级坡折带的成因类型、展布及其勘探意义.石油与天然气地质,24(3):199～214.
王忠诚、吴浩若、邝国敦.1997.桂西晚古生代海相玄武岩的特征及其形成环境.岩石学报,13:260～265.
吴冲龙,汪新庆,刘刚,李绍虎,毛小平,李星.2001.抚顺盆地构造演化动力学研究.中国科学(D)辑,31(6):477～485.
吴根耀,吴浩若,钟大赉,邝国敦,季建清.2000.滇桂交界处古特提斯的洋岛和岛弧火山岩.现代地质,14(4):393～400.
吴浩若,邝国敦,王忠诚.1999.放射虫硅质岩对华南古地理的启示.古地理学报,1(2):28～35.
吴浩若,邝国敦,咸向阳,李曰俊,王忠诚.1994.桂南晚古生代放射虫硅质岩及广西古特提斯的初步探讨.科学通报,39(9):809～812
吴浩若.2000.广西加里东运动构造古地理问题.古地理学报,2(1):70～76.
吴浩若.2003.晚古生代—三叠纪南盘江海的构造古地理问题.古地理学报,5(1):63～76.
吴继远,孙忠.1981.桂西那坡混杂岩的特征及其形成机制.广西地质科技,24:29～37.
殷鸿福、吴顺宝、杜远生、彭元桥.1999.华南是特提斯多岛洋体系的一部分.地球科学-中国地质大学学报,24(1):1～12.
张旗、钱青、王焰.1999.扬子地块西南缘晚古生代基性岩浆岩的性质与古特提斯演化.岩石学报,15(4):576～583 .
张振贤.1998.桂南断裂构造和微粒型金矿的关系.广西地质,11(4):37～43.
周开华,陈春芳,陆刚,田青,李新华,汤新田.2011b.广西田东步兵石炭纪水下沉积灰岩脉及其地质意义.地质论评,57(6):900～905.
周开华,陆刚,陈春芳,田青,蒋亮,李新华,吴立河.2011a.广西古美测区1:5万区调主要成果.华南地质与矿产,27(4):342～351.
周永胜,王东坡,杨丙中,孙春岩,郭少斌.1993.伊舒地堑的构造—沉积演化及其聚油条件.岩相古地理,13(5):1～15.
Algouti A,Algouti Ah,Chbani B and Zaim M.2001.Sedimentation and syn-sedimentary volcanism of the infra-Cambrian Adoudounian Basal series interpreted from two areas in the Moroccan anti-atlas mountains.Journal of African Earth Science,32(4):541～556.
Alvarez W.1990.Pattern of extensional faulting in pelagic carbonates of the Umbria—Marche Apennines of central Italy.Geology,18:407～410.
Amy C G and Ann B K.2013.Strucural geology and geomorphology of the NW Coyote mountains,Elsinore fault zone,Southern California.Geological Society of America,45(7):548.
Bernoulli D,Jenkys H C.1974.Alpine,mediterranean and central Atlantic Mesozoic facies in relation to the early evolution of the Tethys.Modern and ancient geosynclinals sedimentation.Dott R H,Shaver R H (eds).SEPM Spec.Publ.,19:129～160.
Betzler C,Martin J M,Braga J C.2000.Non-tropical carbonates related to rocky submarine cliffs (Miocene,Almeria,southern Spain).Sediment.Geol.,131:51～65.
Bouillin J P,Dumont T,Mouterde J,Somma R,Hippolyte J C.1999.A Liassic to Eocene sub-marine scarp in the Peloritan Dorsale (Sicily,Italy).328:347～352.
Bourrouilh R,Bourque P A,Dansereau P,Bourrouilh-Le Jan F,Weyant P.1998.Synsedimentary tectonics,mud-mounds and sea-leavel changes on a Palaeozoic carbonate platform margin:a Devonian Montagne Noire example (France).Sedimentary Geology,118:95～118.
Catalano R,D’Argenio B.1982.Infraliassic strike-slip tectonics in Sicily and Southern Apennines.Rend Soc.Geol.Ital.,5:5～10.
Chen Kaili.2001a&.Palaeoerosion sedimentary discontinuity type golddeposit of Western GuangXi.Guangxi Geology,14(1):37～40
Chen Kaili.2001b&.Palaeoerosion sedimentary discontinuity type golddeposit of Western GuangXi.Guangxi Geology,14(4):7～14.
Chen Kaili.2000&.Palaeoerosion sedimentary discontinuity type golddeposit of Western GuangXi.Guangxi Geology,13(4):19～22.
Cox S J D,Scholz C H.1988.On the formation and growth of faults:an experimental study.Journal of Structural Geology,10(4):413～430.
Davis G H.1984.Structural Geology of Rocks and Regions,John Willey & Sons,Inc.
Di Stefano P,Galacz A,Mallarino G,Mindszenty A,Voros A.2002.Birth and early evolution of a Jurassic escarpment:Monte Kumeta,Western Sicily.Facies,46:273～298.
Di Stefano P,Mindszenty A.2000.Fe—Mn encrusted “Kamenitza” and associated features in the Jurassic of Monte Kumeta (Sicily):subaerial and /or submarine dissolution.Sediment Geol.,132:37～68.
Du Yuansheng,Gong Yiming,Wu Yi,Feng Qinglai,and Liu Benpei.1997&.Devonian sequence stratigraphy and formation and evolution of intraplatform rift trough in the Guangxi and Guizhou area,China.Acta Sedimentologica Sinica,15(4):11～17.
Du Yuansheng,Huanghu,Yang Jianghai,Huang Hongwei,Tao Ping,Huang Zhiqiang,Hu Lisha,Xie Chunxia.2013&.The basin translation from Late Paleozoic to Triassic of the Youjiang basin and its tectonic signification.Geological Review,59(1):1～10.
Eberli G.1988.The evolution of the southern continental margin of the Jurassic Tethys ocean as recorded in the Allgau Formation of the Austroalpine Nappes of Graubunden (Switzerland).Eclogae Geol.Helv.,81:175～214.
Fernandez-Mendiola P A and Garcia-Mondejar J.1995.Volcaniclastic sediments in the early Albian Manaria carbonate platform (northern Spain).Cretaceous Research,16 (4):451～463.
Gao Zhaodian.2000&.Discussion on marine hydrothermal sedimentary deposit.Guangxi Geology,13(2):23～29
Ge Mengchun,Feng Qinglai,Jiang Yuansheng,Xie Defan,Ma Zhendong.1999&.Variability unconformity in Zhongdian region,Northwestern Yunnan Province,China.Earth Science——Journal of China university of Geosciences,24(6):563～567
Gischler E.1996.Late Devonian—Early Carboniferous deep-water coral assemblages and sedimentation on a Devonian seamount:Iberg Reef,Harz Mts.,Germany.Palaeogeography,Palaeoclimatology,Palaeoecology,123:297～322.
Gullo M,Vitale F P.1986.The “Megabreccia event” in the Upper Cretaceous—Eocene “Scaglia” of Western Sicily.Rend.Soc.Geol.Ital.,9:195～202.
Hou Zhongjian,Chen Hongde,Tian Jiangchun,Qin jianxiong,Peng Jun.2000&.Genesis of sequence boundary and basin evolution in Youjiang basin during the Devonian to the middle Trassic.Acta Sedimentologica Sinica,18( 2):205～209.
Huang Hu,Du Yuansheng,Huang Zhiqiang,Yang Jianghai,Huang Hongwei,Huang Zhiqiang,Xie Chunxia,Hu Lisha.2013#.Depositional chemistry of chert during late Palaeozoic from western Guangxi and its implication for the tectonic evolution of the Youjiang Basin.Science China:Earth Science,56(2):479～493.
Huang Zhiqiang.2003#.The feature and age of sponge-reef and its facies rimmed the Permian isolated carbonate platform in Youjiang basin.South Land Resources,23～26.
Hunt D V,Fitchen W M,Kosa E.2002.Syndepositional deformation of the Permian Capitan reef carbonate platform,Guadalupe Mountains,New Mexico,USA.Sedimentary Geology,154 (3～4):89～126.
Jenkyns H C.1970a.Growth and disintegration of a carbonate platform.Neues Jb Geol Palaont Mh,6:325～344.
Jenkyns H C.1970b.The Jurassic of Western Sicily.In:Geology and History of Sicily.Petr.Expl.Soc.Libya.,245～254
Jenkyns H C.1980.Tethys:past and present.Proc.Geil.Assoc.,91:107～118
Jia Dacheng,Hu Ruizhong.2001&.Analysis of genesis of Carlin-type gold deposits in Yunnan—Guizhou—Guangxi triangle area.Mineral Deposits,20( 4):378～384.
Kang Yunji Zhang Geng,Cai Heqing.2003#.The geochemical signature of magmatic rocks in Youjiang basin.South Land Resources,24～27.
Li Wenyong,Xia Bin,Lu Wenfang.2004&.Discussion on syndepositional & inherited coal-controlling structure——Hutoushan fault in Yuzhou Coalfield.Geological Review,55(1):43～48.
Li Zhenliang.2005#.The parallel unconformities of Devonian—Early Carboniferous strata in Guangxi.South Land Sources,24～29.
Li Rongsen,Lu Gang,Pan Yiwen,Hu Guiang and Peng Yang.2008.Characteristics of escarpmentive pseudo-unconformity in Devonian Tuhu Manganese Deposit of western Guangxi.Journal of Guilin University of Technolog,28 (4) :449～457.
Lin Changsong,Pan Yuanlin,Xiao Jianxin,Kong Fanxian,Liu Jingyan,Zheng Herong.2000&.Structural slope break zone:key concept of stratigraphic sequence analysis and petroleum forecasting in fault subsidence basins.Earth Science——Journal of China University of Geosciences,25( 3):260～266.
Liu Chao,Lu Gang,Zhang Xi,Zhou Fusheng,Huang Xianglin,Du Yuansheng.2014&.Sedimentary characteristics and evolutionary stages in late Paleozoic of Tian’e isolated platform in northwestern Guangxi.Geological Review,60(1):55～70.
Liu Dongzhou,Liu Haibo,Wang Changchun,Chen Cheng.2002&.The relationship between the segmented growth feature of the syngenetic fault and the hydrocarbon.Journal of Southwest Petroleum Institute,24( 3):16～19.
Liu Qiusheng,Li Huoche,He Bizhu,Zhang Yuti,Wang Yahong,Wang Jingyun,Jiang Xiaolin.2001&.“Fenestral structure,rhombic center”——depositional regularity of faulted basins.Oil & Gas Geology,22( 3):210～220.
Lu Gang,Hu Guiang,Zhang Neng,Zhang Geng,Pan Yiwen,Peng Yang.2006&.Recent approach to space—time distribution and sedimentary structural evolution of Permian reef in Youjiang basin.Geological Review,52( 2):190～197.
Lu Gang,Wei Wenlin,Zhang Neng,Hu Guian,Li Wenqiang.2002&.Paleokarst unconformity of late Permian and early Triassic in northwestern Guangxi.Guangxi Geology,15( 4):5～8.
Luca Basilone,Maurizio Gasparo Morticelli,Gabriele Lena.2010.Mesozoic tectonics and volcanism of Tethyan rifted continental margins in western Silicy.Sedimentary Geology,226:54～70.
Luca Basilone.2009.Mesozoic tectono-sedimentary evolution of Rocca Busambra in Western Sicily.Facies,55:115～135.
Luo Yunyi,Tang Bin,Lin Chongxian,Li Guangzao,Li Jiaxiang.2004&.Extension and extensional unconformity of the Youjiang rift in western Guangxi.Geological Bulletin of China,23( 2):160～168.
Ma Xingyuan (legacy works).2004#.Analytical Tectonics.Beijing:Geological Publishing House:274～277.
Maurice E Tucker,V Paul Wright with a chapter by J A D Dichson.1990.Carbonate Sedimentology.Blackwell Scientific Publications:45～255.
Moretti and Colletta.1988.Fault-block tilting:the Gebel Zeit example,Gulf of Suez.Juornal of Structural Geology,10(1):9～19.
Mou Chuanlong.1997&.Devonian sedimentary basins in Hunan:evolution and sequence stratigraphic model.Tethyan Geology,21:85～99.
Peng Yang,Hu Guiang,Lu Gang,Zhang Yuxu,Qiao Xiufu.2004&.Progress in studying on limestone dykes in late Paleozoic strata in northwestern Guangxi.Geological Review,50( 6):1～7.
Peng Yang,Li Yan,Hu Guiang,Lu Gang,Qiao Xiufu.2007&.Limestone dykes and breccia limestone bodies in the upper Devonian Rongxian formation in Miaotou area,Guilin,Guangxi.Geological Review,53( 6):736～743.
Peng Yang,Lu Gang,Hu Guiang,Zhou Min,Qiao Xiufu,Zhang Yuxu.2009a&.Genesis of the Permian limestone neptunian dykes and limestone breccia talus in the Xiajia area,Lingyun county,Guangxi,and its geological significances.
Peng Yang,Lu Gang,Hu Guiang.2013&.Study on carbonate limestone dykes (neptunian dykes) of upper Devonian in Nanbiancun,Guilin,Guangxi.Geological Review,59(2):217～224.
Peng Yang,Lu Gang.2015&.New approach on Devonian—Carboniferous carbonate neptunian dykes and earthquake events in Leye,Guangxi.Geological Review,61(2):1～7.
Peng Yang,Yang Tiannan,Qiao Xiufu,Li Dianzhi,Wang Guozhen,Yang Zhongzhu,Yang Xiaobo.2001&.A study of seismic events in the late Sinian carbonates of Dalian,China.Acta Geological Sinica,75(2):221～227.
Peng Yang.2009b&.Late Palaeozoic Limestone Dyke-breccia Limestone Body——Synsedimentary Fault with Palaeoseismic Record,Guilin-Youjiang.Doctoral Supervisor:Bai Zhiqiang.Beijing:Peking University Ph.D.dissertation.
Qiao Xiufu,Peng Yang,Gao Linzhi.2002&.Interpretation of the seismic origin of Permian limestone dykes in northwestern Guangxi.Geological Bulletin of China,21(2):102～104.
Ren Guangming,Wang Peng,Zhang Linkui,Zhang Binhhui,Dai Jie.2011&.Discussion on geochemical charateristics and sedimentary environment of the Frasnian Radiolarian chert in southeastern Yunnan.Geological Review,57(4):505～514.
Ren Jianye,Lu Yongchao,Zhang Qinglin.2004&.Forming mechanism of structural slope-break and its control on sequence style in faulted basin.Earth Science——Journal of China University of Geoscience,29(5):596～602.
Santantonio M.1993.Facies associations and evolution of pelagic carbonate platform/basin systems:examples from the Italian Jurassic.Sedimentology,40:1039～1067.
Santantonio M.1994.Pelagic carbonate platforms in the geologic record:their classification,and sedimentary and paleotectonic evolution.AAPG Bull.,78:122～141.
Stefano P D,Mindszenty A.2000.Fe—Mn-encrusted “Kamenitza” and associated features in the Jurassic of Monte Kumeta (Sicily):subaerial and/or submarine dissolution.Sedimentary Geology,132:37～68.
Stephen Marshak,M.Scott Wilkerson,Joshua DeFrates.2016.Structural geology of the Baraboo District:an introduction.GSA Field Guides,43:13～36.
Sun Dongsheng.1995&.Numerical simulation of gravity synsedimentary fault.Fault-Block Oil & Gas Field,2(4):1～3.
Tan Fuwen,Pan Guitang,Wang Jian.2001&.Devonian—Triassic basin——range transformation and the tectonic evolution of Palaeo-Tethys in western Yunnan,China.Journal of Mineral Petrol,21(3):179～185.
Tanner L H and Hubert J F.1992.Depositional facies,paleogeography and palaeoclimatology of the Lower Jurassic McCoy Brook Formation,Fundy rift basin,Nova Scotia.Palaeogeography,Palaeoclimatology,Palaeoecology,96(3～4):261～280.
The Bureau of Geology and Mineral Resources of Guangxi Zhuang Autonomous Region.1985#.Regional Geology of Guangxi Zhuang Autonomous Region,People’s Republic of China.Beijing:Geological Publishing House:658～659,680～681.
The Eighth Geological Team,Guangxi Zhuang Autonomous Region and the Huainan Coal College,Anhui Province.1978#.On the discovery of early Permian sedimentary limestone dykes and limestone bodies in Lingyun county,Guangxi Zhuang Autonomous region,China,and their significance in the study of Palaeotectonics.In proceedings of the 25th International Geological Congress by Zhouzhian and in Geomechanics Corpus,(2):32～38.
Thomas W,Dibblee J R.1971.A great middle Tertiary buttress unconformity in the Newberry mountains,Mojave desert,California,and its paleogeologic inplications.GeoRef Record/GeoScienceWorld,3(2):110.
Tian Jingchun,Zeng Yunfu.1995&.The revolution of the isotopic composition of strontium in the Permian palaeo-ocean in south China.Acta Sedimentologica Sinica,13(4):125～130.
Vendeville B,Cobbold P R.1988.How normal faulting and sedimentation interact to produce listric fault profiles and stratigraphic wedges.Journal of Structural Geology,10(7):649～659.
Wang Guibin.1992#.On the special surfaces between Maping Stage—Maokou Stage in Gaolong area,Guangxi——a new type of unconformity.Guangxi Region Geology.Combined issue of 1991～1992:19～24.
Wang Haizhou.1997&.Rifts of late Permian epoch in western Guangxi.Guangxi Geology,10(1):7～10.
Wang Jian,Ning Pugong.1998&.Study on tectonic evolution of Devonian sedimentary basins and Lead—Zinc metallization of Guangxi.Guangxi Geology,11(1):1～6
Wang Shenghai,Qiangzitong,Wen Yingchu,Lu Weiping.1989&.Neptunian dykes and their significance of Jianshuigou upper Permian reef comples in Huaying mountains,Sichuan,China.Journal of Southwestern Petroleum Institute,11(3):16～22.
Wang Xinqiang,Shi Xiaoyin.2008&.Sedimentary characteristics and evolution of the late Paleozoic Leye isolated carbonate platform in northwest Guangxi.Journal of Palaeogeography,10(4):329～340.
Wang Yingmin,Jin Wudi,Liu Shuhui,Qiu Guiqiang,Li Qun,Liu Hao,Xin Renchen,Yang Fei.2003&.Genetic types,distribution and esploration significance of multistage slope breaks in rift lacustrine basin.Oil & Gas Geology,24(3):199～214.
Wang Zhongcheng,Wu Haoruo,Kuang Guodun.1997&.Characteristics of the late Paleozoic oceanic basalts and their eruptive environments in west Guangxi.Acta Petrologica Sinica,13(2):260～265.
Wendt J .1965.Synsedimentaire Bruchtektonik im Jura Westsiziliens.N Jb Geol Palaontol Mh,5:286～311.
Wendt J.1971.Genese and Fauna submariner sedimentaaarer Spaltenfullungen im mediterranen Jura.Palaeontographica A 136:122～192.In:Luca Basilone,Maurizio Gasparo Morticelli,Gabriele Lena.2010.Mesozoic tectonics and volcanism of Tethyan rifted continental margins in western Silicy.Sedimentary Geology,226:54～70.
Winterer E L,Metzler C V,Sarti M.1991.Neptunian dykes and associated breccias (Southern Alps,Italy and Switzerland):role of gravity sliding in open and closed systems.Sedimentology,38:381～404.
Winterer E L,Sarti M.1994.Neptunian dykes and associated features in southern Spain:mechanisms of formation and tectonic implication.Sedimentology,41:1109～1132.
Wu Chonglong,Wang Xinqing,Liu Gang,Li Shaohu,Mao Xiaoping,Li Xing.2001#.On kinetics of tectonic evolution of Fushun basin.Science in China (Series D),31(6):477～485.
Wu Genyao,Wu Haoruo,Zhong Dalai Kuang Guodun,Ji Jianqing.2000&.Volcanic rocks of palaeotethyan oceanic island and island-arc bordering Yunnan and Guangxi,China.Geoscience.Journal of Graduate School,China University of Geosciences,14(4):393～400.
Wu Haoruo,Kuang Guodun,Xian Xiangyang,Li Yuejun,Wang Zhongcheng.1994.On late Palaeozoic Radiolarian chert in south Guangxi and preliminary discuss on palaeotethyan in Guangxi.Chinest Science Bulletin,39( 9):809～812.
Wu Haoruo.1999&.Implications of Radiolarian chert for the palaeogeography of south China.Journal of Palaeogeography,1(2):28～35.
Wu Haoruo.2000&.A discussion on the tectonic palaeogeography related to the Caledonian movement in Guangxi.Journal of Palaeogeography,2(1):70～76.
Wu Haoruo.2003&.Discussion on tectonic palaeogeography of Nanpanjiang sea in the late Palaeozoic and Triassic.Journal of Palaeogeography,5(1):63～76.
Wu Jiyuan,Sun Zhong.1981.The characteristics of Napo mixtite and its formation mechanism.Guangxi Geological Science and Technology,24:29～37.
Yin Hongfu,Wu Shunbao,Du Yuansheng,Peng yuanqiao.1999&.South China defined as part of Tethyan archipelagic ocean system.Earth Science——Journal of China University of Geoscience,24(1):1～12.
Zhang Qi,Qian Qing,Wang Yan.1999&.Late Palaeozoic basic magmatism from SW Yangtze Massif and evolution of the Palaeo-Tethyan Ocean.Acta Petrologica Sinica,15(4):576～583.
Zhang Zhenxian.1998&.Relationship between fault and micrograined disseminated gold deposit southern Guangxi.Guangxi Geology,11(4):37～43.
Zhou Kaihua,Chen Chunfang,Lu Gang,Tian Qing,Li Xinhua,Tang Xintian.2011b&.Genesis of Carboniferous subaqueous limestone dykes in Buding area,Tiandong county,Guangxi.Geological Review,57(6):900～905.
Zhou Kaihua,Lu Gang,Chen Chunfang,Tian Qing,Jiang Liang,Li Xinhua,Wu Lihe.2011a&.New Progresses in 1:50000 regional geological survey in Gumei area,Guangxi.Geology and Mineral Resources of South China,27(4):342～351.
Zhou Yongsheng,Wang Dongpo,Yang Bingzhong,Sun Chunyan,Guo Shaobin.1993&.Tectono-sedimentary evolution and oil accumulation in the Yishu Graben,northeastern China.Lithofacies Palaeogeography (Journal of Palaeogeography),13(5):1～5.
(1) 广西地勘局.1992.定安幅—八渡圩幅1∶5万区域地质调查报告.Guangxi Geological Survey Bureau.1992.Regional Geological Exploration Reports on Ding’an Chart—Baduxu Chart of 1∶50000 Geological Map.
(2) 广西地勘局.1995.乐业幅1∶5万区域地质调查报告.Guangxi Geological Survey Bureau.1995.Regional Geological Exploration Reports on Leye Chart of 1∶50000 Geological Map.
(3) 广西地勘局.1992.金牙—凌云1∶5万区域地质调查报告.Guangxi Geological Survey Bureau.1992.Regional Geological Exploration Reports on Jinya Chart—Lingyun Chart of 1∶50000 Geological Map.
(4) 广西地勘局.2001.凤山—天峨幅1∶5万区域地质调查报告.Guangxi Geological Survey Bureau.2001.Regional Geological Exploration Reports on Fengshan Chart—Tian’e Chart of 1∶50000 Geological Map.
(5) 广西地勘局.2000.甘田镇—浪平幅1∶5万区域地质调查报告.Guangxi Geological Survey Bureau.2000.Regional Geological Exploration Reports on Gantianzhen Chart—Langping Chart of 1∶50000 Geological Map.
(6) 广西地勘局.2004.下雷—上映测区1∶5万区域地质调查报告.Guangxi Geological Survey Bureau.2004.Regional Geological Exploration Reports on Xialei Chart—Shangyin Chart of 1∶50000 Geological Map.
(7) 广西地勘局.1989.广西地质图(1∶250万)说明书.Guangxi Geological Survey Bureau.1989.Specification on 1∶2500000 Guangxi Geological Map.