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柴西第三系构造沉积演化与油气成藏
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摘要
柴达木盆地西部的茫崖坳陷是青海油田公司的主力石油产区,但是到目前为止,虽经近半个世纪的勘探开发,人们对茫崖坳陷第三系的构造沉积演化历史还不清晰,因而严重地影响了人们对油气资源的形成与分布规律的认识,进而严重地影响了油气的勘探开发,使勘探的风险及开发成本提高。
     本论文旨在通过对柴西茫崖坳陷第三系构造沉积演化的深入研究,系统探讨茫崖坳陷第三系油气的形成分布规律,为油气勘探开发服务。
     众所周知,柴西茫崖坳陷夹持于昆仑山与阿尔金山之间,因此决定了茫崖坳陷第三纪构造沉积演化及成藏历史非常复杂,这些复杂性导致了油气分布的复杂及提高了勘探风险。本次研究以西岔沟等剖面精细的地表地质调查和沉积相的综合研究为基础,结合室内资料对茫崖坳陷的沉降沉积史、地热演化史及充填史进行了精细研究,阐明了茫崖坳陷第三纪的构造沉积演化历史,在此基础上阐明了茫崖坳陷第三系的油气形成与分布规律,指出了有利的油气勘探区域,对青海油田的油气勘探开发具有重要的指导意义。
     此外,本次研究的一个重要研究成果是首次在茫崖坳陷发现了第三纪湖相生物礁。这在中国西部的大型盆地中也尚属首次。这一发现对于柴达木盆地第三系油气的勘探开发具有重要的实践意义。
Mangya depression, in the Western Qaidam Basin, is the main oil-production area for the Qinghai oil company. Although the exploration and development lasted for nearly five decades, the depression is hithernto far from being exploited completely in terms of the Tertiary tectonic and sedimentary history, and therefore preventing the unambiguous understanding to the formation of the reservoir and the oil distribution, and furthermore limiting the exploration and development of the oil field, hence resulting in the rise of the exploration and development cost.
    This thesis, on the basis of the deeper research of the Tertiary tectonic and sedimentary evolution of the depression, is mainly to discuss systematically the formation and distribution of the Tertiary oil and gas in Mangya depression, and provide service for the exploration and development.
    It is well known that, the Mangya depression in the Western Qaidam Basin is bounded by the Kunlun and Altun Tagh mountain, therefore determining the extraordinary complexity of the Tertiary tectonic and sedimentary evolvement and the reservoir-formation, and resulting in the complexity of the oil and gas distribution and rise of the exploration cost
    On the basis of detailed field survey for the Xichagou section and comprehensive study on the sedimentary facies and previous research achievements, the sedimentation, thermal and infilling history is studied precisely and in detail, and the Tertiary tectonic and sedimentary evolution is illuminated, and the Tertiary oil and gas formation and distribution, which is based on the research above, is further illuminated, and the favorable exploration zone is pointed out. Hence it is of important directive significance for the exploration and development of the Qinghai oil field.
    Moreover, as an important research achievement, the Tertiary lacustrian reef, which is never reported before in the large West China basin, is discovered in Mangya depression. This discovery is of important and practical significance for the oil exploration and development in the Qaidam basin.
引文
[1]范连顺等.柴达木盆地茫崖坳陷含油气系统及勘探方向.石油实验地质,1999,21(1):42~47.
    [2]范连顺等.柴达木盆地茫崖坳陷含油气系统.青海石油,1997,15(4):40~45.
    [3]邱楠生、顾生党、丁丽华、陈刚、杨乾政.柴达木盆地西部新生代的构造—热演化研究.地质科学,2000,35(4):456~464.
    [4]Dow W.G. Kerogen studies and geological interpretations: Journal of Geochemical. Exploration, 1977, 7(1): 79~99.
    [5]Katz B.J, Phelfer R N. and Schunk D.J Interpretation of discontinuous Vitrinite Reflectance profiles. AAPG Bulletin, 1988, 72(8): 926~931.
    [6]钟建华、韩德馨.早期煤化作用初探.地学探索,1988,1:106~112.
    [7]石广仁.油气盆地数值模拟方法(第二版).北京:石油工业出版社,1999:14~100.
    [8]费琪.成油体系分析与模拟.北京:中国地质大学出版社,1997.10:254~260、269~270.
    [9]信荃麟、刘泽容等.含油气盆地构造岩相分析.北京:地质出版社,1993.8:67~72.
    [10]Dowdeswell, J.A., Whittington, R.J., Jennings, A.E., Andrews, J.T., Mackensen, A. and Marienfeld, P. An origin for laminated glacimarine sediments through sea-ice build-up and suppressed iceberg rafting. Sedimentology, 2000, 47: 557~576.
    [11]Marienfeld, P. Holozane sedimentation sentwicklung in Scoresby Sund, Ost-Gronland. Berichte Polarforschung, 1991,96: 162.
    [12]Terro, H.D. Paterson, T.T. Studies on the ice age in India. Associated Human Culture, 1939.
    [13]李吉均、徐叔鹰.巴基斯坦北部的地貌发育与第四纪冰期问题.地理学报,1983,38(1):11~24.
    [14]李永昭.青藏高原第四纪冰期序列及其意义.成都理工学院学报,1998,25(2):303~308.
    [15]周尚哲,李吉均.冰期之青藏高原新研究.地学前缘,2001,8(1):67~75.
    [16]西尼村B M.关于亚洲高原第四纪冰川问题.地理译报,1958(1):22~30.
    [17]王明业,郑绵平.青藏高原第四纪冰川遗迹.地理学报,1965,31(1):65~72.
    [18]KUHLE M. Subtropical mountain and highland glaciation as Ice Agetriggers and the waning of the glacial periods in the Pleistocene.Ceo Joumal, 1987,14(4):393~421.
    [19]郭鹏飞.祁连山中段地区第四纪冰期探讨.冰川冻土,1984,6(1):6~15.
    [20]李吉均,郑本兴,杨锡金,等.西藏冰川.北京:科学出版社,1986,194~276.
    [21]李炳无,李吉均,崔之久,等.青藏高原第四纪冰川遗迹分布图.北京:科学出版社,1991.
    [22]DERBYSHIRE E, SHI Yafeng, LI Jijun, et al. Quaternary glaciation of Tibet: the geological evidence.Quaternary Science Review, 1991,10: 485~510.
    [23]韩同林.青藏大冰盖.北京:地质出版社,1991,1~109.
    [24]郭宏伟.祁连山冷龙岭南麓冰川序列,黄土记录及阶地系列的初步研究.兰州:兰州大学,1993,47.
    [26]徐道明,沈永平.青藏高原的泛冰盖遗迹与冰期.冰川冻土,1995,17(3):213~229.
    [27]伍光和.祁连山第四纪冰期问题[A].中国科学院兰州冰川冻土研究所集刊,1984,第5号.北京:科学出版社,1984,116~123.
    [28]李吉均,冯兆东,周尚哲.横断山冰川.北京:科学出版社,1996,172.
    [29]Jin Rosc, Dcrbyshire E, Guo Hongwei, et al. Glaciation of the Eastern Qilian Shan, Northwest China[A]. Quaternary Procccdings NO.6[C]. 1998,143~152.
    [30]施雅风.第四纪中期青藏高原冰冻圈的演化及其与全球变化的联系.冰川冻土,1998,20(3):
    
    199~208.
    [31]ZHOU Shangzhe, Li Jijun. The Sequence of Quaternary glaciation in the Bayan Har Mountains. Quatemary Intemational, 1998,45/46: 135~142.
    [32]李吉均,方小敏.青藏高原隆起与环境变化研究.科学通报,1998,43(15):1569~1574.
    [33]Zheng Benxing,Rutter N. On the problem of Quaternary glaciations, and the extent and patterns of Pleistocene ice cover in the Qinghai-xizang (Tibet) plateau. Quaternary International, 1998, 45/46: 109~122.
    [34]Vorren, T.O., Hald, M. and Thomsen, E.Quarternary sediments and environments on the continental shelf off northern Norway. Mar. Geol.,1984,57: 229~257.
    [35]Mackiewicz, N.E., Powell, R.D., Carlson, P.R. and Molnia, B.E Interlaminated ice-proximal glacimarine sediments in Muir Inlet, Alaska. Mar. Geol., 1984,57: 113~147.
    [36]Domack, E.W. Laminated terrigenous sediments from the Antarctic Peninsula: the role of subglacial and marine processes. In:Glacimarine Environments: Processes and Sediments(Ed by J.A. Dowdeswell and J.D. Scourse), Geol. Soc. Spec. Publ.,1990,53: 91~103.
    [37]Cowan, E.A. and Powell, R.D. Suspended sediment transport and deposition of cyclically interlaminated sediment in a temperate glacial fjord, Alaska, USA. In:Glacimarine Environments: Processes and Sediments(Ed. by J.A. Dowdeswell and J.D Scourse), Geol. Soc. Spec. Publ., 1990, 53:75~89.
    [38]Gilbert, R. Rafting in glacimarine environments. In:Glacimarine Environments: Processes and Sediments(Ed. By J.A. Dowdeswell and J.D. Scourse), Geol. Soc. Spec.Publ., 1990,53: 105~120.
    [39]Jennings, A.E. The Quaternary history of Cumberland Sound,southeastern Baffin Island: the marine evidence. Geogr. Phys. Quat.,1993,47:21~42.
    [40]Polyak, L. and Solheim, A. Late-and postglacial environments in the northern Barents Sea west of Franz Josef Land. Polar Res., 1994,13:197~207.
    [41]Lubinski, D.J., Korsun, S., Polyak, L., Forman,S.L., Lehman, S.J., Herlihy, F.A. and Miller, G.H. The last deglaciation of the Franz Victoria Trough, northern Barents Sea. Boreas, 1996,25:89~100.
    [42]Andersen, E.S. Dokken, T.M., Elverhei, A.,Solheim, A. and Fossen,Late Quaternary sedimentation and glacial history of the western Svalbard continental margin. Mar. Geol., 1996,133:123~156.
    [43]吴应生.广西隆林下二叠统生物礁的综合研究.地质论评,1989,35(1):52~59.
    [44]朱忠德.峡东宜昌黄花场下奥陶统生物礁的研究.地质科学,1993,28(1):1~9.
    [45]王永标、张克信、龚一鸣、张志、骆满生.东昆仑地区早二叠世生物礁带的发现及其重要意义.科学通报,1998,43(6):630~632.
    [46]巩恩普、关广岳.中国石炭纪生物礁造礁群落演化.地质论评,1998,44(2):160~164.
    [47]覃建雄、曾允孚、陈洪德、田景春.右江盆地二叠纪生物礁层序地层学研究.地质科学,1999,34(4):506~517.
    [48]吴应生、范嘉松.根据生物礁定量计算茅口全球海平面变化幅度.中国科学(D辑),2001,31(3):233~242.
    [49]田树刚、范嘉松.东昆仑早-中二叠世生物礁建造特征.地质学报,2002,76(2):145~154.
    [50]Hein J. R., Gray S. C., Richmond B. M. and White L. D. Dolomitization Quaternary Reef Limestone, Aitutaki, Cook Islands. Sedimentology, 1992,39:645~661.
    [51]Camoin G. F. and Montaggioni L. F. High Energy Coralgal-Stromatolite Frameworks From Holocene Reefs (Tahiti, French, Polynesia) Sedimentology, 1994,41:655~676.
    [52]Satterley A. K., Marshall J. D.and Fairchild I. J. Diagenesis of An Upper Triassic Reef Complex,
    
    Wilde Kirche, Northern Calcareous Alps, Austria. Sedimentology, 1994,41:935~950.
    [53] Talbot C. J., Stanley W., Soub R. and Al-Sadoun N. Epitaxial Sslt Reefs and Mushrooms in the Southern Dead Sea. International Association of Sedimentoligists, Sedimentology, 1996, 43: 1025~1047.
    [54] Martin J. M., Braga J. C. and Riding R. Late Miocene Halimeda Alga-Microial Segment Reefs in the Marginal Mediterranean Sorbas Basin, Spain. Sedimentology, 1997,44:441~456.
    [55] Strasser, A and Strohmenger C. Early Diagenesis in Pleistocene Coral Reefs, Southern Sinai, Egypt: Response to Tectonics, Sea-Level and Climate. Sedimentology, 1997,44:537~558.
    [56] Insalaco E., Hallam A. and Rosen B. Oxfordian (Upper Jurassic) Coral Reefs In Western Europe:Reef Types and Conceptual Depositional Model. Sedimentology, 1997,44:707~743.
    [57] Dill R.F., Shinn E. A., Jones A. T., Kelly K. and Steinen R. P. Giand Subtidal Stromatolites Forming in Normal Salinity Watres. Nature, 1986, 324(6):55~58.
    [58] Feldmann M. Stromatolite-Thrombolite Associations in a Modem Environment, Lee Stocking Island, Bahamas. Palaios, 1998,V. (13):201~212.
    [59] Narbonne G.M. and James N. P. Mesoproterozoic Dee-Water Reefs From Borden Peninsula, Arctic Canada. Sedimentology, 1996,43:827~848.
    [60] Macintyre I. G., Reid R. P. and Steneck R.S. Growth History of Stromatolites in a Holocene Fringing Reef, Stocking Island, Bahamas. Journal of Sedimentary Research, 1996, 66(1): 231~242.
    [61] Rouchy E. M., Servant M., Fournier M. and Causse C. Extensive Carbonate Algal Bioherms in Upper Pleistocene Saline Lakes of the Central Altiplano of Bolivia. Sedimentology, 1996, 43:973~993.
    [62] Riding R., Martin J. M. and Braga C. Coral-Stromatolite Reef Framework, Upper Miocene, Almeria, Spain. Sedimentology, 1991,38:799~818.
    [63] Feldmann M. and Mckenzie J. A. Messinian Strombolite Association, Santa Pola, SE Spain: An Analoguw For The Palaeozoic? Sedimentology, 1997,44:893~914.
    [64] Pomar L. Reef Geometries, Erosion Surface and High-Frequency Sea-Level Changes, Upper Miocene Reef Complex, Mallorca, Spain. Sedimentology, 1991,38: 243~269.
    [65] 黄汲清、任纪舜、姜春发、张之孟、许志琴.中国大地构造基本轮廓.地质学报,1977,51(2):117~135.
    [66] 任纪舜、姜春发、张正坤等.中国大地构造及其演化.北京:科学出版社.1980.
    [67] 黄汲清.中国大地构造特征的新研究.中国地质科学院院报.北京:地质出版社,1984:5~18.
    [68] 潘桂棠、焦淑沛、徐光耀等.阿尔金地穹系新生代构造及造山性质.地质矿产部青藏高原地质文集编委会编.青藏高原地质论文集(15).北京:地质出版社,1984,113~119.
    [69] 焦淑沛.塔里木—柴达木地洼区的地史演化特征及其归属问题.青藏高原地质文集,1984,121~130.
    [70] 陈国达.地洼学说导论.1985.
    [71] 杨森楠、杨巍然.中国区域大地构造学.北京:地质出版社,1985.
    [72] 黄汉纯、王长利.阿尔金构造带及其对塔里木和柴达木盆地的影响.中国地质科学院院报.北京:地质出版社,1987:17~32.
    [73] 郑剑东.阿尔金断裂带的几何学研究.中国区域地质,1991,(1)54~59.
    [74] 蔡学林.阿尔金地穹系走滑断裂构造样式.成都地质学院学报,1992,19(1):8~17.
    [75] 杨藩、叶素娟、曹春潮等.新生代阿尔金断层中、东段右行走滑特征.地质科学,1994,29(4):
    
    346~353.
    [76]车自成、刘良、刘洪福、罗金海.阿尔金地穹系地区高压变质泥质岩石的发现及其产出环境.科学通报,1995,40(14):1298~1300.
    [77]Da Zhou, Graham. SA. Extrusion of the Altyn Tagh wedge: A Kinematic model for the Altyn Tagh fault and palinspastic reconstruction of northern China. Geology, 1996,24(5): 427~430.
    [78]刘良、车自成、王焰、罗金海、陈丹玲.阿尔金地穹系西段榴辉岩的确定及地质意义.科学通报,1996,41(14):1485~1488.
    [79]孙勇、刘池阳、车自成.阿尔金地穹系拉配泉地区元古宙裂谷火山岩及其构造意义.地质论评,1997,43(1):17~24.
    [80]刘训、姚建新、王永.再论塔里木板块的归属问题.地质论评,1997,43(1):1~9.
    [81]谢晓安、胡素云、卢华复.探讨塔里木盆地巴楚断隆的正反转构造.地质论评,1998,44(1):1~6.
    [82]张建新、许志琴、崔军文.一个韧性转换挤压带的变形分解作用—以阿尔金断裂带东段为例,地质论评,1998,44(4):348~356.
    [83]郭召杰、张志诚.阿尔金盆地群构造类型与演化.地质论评,1998,44(4):357~364.
    [84]高锐、李廷栋、吴功建.青藏高原岩石圈演化与地球动力学过程—亚东—格尔木—额济纳旗地学断面的启示.地质论评,1998,44(4):389~395.
    [85]马宗晋、张家声、汪一鹏.青藏高原三维变形运动学的时段划分和新构造区.地质学报,1998,72(3):209~227.
    [86]葛肖虹、张梅生、刘永江、叶慧文、石采东.阿尔金断裂研究的科学问题与研究思路.现代地质,1998,12(3):295~301.
    [87]刘良、车自成、王焰、吴金海、陈丹玲.阿尔金高压变质带的特征及其构造意义.岩石学报,1999,15(1):57~64.
    [88]张建新、张泽明、许志琴、杨经绥、崔军文.阿尔金西段孔兹岩系的发现及岩石学、同位素年代学初步研究.中国科学(D辑),1999,29(4):299~305.
    [89]崔文军、唐哲民、邓晋福、岳永军、孟顺、余钦范等.阿尔金断褶系.北京:地质出版社,1999.
    [90]周勇、潘裕生.阿尔金断裂早期走滑运动方向及其活动时间探讨.地质论评,1999,45(1):1~9.
    [91]许志琴、杨经绥、张建新等.阿尔金断裂两侧构造单元的对比及岩石圈构造机制.地质学报,1999,73(3):193~204.
    [92]魏国齐、贾承先、施央申、卢华复、王良书.塔里木新生代复合再生前陆盆地构造特征与油气.地质学报,2000,74(2):123~133.
    [93]杨经绥、宋述光、许志琴等.柴达木盆地北缘早古生代高压—超高压变质带中发现典型超高压矿物—柯石英.地质学报,2001,75(2):175~179.
    [94]宋辉龙、谢宗奎、杨刚、宋兵、程桂莲、陈琰.从古地磁资料看柴达木盆地古构造环境.青海石油,18(3):1~6.
    [95]金强.柴达木盆地西部第三系盐湖相有效生油岩的识别.沉积学报,2001,19(1):125~129.
    [96]Hoffmann, E. and Jenkner, A. Die Inkohlung undinre Erkennung in Mikrobild. -Gluckauf, 1932, 68: 81~88.
    [97]Mackowsky, M.T. Neue Kohlenpetrographische Erkenntnisse an Anthrazit -C.r. 3. Congr. Intern. Strat. Géol. Carbonifére, 1952,2:423~428.
    [98]Mackowsky, M.T. Pie quentitatiren Methoden zur Kohlen petrographischen. Anschliffunter suchung, ihre Fehlergrenzen und ihre Anwendungsbereiche. -Brennst. -Chemie. 1954, 35:
    
    193~201; 232~235.
    [99] Hood,A., C.M.Gutjahr and R.L.Peacock. Organic metamorphism and the generation of petroleum. AAPG bulletin, 1975,59:986~996.
    [100] Douglas W. Waples. Time and Temperature in Petroleum Formation: Application of Lopatin's Method to Petroleum Exploration. AAPG Bulletin, 1980, 64(6):916~926.
    [101] Ritter, U. The influence of time and temperature on vitrinite reflectance. Organic Geochemistry, 1984,6:473~480.
    [102] Riediger C L. Solid bitumen reflectance and Rock-Eval Tmax as maturation indicators: An example from the "Nordegg Member", Western Canada Sedimentary Basin. Int. Jour. Goal Geol., 1993, 22(3/4):295~315.
    [103] 肖贤明、刘德汉、傅家漠.沥青反射率作为烃源岩成熟度指标的意义.沉积学报,1991,9(增刊),138~146.
    [104] Burnham, A.K., and J.J.Sweeney. A chemical kinetic model of vitrinite maturation and reflectance. Geochimica et Cosmochimica Acta, 1989,53:2649~2657.
    [105] Jerry J.Sweeney, Alan K.Burnham. Evaluation of a Simple Model of Vitrinite Reflectance Based on Chemical Kinetics. AAPG Bulletin, 1990,74(10):1559~1570.
    [106] 宋党育,秦勇.镜质体反射率反演的EASY%R_0数值模拟新方法.煤田地质与勘探,1998,26(3):15~17.
    [107] 张厚福,张万选.石油地质学(第二版).北京:石油工业出版社,1994:37~49.
    [108] macgergor D S. Hydrocarbon habitat and classification of inverted rift basins. In:Buchanan J G & Buchaanan P G (eds).Basin Inversion(M) Geological Society Special Publication, 1995,88:83~93.
    [109] 付国民等.柴达木盆地干柴沟地区油气成藏条件及其勘探意义.甘肃地质学报,2000,9(1):66~72.
    [110] 刘人和等.青海柴达木盆地咸水泉油田第三系地层裂缝分布评价.矿物岩石,1998,18(2):52~56.
    [111] 李元奎等.柴达木盆地狮子沟地区中深层裂缝性油藏.石油勘探与开发,2001,28(6):12~15.
    [112] 徐怀民,林玉祥等.茫崖坳陷下第三系有机酸形成演化及空间分布.石油勘探与开发,2000,27(6):23~25.
    [113] 李元奎等.南翼山裂缝性油气藏特征及分布规律探讨.天然气工业,2000,20(3):22~25.
    [114] 魏成章等.柴达木盆地南翼山凝析气藏裂缝储层特征.天然气工业,1999,19(4):5~7.

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