岩性油气藏 ›› 2018, Vol. 30 ›› Issue (4): 14–25.doi: 10.12108/yxyqc.20180402

• 油气地质 • 上一篇    下一篇

准噶尔盆地西北缘同沉积构造坡折对层序建造和岩性油气藏富集带的控制

冯有良, 胡素云, 李建忠, 曹正林, 吴卫安, 赵长义, 崔化娟, 袁苗   

  1. 中国石油勘探开发研究院, 北京 100083
  • 收稿日期:2017-12-21 修回日期:2018-04-13 出版日期:2018-07-21 发布日期:2018-07-21
  • 第一作者:冯有良(1963-),男,博士,高级工程师,主要从事含油气盆地分析、区带评价和目标优选等方面的研究工作。地址:(100083)北京市海淀区学院路20号910信箱。Email:fyouliang@petrochina.com.cn。
  • 基金资助:
    中国石油勘探生产分公司科技项目“准噶尔盆地西北缘新层系新区带综合评价与风险勘探目标评价”（编号：2009D-0705-01）资助

Controls of syndepotitional structural slope-break zones on sequence architecture and enrichment zones of lithologic reservoirs in northwestern margin of Junggar Basin

FENG Youliang, HU Suyun, LI Jianzhong, CAO Zhenglin, WU Weian, ZHAO Changyi, CUI Huajuan, YUAN Miao   

  1. PetroChina Research Institute of Petroleum Exploration and Development, Beijing 100083, China
  • Received:2017-12-21 Revised:2018-04-13 Online:2018-07-21 Published:2018-07-21

PDF (PC)

622

摘要： 准噶尔盆地西北缘是该盆地油气最富集的区带，岩性地层油气藏是其主要的勘探领域，同沉积构造坡折对层序建造和岩性油气藏富集带具有控制作用。应用地震、钻井和测井资料，按照构造层序分析的方法，对该区同沉积构造坡折特征及其控制的层序建造进行了系统研究。结果表明：该区发育的同沉积构造坡折按成因可划分为同沉积逆断裂坡折和隐伏断裂挠曲坡折。前者是同期发育的逆断层活动造成的湖底坡度梯度变化带，后者是深部隐伏断裂活动造成的湖底坡度梯度变化带。中—晚二叠世，该区属于断坳转换幕，发育同沉积逆断层坡折及其控制的层序建造。三叠纪以后盆地处于挤压坳陷阶段，发育同沉积逆断裂坡折和隐伏断裂挠曲坡折及其控制的层序建造。同沉积逆断裂坡折控制的层序建造向岸一侧低位域发育冲积扇到辫状河道砾岩，向湖一侧发育辫状河三角洲沉积；湖扩展体系域坡折向岸一侧发育薄层泛滥平原、浅湖及退积型三角洲沉积，向湖一侧发育泛滥平原或半深湖沉积；高位域发育河流、三角洲前缘，其可越过坡折向湖进积。挠曲坡折控制的层序建造低位域坡折向岸一侧发育辫状下切水道充填，向湖一侧发育由滨浅湖滩坝砂体或低位辫状三角洲砂体构成的低位楔；湖扩展体系域坡折向岸一侧发育滨浅湖，向湖一侧发育半深湖沉积；高位域发育河流三角洲及滨浅湖沉积。同沉积构造坡折控制的层序低位域砂砾岩体储层，如冲积扇、辫状河道、低位三角洲及滨浅湖砂体、湖底扇砂体，若有断裂和不整合面与风城组油源沟通，能形成良好成藏条件，有利于岩性油气藏发育。

关键词: 深水区, 中央峡谷, 砂体成因, 展布规律, 琼东南盆地

Abstract: The western margin of Jungger Basin is a petroliferous structural belt,and lithostratigraphic reser-voirs are dominant exploring targets. Syndepositional structural slope-break zone has a strong control effect on sequence architecture and enrichment zones of lithologic reservoirs. On the basis of seismic,drilling and logging data,according to the method of structural sequence analysis,the characteristics of syndepositional structural slope-break zones in the study area and its controlled sequence architecture were studied. The results show that the syndepositional slope-break zones developed in the study area can be divided into two types,namely,the slope-break zone controlled by syndepositional reverse faults and flexure slope-break zone controlled by buried fault,according to the origin. The former is the gradient abrupt zone of lake bed caused by syndepositional reverse fault movement,while the later is the gradient abrupt zone of lake bed resulted by seated-reverse-faults. During Middle to Late Permian period,the study area was in the transition stage from rifted basin to down-warped basin, slope break zones controlled by syndepositional reverse faults and sequence architecture controlled by them were developed. Since Triassic to Paleogene period,the study area was in the compressional down-warped stage, slopebreak zones controlled by syndepositional reverse faults,flexural slop-break zones controlled by buried fault,and sequence architecture controlled by them,were developed. The sequence architecture controlled by syndepositional reverse faults slop-break zone shows that the lowstand systems tract is composed of alluvial fans and braided river deposited at the upward of the zone,and the braided deltas developed at the downward of the zone,the expanding systems tract consists of floodplain,shallow lake and retrogradational deltaic sediments at the upward of the zone,shallow to deep lake deposits at the downward of the zone,and highstand systems tract comprises of fluvial deltas. The sequence architecture controlled by flexural slope break zone is characterized by incised infills deposited at the upward of the flexural slope break zone and shallow lake or lowstand braided deltas deposited at the downward of the zone within lowstand systems tract,shallow to half deep lake developed in expanding systems tract,and fluvial deltaic and shore to shallow lake deposited within highstand systems tracts. Lowstand conglomerate bodies and sand bodies in sequences,such as alluvial fans,deltas of lowstand and sand bodies of shore and shallow lake,have good conditions for hydrocarbon accumulation and are favorable for enrichment of lithologic reservoirs.

Key words: deepwater area, Central Canyon, sandbody genesis, distribution regularity, Qiongdongnan Basin

中图分类号: 

  • TE121.1
[1] 李思田, 程守田, 杨士恭, 等. 鄂尔多斯盆地东北部层序地层及沉积体系分析——侏罗系富煤单元的形成、分布及预测基础.北京:地质出版社, 1992:13-21. LI S T, CHENG S T, YANG S G, et al. Sequence stratigraphy and depositional system analysis of the northeastern Ordos Basin. Beijing:Geological Publishing House, 1992:13-21.
[2] 纪友亮, 张世奇.陆相断陷湖盆层序地层学.北京:石油工业出版社, 1996:1-120. JI Y L, ZHANG S Q. Sequence stratigraphy of the non-marine faulted lacustrine basin. Beijing:Petroleum Industry Press, 1996:1-120.
[3] LIN C S, ERIKSSON K, LI S T, et al. Sequence architecture, depositional systems, and controls on development of lacustrine basin fills in part of the Erlian Basin, Northeast China. AAPG Bulletin, 2001, 85:2017-2043.
[4] 李思田, 蔡希源. 陆相盆地高精度层序地层学.北京:地质出版社, 2003:1-102. LI S T, CAI X Y. High resolution sequence stratigraphy of nonmarine basin. Beijing:Geological Publishing House, 2003:1-102.
[5] 冯有良, 邱以钢.高精度层序地层学在济阳坳陷下第三系隐蔽油气藏勘探中的应用.石油学报, 2003, 24(1):49-52. FENG Y L, QIU Y G. Application of high-resolution sequence stratigraphy to exploration of Lower Tertiary subtle reservoirs in Jiyang Subbasin. Acta Petrolei Sinica, 2003, 24(1):49-52.
[6] 冯有良,李思田, 邹才能.陆相断陷盆地层序地层学研究——以渤海湾盆地东营凹陷为例.北京:科学出版社, 2006:27-181. FENG Y L, LI S T, ZOU C N. Sequence stratigraphy of the non-marine rift Basin-a case study of Dongying depression, Bohai Bay Basin. Beijing:Science Press, 2006:27-181.
[7] 李丕龙, 冯建辉, 陆永潮, 等. 准噶尔盆地构造沉积与成藏.北京:地质出版社, 2010:52-88. LI P L, FENG J H, LU Y C, et al. Structures,sedimentation and hydrocarbon accumulation of the Junggar Basin. Beijing:Geological publishing House, 2010:52-88.
[8] FENG Y L, JIANG S, WANG C F. Sequence stratigraphy, sedimentary systems and petroleum plays in a low-accommodation basin:Middle to upper members of the Lower Jurassic Sangonghe Formation, central Junggar Basin, northwestern China. Journal of Asian Earth Sciences, 2015, 105:85-103.
[9] 林畅松, 郑和荣,任建业, 等.渤海湾盆地东营、沾化凹陷早第三纪同沉积断裂作用对沉积充填的控制.中国科学:D辑地球科学, 2003, 33(11):1025-1036. LIN C S, ZHENG H R, REN J Y, et al. The control of syn-depositional faulting on the Eogene sedimentary basin fills of the Dongying and Zhanhua sags, Bohai Bay Basin. Science in China Series D Earth Science, 2003, 33(11):1025-1036.
[10] 冯有良, 周海民, 任建业, 等.渤海湾盆地东部古近系层序地层及其对构造活动的响应.中国科学:D辑地球科学, 2010, 40(10):1356-1376. FENG Y L, ZHOU H M, REN J Y, et al. Paleogene sequence stratigraphy in the east of the Bohai Bay Basin and its response to structural movement. Science in China Series D Earth Science, 2010, 40(10):1356-1376.
[11] VAN WANGONER J C, MITCHUM R M, CAMPION K M, et al. Siliciclastic sequence stratigraphy in well logs, cores, and outcrops:concepts for high-resolution correlation of time and facies. AAPG Methods in Exploration Series, 1990(7):1-55.
[12] 冯有良. 东营凹陷下第三系层序地层格架及盆地充填模式. 地球科学——中国地质大学学报, 1999, 24(6):635-642. FENG Y L. Lower tertiary sequence stratigraphic framework and basin filling model in Dongying depression. Earth Science-Journal of China University of Geosciences, 1999, 24(6):635-642.
[13] 林畅松, 潘元林, 肖建新, 等."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——中国地质大学学报, 2000, 25(3):260-266. LIN C S, PAN Y L, XIAO J X, et al. Structural slope-break zone:Key concept for stratigraphic sequence analysis and petroleum forecasting in fault subdience basins. Earth Science-Journal of China University of Geosciences, 2000, 25(3):260-266.
[14] 冯有良, 徐秀生.同沉积构造坡折带对岩性油气藏富集带的控制作用——以渤海湾盆地古近系为例.石油勘探与开发, 2006, 33(1):22-25. FENG Y L, XU X S. Syndepositional structural slope-break zone controls on lithologic reservoirs-A case from Paleogene Bohai Bay Basin. Petroleum Exploration and Development, 2006, 33(1):22-25.
[15] 辛仁臣, 蔡希源, 王英民.松辽坳陷深水湖盆层序界面特征及低位域沉积模式.沉积学报, 2004, 22(3):387-392. XIN R C, CAI X Y, WANG Y M. Depositional model of lowstand and characteristics of sequence boundary in deep-water lake, Songliao Depression Basin. Acta Sedimentologica Sinica, 2004, 22(3):387-392.
[16] 耳闯, 王英民,颜耀敏, 等.构造活动盆地层序地层特征与主控因素——以准噶尔盆地克-百地区二叠系为例. 沉积学报, 2009, 27(6):1101-1108. ER C, WANG Y M, YAN Y M, et al. Sequence stratigraphy characteristics and main controlling factors of the tectonic active basin:as an example from Permian of the Kebai area in the northwestern Junggar Basin. Acta Sedimentologica Sinica, 2009, 27(6):1101-1108.
[17] 王英民, 刘豪, 李立诚, 等.准噶尔大型坳陷湖盆坡折带的类型和分布特征. 地球科学——中国地质大学学报, 2002, 27(6):683-688. WANG Y M, LIU H, LI L C. et al. Types and distribution characteristics of slope breaks of large-type down-warped lake basins. Earth Science-Journal of China University of Geosciences, 2002, 27(6):683-688.
[18] 刘豪, 王英民, 王瑗, 等.大型坳陷湖盆坡折带的研究及其意义——以准噶尔盆地西北缘侏罗纪坳陷湖盆为例. 沉积学报, 2004, 22(1):95-102. LIU H, WANG Y M, WANG Y, et al. Study on slope break in large down warped lake basin and its significance. Acta Sedimentologica Sinica, 2004, 22(1):95-102.
[19] NOVIKOV I S. Reconstructing the stages of orogeny around the Junggar Basin from the lithostratigraphy of Late Paleozoic, Mesozoic, and Cenozoic sediments. Russian Geology and Geophysics, 2013, 54(2):138-152.
[20] CHOULET F, FAURE M, CLUZEL D, et al. Architecture and evolution of accretionary Orogens in the Altaids collage:the early Paleozoic West Junggar(NW China). American Journal of Science, 2012, 312(312):1098-1145.
[21] PING S, PAN H, XIA W, et al. Early Carboniferous intra-oceanic arc and back-arc basin system in the west Junggar, NW China. International Geology Review, 2013, 55(16):1991-2007.
[22] XIAO Q, HE S, YANG Z, et al. Petroleum secondary migration and accumulation in the central Junggar Basin, northwest China:Insights from basin modeling. AAPG Bulletin, 2010, 94(7):937-955.
[23] YANG W, JOLIVET M, DUPONT-NIVET G, et al. Source to sink relations between the Tian Shan and Junggar Basin(northwest China)from Late Palaeozoic to Quaternary:Evidence from detrital U-Pb zircon geochronology. Basin Research, 2013, 25(2):219-240.
[24] EBERTH D A, BRINKMAN D B, CHEN P J, et al. Sequence stratigraphy, paleoclimate patterns, and vertebrate fossil preservation in Jurassic-Cretaceous strata of the Junggar Basin, Xinjiang autonomous region,People's Republic of China. Canadian Journal of Earth Science, 2001, 38(12):1627-1644.
[25] 冯有良, 王瑞菊, 吴卫安, 等. 准噶尔盆地西北缘二叠纪古构造对层序地层建造及沉积体系的控制.山东科技大学学报:自然科学版, 2013, 32(5):42-52. FENG Y L, WANG R J, WU W A, et al. Controls of Permian paleostructures on stratal architecture of sequences and sedimentary systems deposited in northwestern margin Junggar Basin. Journal of Shandong University of Science and Technology (Natural Science), 2013, 32(5):42-52.
[26] VAIL P R, AUDEMARD F, BOWMAN S A, et al. The stratigraphic signatures of tectonics, eustasy and sedimentology-An overview//EINSELE G, RICKEN W, SEILACHER A. Cycles and events in stratigraphy, Berlin:Springer-Verlag, 1991:617-659.
[27] HOWELL J A, FLINTS S. A model for high resolution sequence stratigraphy with extensional basins//HOWELL J A, AITIKEN J F. High resolution stratigraphy:Innovations and applications. London:Geology Society Special Puplication, 1996:129-137.
[28] 冯有良, 周海民, 李思田, 等.陆相断陷盆地层序类型与构造特征.地质论评, 2004, 50(1):43-49. FENG Y L, ZHOU H M, LI S T, et al. Sequence types and structural characteristics in continental rift-subsidence basins. Geological Review, 2004, 50(1):43-49.
[29] FENG Y L, JIANG S, HU S Y, et al. Sequence stratigraphy and importance of syndepositional structural slope-break for architecture of Paleogene syn-rift lacustrine strata, Bohai Bay Basin, E. China. Marine and Petroleum Geology, 2016, 69:183-204.
[30] BROWN J R L F, LOUCKS R G, TREVINO R H, et al. Understanding growth-faulted, intraslope subbasins by applying sequencestratigraphic principles:Examples fromthe south Texas Oligocene Frio Formation. AAPG Bulletin, 2004, 88(11):1501-1522.
[31] 冯有良, 张义杰, 王瑞菊, 等. 准噶尔盆地西北缘风城组白云岩成因及油气富集因素.石油勘探与开发, 2011, 38(6):685-692. FENG Y L, ZHANG Y J, WANG R J, et al. Dolomites genesis and hydrocarbon enrichment of Fengcheng Formation in the northwestern margin of Junggar Basin. Petroleum Exploration and Development, 2011, 38(6):685-692.
[32] 匡立春, 吕焕通, 齐雪峰, 等.准噶尔盆地岩性油气藏勘探成果和方向.石油勘探与开发, 2005, 32(6):32-37. KUANG L C, LYU H T, QI X F, et al. Exploration and targets for lithologic reservoirsin Junggar Basin,NW China. Petroleum Exploration and Development, 2005, 32(6):32-37.
[33] 李啸, 刘海磊, 王学勇, 等.坡折带砂体成因及分布规律——以准噶尔盆地车排子地区下白垩统清水河组为例.岩型油气藏, 2017, 29(1):35-42. LI X, LIU H L, WANG X Y, et al. Origin and distribution of sandbody in slope break zone:a case study of the Lower Cretaceous Qingshuihe Formation in Chepaizi area, Junggar Basin. Lithologic Revervoirs, 2017, 29(1):35-42.
[1] 黄向胜, 闫琢玉, 张东峰, 黄合庭, 罗程飞. 琼东南盆地Ⅱ号断裂带新生界多期热流体活动与天然气运聚特征[J]. 岩性油气藏, 2024, 36(5): 67-76.
[2] 屈童, 高岗, 徐新德, 王瑞, 甘军, 梁刚, 游君君. 三角洲—浅海沉积体系泥质沉积规律模拟实验——以琼东南盆地崖南凹陷为例[J]. 岩性油气藏, 2022, 34(1): 24-33.
[3] 王玥, 郭彦如, 张延玲, 刘俊榜, 田鸣威. 鄂尔多斯盆地东北部山西组层序格架下的砂体成因类型、构型及分布[J]. 岩性油气藏, 2018, 30(3): 80-91.
[4] 毛雪莲, 朱继田, 姚哲, 徐守立, 唐历山. 琼东南盆地深水区中央峡谷砂体成因与展布规律[J]. 岩性油气藏, 2017, 29(6): 60-68.
[5] 蔡佳. 琼东南盆地长昌凹陷新近系三亚组沉积相[J]. 岩性油气藏, 2017, 29(5): 46-54.
[6] 武爱俊, 徐建永, 滕彬彬, 肖伶俐, 康波, 李凡异, 印斌浩. “动态物源”精细刻画方法与应用——以琼东南盆地崖南凹陷为例[J]. 岩性油气藏, 2017, 29(4): 55-63.
[7] 李啸, 刘海磊, 王学勇, 卞保力, 杨帆, 陈刚强. 坡折带砂体成因及分布规律——以准噶尔盆地车排子地区下白垩统清水河组为例[J]. 岩性油气藏, 2017, 29(1): 35-42.
[8] 杨雪飞，王兴志,代林呈,杨跃明,谢继荣,罗文军. 川中地区下寒武统龙王庙组沉积相特征[J]. 岩性油气藏, 2015, 27(1): 95-101.
[9] 刘 畅,苏 龙,关宝文,郑有伟,常 江，郑建京 . 茂名油页岩生烃演化特征及热解动力学—— — 以琼东南盆地地质模型为例[J]. 岩性油气藏, 2014, 26(6): 89-97.
[10] 金莉，骆宗强，李萍. 澳大利亚布劳斯盆地深水区Jamieson组AVO 异常成因分析[J]. 岩性油气藏, 2013, 25(2): 70-75.
[11] 庞军刚，卢涛，国吉安，李文厚. 鄂尔多斯盆地延长期原型湖盆恢复及中部砂体成因[J]. 岩性油气藏, 2012, 24(4): 56-63.
[12] 乔博，张昌民，杜家元，朱锐. 珠江口盆地浅水区和深水区重力流沉积特征对比[J]. 岩性油气藏, 2011, 23(2): 59-63.
Viewed
Full text


Abstract

Cited
  Shared   
  Discussed   
[1] . 2022年 34卷 2 期 封面[J]. 岩性油气藏, 2022, 34(2): 0 .
[2] 李在光, 李琳. 以井数据为基础的AutoCAD 自动编绘图方法[J]. 岩性油气藏, 2007, 19(2): 84 -89 .
[3] 程玉红, 郭彦如, 郑希民, 房乃珍, 马玉虎. 井震多因素综合确定的解释方法与应用效果[J]. 岩性油气藏, 2007, 19(2): 97 -101 .
[4] 刘俊田,靳振家,李在光,覃新平,郭　林,王　波,刘玉香. 小草湖地区岩性油气藏主控因素分析及油气勘探方向[J]. 岩性油气藏, 2007, 19(3): 44 -47 .
[5] 商昌亮,付守献. 黄土塬山地三维地震勘探应用实例[J]. 岩性油气藏, 2007, 19(3): 106 -110 .
[6] 王昌勇, 郑荣才, 王建国, 曹少芳, 肖明国. 准噶尔盆地西北缘八区下侏罗统八道湾组沉积特征及演化[J]. 岩性油气藏, 2008, 20(2): 37 -42 .
[7] 王克, 刘显阳, 赵卫卫, 宋江海, 时振峰, 向惠. 济阳坳陷阳信洼陷古近纪震积岩特征及其地质意义[J]. 岩性油气藏, 2008, 20(2): 54 -59 .
[8] 孙洪斌, 张凤莲. 辽河坳陷古近系构造-沉积演化特征[J]. 岩性油气藏, 2008, 20(2): 60 -65 .
[9] 李传亮. 地层抬升会导致异常高压吗?[J]. 岩性油气藏, 2008, 20(2): 124 -126 .
[10] 魏钦廉，郑荣才，肖玲，马国富，窦世杰，田宝忠. 阿尔及利亚438b 区块三叠系Serie Inferiere 段储层平面非均质性研究[J]. 岩性油气藏, 2009, 21(2): 24 -28 .

陇ICP备17006252号
版权所有© 2018 中国石油集团西北地质研究所有限公司《岩性油气藏》编辑部

地址：甘肃省兰州市城关区雁儿湾路535号(陇ICP备17006252号)    电话：0931-8686158;8686058;8686288    邮箱：yxyqc@petrochina.com.cn

甘公网安备 62010202002827号

本系统由北京玛格泰克科技发展有限公司设计开发