渤海湾盆地车西洼陷陡坡带古近系沙河街组沙三下段“源-汇”系统

doi:10.7605/gdlxb.2016.01.005

摘要
图/表
参考文献 (0)
相关文章 (15)
点击分布统计
下载分布统计

全文: PDF (22010 KB) RICH HTML
输出: BibTeX | EndNote (RIS) 背景资料

摘要

依据渤海湾盆地车镇凹陷车西洼陷陡坡带古近系沙河街组沙三下段岩心、测井以及三维地震资料,对研究区的“源-汇”系统进行了研究。结果表明:(1)车西洼陷沙三下段为一个三级层序,并可进一步划分为低位、湖侵与高位3个体系域,其陡坡带沙三下段发育杂基支撑中砾岩、碎屑支撑中砾岩、杂基支撑细砾岩、碎屑支撑细砾岩、砂质砾岩、含砾砂岩、粗砂岩、中砂岩、细砂岩、递变层理砂岩、滑塌岩等11种重力流成因岩石类型及深湖泥岩,表现为典型的近岸水下扇沉积;不同体系域时期扇体规模整体呈“由大变小,再变大”的演化趋势。(2)车西洼陷陡坡带自西向东识别出6套供源体系,可分为有沟道为主供源体系和滑塌为主供源体系,分别形成沟道供源为主近岸水下扇和滑塌供源为主近岸水下扇类型,其中滑塌供源为主近岸水下扇中的滑塌变形构造更发育、更普遍,但其扇体规模较沟道供源为主近岸水下扇小。(3)进一步的“溯源”分析结果表明,沙三下段沉积时期,研究区物源区母岩以碳酸盐岩为主,其在强烈的构造活动、湿热气候作用下,易于发育石漠化古地貌,剥蚀作用较为强烈,由此形成的频发的季节性重力流进入湖盆,形成该地区的近岸水下扇沉积;不同体系域时期扇体规模的差异主要受物源区气候和植被覆盖的控制。

	服务

	把本文推荐给朋友
	加入我的书架
	加入引用管理器
	E-mail Alert
	RSS
	作者相关文章
	王星星
	朱筱敏
	宋爽
	吴陈冰洁
	贺敬聪
	曹刚

关键词 ： &#x0201c, 源-汇&#x0201d, 系统, 沙三下段, 陡坡带, 车西洼陷, 车镇凹陷, 渤海湾盆地

Abstract：

Based on core observation, well logs and 3-D seismic data, the research in the “source-to-sink” system of the Lower Member 3 of Paleogene Shahejie Formation in the steep slope zone of Western Chezhen sub-sag of Chezhen sag, Bohai Bay Basin, is conducted. The results show that:(1)The Lower Member 3 of Shahejie Formation is a third-order sequence which can be divided into three system tracts, including the lowstand system tract, transgressive system tract and highstand system tract, and in the steep slope zone, 11 gravity flow rock types and deep-lacustrine mudstone can be identified,and the gravity flow rock types include matrix-supported medium-grained conglomerates,clast-supported medium-grained conglomerates,matrix-supported fine-grained conglomerates,clast-supported fine-grained conglomerates,sandy conglomerate,conglomeratic sandstones,coarse sandstones,medium sandstones,fine sandstones,graded bedding sandstones and slumps,they are all the typical characteristics of the near-shore subaqueous fan. The evolution tendency of fan scales is from increasing to decreasing,and then increasing again as a whole. (2)Six provenance supplying systems can be identified in the steep slope zone of Western Chezhen sub-sag,and they can be divided into two types,namely,gully-dominated provenance supplying systems and slump-dominated provenance supplying system. The slump structure are much more widely developed in the fans associated with the slump-dominated provenance supplying systems than the fans associated with the gully-dominated provenance supplying systems,in addition,the scale of slump near-shore subaqueous fans is smaller than the fans associated with gully. (3)The further study on the “source”area’s characteristics shows that,the parent rock developed in the depositional period of the Lower Member 3 of Shahejie Formation of the source area was mainly the carbonate rocks; under the action of strong tectonic activities and warm-wet climate,the source area may developed stony desertification palaeogeomorphology and strong erosion,which would cause frequent seasonal gravity to be transported into the lacustrine and form the near-shore subaqueous fans; the scale difference of the fans developed in different system tracts were mainly controlled by the climatic variation and vegetation cover of the source area.

Key words： &#x0201c source-to-sink&#x0201d system Lower Member 3 of Shahejie Formation steep slope zone Western Chezhen sub-sag Chezhen sag Bohai Bay Basin

收稿日期: 2015-04-10 出版日期: 2016-02-01

ZTFLH:

P531

基金资助:

国家油气重大专项子课题(编号：2011ZX05009-002,2012ZX05001-002)、国家自然科学基金项目(编号:41272133)、国家自然科学基金青年科学基金项目(编号:41202107)联合资助

作者简介: 王星星,男,1991年生,浙江大学博士研究生,专业为层序地层学与沉积学。E-mail: 312347272@163.com。通讯作者简介: 朱筱敏,男,1960年生,中国石油大学(北京)教授,博士生导师,研究方向为层序地层学、沉积学、储集层地质学和地震沉积学。E-mail: xmzhu@cup.edu.cn。

引用本文:

王星星,朱筱敏,宋爽等. 渤海湾盆地车西洼陷陡坡带古近系沙河街组沙三下段“源-汇”系统[J]. 古地理学报, 2016, 18(1): 65-79.

Wang Xingxing,Zhu Xiaomin,Song Shuang et al. “Source-to-sink” system of the Lower Member 3 of Paleogene Shahejie Formation in steep slope zone of Western Chezhen sub-sag, Bohai Bay Basin[J]. JOPC, 2016, 18(1): 65-79.

链接本文:

http://journal09.magtechjournal.com/gdlxb/CN/10.7605/gdlxb.2016.01.005 或 http://journal09.magtechjournal.com/gdlxb/CN/Y2016/V18/I1/65

[1] 冯友良,周海民,任建业,郑和荣,苗顺德. 2010. 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:地球科学,40(10):1356-1376. [Feng Y L,Zhou H M,Ren J Y,Zheng H R,Miao S D. 2010. Response to tectonic activity to paleogene sequence stratigraphy in east of Bohai Bay Basin. Scientia Sinica Terrae,40(10):1356-1376]
[2] 加东辉,徐长贵,杨波,杨香华,吴小红,周心怀,滕玉波,赖维成. 2007. 辽东湾辽东带中南部古近纪古地貌恢复和演化及其对沉积体系的控制. 古地理学报,9(2):155-166. [Jia D H,Xu C G,Yang B,Yang X H,Wu X H,Zhou X H,Teng Y B,Lai W C. 2007. Paleogene palaeogeomorphology reconstruction and evolution and its control on sedimentary systems in central southern Liaodong zone,Liaodongwan Bay. Journal of Palaeogeography(Chinese Edition),9(2):155-166]
[3] 康志成,李焯芬,马蔼乃,罗锦添. 2004. 中国泥石流研究. 北京: 科学出版社. [Kang Z C,Li Z F,Ma A N,Luo J T. 2004. Research on Debris Flow in China. Beijing:Science Press]
[4] 李存磊,任伟伟,唐明明. 2012. 流体性质转换机制在重力流沉积体系分析中应用初探. 地质论评,58(2):285-296. [Li C L,Ren W W,Tang M M. 2012. Preliminary study on gravity flow depositional system based on fluid properties conversion theory. Geological Review,58(2):285-296]
[5] 李守军,王明镇,郑德顺,赵秀丽. 2003. 山东济阳坳陷古近纪的气候恢复. 山东科技大学学报(自然科学版),22(3):6-9. [Li S J,Wang M Z,Zheng D S,Zhao X L. 2003. Recovery of climate of Palaeogene in Jiyang Depression of Shandong. Journal of Shandong University of Science and Technology(Natural Science),22(3):6-9]
[6] 李忠,徐建强,高剑. 2013. 盆山系统沉积学—兼论华北和塔里木地区研究实例. 沉积学报,31(5):757-772. [Li Z,Xu J Q,Gao J. 2013. Basin-range system sedimentology and case studies in North China and Tarim areas,China. Acta Sedimentologica Sinica,31(5):757-772]
[7] 梁官忠,谭建财,魏莉,王芳,姜燕,曹伟,吴旺林,郭晓光. 2013. 内蒙古二连盆地阿北凹陷下白垩统近岸水下扇沉积特征. 古地理学报,15(1):31-42. [Liang G Z,Tan J C,Wei L,Wang F,Jiang Y,Cao W,Wu W L,Guo X G. 2013. Sedimentary characteristics of nearshore subaqueous fans of the Lower Cretaceous in Abei Sag of Erlian Basin,inner Mongolia. Journal of Palaeogeography(Chinese Edition),15(1):31-42]
[8] 林畅松,夏庆龙,施和生,周心怀. 2015. 地貌演化、源-汇过程与盆地分析. 地学前缘,22(1):9-20. [Lin C S,Xia Q L,Shi H S,Zhou X H. 2015. Geomorphological evolution,source to sink system and basin analysis. Earth Science Frontiers,22(1):9-20]
[9] 苗长盛,刘招君,方石,张革,张君龙,胡菲,孙晓娟. 2011. 塔南凹陷南屯组近岸水下扇沉积特征及有利含油相带分析. 中国石油大学学报(自然科学版),35(1):34-39. [Miao C S,Liu Z J,Fang S,Zhang G,Zhang J L,Hu F,Sun X J. 2011. Sedimentary characteristics and favorable oil-bearing facies belts analysis of near-shore subaqueous fan of Nantun formation in Tanan Depression. Journal of China University of Petroleum(Edition of Natural Science),35(1):34-39]
[10] 邱楠生,苏向光,李兆影,柳忠泉,李政. 2006. 济阳坳陷新生代构造—热演化历史研究. 地球物理学报,49(4):1127-1135. [Qiu N S,Su X G,Li Z Y, Liu Z Q,Li Z. 2006. The Cenozoic tectono-thermal evolution of Jiyang Depression,Bohai Bay Basin,East China. Chinese Journal of Geophysics,49(4):1127-1135]
[11] 王冠名,林国松. 2012. 济阳坳陷古近纪的古气候区分析. 矿物岩石地球化学通报,31(5):505-509. [Wang G M,Lin G S. 2012. Eogene paleoclimate zone study in the Jiyang Depression. Bulletin of Mineralogy,Petrology and Geochemistry,31(5):505-509]
[12] 王世杰,李阳兵. 2007. 喀斯特石漠化研究存在的问题和发展趋势. 地球科学进展,22(6):573-582. [Wang S J,Li Y B. 2007. Problems and development trends about researches on karst rocky desertification. Advances in Earth Science,22(6):573-582]
[13] 鲜本忠,万锦峰,董艳蕾,马乾,张建国. 2013. 湖相深水块状砂岩特征、成因及发育模式: 以南堡凹陷东营组为例. 岩石学报,29(9):3287-3299. [Xian B Z,Wan J F,Dong Y L,Ma Q,Zhang J G. 2013. Sedimentary characteristics,origin and model of lacustrine deepwater massive sandstone:An example from Dongying Formation in Nanpu Depression. Acta Petrologica Sinica,29(9):3287-3299]
[14] 鲜本忠,王永诗,周廷全,孙立东. 2007. 断陷湖盆陡坡带砂砾岩体分布规律及控制因素: 以渤海湾盆地济阳坳陷车镇凹陷为例. 石油勘探与开发,34(4):429-436. [Xian B Z,Wang Y S,Zhou T Q,Sun L D. 2007. Distribution and controlling factors of glutinite bodies in the actic region of a rift basin:An example from Chezhen Sag,Bohai Bay Basin. Petroleum Exploration and Development,34(4):429-436]
[15] 谢习农,任建业,雷超. 2012. 盆地动力学研究综述及展望. 地质科技情报,31(5):76-84. [Xie X N,Ren J Y,Lei C. 2012. Reviews and prospects of depositional basin dynamics. Geological Science and Technology Information,31(5):76-84]
[16] 袁道先,章程. 2008. 岩溶动力学的理论探索与实践. 地球学报,29(3):355-365. [Yuan D X,Zhang C. 2008. Karst dynamics theory in China and its practice. Acta Geoscientica Sinica,29(3):355-365]
[17] 袁淑琴,刘子藏,李勇,肖敦清,蒲秀刚. 2010. 黄骅坳陷缓坡带沙河街组物源体系分析. 成都理工大学学报(自然科学版),37(1):36-43. [Yuan S Q,Liu Z C,Li Y,Xiao D Q,Pu X G. 2010. Provenance system of paleogene Shahejie Formation in the gentle slope(ramp)of the Huanghua Depression in Bohai Gulf,China. Journal of Chengdu University of Technology(Science & Technology Edition),37(1):36-43]
[18] 张本琪. 2005. 车镇凹陷层序地层与石油地质研究. 广东广州: 中国科学院广州地球化学研究所. [Zhang B Q. 2005. Research on sequence stratigraphy and oil geology. Guangzhou of Guangdong: Guangzhou Institute of Geochemistry,Chinese Academy of Sciences]
[19] 张世奇,纪友亮. 1997. 东营凹陷早第三纪古气候变化对层序发育的控制. 石油大学学报(自然科学版),22(6):29-33. [Zhang S Q,Ji Y L. 1997. Early Tertiary paleoclimate change control sequence development. Journal of China University of Petroleum(Edition of Natural Sciences),22(6):29-33]
[20] 郑四兵,鲜本忠. 2008. 车镇凹陷古近系层序地层格架及发育模式. 沉积与特提斯地质,28(1):48-54. [Zheng S B,Xian B Z. 2008. Sequence stratigraphic framework and model for the Palaeogene strata in the Chezhen depression. Sedimentary Geology and Tethyan Geology,28(1):48-54]
[21] 郑永春,王世杰. 2002. 贵州山区石灰土侵蚀及石漠化的地质原因分析. 长江流域资源与环境,11(5):461-465. [Zheng Y C,Wang S J. 2002. Geological cause of Calcareous soil erosion and land rocky desertification in karst area,Guizhou Province. Resources and Environment in the Yangtze Basin,11(5):461-465]
[22] 周路,韦红,唐勇,孔玉华,任本兵,吴勇,关旭. 2013. 准噶尔盆地车排子地区侏罗系八道湾组沉积古地貌及岩性分布. 古地理学报,15(3):383-400. [Zhou L,Wei H,Tang Y,Kong Y H,Ren B B,Wu Y,Guan X. 2013. Sedimentary palaeogeomorphology and lithology distribution of the Jurassic Badaowan formation in Chepaizi area of Jungar Basin. Jounal of Palaeogeography(Chinese Edition),15(3):383-400]
[23] 朱筱敏,赵东娜,姜淑贤,葛家旺,张守鹏,韩雪芳,刘新. 2014. 渤海湾盆地车镇凹陷陡坡带沙河街组近岸水下扇低孔低渗储集层成岩序列. 地球科学与环境学报,36(2):1-9. [Zhu X M,Zhao D N,Jiang S X,Ge J W,Zhang S P,Han X F,Liu X. 2014. Diagenetic sequence of Low porosity and permeability reservoirs from nearshore subaqeous fan of Shahejie Formation in the steep slope zone of Chezhen Depression,Bohai Bay Basin. Journal of Earth Sciences and Environment,36(2):1-9]
[24] 朱筱敏,查明,张卫海. 1995. 陆西凹陷上侏罗统近岸水下扇沉积特征. 石油大学学报(自然科学版),19(1):1-6. [Zhu X M,Zha M,Zhang W H. 1995. Sedimentary features of Upper Jurassic nearshore subaqueous fan in Luxi Depression. Journal of the University of Petroleum,China,19(1):1-6]
[25] 朱学稳. 2010. 峰林和峰丛喀斯特丛论. 见:朱学稳. 喀斯特与洞穴研究:朱学稳论文选集.北京:地质出版社,241-274. [Zhu X W. 2010. The Review of Peak Forest and Peak Clusters Karst. In:Zhu X W (ed). The Research of Karst and Caves:The Papers Collection of Zhu Xuewen. Beijing:Geological Publishing House,241-274]
[26] Cloetingh S A P L,Ziegler P A,Bogaard P J F,Andriessen P A M,Artemiieva I M,Bada G,van Balen R T, Beekman F, Ben-Avraham Z,Brum J P, Bunge H P,Burov E B,Carbonell R, Facenana C, Friedrich A, Gallart J,Green A G, Heidbach O,Jones A G, Matenco L, Mosar J,Oncken O, Pascal C,Peters G, Sliaupa S, Soesoo A, Spakman W, Stephenson R A,Thybo H, Torsvik T, de Vicente G, Wenzel F,Wortel M J R, TOPO-EUROPE Working Group. 2007. TOPO-EUROPE:The geoscience of coupled deep Earth-surface processes. Global and Planetary Change,58:1-118.
[27] Felix M,Peakall J. 2006. Transformation of debris flows into turbidity currents:Mechanisms inferred from laboratory experiments. Sedimentology,53(1):107-123.
[28] Liviu M,Paul A,SourceSink Network. 2013. Quantifying the mass transfer from mountain ranges to deposition in sedimentary basins:Source to sink studies in the Danube Basin-Black Sea system. Global and Planetary Change,103:1-18.
[29] Marr J G , Swenson J B, Paola C, Voller V R. 2010. A two-diffusion model of fluvial stratigraphy in closed depositional basins. Basin Research,12:381-398.
[30] Michael R L. 2011. Tectonic sedimentology:Sediment systems deciphering global to local tectonics. Sedimentology, 58:2-56.
[31] Philip A A. 2008a. From landscape into geological history. Nature,451:274-276.
[32] Philip A A. 2008b. Time scales of tectonic landscapes and their sediment routing systems. In: Gallacher K,Jones S J,Wainwright J(eds). Landscape evolution:Denudation,climate and tectonics over different time and space scales. London:Special Publications,296,7-28.
[33] Philip A A,John R A. 2013. Basin Analysis-Principles and Application to Petroleum Play Assessment(3 rd Edition). West Sussex:Wiley & Sons,Ltd,225-283.
[34] Posamentier H W,Kolla V. 2003. Seismic geomorphology and stratigraphy of depositional elements in deep-water settings. Journal of Sediment Research,73(3):367-388.
[35] Richard J H. 2011. Fundamentals of Geomorphology(3 rd Edition). Taylor & Francis e-library,389-432.
[36] Shanmugam G. 2012. New Perspectives on Deep-water Sandstones:Origin,Recognition,Initiation and Reservoir Quality. Oxford:Elsevier Science Press.
[37] Tor O S,Christopher A-L J. 2013. Source-to-sink analysis of ancient sedimentary systems using a subsurface case study from the More-Trondelag area of southern Norway:Part2-depositional setting and fan evolution. Basin Research,25:512-531.
[38] Tor O S,Christopher A-L J,MonicaV. 2013. Source-to-sink analysis of ancient sedimentary systems using a subsurface case study from the More-Trondelag area of southern Norway: Part1-depositional setting and fan evolution. Basin Research,25:489-511.
[39] Tor O S,David J W P,Mark E D, William H H. 2011. Linking onshore-offshore sediment dispersal in the Golo source-to-sink system(Corsica,France)during the Late Quaternary. Journal of Sediment Research,81:118-137.