下刚果盆地Madingo组海相烃源岩岩相特征和沉积模式

doi:10.7623/syxb201710007

石油学报 ›› 2017, Vol. 38 ›› Issue (10): 1168-1182.DOI: 10.7623/syxb201710007

下刚果盆地Madingo组海相烃源岩岩相特征和沉积模式

黄兴^1,2, 杨香华^1,2, 朱红涛^1,2, 康洪全³, 贾建忠³, 王波^1,2, 季少聪^1,2

1. 中国地质大学构造与油气资源教育部重点实验室湖北武汉 430074;
2. 中国地质大学资源学院湖北武汉 430074;
3. 中海油研究总院北京 100028

收稿日期:2017-03-11 修回日期:2017-08-05 出版日期:2017-10-25 发布日期:2017-11-02
通讯作者: 杨香华,男,1964年12月生,1987年获武汉地质学院石油系学士学位,2001年获中国地质大学(武汉)资源学院博士学位,现为中国地质大学(武汉)资源学院教授,主要从事沉积学、层序地层学及储层预测方向的教学与科研工作.Email:xhyang111@vip.sina.com
作者简介:黄兴,男,1989年3月生,2012年获长江大学勘查技术与工程专业学士学位,现为中国地质大学(武汉)矿产普查与勘探专业硕士研究生,主要从事盆地沉积学、层序地层学及储层预测方向的研究工作.Email:huangxing0315@yeah.net
基金资助:
国家重大科技专项（2016ZX05032-001）资助。

Lithofacies characteristics and sedimentary pattern of Madingo Formation marine hydrocarbon source rocks in Lower Congo Basin

Huang Xing^1,2, Yang Xianghua^1,2, Zhu Hongtao^1,2, Kang Hongquan³, Jia Jianzhong³, Wang Bo^1,2, Ji Shaocong^1,2

1. Key Laboratory of Tectonics and Petroleum Resources of the Ministry of Education, China University of Geosciences, Hubei Wuhan 430074, China;
2. Faculty of Earth Resources, China University of Geosciences, Hubei Wuhan 430074, China;
3. CNOOC Research Institute, Beijing 100028, China

Received:2017-03-11 Revised:2017-08-05 Online:2017-10-25 Published:2017-11-02

摘要/Abstract

摘要：

通过薄片镜下观察、扫描电镜、X射线衍射和常微量元素测量等分析结果，根据细粒沉积物矿物组成、岩石组构、微古生物与典型矿物特征，在下刚果盆地Madingo组海相烃源岩中识别出了6种烃源岩岩相：粉砂质细粒岩相、富放射虫细粒岩相、磷质细粒岩相、富有孔虫细粒岩相、灰质细粒岩相（灰泥）和黏土质细粒岩相。细粒沉积物岩相、微古生物化石、微常量元素和地震资料综合分析表明Madingo组海相烃源岩中发育含生物硅的生物沉积、含磷酸岩质的上升流沉积、富含硅质碎屑颗粒的悬浮沉积和粒序层理的底流沉积。下刚果盆地Madingo组海相烃源岩的沉积背景总体上属于裂后期陆架内部低能水介质条件下的还原环境，其沉积早期在大陆架内部发育半封闭—封闭的局限海环境，堆积了富含放射虫的优质烃源岩；Campanian期以后，区域地质背景转变为开阔陆架，发育与陆架上升流相关的富含磷酸盐与有孔虫的优质烃源岩。

关键词: 下刚果盆地, Madingo组, 岩相特征, 沉积作用, 沉积模式

Abstract:

Based on analyzing thin section by microscopic observation, scanning electron microscopy, X-ray diffraction as well as constant and trace element measurement, and considering the mineral composition of fine-grained sediment, lithologic fabric, micro-palaeontological characteristics and typical minerals, 6 types of hydrocarbon source rock lithofacies have been identified in marine source rocks of Madingo Formation:the silt fine-grained lithofacies, radiolarian enriched fine-grained lithofacies, phosphatic fine-grained lithofacies, foraminiferan enriched fine-grained lithofacies, cinereal fine-grained lithofacies (lime mud)and clayey fine-grained lithofacies. As demonstrated by the comprehensive analysis of fine-grained sediment lithofacies, micro-palaeontological fossils, constant and trace elements as well as seismic data, the biogenic deposit containing biosilicon, upwelling sediment containing phosphate rock, suspension sediment enriched with silicious clastic particles and bottom current sediment with graded bedding were developed in marine source rocks from Madingo Formation. As a whole, marine source rocks in Madingo Formation of the Lower Congo Basin were deposited under a reducing environment with low-energy water medium in post-rift continental shelf, and in the early deposition stage the semi-closed-closed restricted sea environment was developed in the continental shelf and the high-quality source rocks enriched with radiolarian were accumulated; and following the Campanian period, the regional geological background was converted to a wide continental shelf where high-quality source rocks enriched with phosphate and foraminiferan were developed due to upwelling on the continental shelf.

Key words: Lower Congo Basin, Madingo Formation, lithofacies characteristics, sedimentation, sedimentary pattern

中图分类号:

TE122.2

黄兴, 杨香华, 朱红涛, 康洪全, 贾建忠, 王波, 季少聪. 下刚果盆地Madingo组海相烃源岩岩相特征和沉积模式[J]. 石油学报, 2017, 38(10): 1168-1182.

Huang Xing, Yang Xianghua, Zhu Hongtao, Kang Hongquan, Jia Jianzhong, Wang Bo, Ji Shaocong. Lithofacies characteristics and sedimentary pattern of Madingo Formation marine hydrocarbon source rocks in Lower Congo Basin[J]. Acta Petrolei Sinica, 2017, 38(10): 1168-1182.

参考文献

[1] BROWNFIELD M E,CHARPENTIER R R.Geology and total petroleum systems of the West-Central Coastal Province (7203),West Africa[R].Reston,Va.:U.S .Geological Survey Bulletin,2006,2207 B:52.
[2] 龚承林,王英民,官宝聪,等.典型被动大陆边缘深水盆地构造演化与层序地层学分析[J].沉积学报,2010,28(3):419-425.
GONG Chenglin,WANG Yingmin,GUAN Baocong,et al.The tectonic evolution and sequence stratigraphy of passive continental margins deep-water basin[J].Acta Sedimentologica Sinica,2010,28(3):419-425.
[3] 张树林,邓运华. 下刚果盆地油气勘探策略[J].海洋地质动态,2009,25(9):24-29.
ZHANG Shulin,DENG Yunhua.Petroleum exploration strategy of lower Congo Basin[J].Marine Geology Letters,2009,25(9):24-29.
[4] 赵红岩,陶维祥,于水,等.下刚果盆地烃源岩对油气分布的控制作用分析[J].中国海上油气,2012,24(5):16-20.
ZHAO Hongyan,TAO Weixiang,YU Shui,et al.An analysis of the source rock control on hydrocarbon distribution in lower Congo Basin[J].China Offshore Oil and Gas,2012,24(5):16-20.
[5] 徐微,吕明.多级坡折地区的碳酸盐岩沉积储层预测:第十三届全国古地理学及沉积学学术会议论文摘要集,北京,2014-10[C].北京:中国矿物岩石地球化学学会岩相古地理专业委员会,2014.
XU Wei,LV Ming.Prediction of carbonate sedimentary reservoirs in multi grade slope fold area:The Thirteenth National Symposium on Palaeogeography and Sedimentology,Beijing,October,2014[C].Beijing:Chinese Society of Mineral Geochemistry Lithofacies Palaeogeography Specialized Committee,2014.
[6] 解吉高,刘春成,刘志斌,等.下刚果盆地北部中新统深水浊积岩储层及含油性地震预测[J].石油学报,2015,36(1):33-40.
XIE Jigao,LIU Chuncheng,LIU Zhibin,et al.Seismic prediction of the reservoir and oil-bearing property of Miocene deep-water turbidite in northern Lower Congo Basin[J].Acta Petrolei Sinica,2015,36(1):33-40.
[7] 张彪,于水,李红,等.下刚果盆地碳酸盐岩盐筏体沉积规律[J].石油学报,2016,37(3):360-370.
ZHANG Biao,YU Shui,LI Hong,et al.Sedimentary laws of carbonate salt raft in Lower Congo Basin[J].Acta Petrolei Sinica,2016,37(3):360-370.
[8] 曹军,钟宁宁,邓运华,等.下刚果盆地海相烃源岩地球化学特征、成因及其发育的控制因素[J].地球科学与环境学报,2014,36(4):87-98.
CAO Jun,ZHONG Ningning,DENG Yunhua,et al.Geochemical characteristics,origin and factors controlling formation of marine source rock in Lower Congo Basin[J].Journal of Earth Sciences and Environment,2014,36(4):87-98.
[9] ANKA Z,SÉRANNE M,DI PRIMIO R.Evidence of a large upper-Cretaceous depocentre across the Continent-Ocean boundary of the Congo-Angola Basin.Implications for palaeo-drainage and potential ultra-deep source rocks[J].Marine and Petroleum Geology,2010,27(3):601-611.
[10] BURWOOD R,CORNET P J,JACOBS L,et al.Organofacies variation control on hydrocarbon generation:a lower Congo coastal Basin (Angola)case history[J] .Organic Geochemistry,1990,16(1/3):325-338.
[11] BURWOOD R.Angola:source rock control for lower Congo coastal and Kwanza Basin petroleum systems[C]//The Oil and Gas Habitats of the South Atlantic.London:Geological Society Special Publications,1999:181-194.
[12] ANDERSON J E,CARTWRIGHT J,DRYSDALL S J,et al.Controls on turbidite sand deposition during gravity-driven extension of a passive margin:examples from Miocene sediments in Block 4,Angola[J].Marine and Petroleum Geology, 2000,17(10):1165-1203.
[13] COLE G A,REQUEJO A G,ORMEROD D,et al.Petroleum geochemical assessment of the Lower Congo Basin[C]//MELLO M R,KATZ B J.Petroleum Systems of South Atlantic Margins.Tulsa:American Association of Petroleum Geologist,2000.
[14] 赵红岩,陶维祥,于水,等.下刚果盆地深水区油气成藏要素特征及成藏模式研究[J].中国石油勘探,2013,18(1):75-79.
ZHAO Hongyan,TAO Weixiang,YU Shui,et al.Hydrocarbon accumulation characteristics and model of deepwater zone of lower Congo Basin[J].China Petroleum Exploration,2013,18(1):75-79.
[15] 于水,文华国,郝立华,等.下刚果盆地A区块下白垩统Albian阶沉积层序与古地理演化[J].成都理工大学学报:自然科学版,2012,39(4):353-361.
YU Shui,WEN Huaguo,HAO Lihua,et al.Sedimentary sequence and paleogeographic evolution of Albian Stage,Lower Cretaceous in Block A of Lower Congo Basin[J].Journal of Chengdu University of Technology:Science & Technology Edition,2012,39(4):353-361.
[16] 杨晓娟,李军,于炳松.下刚果盆地构造特征及油气勘探潜力[J].地球物理学进展,2012,27(6):2585-2593.
YANG Xiaojuan,LI Jun,YU Bingsong.Structural feature and exploratory potential of the Lower Congo Basin[J].Progress in Geophysics,2012,27(6):2585-2593.
[17] 张顺,陈世悦,谭明友,等.东营凹陷西部沙河街组三段下亚段泥页岩沉积微相[J].石油学报,2014,35(4):633-645.
ZHANG Shun,CHEN Shiyue,TAN Mingyou,et al.Characterization of sedimentary microfacies of shale in the lower third sub-member of Shahejie Formation,western Dongying sag[J].Acta Petrolei Sinica,2014,35(4):633-645.
[18] 刘传联.琼东南盆地渐新统烃源岩微观沉积特征与沉积环境[J].石油学报,2010,31(4):573-578.
LIU Chuanlian.Sedimentary environment and micro-sediment characteristics of Oligocene source rocks in Qiongdongnan Basin[J].Acta Petrolei Sinica,2010,31(4):573-578.
[19] 王志峰,张元福,梁雪莉,等.四川盆地五峰组-龙马溪组不同水动力成因页岩岩相特征[J].石油学报,2014,35(4):623-632.
WANG Zhifeng,ZHANG Yuanfu,LIANG Xueli,et al.Characteristics of shale lithofacies formed under different hydrodynamic conditions in the Wufeng-Longmaxi Formation,Sichuan Basin[J].Acta Petrolei Sinica,2014,35(4):623-632.
[20] 梁超,姜在兴,杨镱婷,等.四川盆地五峰组—龙马溪组页岩岩相及储集空间特征[J].石油勘探与开发,2012,39(6):691-698.
LIANG Chao,JIANG Zaixing,YANG Yiting,et al.Characteristics of shale lithofacies and reservoir space of the Wufeng-Longmaxi Formation,Sichuan Basin[J].Petroleum Exploration and Development,2012,39(6):691-698.
[21] 吴蓝宇,胡东风,陆永潮,等.四川盆地涪陵气田五峰组—龙马溪组页岩优势岩相[J].石油勘探与开发,2016,43(2):189-197.
WU Lanyu,HU Dongfeng,LU Yongchao,et al.Advantageous shale lithofacies of Wufeng Formation-Longmaxi Formation in Fuling gas field of Sichuan Basin,SW China[J].Petroleum Exploration and Development,2016,43(2):189-197.
[22] CALVERT S E.Oceanographic controls on the accumulation of organic matter in marine sediments[J].Geological Society,London,Special Publications,1987,26(1):137-151.
[23] 周洋,陈芳,孙桂华,等.台湾海峡西北部表层沉积物中有孔虫分布对沿岸上升流存在的响应[J].海洋地质与第四纪地质,2015,35(1):111-119.
ZHOU Yang,CHEN Fang,SUN Guihua,et al.Foraminiferal distribution in surface sediments of the northwestern Taiwan strait and its response to the coastal upwelling current[J].Marine Geology & Quaternary Geology,2015,35(1):111-119.
[24] 张水昌,张宝民,边立曾,等.中国海相烃源岩发育控制因素[J].地学前缘,2005,12(3):39-48.
ZHANG Shuichang,ZHANG Baomin,BIAN Lizeng,et al.Development constraints of marine source rocks in China[J].Earth Science Frontiers,2005,12(3):39-48.
[25] STOW D A V,HUC A Y,BERTRAND P.Depositional processes of black shales in deep water[J].Marine and Petroleum Geology,2001,18(4):491-498.
[26] APLIN A C,MACQUAKER J H S.Mudstone diversity:origin and implications for source,seal,and reservoir properties in petroleum systems[J].AAPG Bulletin,2011,95(12):2031-2059.
[27] HOWER J,ESLINGER E V,HOWER M E,et al.Mechanism of burial metamorphism of argillaceous sediment:1.Mineralogical and chemical evidence[J].Geological Society of America Bulletin,1976,87(5):725-737.
[28] PELTONEN C,MARCUSSEN Ø,BJØRLYKKE K,et al.Clay mineral diagenesis and quartz cementation in mudstones:the effects of smectite to illite reaction on rock properties[J].Marine and Petroleum Geology,2009,26(6):887-898.
[29] 姜在兴,梁超,吴靖,等.含油气细粒沉积岩研究的几个问题[J].石油学报,2013,34(6):1031-1039.
JIANG Zaixing,LIANG Chao,WU Jing,et al.Several issues in sedimentological studies on hydrocarbon-bearing fine-grained sedimentary rocks[J].Acta Petrolei Sinica,2013,34(6):1031-1039.
[30] SCHIEBER J,SOUTHARD J,THAISEN K.Accretion of mudstone beds from migrating floccule ripples[J].Science,2007,318(5857): 1760-1763.
[31] LOUCKS R G,RUPPEL C.Mississippian Barnett Shale:lithofacies and depositional setting of a deep-water shale-gas succession in the Fort Worth Basin,Texas[J].AAPG Bulletin,2007,91(4):579-601.
[32] 王玉满,董大忠,李建忠,等.川南下志留统龙马溪组页岩气储层特征[J].石油学报,2012,33(4):551-561.
WANG Yuman,DONG Dazhong,LI Jianzhong,et al.Reservoir characteristics of shale gas in Longmaxi Formation of the Lower Silurian,southern Sichuan[J].Acta Petrolei Sinica,2012,33(4):551-561.
[33] HOLDAWAY H K,CLAYTON C J.Preservation of shell microstructure in silicified brachiopods from the Upper Cretaceous Wilmington Sands of Devon[J].Geological Magazine,1982,119(4): 371-382.
[34] ROSS D J K,BUSTIN R M.Investigating the use of sedimentary geochemical proxies for paleoenvironment interpretation of thermally mature organic-rich strata:examples from the Devonian-Mississippian shales,Western Canadian SedimentaryBasin[J].Chemical Geology,2009,260(1/2):1-19.
[35] 黄金亮,邹才能,李建忠,等.川南志留系龙马溪组页岩气形成条件与有利区分析[J].煤炭学报,2012,37(5):782-787.
HUANG Jinliang,ZOU Caineng,LI Jianzhong,et al.Shale gas accumulation conditions and favorable zones of Silurian Longmaxi Formation in south Sichuan Basin,China[J].Journal of China Coal Society,2012,37(5):782-787.
[36] Harvey R.Young,Rongyu Li.Silicification in Mississippian Lodgepole Formation,northeastern flank of Williston Basin,Manitoba,Canada[J].Journal of Earth Science,2012,23(1):1-18.
[37] ROWE H D,LOUCKS R G,RUPPEL S C,et al.Mississippian Barnett formation,fort worth Basin,Texas:bulk geochemical inferences and Mo-TOC constraints on the severity of hydrographic restriction[J].Chemical Geology,2008,257(1/2):16-25.
[38] 韦刚健,刘颖,李献华,等.南海沉积物中过剩铝问题的探讨[J].矿物岩石地球化学通报,2003,22(1):23-25.
WEI Gangjian,LIU Ying,LI Xianhua,et al.Excess Al in the sediments from South China Sea[J].Bulletin of Mineralogy,Petrology and Geochemistry,2003,22(1):23-25.
[39] 李小洁,梁莲姬,吴枫,等.南海北部沉积物常量元素变化、碳酸盐旋回及其古环境意义[J].第四纪研究,2015,35(2):411-421.
LI Xiaojie,LIANG Lianji,WU Feng,et al.Variations of major elements and carbonate cycle of the northern South China Sea sediments and their paleoenvironmental significance[J].Quaternary Sciences,2015,35(2):411-421.
[40] 王淑芳,邹才能,董大忠,等.四川盆地富有机质页岩硅质生物成因及对页岩气开发的意义[J].北京大学学报:自然科学版,2014,50(3):476-486.
WANG Shufang,ZOU Caineng,DONG Dazhong,et al.Biogenic silica of organic-rich shale in Sichuan Basin and its significance for shale gas[J].Acta Scientiarum Naturalium Universitatis Pekinensis,2014,50(3):476-486.
[41] BOSTRÖM K,KRAEMER T,GARTNER S.Provenance and accumulation rates of opaline silica,Al,Ti,Fe,Mn,Cu,Ni and Co in Pacific pelagic sediments[J].Chemical Geology,1973,11(2):123-148.
[42] 张宝民,张水昌,边立曾,等.浅析中国新元古—下古生界海相烃源岩发育模式[J].科学通报,2007,52(S1):58-69.
ZHANG Baomin,ZHANG Shuichang,BIAN Lizeng,et al.Developmental modes of the Neoproterozoic-Lower Paleozoic marine hydrocarbon source rocks in China[J].Chinese Science Bulletin,2007,52(S1):77-91.
[43] 柴华,胡望水,唐友军,等.安徽宿松地区中二叠统栖霞组上升流相烃源岩地球化学特征[J].石油天然气学报,2012,34(3):1-6.
CHAI Hua,HU Wangshui,TANG Youjun,et al.Geochemistry features of up-current facies source rocks from Qixia Formation of middle Permian in the Susong area of Anhui province[J].Journal of Oil and Gas Technology,2012,34(3):1-6.
[44] 吕炳全,胡望水,王红罡,等.华北地块中—上元古界上升流沉积相及其与油气的关系[J].海洋地质与第四纪地质,2005,25(3):83-88.
LV Bingquan,HU Wangshui,WANG Honggang,et al.Neoproterozoic-mesoproterozoic upwelling facies and its relationship with hydrocarbon in North China[J].Marine Geology & Quaternary Geology,2005,25(3):83-88.
[45] 吴日升,李立.南海上升流研究概述[J].台湾海峡,2003,22(2):269-277.
WU Risheng,LI Li.Summarization of study on upwelling system in the South China Sea[J].Journal of Oceanography in Taiwan Strait,2003,22(2):269-277.
[46] 吕炳全,蔡进功,刘峰,等.栖霞组中台缘斜坡上升流沉积相及其与烃源岩的关系[J].海洋地质与第四纪地质, 2010,30(5):109-118.
LV Bingquan,CAI Jingong,LIU Feng,et al.Upwelling deposits at the marginal slope of a carbonate platform in Qixia stage and its relation with hydrocarbon source rocks[J].Marine Geology & Quaternary Geology,2010,30(5):109-118.
[47] 张尚锋,许光彩,朱锐,等.上升流沉积的研究现状和发展趋势[J].石油天然气学报,2012,34(1):7-11.
ZHANG Shangfeng,XU Guangcai,ZHU Rui,et al.Research status and development tendency of upwelling sediments[J].Journal of Oil and Gas Technology,2012,34(1):7-11.
[48] S HANMUGAM G.50 years of the turbidite paradigm (1950s-1990s):deep-water processes and facies models—a critical perspective[J].Marine and Petroleum Geology,2000,17(2):285-342.
[49] 李胜利,于兴河,谢玉洪,等.滨浅海泥流沟谷识别标志、类型及沉积模式—以莺歌海盆地东方1-1气田为例[J].沉积学报,2010,28(6):1076-1080.
LI Shengli,YU Xinghe,XIE Yuhong,et al.Mud flow gully identification mark,type and depositional model in the littoral and neritic marine:a case study of Dongfang1-1 gas field in Yinggehai Basin[J].Acta Sedimentologica Sinica,2010,28(6):1076-1080.
[50] 冯增昭,王英华,刘焕杰,等.中国沉积学[M].北京:石油工业出版社,1994.
FENG Zengzhao,WANG Yinghua,LIU Huanjie,et al.Sedimentology in China[M].Beijing:Petroleum Industry Press,1994.
[51] COTTER E,DRIESE S G.Incised-valley fills and other evidence of sea-level fluctuations affecting deposition of the Catskill Formation (Upper Devonian),Appalachian foreland Basin,Pennsylvania[J].Journal of Sedimentary Research,1998,68(2):347-361.
[52] 范洪耀,陶维祥,张金淼,等.下刚果—刚果扇盆地断裂特征及其对油气成藏的影响[J].海洋石油,2012,32(1):39-44.
FAN Hongyao,TAO Weixiang,ZHANG Jinmiao,et al.The fracture characteristics and its impacts on hydrocarbon accumulation in Lower Congo Basin and Congo Fan Basin[J].Offshore Oil,2012,32(1):39-44.
[53] 赵灿,郑荣才,于水,等.下刚果盆地A区块下白垩统阿尔布阶混积相研究[J].岩性油气藏,2011,23(3):84-90.
ZHAO Can,ZHENG Rongcai,YU Shui,et al.Study on mixed sedimentary facies of Lower Cretaceous Albian in block A of Lower Congo Basin[J].Lithologic Reservoirs,2011,23(3):84-90.
[54] CALVERT S E,PEDERSEN T F.Geochemistry of Recent oxic and anoxic marine sediments:implications for the geological record[J].Marine Geology,1993,113(1/2):67-88.
[55] ALGEO T J,MAYNARD J B.Trace-element behavior and redox facies in core shales of Upper Pennsylvanian Kansas-type cyclothems[J].Chemical Geology,2004,206(3/4):289-318.
[56] 李艳芳,邵德勇,吕海刚,等.四川盆地五峰组—龙马溪组海相页岩元素地球化学特征与有机质富集的关系[J].石油学报,2015,36(12):1470-1483.
LI Yanfang,SHAO Deyong,LV Haigang,et al.A relationship between elemental geochemical characteristics and organic matter enrichment in marine shale of Wufeng Formation—Longmaxi Formation,Sichuan Basin[J].Acta Petrolei Sinica, 2015,36(12):1470-1483.
[57] 赵建华,金之钧,金振奎,等.四川盆地五峰组—龙马溪组页岩岩相类型与沉积环境[J].石油学报,2016,37(5):572-586.
ZHAO Jianhua,JIN Zhijun,JIN Zhenkui,et al.Lithofacies types and sedimentary environment of shale in Wufeng-Longmaxi Formation,Sichuan Basin[J].Acta Petrolei Sinica,2016,37(5):572-586.
[58] JONES B,MANNING D A C.Comparison of geochemical indices used for the interpretation of palaeoredox conditions in ancient mudstones[J].Chemical Geology,1994,111(1/4):111-129.
[59] HAQ B U,HARDENBOL J,VAIL P R.Chronology of fluctuating sea levels since the Triassic[J].Science,1987,235(4793):1156-1167.
[60] SCHIEBER J,ZIMMERLE W.The history and promise of shale research[C]//SCHIEBER J,ZIMMERLE W,SETHI P.Shale and Mudstones (Vol.1):Basin Studies,Sedimentology and Paleontology.Stuttgart:Schweizerbart’sche Verlagsbuchhandlung,1998:1-10.
[61] BEGLINGER S E,DOUST H,CLOETINGH S.Relating petroleum system and play development to basin evolution:west African South Atlantic Basins[J].Marine and Petroleum Geology,2012,30(1):1-25.
[62] HUC A Y.Petroleum in the South Atlantic[J].Oil & Gas Science and Technology-Rev.IFP,2004,59(3):243-253.

下刚果盆地Madingo组海相烃源岩岩相特征和沉积模式

Lithofacies characteristics and sedimentary pattern of Madingo Formation marine hydrocarbon source rocks in Lower Congo Basin

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