珠江口盆地早中新世碳酸盐岩生长发育、消亡的历程与受控因素
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摘要
碳酸盐岩(台地)的消亡是沉积学研究的前沿和热点科学问题。南海东北部珠江口盆地东沙隆起所发育的下中新统珠江组碳酸盐岩是我国海相碳酸盐岩的最高层位,东沙台地珠江组碳酸盐岩的生长、繁盛和消亡过程提供了中国南海乃至世界范围内一个典型的受构造、海平面变化和物源共同控制的研究实例。依据采自钻井岩心钙质超微化石和浮游有孔虫化石带将珠江组的上界置于钙质超微化石带NN4与NN5的界线,即中、下中新统界线,下界置于浮游有孔虫N4的底部附近,即位于中新统与渐新统界线。有孔虫属为N4-N8带,钙质超微化石为NN2-NN4带,底界年龄为23.03Ma,顶界年龄为15.97Ma,地震反射上位于T40-T60之间。而其中碳酸盐岩地层最早于21Ma左右开始生长,最晚于16.5Ma被泥岩淹没。早期的东沙隆起北低南高,21Ma以后,东沙隆起沉降而丧失了向珠一凹陷提供物源的功能,沉降较快的东沙隆起北北部地区发育碳酸盐岩;初期为一套碳酸岩缓坡沉积,20Ma以后隆起整体被淹没,开始了大规模的碳酸盐岩建造,实现了由碳酸盐岩缓坡向台地的转变,随沉降向南推移,隆起逐渐转变为北高南低,整个碳酸盐岩台地持续向东南方向退缩,台地沉积逐渐萎缩为局部礁滩复合体,北部古地貌的高部位残存零星点礁;16.5Ma以后,沉降中心向珠二凹陷迁移,北部、北西部碎屑物质持续向东沙隆起前积导致台地消亡。结合珠江组沉积时期的地质事件的分析,本文认为早期碳酸盐岩的消亡是由于这一时期的全球海平面下降到最低位,引起区域上的物源供给加快,灰岩直接被北部沉积物退覆淹没所致;20±0.5Ma~18.3±0.5Ma的碳酸盐岩的消亡时间受制于沉降造成的相对海平面的变化,基底的火山作用及沉降中心的迁移等事件,最晚一期碳酸盐岩(流花地区碳酸盐岩)的消亡应该是构造反转后,北部物源对凹陷的持续填平补齐作用引起碳酸盐岩的生长环境变化所致。由此看,陆源碎屑的注入、沉降中心的迁移、相对海平面的升降及原始古地貌形态是碳酸盐岩生长发育及消亡的主要控制因素。
The disappearance of the carbonate platform is the frontier and hot field of sedimentary research.The Lower Miocene Zhujiang Formation carbonate deposited in the Dongsha uplift of Pearl River Mouth Basin is the latest marine carbonate in China.The process of origin,development and perished of the Zhujiang Formation carbonate is controlled by the tectonic movement,sea-level change and provenance,the research of this pattern can be served as a classical case study in the South China Sea and even in the world.According to the calcareous nannofossils and planktonic foraminifer zones collected from the drilling core,the upper bond of the Zhujiang Formation and the Middle-Lower Miocene boundary are classified in the boundary between calcareous nannofossil NN4 zone and NN5 zone,the lower bond of the Zhujiang Formation and the Miocene-Neocene boundary are divided in the bottom of foraminifer N4 zone.The ages of the foraminiferal N4-N8 zones and the calcareous nannofossils NN2-NN4 zones are determined,the lowest and the topmost boundary are 23.03Ma and 15.97Ma respectively,and the seismic reflection is located between T40 and T60.The carbonate platform firstly formed in 21Ma,and then was submerged by mudstone in 16.5Ma.Earlier Dongsha uplift was higher in the south and lower in the north.After 21Ma,because of subsidence of the Dongsha uplift,the function of the provenance to Zhu 1 depression was lost.Carbonate platform was developed in the north of Dongsha uplift which subsided quickly.At the early stage,there was a carbonate ramp.After 20Ma,the whole Dongsha uplift was submerged,and then extensive development of carbonate formations was start,including the transition from carbonate ramp to platform.As the settle expanded to the southern,the Dongsha uplift gradually changed to higher in the north,the whole platform expanded continuously to the southeast,the platform sedimentary is gradually shrinking to local reel flat complexes,the top of northern paleogeomorphic remanet fragmentary patch reefs.After 16.5Ma,the center of subsidence had been migrated to Zhu 2 sag,then the fragments from northern and northwest prograde continuously to Dongsha uplift,ultimately led to the termination of the platform.Combined with the analysis of geological events in the Zhujiang Formation period,this paper argues that the demise of early carbonate rocks is due to the global sea level down to the lowest at this time,which accelerate the supply of sediment in the region.The limestone is directly submerged by the sediment from the north.The disappearance time of carbonate rocks(formed from 20±0.5Ma to 18.3±0.5Ma)is controlled by the change of relative sea level,volcanic action of basement and the migration of subsidence center.The dead time of the late phase carbonate may be after the tectonic inversion and the growth environment of carbonate rocks has changed which are caused by clastic sediment from the north.Therefore,the terrigenous clastic injection,subsidence center migration,relative sea level changes and ancient landform control the growth and death of carbonate rocks.
The disappearance of the carbonate platform is the frontier and hot field of sedimentary research.The Lower Miocene Zhujiang Formation carbonate deposited in the Dongsha uplift of Pearl River Mouth Basin is the latest marine carbonate in China.The process of origin,development and perished of the Zhujiang Formation carbonate is controlled by the tectonic movement,sea-level change and provenance,the research of this pattern can be served as a classical case study in the South China Sea and even in the world.According to the calcareous nannofossils and planktonic foraminifer zones collected from the drilling core,the upper bond of the Zhujiang Formation and the Middle-Lower Miocene boundary are classified in the boundary between calcareous nannofossil NN4 zone and NN5 zone,the lower bond of the Zhujiang Formation and the Miocene-Neocene boundary are divided in the bottom of foraminifer N4 zone.The ages of the foraminiferal N4-N8 zones and the calcareous nannofossils NN2-NN4 zones are determined,the lowest and the topmost boundary are 23.03Ma and 15.97Ma respectively,and the seismic reflection is located between T40 and T60.The carbonate platform firstly formed in 21Ma,and then was submerged by mudstone in 16.5Ma.Earlier Dongsha uplift was higher in the south and lower in the north.After 21Ma,because of subsidence of the Dongsha uplift,the function of the provenance to Zhu 1 depression was lost.Carbonate platform was developed in the north of Dongsha uplift which subsided quickly.At the early stage,there was a carbonate ramp.After 20Ma,the whole Dongsha uplift was submerged,and then extensive development of carbonate formations was start,including the transition from carbonate ramp to platform.As the settle expanded to the southern,the Dongsha uplift gradually changed to higher in the north,the whole platform expanded continuously to the southeast,the platform sedimentary is gradually shrinking to local reel flat complexes,the top of northern paleogeomorphic remanet fragmentary patch reefs.After 16.5Ma,the center of subsidence had been migrated to Zhu 2 sag,then the fragments from northern and northwest prograde continuously to Dongsha uplift,ultimately led to the termination of the platform.Combined with the analysis of geological events in the Zhujiang Formation period,this paper argues that the demise of early carbonate rocks is due to the global sea level down to the lowest at this time,which accelerate the supply of sediment in the region.The limestone is directly submerged by the sediment from the north.The disappearance time of carbonate rocks(formed from 20±0.5Ma to 18.3±0.5Ma)is controlled by the change of relative sea level,volcanic action of basement and the migration of subsidence center.The dead time of the late phase carbonate may be after the tectonic inversion and the growth environment of carbonate rocks has changed which are caused by clastic sediment from the north.Therefore,the terrigenous clastic injection,subsidence center migration,relative sea level changes and ancient landform control the growth and death of carbonate rocks.
引文
An ZS,Zhang PZ,Wang EQ,Wang SM,Qiang XK,Li L,Song YG,Chang H,Liu XD,Zhou WJ,Liu WG,Cao JJ,Li XQ,Shen J,Liu Y and Ai L.2006.Changes of the monsoon-arid environment in China and growth of the Tibetan Plateau since the Miocene.Quaternary Science,26(5):678-693(in Chinese with English abstract)
Bachtel SL,Kissling RD,Martono D,Rahardjanto SP,Dunn PA and Mac Donald BA.2004.Seismic stratigraphic evolution of the Miocene-Pliocene segitiga platform,East Natuna Sea,Indonesia:The origin,growth,and demise of an isolated carbonate platform.In:Eberli GP,Massaferro JL and Sarg JFR.(eds.).Seismic Imaging of Carbonate Reservoirs and Systems.Tulsa:AAPG,81:309-328
Bassant P,Van BF,Strasser A and Lomando A.2004.A comparison of two Early Miocene carbonate margins:The Zhujiang carbonate platform(subsurface,South China Sea)and the Pirin?platform(outcrop,Southern Turkey).In:Grammer GM,Harris PMM and Eberli GP(eds.).Integration of Outcrop and Modern Analogs in Reservoir Modeling.Tulsa:AAPG,153-170
Chen CM.2000.Petroleum geology and conditions for hydrocarbon accumulation in the eastern Pearl River Mouth Basin.China Offshore Oil and Gas(Geology),14(2):73-83(in Chinese with English abstract)
Chen HZ,Wu XJ,Zhou D,Wang WY and Hao HJ.2005.MesoCenozoic faults in Zhujiang River Mouth Basin and their geodynamic background.Journal of Tropical Oceanography,24(2):52-61(in Chinese with English abstract)
Erlich RN,Barrett SF and Ju GB.1990.Seismic and geologic characteristics of drowning events on carbonate platforms.AAPGBulletin,74(10):1523-1537
Erlich RN,Longo AP Jr and Hyare S.1993.Response of carbonate platform margins to drowning:Evidence of environmental collapse.In:Loucks RG and Sarg JF.(eds.).Carbonate Sequence Stratigraphy:Recent Developments and Applications.Tulsa:AAPG,57:241-266
Fulthorpe CS and Schlanger SO.1989.Paleo-oceanographic and tectonic settings of Early Miocene reefs and associated carbonates of offshore Southeast Asia.AAPG Bulletin,73(6):729-756
Fyhn MBW,Boldreel LO,Nielsen LH,Giang TC,Nga LH,Hong NTM,Nguyen ND and Abatzis I.2013.Carbonate platform growth and demise offshore Central Vietnam:Effects of Early Miocene transgression and subsequent onshore uplift.Journal of Asian Earth Sciences,76:152-168
Guo ZT,Ruddiman WF,Hao QZ et al.2002.Onset of Asian desertification by 22Myr ago inferred from loess deposits in China.Nature,416(6877):159-163
Haq BU,Hardenbol J and Vail PR.1988.Mesozoic and Cenozoic chronostratigraphy and cycles of sea-level change.In:Wilgus CK,Hastings BS,Posamentier H et al(eds.).Sea-Level Change:An Integrated Approach.Society of Economic Paleontologists and Mineralogists,Special Publication,42:71-108
He Y and Hu PZ.1995.Early Miocene large foraminifera from biogenetic reef complexes of Dongsha massif,South China Sea.Acta Palaeontologica Sinica,34(1):18-39(in Chinese with English abstract)
Huang C,Fu H,Wang RL,Zhou XK and Tao BE.2010.Identification and division of Tertiary Zhujiang sequence boundaries in Dongsha uplift,Pearl River Mouth Basin.Marine Origin Petroleum Geology,15 (3):32-39(in Chinese with English abstract)
Karig DE.1971.Origin and development of marginal basins in the Western Pacific.Journal of Geophysical Research,76(11):2542-2561
Li AC,Huang J,Jiang HY and Wan SM.2011.Sedimentary evolution in the northern slope of South China Sea since Oligocene and its responses to tectonics.Chinese Journal of Geophysics,54(12):3233-3245(in Chinese with English abstract)
Li PL.1999.A proposal for the division of tectonic units in the northern basin of South China Sea.China Offshore Oil and Gas(Geology),13(6):460-462(in Chinese with English abstract)
Li QY,Lourens L and Wang PX.2007.New ages for Neogene marine biostratigraphic events.Journal of Stratigraphy,31(3):197-208(in Chinese with English abstract)
Li XH,Wei GJ,Shao L,Liu Y,Liang XR,Jian ZM,Sun M and Wang PX.2003.Geochemical and Nd isotopic variations in sediments of the South China Sea:A response to Cenozoic tectonism in SE Asia.Earth and Planetary Science Letters,211(3-4):207-220
Li Y,Zheng RC,Gao BY,Hu XQ and Dai CC.2011.Characteristics of the detrital response to Oligocene/Miocene geological events in Baiyun sag,Pearl River Mouth Basin.Geoscience,25(3):476-481(in Chinese with English abstract)
Liu A.2007.The tectonic evolution history of Dongsha rise in Pearl River Mouth Basin and its controls over hydrocarbon resources.Master Degree Thesis.Guangzhou:Sun Yat-Sen University,1-129(in Chinese with English summary)
Liu J,Shi HS,Du JY and Gao P.2007.Forming conditions and exploration direction of reef oil-gas pool in carbonate platform of Dongsha massif.Journal of Tropical Oceanography,26(1):22-27(in Chinese with English abstract)
Menier D,Pierson B,Chalabi A,Ting KK and Pubellier M.2014.Morphological indicators of structural control,relative sea-level fluctuations and platform drowning on present-day and Miocene carbonate platforms.Marine and Petroleum Geology,58:776-788
Moldovanyi EP,Wall FM and Yan ZJ.1995.Regional exposure events and platform evolution of Zhujiang Formation carbonates,Pearl River Mouth basin:Evidence From Primary and Diagenetic Seismic Facies.In:Budd DA,Saller H and Harris PM(eds.).M63:Unconformities and Porosity in Carbonate Strata.Tulsa:AAPG,63:125-140
Pang X,Chen CM,Shao L,Wang CS,Zhu M,He M,Shen J,Lian SYand Wu XJ.2007a.Baiyun movement,a great tectonic event on the Oligocene-Miocene boundary in the northern South China Sea and its implications.Geological Review,53(2):145-151(in Chinese with English abstract)
Pang X,Chen CM,Peng DJ,Zhu M and He M.2007b.Petroleum in Deep-Water Fan System of the Pearl River in the South China Sea.Beijing:Science Press(in Chinese)
Sattler U,Zampetti V,Schlager W and Immenhauser A.2004.Late leaching under deep burial conditions:A case study from the Miocene Zhujiang carbonate reservoir,South China Sea.Marine and Petroleum Geology,21(8):977-922
Sattler U,Immenhauser A,Schlager W and Zampetti V.2009.Drowning history of a Miocene carbonate platform(Zhujiang Formation,South China Sea).Sedimentary Geology,219(1-4):318-331
Schlager W.1998.Exposure,drowning and sequence boundaries on carbonate platforms.In:Camoin GF and Davies PJ(eds.).Reefs and Carbonate Platforms in the Pacific and Indian Oceans.International Association of Sedimentologists Special Publication,25:3-21
Shao L,Li XH,Wang PX,Jian ZM,Wei GJ,Pang X and Liu Y.2004.Sedimentary record of the tectonic evolution of the South China Sea since the Oligocene:Evidence from deep sea sediments of ODP Site1148.Advances in Earth Science,19(4):539-544(in Chinese with English abstract)
Shao L,Pang X,Qiao PJ,Chen CM,Li QY and Miao WL.2008.Sedimentary filling of the Pearl River Mouth Basin and its response to the evolution of the Pearl River.Acta Sedimentologica Sinica,26(2):179-185(in Chinese with English abstract)
Story C,Peng P,Heubeck C,Sullivan C and Lin JD.2000.Liuhua 11-1 Field,South China Sea:A shallow carbonate reservoir developed using ultrahigh-resolution 3-D seismic,inversion,and attribute-based reservoir modeling.The Leading Edge,19(8):834-844
Sun Z,Pang X,Zhong ZH,Zhou D,Chen CM,Hao HJ,He M,Huang CJ and Xu HH.2005.Dynamics of Tertiary tectonic evolution of the Baiyun sag in the Pearl River Mouth Basin.Earth Science Frontiers,12(4):489-498(in Chinese with English abstract)
Ting KK,Chung E and Al Jaadi O.2010.Evolution and controlling factors of Miocene carbonate build-up in Central Luconia,SE Asia:Insights from integration of geological and seismic characterization.Integrated Petroleum Engineering and Geosciences(ICIPEG),15-17
Ting KK,Pierson BJ,Al-Jaadi O and Hague PF.2011.Effects of syndepositional tectonics on platform geometry and reservoir characters in Miocene carbonate platforms of Central Luconia,Sarawak.Bangkok,Thailand:International Petroleum Technology Conference,15-17
Ting KK,Pierson BJ,Pubellier M,Menier D,Warrlich G and Fatiyah SN.2012.Dating the birth,growth and death of Miocene carbonate platforms in the South China Sea.Central Luconia Province,Sarawak:AGU,3-7
Wagner PD,Tasker DR and Wahlman GP.1995.Reservoir degradation and compartmentalization below subaerial unconformities:Limestone examples from West Texas,China,and Oman.In:Budd DA,Saller AH and Harris PM(eds.).M63:Unconformities and Porosity in Carbonate Strata.Tulsa:AAPG,63:177-196
Wang CX.1996.Sequence stratigraphic analysis of marine Miocene formations in the Pearl River Mouth Basin and its significance.China Offshore Oil and Gas(Geology),10(5):279-288(in Chinese with English abstract)
Wang PX,Zhao QH,Jian ZM,Cheng XR,Huang W,Tian J,Wang JL,Li QY,Li BH and Su X.2003.Thirty million year deep sea records in the South China Sea.Chinese Science Bulletin,48(23):2524-2535
Wilson MEJ and Evans MJ.2002.Sedimentology and diagenesis of Tertiary carbonates on the Mangkalihat Peninsula,Borneo:Implications for subsurface reservoir quality.Marine and Petroleum Geology,19(7):873-900
Wu JM.1994.Evaluation and models of Cenozoic sedimentation in the South China Sea.Tectonophysics,235(1-2):77-98
Xie JL,Yu HZ,Tang LM,Fu JJ and Wu JY.2010.The basement features and basin types of Cenozoic sediments in South China Sea.Marine Origin Petroleum Geology,15(4):35-47(in Chinese with English abstract)
Yao BC,Wan L and Liu ZH.2004.Tectonic dynamics of Cenozoic sedimentary basins and hydrocarbon resources in the South China Sea.Earth Science,29(5):543-549(in Chinese with English abstract)
Yu HB and Du JY.2011.Tide-influenced delta deposits of Wellblock Ain Lower Zhujiang Formation of Pearl River Mouth Basin.Journal of Yangtze University(Natural Science Edition),8(1):64-66(in Chinese with English abstract)
Yu HS.1990.The Pearl River Mouth Basin:A rift basin and its geodynamic relationship with the southeastern Eurasian margin.Tectonophysics,183(1-4):177-186
Zachos J,Pagani M,Sloan L,Thomas E and Billups K.2001.Trends,rhythms,and aberrations in global climate 65Ma to present.Science,292(5517):686-693
Zampetti V,Sattler U and Braaksma H.2005.Well log and seismic character of Liuhua 11-1 Field,South China Sea:Relationship between diagenesis and seismic reflections.Sedimentary Geology,175(1-4):217-236
Zhang XT,Chen L,She QH,Zhang SF,Qiao PJ and Shao L.2012.Provenance evolution of the Paleo-Hanjiang River in the North South China Sea.Marine Geology&Quaternary Geology,32(4):41-48(in Chinese with English abstract)
Zhao HT.2011.Sedimentary evolution and reservoir characteristics of reef carbonate in Dongsha massif of Pearl River Mouth Basin,South China Sea.Master Degree Thesis.Qingdao:Institute of Oceanology,Chinese Academy of Sciences,1-64(in Chinese)
安芷生,张培震,王二七,王苏民,强小科,李力,宋友桂,常宏,刘晓东,周卫健,刘卫国,曹军骥,李小强,沈吉,刘禹,艾莉.2006.中新世以来我国季风-干旱环境演化与青藏高原的生长.第四纪研究,26(5):678-693
陈长民.2000.珠江口盆地东部石油地质及油气藏形成条件初探.中国海上油气(地质),14(2):73-83
陈汉宗,吴湘杰,周蒂,王万银,郝沪军.2005.珠江口盆地中新生代主要断裂特征和动力背景分析.热带海洋学报,24(2):52-61
何炎,胡平忠.1995.南海东沙隆起早中新世生物礁中的大有孔虫.古生物学报,34(1):18-39
黄诚,傅恒,汪瑞良,周小康,陶碧娥.2010.珠江口盆地东沙隆起珠江组层序界面的识别及划分.海相油气地质,15(3):32-39
李安春,黄杰,蒋恒毅,万世明.2011.渐新世以来南海北部陆坡区沉积演化及其对构造的响应.地球物理学报,54(12):3233-3245
李平鲁.1999.南海北部陆缘盆地构造单元划分命名建议.中国海上油气(地质),13(6):460-462
李前裕,Lourens L,汪品先.2007.新近纪海相生物地层事件年龄新编.地层学杂志,31(3):197-208
李云,郑荣才,高博禹,胡晓庆,戴朝成.2011.珠江口盆地白云凹陷渐新世/中新世地质事件的碎屑组分响应.现代地质,25(3):476-481
刘安.2007.珠江口盆地东沙隆起的构造演化及其对油气的影响.硕士学位论文.广州:中山大学,1-129
刘军,施和生,杜家元,高鹏.2007.东沙隆起台地生物礁、滩油藏成藏条件及勘探思路探讨.热带海洋学报,26(1):22-27
庞雄,陈长民,邵磊,王成善,朱明,何敏,申俊,连世勇,吴湘杰.2007a.白云运动:南海北部渐新统-中新统重大地质事件及其意义.地质论评,53(2):145-151
庞雄,陈长民,彭大钧,朱明,何敏.2007b.南海珠江深水扇系统及油气.北京:科学出版社
邵磊,李献华,汪品先,翦知湣,韦刚健,庞雄,刘颖.2004.南海渐新世以来构造演化的沉积记录---ODP 1148站深海沉积物中的证据.地球科学进展,19(4):539-544
邵磊,庞雄,乔培军,陈长民,李前裕,苗卫良.2008.珠江口盆地的沉积充填与珠江的形成演变.沉积学报,26(2):179-185
孙珍,庞雄,钟志洪,周蒂,陈长民,郝沪军,何敏,黄春菊,许鹤华.2005.珠江口盆地白云凹陷新生代构造演化动力学.地学前缘,12(4):489-498
王春修.1996.珠江口盆地海相中新统层序地层分析及其意义.中国海上油气(地质),10(5):279-288
汪品先,赵泉鸿,翦知湣,成鑫荣,黄维,田军,王吉良,李前裕,李保华,苏新.2003.南海三千万年的深海记录.科学通报,48(21):2206-2215
谢锦龙,余和中,唐良民,傅瑾君,武金云.2010.南海新生代沉积基底性质和盆地类型.海相油气地质,15(4):35-47
姚伯初,万玲,刘振湖.2004.南海海域新生代沉积盆地构造演化的动力学特征及其油气资源.地球科学,29(5):543-549
余海波,杜家元.2011.珠江口盆地A井区珠江组下段潮汐作用对三角洲沉积影响的研究.长江大学学报(自然科学版),8(1):64-66
张向涛,陈亮,佘清华,张素芳,乔培军,邵磊.2012.南海北部古韩江物源的演化特征.海洋地质与第四纪地质,32(4):41-48
赵撼霆.2011.珠江口盆地东沙隆起生物礁碳酸盐岩沉积演化及储层特征.硕士学位论文.青岛:中国科学院海洋研究所,1-64
(1)胡平忠.1994.流花11-1礁(滩)型大油田地质规律与勘探经验.内部资料
Bachtel SL,Kissling RD,Martono D,Rahardjanto SP,Dunn PA and Mac Donald BA.2004.Seismic stratigraphic evolution of the Miocene-Pliocene segitiga platform,East Natuna Sea,Indonesia:The origin,growth,and demise of an isolated carbonate platform.In:Eberli GP,Massaferro JL and Sarg JFR.(eds.).Seismic Imaging of Carbonate Reservoirs and Systems.Tulsa:AAPG,81:309-328
Bassant P,Van BF,Strasser A and Lomando A.2004.A comparison of two Early Miocene carbonate margins:The Zhujiang carbonate platform(subsurface,South China Sea)and the Pirin?platform(outcrop,Southern Turkey).In:Grammer GM,Harris PMM and Eberli GP(eds.).Integration of Outcrop and Modern Analogs in Reservoir Modeling.Tulsa:AAPG,153-170
Chen CM.2000.Petroleum geology and conditions for hydrocarbon accumulation in the eastern Pearl River Mouth Basin.China Offshore Oil and Gas(Geology),14(2):73-83(in Chinese with English abstract)
Chen HZ,Wu XJ,Zhou D,Wang WY and Hao HJ.2005.MesoCenozoic faults in Zhujiang River Mouth Basin and their geodynamic background.Journal of Tropical Oceanography,24(2):52-61(in Chinese with English abstract)
Erlich RN,Barrett SF and Ju GB.1990.Seismic and geologic characteristics of drowning events on carbonate platforms.AAPGBulletin,74(10):1523-1537
Erlich RN,Longo AP Jr and Hyare S.1993.Response of carbonate platform margins to drowning:Evidence of environmental collapse.In:Loucks RG and Sarg JF.(eds.).Carbonate Sequence Stratigraphy:Recent Developments and Applications.Tulsa:AAPG,57:241-266
Fulthorpe CS and Schlanger SO.1989.Paleo-oceanographic and tectonic settings of Early Miocene reefs and associated carbonates of offshore Southeast Asia.AAPG Bulletin,73(6):729-756
Fyhn MBW,Boldreel LO,Nielsen LH,Giang TC,Nga LH,Hong NTM,Nguyen ND and Abatzis I.2013.Carbonate platform growth and demise offshore Central Vietnam:Effects of Early Miocene transgression and subsequent onshore uplift.Journal of Asian Earth Sciences,76:152-168
Guo ZT,Ruddiman WF,Hao QZ et al.2002.Onset of Asian desertification by 22Myr ago inferred from loess deposits in China.Nature,416(6877):159-163
Haq BU,Hardenbol J and Vail PR.1988.Mesozoic and Cenozoic chronostratigraphy and cycles of sea-level change.In:Wilgus CK,Hastings BS,Posamentier H et al(eds.).Sea-Level Change:An Integrated Approach.Society of Economic Paleontologists and Mineralogists,Special Publication,42:71-108
He Y and Hu PZ.1995.Early Miocene large foraminifera from biogenetic reef complexes of Dongsha massif,South China Sea.Acta Palaeontologica Sinica,34(1):18-39(in Chinese with English abstract)
Huang C,Fu H,Wang RL,Zhou XK and Tao BE.2010.Identification and division of Tertiary Zhujiang sequence boundaries in Dongsha uplift,Pearl River Mouth Basin.Marine Origin Petroleum Geology,15 (3):32-39(in Chinese with English abstract)
Karig DE.1971.Origin and development of marginal basins in the Western Pacific.Journal of Geophysical Research,76(11):2542-2561
Li AC,Huang J,Jiang HY and Wan SM.2011.Sedimentary evolution in the northern slope of South China Sea since Oligocene and its responses to tectonics.Chinese Journal of Geophysics,54(12):3233-3245(in Chinese with English abstract)
Li PL.1999.A proposal for the division of tectonic units in the northern basin of South China Sea.China Offshore Oil and Gas(Geology),13(6):460-462(in Chinese with English abstract)
Li QY,Lourens L and Wang PX.2007.New ages for Neogene marine biostratigraphic events.Journal of Stratigraphy,31(3):197-208(in Chinese with English abstract)
Li XH,Wei GJ,Shao L,Liu Y,Liang XR,Jian ZM,Sun M and Wang PX.2003.Geochemical and Nd isotopic variations in sediments of the South China Sea:A response to Cenozoic tectonism in SE Asia.Earth and Planetary Science Letters,211(3-4):207-220
Li Y,Zheng RC,Gao BY,Hu XQ and Dai CC.2011.Characteristics of the detrital response to Oligocene/Miocene geological events in Baiyun sag,Pearl River Mouth Basin.Geoscience,25(3):476-481(in Chinese with English abstract)
Liu A.2007.The tectonic evolution history of Dongsha rise in Pearl River Mouth Basin and its controls over hydrocarbon resources.Master Degree Thesis.Guangzhou:Sun Yat-Sen University,1-129(in Chinese with English summary)
Liu J,Shi HS,Du JY and Gao P.2007.Forming conditions and exploration direction of reef oil-gas pool in carbonate platform of Dongsha massif.Journal of Tropical Oceanography,26(1):22-27(in Chinese with English abstract)
Menier D,Pierson B,Chalabi A,Ting KK and Pubellier M.2014.Morphological indicators of structural control,relative sea-level fluctuations and platform drowning on present-day and Miocene carbonate platforms.Marine and Petroleum Geology,58:776-788
Moldovanyi EP,Wall FM and Yan ZJ.1995.Regional exposure events and platform evolution of Zhujiang Formation carbonates,Pearl River Mouth basin:Evidence From Primary and Diagenetic Seismic Facies.In:Budd DA,Saller H and Harris PM(eds.).M63:Unconformities and Porosity in Carbonate Strata.Tulsa:AAPG,63:125-140
Pang X,Chen CM,Shao L,Wang CS,Zhu M,He M,Shen J,Lian SYand Wu XJ.2007a.Baiyun movement,a great tectonic event on the Oligocene-Miocene boundary in the northern South China Sea and its implications.Geological Review,53(2):145-151(in Chinese with English abstract)
Pang X,Chen CM,Peng DJ,Zhu M and He M.2007b.Petroleum in Deep-Water Fan System of the Pearl River in the South China Sea.Beijing:Science Press(in Chinese)
Sattler U,Zampetti V,Schlager W and Immenhauser A.2004.Late leaching under deep burial conditions:A case study from the Miocene Zhujiang carbonate reservoir,South China Sea.Marine and Petroleum Geology,21(8):977-922
Sattler U,Immenhauser A,Schlager W and Zampetti V.2009.Drowning history of a Miocene carbonate platform(Zhujiang Formation,South China Sea).Sedimentary Geology,219(1-4):318-331
Schlager W.1998.Exposure,drowning and sequence boundaries on carbonate platforms.In:Camoin GF and Davies PJ(eds.).Reefs and Carbonate Platforms in the Pacific and Indian Oceans.International Association of Sedimentologists Special Publication,25:3-21
Shao L,Li XH,Wang PX,Jian ZM,Wei GJ,Pang X and Liu Y.2004.Sedimentary record of the tectonic evolution of the South China Sea since the Oligocene:Evidence from deep sea sediments of ODP Site1148.Advances in Earth Science,19(4):539-544(in Chinese with English abstract)
Shao L,Pang X,Qiao PJ,Chen CM,Li QY and Miao WL.2008.Sedimentary filling of the Pearl River Mouth Basin and its response to the evolution of the Pearl River.Acta Sedimentologica Sinica,26(2):179-185(in Chinese with English abstract)
Story C,Peng P,Heubeck C,Sullivan C and Lin JD.2000.Liuhua 11-1 Field,South China Sea:A shallow carbonate reservoir developed using ultrahigh-resolution 3-D seismic,inversion,and attribute-based reservoir modeling.The Leading Edge,19(8):834-844
Sun Z,Pang X,Zhong ZH,Zhou D,Chen CM,Hao HJ,He M,Huang CJ and Xu HH.2005.Dynamics of Tertiary tectonic evolution of the Baiyun sag in the Pearl River Mouth Basin.Earth Science Frontiers,12(4):489-498(in Chinese with English abstract)
Ting KK,Chung E and Al Jaadi O.2010.Evolution and controlling factors of Miocene carbonate build-up in Central Luconia,SE Asia:Insights from integration of geological and seismic characterization.Integrated Petroleum Engineering and Geosciences(ICIPEG),15-17
Ting KK,Pierson BJ,Al-Jaadi O and Hague PF.2011.Effects of syndepositional tectonics on platform geometry and reservoir characters in Miocene carbonate platforms of Central Luconia,Sarawak.Bangkok,Thailand:International Petroleum Technology Conference,15-17
Ting KK,Pierson BJ,Pubellier M,Menier D,Warrlich G and Fatiyah SN.2012.Dating the birth,growth and death of Miocene carbonate platforms in the South China Sea.Central Luconia Province,Sarawak:AGU,3-7
Wagner PD,Tasker DR and Wahlman GP.1995.Reservoir degradation and compartmentalization below subaerial unconformities:Limestone examples from West Texas,China,and Oman.In:Budd DA,Saller AH and Harris PM(eds.).M63:Unconformities and Porosity in Carbonate Strata.Tulsa:AAPG,63:177-196
Wang CX.1996.Sequence stratigraphic analysis of marine Miocene formations in the Pearl River Mouth Basin and its significance.China Offshore Oil and Gas(Geology),10(5):279-288(in Chinese with English abstract)
Wang PX,Zhao QH,Jian ZM,Cheng XR,Huang W,Tian J,Wang JL,Li QY,Li BH and Su X.2003.Thirty million year deep sea records in the South China Sea.Chinese Science Bulletin,48(23):2524-2535
Wilson MEJ and Evans MJ.2002.Sedimentology and diagenesis of Tertiary carbonates on the Mangkalihat Peninsula,Borneo:Implications for subsurface reservoir quality.Marine and Petroleum Geology,19(7):873-900
Wu JM.1994.Evaluation and models of Cenozoic sedimentation in the South China Sea.Tectonophysics,235(1-2):77-98
Xie JL,Yu HZ,Tang LM,Fu JJ and Wu JY.2010.The basement features and basin types of Cenozoic sediments in South China Sea.Marine Origin Petroleum Geology,15(4):35-47(in Chinese with English abstract)
Yao BC,Wan L and Liu ZH.2004.Tectonic dynamics of Cenozoic sedimentary basins and hydrocarbon resources in the South China Sea.Earth Science,29(5):543-549(in Chinese with English abstract)
Yu HB and Du JY.2011.Tide-influenced delta deposits of Wellblock Ain Lower Zhujiang Formation of Pearl River Mouth Basin.Journal of Yangtze University(Natural Science Edition),8(1):64-66(in Chinese with English abstract)
Yu HS.1990.The Pearl River Mouth Basin:A rift basin and its geodynamic relationship with the southeastern Eurasian margin.Tectonophysics,183(1-4):177-186
Zachos J,Pagani M,Sloan L,Thomas E and Billups K.2001.Trends,rhythms,and aberrations in global climate 65Ma to present.Science,292(5517):686-693
Zampetti V,Sattler U and Braaksma H.2005.Well log and seismic character of Liuhua 11-1 Field,South China Sea:Relationship between diagenesis and seismic reflections.Sedimentary Geology,175(1-4):217-236
Zhang XT,Chen L,She QH,Zhang SF,Qiao PJ and Shao L.2012.Provenance evolution of the Paleo-Hanjiang River in the North South China Sea.Marine Geology&Quaternary Geology,32(4):41-48(in Chinese with English abstract)
Zhao HT.2011.Sedimentary evolution and reservoir characteristics of reef carbonate in Dongsha massif of Pearl River Mouth Basin,South China Sea.Master Degree Thesis.Qingdao:Institute of Oceanology,Chinese Academy of Sciences,1-64(in Chinese)
安芷生,张培震,王二七,王苏民,强小科,李力,宋友桂,常宏,刘晓东,周卫健,刘卫国,曹军骥,李小强,沈吉,刘禹,艾莉.2006.中新世以来我国季风-干旱环境演化与青藏高原的生长.第四纪研究,26(5):678-693
陈长民.2000.珠江口盆地东部石油地质及油气藏形成条件初探.中国海上油气(地质),14(2):73-83
陈汉宗,吴湘杰,周蒂,王万银,郝沪军.2005.珠江口盆地中新生代主要断裂特征和动力背景分析.热带海洋学报,24(2):52-61
何炎,胡平忠.1995.南海东沙隆起早中新世生物礁中的大有孔虫.古生物学报,34(1):18-39
黄诚,傅恒,汪瑞良,周小康,陶碧娥.2010.珠江口盆地东沙隆起珠江组层序界面的识别及划分.海相油气地质,15(3):32-39
李安春,黄杰,蒋恒毅,万世明.2011.渐新世以来南海北部陆坡区沉积演化及其对构造的响应.地球物理学报,54(12):3233-3245
李平鲁.1999.南海北部陆缘盆地构造单元划分命名建议.中国海上油气(地质),13(6):460-462
李前裕,Lourens L,汪品先.2007.新近纪海相生物地层事件年龄新编.地层学杂志,31(3):197-208
李云,郑荣才,高博禹,胡晓庆,戴朝成.2011.珠江口盆地白云凹陷渐新世/中新世地质事件的碎屑组分响应.现代地质,25(3):476-481
刘安.2007.珠江口盆地东沙隆起的构造演化及其对油气的影响.硕士学位论文.广州:中山大学,1-129
刘军,施和生,杜家元,高鹏.2007.东沙隆起台地生物礁、滩油藏成藏条件及勘探思路探讨.热带海洋学报,26(1):22-27
庞雄,陈长民,邵磊,王成善,朱明,何敏,申俊,连世勇,吴湘杰.2007a.白云运动:南海北部渐新统-中新统重大地质事件及其意义.地质论评,53(2):145-151
庞雄,陈长民,彭大钧,朱明,何敏.2007b.南海珠江深水扇系统及油气.北京:科学出版社
邵磊,李献华,汪品先,翦知湣,韦刚健,庞雄,刘颖.2004.南海渐新世以来构造演化的沉积记录---ODP 1148站深海沉积物中的证据.地球科学进展,19(4):539-544
邵磊,庞雄,乔培军,陈长民,李前裕,苗卫良.2008.珠江口盆地的沉积充填与珠江的形成演变.沉积学报,26(2):179-185
孙珍,庞雄,钟志洪,周蒂,陈长民,郝沪军,何敏,黄春菊,许鹤华.2005.珠江口盆地白云凹陷新生代构造演化动力学.地学前缘,12(4):489-498
王春修.1996.珠江口盆地海相中新统层序地层分析及其意义.中国海上油气(地质),10(5):279-288
汪品先,赵泉鸿,翦知湣,成鑫荣,黄维,田军,王吉良,李前裕,李保华,苏新.2003.南海三千万年的深海记录.科学通报,48(21):2206-2215
谢锦龙,余和中,唐良民,傅瑾君,武金云.2010.南海新生代沉积基底性质和盆地类型.海相油气地质,15(4):35-47
姚伯初,万玲,刘振湖.2004.南海海域新生代沉积盆地构造演化的动力学特征及其油气资源.地球科学,29(5):543-549
余海波,杜家元.2011.珠江口盆地A井区珠江组下段潮汐作用对三角洲沉积影响的研究.长江大学学报(自然科学版),8(1):64-66
张向涛,陈亮,佘清华,张素芳,乔培军,邵磊.2012.南海北部古韩江物源的演化特征.海洋地质与第四纪地质,32(4):41-48
赵撼霆.2011.珠江口盆地东沙隆起生物礁碳酸盐岩沉积演化及储层特征.硕士学位论文.青岛:中国科学院海洋研究所,1-64
(1)胡平忠.1994.流花11-1礁(滩)型大油田地质规律与勘探经验.内部资料