Marine transgressions and characteristics of tide-dominated sedimentary systems in the Oligocene,Xihu sag,East China Sea Shelf Basin
Li Shun-Li1, Xu Lei2, Yu Xing-He1, Hou Guo-Wei3, Hu Yong4, Gao Zhao-Pu5
1 School of Energy Resources,China University of Geosciences(Beijing),Beijing 100083; 2 CNOOC Research Institute Co.,Ltd.,Beijing 100028; 3 CNOOC Research Institute Shanghai Branch Co.,Ltd.,Shanghai 200030; 4 College of Resources and Environment,Yangtze University,Wuhan 430100,Hubei; 5 Research Institute of Exploration and Production in SINOPEC North Branch,Zhengzhou 450000,Henan;
Abstract:The Xihu sag is located in the eastern depression of the East China Sea Shelf Basin,which is the largest hydrocarbon-bearing sag. This study was mainly based on well-log,seismic,and core data,combining with geochemical parameters. Characteristics of sterane in mudstone and autogenous glauconites indicate that the southern Xihu sag was in a transitional environment between marine and terrestrial in the Oligocene,which experienced five major marine transgressions. The Oligocene in the Xihu sag was characterized by thick-bedded sandstone and thin-bedded mudstone,developing typical bidirectional cross-beddings,double mud layer,flaser beddings,and mud drapes. Four types of lithofacies were identified: Structureless medium-to-coarse grained sandstone with mudclasts,cross-bedded fine-to-medium grained sandstone,rippled siltstone and fine-grained sandstone,laminated mudstone. During the Oligocene,tide-dominated estuary systems were mainly developed in the southern Xihu sag,which was comprised of sedimentary units of tidal channel,tidal bar,sand flat,and mud flat. The estuary systems widened toward SW,which suggests feeding fluvial systems were from northeast,and the tidal currents were from southwest. In the Oligocene,the southern Xihu sag was connected with the open marine,strongly reworked by tidal currents on the gentle slope gradients without large volume of fluvial sediment flux during marine transgressions,forming tide-dominated estuary systems.
Li Shun-Li,Xu Lei,Yu Xing-He et al. Marine transgressions and characteristics of tide-dominated sedimentary systems in the Oligocene,Xihu sag,East China Sea Shelf Basin[J]. JOPC, 2018, 20(6): 1023-1032.
[1] 陈琳琳,谢月芳. 1998. 东海西湖凹陷花港组沉积模式初探. 海洋石油,(4): 15-21. [Chen L L,Xie Y F.1998. Discussion on depositional mode of Huagang Formation in Xihu Trough,the East China Sea. Marine Petroleum,(4): 15-21] [2] 胡明毅,柯岭,梁建设. 2010. 西湖凹陷花港组沉积相特征及相模式. 石油天然气学报, 32(5): 1-5. [Hu M Y,Ke L,Liang J S.2010. The Characteristics and pattern of sedimentary facies of Huagang Formation in Xihu Depression. Journal of Oil and Gas Technology, 32(5): 1-5] [3] 孙思敏,彭仕宓. 2006. 东海西湖凹陷平湖油气田花港组沉积相及沉积演化. 西北大学学报(自然科学版), 36(1): 63-67. [Sun S M,Peng S M.2006. Sedimentary facies and evolution of Huagang Formation of Pinghu Oilfield in Xihu Sag,the East China. Journal of Northwest University(Natural Science Edition), 36(1): 63-67] [4] 王果寿,周卓明,肖朝辉,李美洲,周维奎,王琳. 2002. 西湖凹陷春晓区带下第三系平湖组、花港组沉积特征. 石油与天然气地质, 23(3): 257-261. [Wang G S,Zhou Z M,Xiao Z H, Li M Z, Zhou W K, Wang L.2002. Sedimentary characteristics of Eogene Pinghu Formation and Huagang Formation in Chunxiao zone of Xihu Lake Depression. Oil and Gas Geology, 23(3): 257-261] [5] 武法东,陆永潮,陈平,周平. 1997. 东海西湖凹陷渐新统花港组海绿石的发现及其意义. 沉积学报, 15(3): 158-161. [Wu F D,Lu Y C,Chen P,Zhou P.1997. The discovery and significance of glauconites in the Huagang Formation of the Oligocene,Xihu Depression,East China Sea. Acta Sedimentologica Sinica, 15(3): 158-161] [6] 于兴河,李顺利,曹冰,侯国伟,王亚风,皇甫致远. 2017. 西湖凹陷渐新世层序地层格架与沉积充填响应. 沉积学报, 35(2): 299-314. [Yu X H,Li S L,Cao B,Hou G W,Wang Y F,Huangfu Z Y.2017. Oligocene sequence framework and depositional response in the Xihu Depression,East China Sea Shelf Basin. Acta Sedimentologica Sinica, 35(2): 299-314] [7] 张国华,张建培. 2015. 东海陆架盆地构造反转特征及成因机制探讨. 地学前缘, 22(1): 260-270. [Zhang G H,Zhang J P.2015. A discussion on the tectonic inversion and its genetic mechanism in the East China Sea Shelf Basin. Earth Science Frontiers, 22(1): 260-270] [8] 张绍亮,秦兰芝,余逸凡,唐贤君. 2014. 西湖凹陷渐新统花港组下段沉积相特征及模式. 石油地质与工程, 28(2): 5-8. [Zhang S L,Qin L Z,Yu Y F,Tang X J.2014. Sedimentary facies characteristics and its mode of lower member of Oilgocene Huagang Formation in Xihu Sag. Petroleum Geology and Engineering, 28(2): 5-8] [9] 朱纯,潘建明,卢冰,扈传昱,刘小涯,叶新荣,薛斌. 2005. 长江、老黄河口及东海陆架沉积有机质物源指标及有机碳的沉积环境. 海洋学研究, 23(3): 36-46. [Zhu C,Pan J M,Lu B,Hu C Y,Liu X Y,Ye X R,Xue B.2005. Source indication and accumulative effect of sedimentary organic matter in the Changjiang Estuary,the old Huanghe River subaqueous delta and the East China Sea shelf. Journal of Marine Scineces,23(3): 36-46] [10] Cukur D,Horozal S,Kim D C,Han H C.2011. Seismic stratigraphy and structural analysis of the northern East China Sea Shelf Basin interpreted from multi-channel seismic reflection data and cross-section restoration. Marine and Petroleum Geology, 28: 1003-1022. [11] Cukur D,Horozal S,Lee G H,Kim D C,Han H C.2012. Timing of trap formation and petroleum generation in the northern East China Sea Shelf Basin.Marine and Petroleum Geology, 36: 154-163. [12] Dalrymple R W,Makino Y,Zaitlin B A.1991. Temporal and spatial patterns of rhythmite deposition on mud flats in the macrotidal Cobequid Baya Salmon river estuary,Bay of Fundy,Canada. In: Smith D G,Reinson G E,Zaitlin B A,Rahmani R A(eds). Clastic Tidal Sedimentology.Canadian Society Petroleum Geologists Memories, 16: 137-160. [13] Embry A F.2009. Practical sequence stratigraphy. Canadian Society of Petroleum Geologists:81. [14] Li C F,Zhou Z Y,Ge H P,Mao Y X.2009. Rifting process of the Xihu Depression,East China Sea Basin. Tectonophysics, 472: 135-147. [15] Li S,Yu X,Zhu X,Li S,Cao B,Hou G.2018. Transition from Tide-influenced Delta to Tide-dominated Estuary in the East China Sea Shelf Basin: Implication for Changes from Source to Sink Controlling on Sedimentation. Sedimentology, doi:10.1111/sed.12466. [16] Huang W-Y,Meinschein W G.1979. Sterols as ecological indicators.Geochimicaet Cosmochimica Acta, 43: 739-745. [17] Miller K G,Kominz M A,Browning J V,Wright J D,Mountain G S,Katz M E,Sugarman P J,Cramer B S,Christie-Blick N,Pekar S F.2005. The phanerozoic record of global sea-level change. Science, 310: 1293-1298. [18] Yang S,Hu S,Cai D,Feng X,Chen L,Gao L.2004. Present-day heat flow,thermal history and tectonic subsidence of the East China Sea Basin.Marine and Petroleum Geology, 21: 1095-1105. [19] Zhou Z Y,Jiang J Y,Liao Z T,Yang F L,Shang K Y.2001. Basin inversion in Xihu Depression,East China Sea.Gondwana Research, 4: 844-845.