32~10.5 Ma古韩江三角洲沉积演化与控制因素

刘辰生; 侯文锋; 邱争科; 王涛; 张向涛; 汪旭东

doi:10.11781/sysydz201904482

32~10.5 Ma古韩江三角洲沉积演化与控制因素

doi: 10.11781/sysydz201904482

刘辰生^1,2,3,
侯文锋⁴,
邱争科⁴,
王涛⁴,
张向涛⁵,
汪旭东⁵

1. 有色金属成矿预测与地质环境监测教育部重点实验室(中南大学), 长沙 410083;
2. 有色资源与地质灾害探查湖南省重点实验室, 长沙 410083;
3. 中南大学地球科学与信息物理学院, 长沙 410083;
4. 中国石油新疆油田分公司采油二厂, 新疆克拉玛依 834009;
5. 中海石油深圳分公司, 广东深圳 518054

基金项目:

湖南省自然科学基金项目"湘中和湘南地区下古生界原型盆地对细粒沉积控制作用"（2017JJ1034）资助。

详细信息

作者简介:
刘辰生(1976-),男,博士,副教授,从事层序地层学和沉积学教学和研究。E-mail:lcsjed@163.com。

中图分类号: TE121.3
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出版历程
- 收稿日期: 2018-10-24
- 修回日期: 2019-05-17
- 刊出日期: 2019-07-28

Sedimentary evolution and controls in paleo-Hanjiang delta from 32 to 10.5 Ma

1. Key Laboratory of Metallogenic Prediction of Nonferrous Metals and Geological Environment Monitoring of Ministry of Education(Central South University), Changsha, Hunan 410083, China;
2. Key Laboratory of Non-ferrous Resources and Geological Hazard Detection, Changsha, Hunan 410083, China;
3. School of Geosciences and Info-physics, Central South University, Changsha, Hunan 410083, China;
4. Second Oil Recovery Plant, Xinjiang Oilfield, PetroChina, Karamay, Xinjiang 834009, China;
5. Shenzhen Branch of CNOOC Limited, Shenzhen, Guangdong 518054, China

摘要

摘要: 近年来，古韩江三角洲已成为我国南海油气勘探的热点，对其开展沉积演化分析有助于评价珠江口盆地油气资源潜力，预测有利勘探区块。依据岩心、测井、钻井和地震资料，分析陆丰-韩江凹陷区32~10.5 Ma沉积相类型和古韩江三角洲演化。韩江-陆丰凹陷古韩江三角洲相可划分为三角洲平原、前缘和前三角洲亚相。古韩江三角洲演化分为3个阶段：第一阶段，渐新统珠海组至中新统珠江组沉积期，古韩江三角洲沉积物粒度粗，三角洲延伸远，主要分布在陆丰凹陷；第二阶段，中新统韩江组下段沉积期，随着海平面上升，古韩江三角洲逐渐向物源区退缩，陆丰和韩江地区以碳酸盐岩台地相和浅海陆棚相为主，海平面在韩江组下段沉积时期达到最大，古韩江三角洲面积达到最小；第三阶段，韩江组上段沉积期，随着海平面下降，古韩江三角洲又开始向盆地推进。
- 物源 /
- 海平面变化 /
- 珠江三角洲 /
- 古韩江三角洲 /
- 珠海组 /
- 珠江组 /
- 韩江组 /
- 珠江口盆地
Abstract: The paleo-Hanjiang delta has become a focus of petroleum exploration in the South China Sea. The sedimentary evolution analysis of the paleo-Hanjiang delta is helpful to evaluate the potential of petroleum resources in the Pearl River Mouth Basin and predict favorable exploration blocks. The sedimentary facies types and evolution of the paleo-Hanjiang delta in the Lufeng-Hanjiang sags from 32-10.5 Ma were analyzed based on core, logging, drilling and seismic data. The results show that paleo-Hanjiang delta can be subdivided into delta plain, delta front and pre-delta in the Hanjiang-Lufeng sags. The evolution of the paleo-Hanjiang delta has experienced three stages. In the first stage, during the sedimentary period from the Zhuhai Formation to the Zhujiang Formation, the sediments of the paleo-Hanjiang delta were coarse in grain size and extended in the delta, mainly distributed in the Lufeng Sag. In the second stage, during deposition of the lower part of Hanjiang Formation, the paleo-Hanjiang delta gradually had reduced provenance in response to increasing sea level. Shallow shelf and carbonate platform were dominant in the Lufeng and Hanjiang area. The sea level reached its maximum in the lower section of the Hanjiang Formation, and the area of the paleo-Hanjiang delta reached its smallest. In the third stage, during the sedimentary period of the upper section of Hanjiang Formation, the paleo-Hanjiang delta began to advance to the basin as the sea level fell.
- provenance /
- change of sea level /
- Pearl River delta /
- paleo-Hanjiang delta /
- Zhuhai Formation /
- Zhujiang Formation /
- Hanjiang Formation /
- Pearl River Mouth Basin

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参考文献(30)

[1]	涂乙,杨娇,王秀玲,等.珠江口盆地B油田储量参数概率分布[J].石油实验地质,2017,39(4):573-579. TU Yi,YANG Jiao,WANG Xiuling,et al.Probability distribution of reservoir parameters in the B oil field,Pearl River Mouth Basin[J].Petroleum Geology & Experiment,2017,39(4):573-579.
[2]	杜家元,丁琳,张向涛,等.珠江口盆地惠州凹陷西南部新近系岩性油气藏勘探思路与关键技术[J].石油实验地质,2017,39(6):858-864. DU Jiayuan,DING Lin,ZHANG Xiangtao,et al.Exploration approach and techniques for the Neogene lithologic reservoirs in the southwestern Huizhou Sag,Pearl River Mouth Basin[J].Petroleum Geology & Experiment,2017,39(6):858-864.
[3]	孙珍,庞雄,钟志洪,等.珠江口盆地白云凹陷新生代构造演化动力学[J].地学前缘,2005,12(4):489-498. SUN Zhen,PANG Xiong,ZHONG Zhihong,et al.Dynamics of Tertiary tectonic evolution of the Baiyun Sag in the Pearl River Mouth Basin[J].Earth Science Frontiers,2005,12(4):489-498.
[4]	韦惺,吴超羽.全新世以来珠江三角洲的地层层序和演变过程[J].中国科学(地球科学),2011,41(8):1134-1149. WEI Xing,WU Chaoyu.Holocene delta evolution and sequence stratigraphy of the Pearl River Delta in South China[J].Science China(Earth Science),2011,54(10):1523-1541.
[5]	杜家元,施和生,丁琳,等.珠江口盆地(东部)地层岩性油气藏勘探有利区域分析[J].中国海上油气,2014,26(3):30-36. DU Jiayuan SHI Hesheng DING Lin,et al.An analysis of favorable exploration areas for stratigraphic-lithologic hydrocarbon accumulation in the eastern Pearl River Mouth Basin[J].China Offshore Oil and Gas,2014,26(3):30-36.
[6]	柳保军,庞雄,颜承志,等.珠江口盆地白云深水区渐新世-中新世陆架坡折带演化及油气勘探意义[J].石油学报,2011,32(2):234-242. LIU Baojun,PANG Xiong,YAN Chengzhi,et al.Evolution of the Oligocene-Miocene shelf slope-break zone in the Baiyun deep-water area of the Pearl River Mouth Basin and its significance in oil-gas exploration[J].Acta Petrolei Sinica,2011,32(2):234-242.
[7]	刘雨晴,吴智平,张杰,等.南海南部陆缘盆地反转构造及其油气成藏意义:以礼乐盆地北部坳陷为例[J].断块油气田,2018,25(01):1-5. LIU Yuqing,WU Zhiping,ZHANG Jie,et al.Characteristics of inversion tectonic and its impact on hydrocarbon accumulation in southern continental basins of South China Sea:a case study of northern Depression, Reed Basin[J].Fault-Block Oil and Gas Field,2018,25(1):1-5.
[8]	赵撼霆,吴时国,马玉波,等.南海珠江口盆地东沙隆起区生物礁演化模式[J].海洋地质与第四纪地质,2012,32(1):43-50. ZHAO Hanting,WU Shiguo,MA Yubo,et al.An evolutionary model of bio-reefs at the Dongsha Uplift,Zhujiangkou Basin,South China Sea[J].Marine Geology & Quaternary Geology,2012,32(1):43-50.
[9]	朱伟林,张功成,高乐.南海北部大陆边缘盆地油气地质特征与勘探方向[J].石油学报,2008,29(1):1-9. ZHU Weilin,ZHANG Gongcheng,GAO Le.Geological characteristics and exploration objectives of hydrocarbons in the northern continental margin basin of South China Sea[J].Acta Petrolei Sinica,2008,29(1):1-9.
[10]	邵磊,庞雄,张功成,等.南海北部渐新世末的构造事件[J].地球科学,2009,34(5):717-724. SHAO Lei,PANG Xiong,ZHANG Gongcheng,et al.Late Oligocene tectonic event in the northern South China Sea and its implications[J].Earth Science,2009,34(5):717-724.
[11]	张伟,曹仁义,罗东红,等.南海珠江口盆地海相砂岩油藏高倍数水驱驱替特征[J].油气地质与采收率,2018,25(2):64-71. ZHANG Wei,CAO Renyi,LUO Donghong,et al. Displacement characteristics of high-multiple water drive in marine sandstone reservoirs in the Pearl River Mouth Basin,South China Sea[J].Petroleum Geology and Recovery Efficiency,2018,25(2):64-71.
[12]	涂乙,刘伟新,戴宗,等.基于熵权法的储层非均质性定量评价:以珠江口盆地A油田为例[J].油气地质与采收率,2017,24(5):27-33. Tu Yi,Liu Weixin,Dai Zong,et al.Quantitative evaluation for reservoir heterogeneity based on entropy weight method:a case study of A Oilfield in Pearl River Mouth Basin[J].Petroleum Geology and Recovery Efficiency,2017,24(5):27-33.
[13]	兰叶芳,黄思静,黄可可,等.珠江口盆地珠江组碳酸盐岩阴极发光特征及成岩阶段划分[J].油气地质与采收率,2017,24(1):34-42. LAN Yefang,HUANG Sijing,HUANG Keke,et al.Cathodoluminescence features and diagenetic stage division of carbonates in the Zhujiang Formation,Pearl River Mouth Basin[J].Petroleum Geology and Recovery Efficiency,2017,24(1):34-42.
[14]	施和生,代一丁,刘丽华,等.珠江口盆地珠一坳陷油气藏地质特征与分布发育基本模式[J].石油学报,2015,36(S2):120-133. SHI Hesheng,DAI Yiding,LIU Lihua,et al.Geological characteristics and distribution model of oil and gas reservoirs in Zhu I Depression,Pearl River Mouth Basin[J].Acta Petrolei Sinica,2015,36(S2):120-133.
[15]	施和生,何敏,张丽丽,等.珠江口盆地(东部)油气地质特征、成藏规律及下一步勘探策略[J].中国海上油气,2014,26(3):11-22. SHI Hesheng,HE Min,ZHANG Lili,et al.Hydrocarbon geology,accumulation pattern and the next exploration strategy in the eastern Pearl River Mouth Basin[J].China Offshore Oil and Gas,20L4,26(3):11-22.
[16]	崔莎莎,何家雄,陈胜红,等.珠江口盆地发育演化特征及其油气成藏地质条件[J].天然气地球科学,2009,20(3):384-391. CUI Shasha,HE Jiaxiong,CHEN Shenghong,et al.Development characteristics of Pearl River Mouth Basin and its geological conditions for oil and gas accumulation[J].Natural Gas Geoscience,2009,20(3):384-391.
[17]	李友川,陶维祥,孙玉梅,等.珠江口盆地惠州凹陷及其邻区原油分类和分布特征[J].石油学报,2009,30(6):830-834. LI Youchuan,TAO Weixiang,SUN Yumei,et al.Classification and distribution of oil in Huizhou Depression of Pearl River Mouth Basin[J].Acta Petrolei Sinica,2009,30(6):830-834.
[18]	何家雄,刘海龄,姚永坚,等.南海北部边缘盆地油气地质及资源前景[M].北京:石油工业出版社,2008. HE Jiaxiong,LIU Hailing,YAO Yongjian,et al.The petroleum geology and the resource potential of the marginal basin in the northern South China Sea[M].Beijing:Petroleum Industry Press,2008.
[19]	朱红涛,李森,刘浩冉,等.陆相断陷湖盆迁移型层序构型及意义:以珠Ⅰ坳陷古近系文昌组为例[J].地球科学,2016,41(3):361-372. ZHU Hongtao,LI Sen,LIU Haoran,et al.The types and implication of migrated sequence stratigraphic architecture in continental lacustrine rift basin:an example from the Paleogene Wenchang Formation of Zhu Ⅰ Depression,Pearl River Mouth Basin[J].Earth Science,2016,41(3):361-372.
[20]	许新明,陈胜红,王福国,等.珠江口盆地恩平凹陷断层特征及其对新近系油气成藏的影响[J].现代地质,2014,28(3):543-550. XU Xinming,CHEN Shenghong,WANG Fuguo,et al.Structural features and its impacts on hydrcarbon accumulation of Neogene in Enping Sag,Pearl River Mouth Basin[J].Geoscience,2014,28(3):543-550.
[21]	刘明辉,梅廉夫,杨亚娟,等.珠江口盆地惠州凹陷北部裂陷期与拗陷期沉降作用时空差异及主控因素[J].地球科学与环境学报,2015,37(2):31-43. LIU Minghui,MEI Lianfu,YANG Yajuan,et al.Temporal-spatial differences of subsidence between Syn-and post-rift stages in northern Huizhou Sag of Pearl River Mouth Basin and their main control factors[J].Journal of Earth Sciences and Environment,2015,37(2):31-43.
[22]	于水明,陈雪芳,梅廉夫,等.珠一坳陷断层特征及对油气成藏的作用[J].石油天然气学报,2012,34(1):50-54. YU Shuiming,CHEN Xuefang,MEI Lianfu,et al.The effect of fault zone characteristics of Zhu 1 Depression on hydrocarbon accumulation[J].Journal of Oil and Gas Technology,2012,34(1):50-54.
[23]	PINOUS O V,KAROGODIN Y N,ERSHOV S V,et al.Sequence stratigraphy,facies,and Sea level change of the Hauterivian productive complex,Priobskoe oil Field (West Siberia)[J].AAPG Bulletin,1999,83(6):972-989.
[24]	PEROV G,BHATTACHARYA J P.Pleistocene shelf-margin delta:intradeltaic deformation and sediment bypass,northern Gulf of Mexico[J].AAPG Bulletin,2011,95(9):1617-1641.
[25]	HENRICH R,CHERUBINI Y,MEGGERS H.Climate and sea level induced turbidite activity in a canyon system offshore the hyperarid Western Sahara (Mauritania):the Timiris Canyon[J].Marine Geology,2010,275(1/4):178-198.
[26]	HAQ B U,HARDENBOL J,VAIL P R.Chronology of fluctuating sea levels since the Triassic[J].Science,1987,235(4793):1156-1167.
[27]	VAIL P R,MITCHUM R M JR,TODD R G,et al.Seismic stratigraphy and global changes of sea level[C]//Payton C E.Seismic strati-graphy:applications to hydrocarbon exploration.Tulsa:AAPG,1977,26:49-212.
[28]	米立军,张功成,沈怀磊,等.珠江口盆地深水区白云凹陷始新统-下渐新统沉积特征[J].石油学报,2008,29(1):29-34. MI Lijun,ZHANG Gongcheng,SHEN Huailei,et al.Eocene-Lower Oligocene sedimentation characteristics of Baiyun Sag in the deep water area of Pearl River Mouth Basin[J].Acta Petrolei Sinica,2008,29(1):29-34.
[29]	刘辰生,张琳婷,郭建华.塔里木盆地白垩系层序地层学[J].中南大学学报(自然科学版),2012,43(7):2683-2690. LIU Chensheng,ZHANG Linting,GUO Jianhua.Sequence of Cretaceous in Tarim Basin[J].Journal of Central South University (Science and Technology),2012,43(7):2683-2690.
[30]	郑超,李静,高达,陈军,张童.沙湾凹陷百口泉组层序地层及沉积体系研究[J]. 特种油气藏,2017,24(6):48-54. ZHENG Chao,LI Jing,GAO Da,et al. Study on sequence stratigraphy and deposit systems of the Baikouquan Formation in Shawan Sag[J]. Special Oil & Gas Reservoirs,2017,24(6):48-54.