吉林大学学报(地球科学版) ›› 2019, Vol. 49 ›› Issue (1): 131-138.doi: 10.13278/j.cnki.jjuese.20180129

• 海洋地质与资源 • 上一篇    

东海陆架盆地南部中生界沉积模式

王蛟1,2, 李智高3, 蔡来星1,2, 龚奇勇1,2   

  1. 1. 中国地质调查局青岛海洋地质研究所, 山东 青岛 266071;
    2. 青岛海洋科学与技术试点国家实验室海洋矿产资源评价与探测技术功能实验室, 山东 青岛 266071;
    3. 中海石油(中国)有限公司深圳分公司, 广东 深圳 518000
  • 收稿日期:2018-05-24 发布日期:2019-01-18
  • 通讯作者: 蔡来星(1985-),男,在站博士后,主要从事油气地质学方面的研究,E-mail:qingxin717717@126.com E-mail:qingxin717717@126.com
  • 作者简介:王蛟(1977-),男,研究员,博士,主要从事沉积学方面的研究,E-mail:wangjiao004@sina.com
  • 基金资助:
    国家自然科学基金项目（41476053）；国家海洋地质专项（DD20160147）；中国地质调查局项目（DD20160153，DD20190211）

Sedimentary Model of Mesozoic in the Southern Part of the East China Sea Shelf Basin

Wang Jiao1,2, Li Zhigao3, Cai Laixing1,2, Gong Qiyong1,2   

  1. 1. Qingdao Institute of Marine Geology, China Geological Survey, Qingdao 266071, Shandong, China;
    2. Laboratory for Marine Mineral Resources, Pilot National Laboratory for Marine Science and Technology(Qingdao), Qingdao 266071, Shandong, China;
    3. Shenzhen Branch, Cnooc(China) co., LTD. Shenzhen 518000, Guangdong, China
  • Received:2018-05-24 Published:2019-01-18
  • Supported by:
    Supported by National Natural Science Foundation of China (41476053),National Marine Geology Special Project of China (DD20160147) and Project of China Geological Survey (DD20160153,DD20190211)

PDF (PC)

271

摘要： 在沉积相综合分析基础之上，通过地震相分析的手段明确了东海陆架盆地南部中生界的沉积特征；结合古地理背景分析，建立了该区侏罗纪和白垩纪的沉积模式。侏罗纪时雁荡低凸起和瓯江凹陷均未形成，闽江凹陷和基隆凹陷连为一体，物源来自浙闽隆起区，发育滨浅海沉积体系，火山作用较为强烈。白垩纪晚期-古新世，随着太平洋板块俯冲角度的加大，浙闽隆起区发生裂陷，雁荡低凸起形成。西部的瓯江凹陷沉积了一套陆相的冲积扇-河流-三角洲-湖泊沉积体系；由于此间台北低凸起尚未起到分割作用，东部的闽江凹陷与基隆凹陷仍然连为一体，物源来自浙闽隆起带和台北水下火山岩带，发育滨浅海沉积体系，火山作用影响强烈。

关键词: 东海陆架盆地, 中生界, 沉积体系, 沉积模式

Abstract: Based on the comprehensive study of sedimentary facies, the authors clarified the sedimentary characteristics of Mesozoic in the southern part of the East China Sea Shelf basin by means of seismic facies analysis. After the unit analysis of paleo-geographic setting,the sedimentary model of Jurassic and Cretaceous in this area is established. In Jurassic, neither Yandang low uplift nor Oujiang pit was formed, and the Minjiang pit and the Keelung pit were integrated. During the Late Cretaceous-Paleocene, with the increase of the subduction angle of the Pacific plate, the Zhejiang-Fujian uplift area was destroyed, forming the Yandang low uplift, and a continental alluvial fan fluvial River delta lake depositional system was deposited in the Oujiang pit in western China. Because the Taipei low uplift had not yet played the role of segmentation, the Minjiang pit in the East and the Keelung pit were still connected, the source came from the Zhejiang-Fujian uplift zone and the Taipei underwater volcanic rock zone. The coastal shallow sea depositional system was developed, and the volcanism had a strong influence.

Key words: East China Sea Shelf basin, Mesozoic, depositional system, sedimentary model

中图分类号: 

  • P618.13
[1] 李刚,龚建明,杨长清,等."大东海"中生代地层分布:值得关注的新领域[J].海洋地质与第四纪地质,2012,32(3):97-104. Li Gang,Gong Jianming,Yang Changqing,et al.Stratigraphic Features of the Mesozoic "Great East China Sea":A New Exploration Field[J].Marine Geology & Quaternary Geology,2012,32(3):97-104.
[2] 杨长清,杨传胜,李刚,等.东海陆架盆地南部中生代构造演化与原型盆地性质[J].海洋地质与第四纪地质,2012,32(3):105-111. Yang Changqing,Yang Chuansheng,Li Gang,et al.Mesozoic Tectonic Evolution and Prototype Basin Characters in the Southern East China Sea Shelf Basin[J].Marine Geology & Quaternary Geology,2012,32(3):105-111.
[3] 梁若冰.东海陆架盆地南部中生界分布浅析[J].海洋石油,2012,32(3):18-22. Liang Ruobing.The Distribution of Mesozoic in the Southern Part of East China Sea Shelf Basin[J].Offshore Oil,2012,32(3):18-22.
[4] 龚建明,李刚,杨长清,等.东海南部三叠纪地层分布[J].海洋地质与第四纪地质,2012,32(3):119-124. Gong Jianming,Li Gang,Yang Changqing,et al.Distribution of Triassic Strata in the Southern East China Sea[J].Marine Geology & Quaternary Geology,2012,32(3):119-124.
[5] 李智高,龚建明,操应长,等.东海南部及邻区海陆中生代沉积特征对比[J].海洋地质与第四纪地质,2015,35(1):29-35. Li Zhigao,Gong Jianming,Cao Yingchang,et al.Comparision of Sedimentary Characteristics of the Mesozoic in Southern East China Sea and Adjacent Uplifting Areas[J].Marine Geology & Quaternary Geology,2015,35(1):29-35.
[6] Li Sanzhong,Zhao Guohun,Dai Liming,et al.Mesozoic Basins in Eastern China and Their Bearings on the Deconstruction of the North China Craton[J].Journal of Asian Earth Sciences,2012,47:64-79.
[7] 杨艳秋,李刚,戴春山.东海陆架盆地西部坳陷带中生界分布特征及其有利区探讨[J].世界地质,2011,30(3):396-403. Yang Yanqiu,Li Gang,Dai Chunshan.Characteristics of Mesozoic Distribution and Discussion on Its Favourable Area in Western Depression Zone of East China Sea Shelf Basin[J].Global Geology,2011,30(3):396-403.
[8] 姜亮.东海陆架盆地油气资源勘探现状及含油气远景[J].中国海上油气:地质,2003,17(1):1-5. Jiang Liang.Exploration Status and Perspective of Petroleum Resources in East China Sea Shelf Basin[J].China Offshore Oil and Gas:Geology,2003,17(1):1-5.
[9] 冯晓杰,张川燕,王春修,等.东海陆架和台西南盆地中生界及其油气勘探潜力[J].中国海上油气:地质,2001,15(5):306-310,316. Feng Xiaojie,Zhang Chuanyan,Wang Chunxiu,et al.Mesozoic in the East China Sea Shelf and Taixinan Basin and Its Petroleum Potential[J].China Offshore Oil and Gas:Geology,2001,15(5):306-310,316.
[10] 高乐.东海陆架中生代残余盆地特征及勘探方向探讨[J].中国海上油气:地质,2005,17(3):148-152. Gao Le.Mesozoic Remnant Basin Characteristics and Hydrocarbon Exploration Direction on East China Sea Shelf[J].China Offshore Oil and Gas:Geology,2005,17(3):148-152.
[11] 龚建明,李刚,杨传胜,等.东海陆架盆地南部中生界分布特征与油气勘探前景[J].吉林大学学报(地球科学版),2013,43(1):20-27. Gong Jianming,Li Gang,Yang Chuansheng,et al.Hydrocarbon Prospecting of Mesozoic Strata in Southern East China Sea Shelf Basin[J].Journal of Jilin Unviersity(Earth Science Edition),2013,43(1):20-27.
[12] 刘金水,廖宗廷,贾健谊,等.东海陆架盆地地质结构及构造演化[J].上海地质,2003(3):1-6. Liu Jinshui,Liao Zongting,Jia Jianyi,et al.The Geological Structure and Tectonic Evolution of the East China Sea Shelf Basin[J].Shanghai Geology,2003(3):1-6.
[13] 胡文博.东海陆架盆地南部中生界沉积体系研究[D].北京:中国地质大学,2012. Hu Wenbo.The Mesozoic Sedimentary Systems in the Southern East China Sea Shelf Basin[D].Beijing:China Universtiy of Geosciences,2012.
[14] 索艳慧,李三忠,戴黎明,等.东海陆架盆地构造单元划分与特征[J].海洋地质与第四纪地质,2010,30(6):49-58. Suo Yanhui,Li Sanzhong,Dai Liming,et al.Division and Characteristics of Tectonic Units of the East China Sea Shelf Basin[J].Marine Geology & Quaternary Geology,2010,30(6):49-58.
[15] 杨文达,崔征科,张异彪.东海地质与矿产[M].北京:海洋出版社,2010:390-405. Yang Wenda,Cui Zhengke,Zhang Yibiao.Geology and Mineral Resources of the East China Sea[M].Beijing:Marine Press,2010:390-405.
[16] 杨传胜,李刚,杨长清,等.东海陆架盆地及其邻域岩浆岩时空分布特征[J].海洋地质与第四纪地质,2012,32(3):125-133. Yang Chuansheng,Li Gang,Yang Changqing,et al.Marine Geology & Quaternary Geology,2012,32(3):125-133.
[17] 李家彪.东海区域地质[M].北京:海洋出版社,2008:452-519. Li Jiabiao.Regional Geology of the East China Sea[M].Beijing:China Ocean Press,2008:452-519.
[18] 杨长清,李刚,龚建明,等.中国东南海域中生界油气地质条件与勘探前景[J].吉林大学学报(地球科学版),2015,45(1):1-12. Yang Changqing,Li Gang,Gong Jianming,et al.Petroleum Geological Conditions and Exploration Prospect of the Mesozoic in Southeast China Sea Area[J].Journal of Jilin University(Earth Science Edition),2015,45(1):1-12.
[1] 朱兆群, 林承焰, 张宪国, 李志鹏, 谢晶晶, 魏肃东, 程平. 断陷湖盆早期浅水三角洲沉积——以高邮凹陷永安地区戴一段为例[J]. 吉林大学学报(地球科学版), 2017, 47(3): 659-673.
[2] 耿晓洁, 朱筱敏, 董艳蕾. 地震沉积学在近岸水下扇沉积体系分析中的应用以泌阳凹陷东南部古近系核三上亚段为例[J]. 吉林大学学报(地球科学版), 2016, 46(1): 57-64.
[3] 单敬福, 张吉, 王继平, 赵忠军, 李浮萍, 陈治华, 石林辉, 刘利峰. 苏里格气田西区盒8下亚段辫状河沉积论证与分析[J]. 吉林大学学报(地球科学版), 2015, 45(6): 1597-1607.
[4] 张宇焜, 胡晓庆, 牛涛, 张显文, 高玉飞, 王晖, 范廷恩, 卜范青. 古地貌对渤海石臼坨凸起古近系沉积体系的控制作用[J]. 吉林大学学报(地球科学版), 2015, 45(6): 1589-1596.
[5] 张晶, 刘化清, 李双文, 冀虎山, 袁淑琴, 洪忠. 断陷湖盆深水重力流水道的识别标志及沉积模式——以歧口凹陷歧南斜坡沙一段为例[J]. 吉林大学学报(地球科学版), 2015, 45(3): 701-711.
[6] 赵小青, 程日辉, 于振锋, 孙凤贤, 王鹏, 高会军. 海拉尔盆地乌尔逊凹陷南一段物源-沉积体系与构造背景[J]. 吉林大学学报(地球科学版), 2015, 45(1): 61-80.
[7] 张银国,梁杰. 南黄海盆地二叠系至三叠系沉积体系特征及其沉积演化[J]. 吉林大学学报(地球科学版), 2014, 44(5): 1406-1418.
[8] 孙乃泉，云露，蒲仁海，杨素举. 塔里木盆地顺9井区柯坪塔格组下段沉积微相与储层展布[J]. 吉林大学学报(地球科学版), 2013, 43(6): 1716-1725.
[9] 龚建明，李刚，杨传胜，须雪豪，张锦伟，王海荣，徐立明. 东海陆架盆地南部中生界分布特征与油气勘探前景[J]. 吉林大学学报(地球科学版), 2013, 43(1): 20-27.
[10] 张茂恒, 孔兴功. 江苏盱眙震旦纪混合沉积体系的特征[J]. J4, 2011, 41(5): 1448-1457.
[11] 李顺明, 宋新民, 刘曰强, 王友启, 李艳明, 唐后军. 温米退积型与进积型浅水辫状河三角洲沉积模式[J]. J4, 2011, 41(3): 665-672.
[12] 伊振林, 吴胜和, 杜庆龙, 张保国, 岳大力, 李艳平. 冲积扇储层构型精细解剖方法--以克拉玛依油田六中区下克拉玛依组为例[J]. J4, 2010, 40(4): 939-946.
[13] 曹瑞成, 李军辉, 卢双舫, 张大智, 刘秋宏, 陈学海, 赵莹, 胡寿梅. 海拉尔盆地呼和湖凹陷白垩系层序地层特征及沉积演化[J]. J4, 2010, 40(3): 535-541.
[14] 孔庆莹, 程日辉. 塔里木盆地孔雀河地区寒武系-下奥陶统沉积特征[J]. J4, 2010, 40(3): 527-534.
[15] 孙伟，樊太亮，赵志刚，王宏语，高志前，段锐晖. 乌石凹陷古近系层序地层特征及充填演化[J]. J4, 2008, 38(2): 233-0239.
Viewed
Full text


Abstract

Cited
  Shared   
  Discussed   
No Suggested Reading articles found!
版权所有 © 《吉林大学学报(地球科学版)》编辑部
地址：长春市西民主大街938号(130026)　电话：+86-431-88502374；13756165364　E-mail: xuebao1956@jlu.edu.cn
本系统由北京玛格泰克科技发展有限公司设计开发