• RSS
  • E-mail Alert
  • 收藏主页

古地理学报 ›› 2015, Vol. 17 ›› Issue (3): 335-346. doi: 10.7605/gdlxb.2015.03.28

• 岩相古地理学及沉积学 • 上一篇    下一篇

川东及其周缘地区下寒武统龙王庙组沉积相

任影1,2,钟大康1,2,高崇龙1,2,党录瑞3,彭平3,陈卫东3,毛亚坤1,2,胡小林1,2   

  1. 1 中国石油大学(北京)地球科学学院,北京 102249
    2 中国石油大学(北京)油气资源与探测国家重点实验室,北京 102249
    3 中国石油西南油气田分公司重庆气矿,重庆 400021
  • 收稿日期:2014-10-28 修回日期:2015-01-05 出版日期:2015-06-01 发布日期:2015-06-01
  • 作者简介:任影,女,1989年生,中国石油大学(北京)地球科学学院博士研究生,主要从事沉积学与储集层研究。E-mail: renying19890701@126.com。
       通讯作者简介 钟大康,男,1961年生,博士,教授,现主要从事沉积学与储集层研究。联系电话:010-89733322;E-mail: Zhongdakang@263.net。
  • 基金资助:
    国家自然科学基金重点项目(编号:41472094)和国家重点基础研究发展计划(“973”)项目(编号:2011CB201104)联合资助

Sedimentary facies of the Lower Cambrian Longwangmiao Formation in eastern Sichuan Basin and its adjacent areas

Ren Ying1,2, Zhong Dakang1,2, Gao Chonglong1,2, Dang Lurui3
Peng Ping3, Chen Weidong3, Mao Yakun1,2, Hu Xiaolin1,2   

  1. 1 College of Geosciences,China University of Petroleum(Beijing),Beijing 102249
    2 State Key Laboratory of Petroleum Resource and Prospecting,China University of Petroleum(Beijing),Beijing 102249
    3 Chongqing Gas District,Southwest Oil and Gas Field Co.,Ltd.,PetroChina,Chongqing 400021
  • Received:2014-10-28 Revised:2015-01-05 Online:2015-06-01 Published:2015-06-01
  • About author:Ren Ying,born in 1989,is a doctoral candidate of China University of Petroleum(Beijing). Now she is mainly engaged in sedimentology and reservoir geology. E-mail:renying19890701@126.com.
       About the corresponding author Zhong Dakang,born in 1961,is a professor of China University of Petroleum(Beijing). He is mainly engaged in sedimentology and reservoir geology. E-mail: Zhongdakang@263.net.

RichHTML

PDF

摘要： 通过野外露头、钻测井、三维地震及区域地质调查等资料的综合研究发现,川东及其周缘地区下寒武统龙王庙组岩石类型以碳酸盐岩(粉晶白云岩、颗粒白云岩、泥晶灰岩和颗粒灰岩)为主,局部发育大套蒸发岩(膏岩和云质膏岩)及碳酸盐岩与碎屑岩的混合沉积;识别出局限台地相、开阔台地相、蒸发台地相和混积台地相4种沉积相类型,以局限台地相最为发育;川东及其周缘地区龙王庙组各沉积相带呈北东—南西向展布,混积台地相分布于研究区西北部,蒸发台地相集中发育在研究区西部华蓥山断裂东侧,局限台地相分布于混积台地相以东到盆地东边界以西的地区,开阔台地相分布于局限台地相以东到广海的部分地区。

关键词: 四川盆地, 下寒武统, 龙王庙组, 沉积相

Abstract: Based on outcrops,logging data,seismic data and regional survey reports, the main rocks of the Lower Cambrian Longwangmiao Formation in eastern Sichuan Basin and its adjacent areas carbonate rocks(i.e., silt￣sized crystalline dolostone, grain dolostone, micritic limstone and grain limestone), and some locally-developed large sets of evaporites(gypsum rock and dolomitic gypsum rock)and mixed carbonate-clastic deposits can be seen. Four types of sedimentary facies are identified from northwest to southeast, i.e.,mixed platform,restricted platform,evaporitic platform and open platform,among which,the restricted platform is most widely developed. Generally,all the facies are distributed in a southwest-northeast trending. The mixed platform is mainly distributed in the northwestern study area,the evaporitic platform is mainly distributed on the eastern side of Huayingshan Fault in the western study area,and eastwards, the restricted platform and the open platform are developed respectively.

Key words: Sichuan Basin, Lower Cambrian, Longwangmiao Formation, sedimentary facies

中图分类号: