必须声明标量变量 "@Script_ID"。 下刚果盆地海相烃源岩地球化学特征、成因及其发育的控制因素-《地球科学与环境学报》
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[1]曹军,钟宁宁,邓运华,等.下刚果盆地海相烃源岩地球化学特征、成因及其发育的控制因素[J].地球科学与环境学报,2014,36(04):87-98.
 CAO Jun,ZHONG Ning-ning,DENG Yun-hua,et al.Geochemical Characteristics, Origin and Factors Controlling Formation of Marine Source Rock in Lower Congo Basin[J].Journal of Earth Sciences and Environment,2014,36(04):87-98.
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《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:
第36卷
期数:
2014年第04期
页码:
87-98
栏目:
基础地质与矿产地质
出版日期:
2014-12-15

文章信息/Info

Title:
Geochemical Characteristics, Origin and Factors Controlling Formation of Marine Source Rock in Lower Congo Basin
文章编号:
1672-6561(2014)04-0087-12
作者:
曹军钟宁宁邓运华康洪全孙玉梅刘岩戴娜黄小艳朱顺玲
1. 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; 2. 中海油研究总院,北京 100028; 3. 长江大学计算机科学学院,湖北 荆州 434023
Author(s):
CAO JunZHONG Ning-ningDENG Yun-huaKANG Hong-quanSUN Yu-meiLIU YanDAI NaHUANG Xiao-yanZHU Shun-ling
1. State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum,Beijing 102249, China; 2. CNOOC Research Institute, Beijing 100028, China; 3. School of Computer Science, Yangtze University, Jingzhou 434023, Hubei, China
关键词:
地球化学海相烃源岩生烃潜力生源输入沉积环境成因类型控制因素下刚果盆地
Keywords:
geochemistry marine source rock hydrocarbon potential organic matter input sedimentary environment genetic type controlling factor Lower Congo Basin
分类号:
P618.130.2+7;TE122
DOI:
-
文献标志码:
A
摘要:
下刚果盆地深水区的油气显示出了海相原油的特征,盐上海相烃源岩开始受到关注。通过对下刚果盆地海相烃源岩地球化学资料分析,综合评价了盐上4套海相烃源岩的地球化学特征和生烃潜力,研究了其成因并划分了成因类型,同时探讨了不同成因类型烃源岩发育的主控因素。结果表明:下刚果盆地盐岩层之上发育海相烃源岩,有机质丰度中等—好,干酪根类型为Ⅱ、Ⅲ型,成因上以海相内源型和海相混合生源型为主;盆地海相烃源岩整体在3500m左右深度进入生油窗,成熟的海相烃源岩是下刚果盆地深水区油气的重要来源之一;由于上升洋流、缺氧环境(大洋缺氧事件)和古河流的作用,以及海洋、河流两种地质营力此消彼长的关系,自晚白垩世至中新世,盆地沉积环境从海湾变迁到受河流作用逐渐加强的开阔海洋,有机质来源从以海洋有机质为主过渡到河流携带来的陆源有机质比例加重,直到以陆源有机质为主;海陆二元有机质输入量的相对变化和海洋沉积环境的变迁从根本上决定了海相烃源岩的特征。
Abstract:
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参考文献/References:

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备注/Memo

备注/Memo:
收稿日期:2014-06-10
基金项目:国家科技重大专项项目(2011ZX05030-001)
作者简介:曹军(1983-),男,重庆市人,理学博士研究生,E-mail:277847115@qq.com。
通讯作者:钟宁宁(1960-),男,广东佛冈人,教授,博士研究生导师,理学博士,E-mail:nnzhongxp@cup.edu.cn。
更新日期/Last Update: 2014-12-16