云南景谷盆地中新统生油条件分析

留言板

尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

姓名

邮箱

手机号码

标题

留言内容

验证码

基金项目: 国家自然科学基金(编号49572169);滇黔桂石油勘探局资助项目

ANALYSIS ON THE HYDROCARBON-GENERATION CONDITIONS OF THE MIOCENE IN THE JINGGU BASIN, YUNNAN

1.
Department of Petroleum, Chengdu College of Technology, Chengdu 610059, China
2. Dianqiangui Bureau of Petroleum Exploration, Kunming 650200, China

摘要: 本文通过系统的有机地化研究后认为:下中新统三号沟组暗色泥质岩系是盆地重要的烃源层,中-上中新统回环组暗色泥质岩系是潜在的烃源层。中新世良好的古气候条件和还原的沉积水介质环境有利于中新统生油岩系的发育。
- 古环境 /
- 古气候 /
- 烃源岩
Abstract: Based on systematic organic geochemical research,it is considered that the dark argillite series in the Lower Miocene Sanhaogou Formation is the important hydrocarbon source layer of the basin,the dark argillite series in the Middle-Upper Miocene Huihuan Formation is the potential hydrocarbon source layer.The good paleoclimate conditions and the reducing water medium environment for sedimentation in the Miocene are favorable for the development of the Miocene hydrocarbon source rock series.
- paleoenvironment /
- paleoclimate /
- hydrocarbon source rock

[1]	宁建国,等.古地理、古气候与烃源岩[J].石油学报,1993,14(1):51～53.
[2]	周铁明.云南景谷盆地晚第三纪地层[J].石油学报,1992,13(2):159～164.
[3]	王铁冠,等.生物标志物地球化学研究[M].北京:中国地质大学出版社,1990.55～65.