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云南陆良盆地第三系含气系统基本过程研究
引用本文:刘树根,戴苏兰,赵永胜,赵泽江.云南陆良盆地第三系含气系统基本过程研究[J].成都理工大学学报(自然科学版),1999(2):135-141.
作者姓名:刘树根  戴苏兰  赵永胜  赵泽江
作者单位:1. 成都理工学院"油气藏地质及开发工程"国家重点实验室,成都,610059
2. 西南石油地质局勘探开发研究院
摘    要:陆良盆地是云南第三系沉积盆地的典型代表。盆地的形成过程决定了第三系含气系统的形成过程。盆地第三系有一个含气系统,即N2c2-N2c3(!)含气系统。上第三系茨营组二段(N2c2)为主力烃源岩,三段(N2c3)为优势储集岩,而N2c4为区域盖层。N2c2-N2c3(!)含气系统的关键时期是距今1.64Ma,圈闭形成于N2c1-N2c4,油气生成-运移-聚集发生在N2c2至今。

关 键 词:含(油)气系统  盆地形成过程  陆良盆地

STUDY ON THE FORMATION OF NEOGENE GAS SYSTEM IN LULIANG BASIN, YUNNAN PROVINCE
Liu Shugen,Dai Sulan,Zhao Yongsheng,Zhao Zejiang.STUDY ON THE FORMATION OF NEOGENE GAS SYSTEM IN LULIANG BASIN, YUNNAN PROVINCE[J].Journal of Chengdu University of Technology: Sci & Technol Ed,1999(2):135-141.
Authors:Liu Shugen  Dai Sulan  Zhao Yongsheng  Zhao Zejiang
Abstract:Luliang Basin is a typical representative of the Tertiary sedimentary basins in Yunnan Province. The formation of the basin results in the formation of the gas system in the basin. There is a gas system in the basin, i.e. the N 2 c 2 - N 2 c 3 gas system. The Second Member of the Neogene Ciying Formation (N 2 c 2) is the main source rock, the Third Member of the Neogene Ciying Formation (N 2 c 3) is the main reservoir rock, and the Forth Member of the Neogene Ciying Formation ( N 2 c 4) is the main cap rock. The critical time of the gas system is about 1.64 Ma. The traps in the basin formed during N 2 c 1 - N 2 c 4. The generation migration accumulation of the gas has occurred from N 2 c 1 to today.
Keywords:gas (petroleum) system  formation and evolution of basin  Luliang Basin  
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