摘要
在分析了广西大厂矿田巴力—龙头山生物礁古油气藏的构造背景和特征后 ,提出了该生物礁古油气藏的成因与泥盆纪海底热液活动密切相关、其破坏作用则归结于印支—燕山期的构造
Based on the analyses of the tectonic background and characteristics, the origin and evolution of the ancient oil and gas accumulation in Bali—Longtoushan organic reef in Dachang ore field is studied in this paper. A new model is proposed in which the ancient oil and gas accumulation in Bali—Longtoushan organic reef in Dachang ore field is considered to be related to the devonian submarine hydrothermal process and its destruction is due to tectonic-magmatic intrusion in Indosinian-Yanshan period.
出处
《同济大学学报（自然科学版）》
EI
CAS
CSCD
北大核心
1999年第1期92-95,共4页
Journal of Tongji University:Natural Science
基金
同济大学跨学科青年科学基金
关键词
生物礁古油气藏
热液活动
大厂矿田
矿床
Ancient oil and gas accumulation in organic reef
Hydrothermal process
Dachang ore field
