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鄂西渝东中-新生代构造-热演化及烃源岩生烃预测; Tectonothermal Evolution of Meso-Cenozoic and predicition of hydrocarbon generation potential in Western Hubei-Eastern Chongqing Area
石红才
Subtype硕士
Thesis Advisor施小斌
2011
Degree Discipline海洋地质
Keyword鄂西渝东 裂变径迹 U-th)/he 构造-热演化 烃源岩
Abstract本文利用磷灰石裂变径迹、磷灰石与锆石(U-Th)/He及镜质体反射率Ro等古温标方法相互制约,估算了鄂西渝东地区主要不整合面剥蚀厚度、恢复其沉积埋藏史,在此基础上联合反演了鄂西渝东地区热演化历史,且详细讨论了鄂西渝东自晚侏罗世以来构造-热演化历程,为约束鄂西渝东褶皱带变形时代提供低温热年代学证据,最后分析了研究区烃源岩成熟度历史及生烃预测,其研究结果如下:
Subject Area构造地质与地热学
Funding Project企、事业单位委托项目
Document Type学位论文
Identifierhttp://ir.scsio.ac.cn/handle/344004/14154
Collection学位论文(硕士)
Affiliation施小斌
Recommended Citation
GB/T 7714
石红才. 鄂西渝东中-新生代构造-热演化及烃源岩生烃预测, Tectonothermal Evolution of Meso-Cenozoic and predicition of hydrocarbon generation potential in Western Hubei-Eastern Chongqing Area[D],2011.
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