地质科学2013，Vol.48Issue(1)：149-166,18.DOI:10.3969/j.issn.0563-5020.2013.01.009
哈密坳陷二叠纪—三叠纪原型盆地恢复及沉积中心演化特征
Permian-Triassic prototype basin restoration and depocenter evolution feature in Hami Depression
摘要
Abstract
On the basis of field outcrop, seismic and well data, Permian-Triassic strata erosion thickness of Hami Depression can be calculated by means of balanced section, seismic stratigraphy, horizon comparison , proximity thickness ratio and deposition rate. Accordingly, the Permian-Triassic original formation thickness can be recovered. Consequently the Permian-Triassic prototype basin of Hami Depression can be recovered and its depocenter evolution is also discussed in the paper.关键词
哈密坳陷/二叠纪—三叠纪/剥蚀厚度/原始地层厚度/原型盆地/沉积中心Key words
Hami Depression,Erosion thickness,Original formation thickness,Prototype bisin,Sedimentary evolution分类
天文与地球科学引用本文复制引用
王军..哈密坳陷二叠纪—三叠纪原型盆地恢复及沉积中心演化特征[J].地质科学,2013,48(1):149-166,18.基金项目
国家重点基础研究发展计划"973"项目"中国西部典型叠合盆地油气成藏机制与分布规律"(编号:2006CB202306)资助. （编号:2006CB202306）
