东濮凹陷盐岩形成环境

THE DEPOSITIONAL ENVIRONMENT OF SALT ROCKS IN DONGPU DEPRESSION

顾家裕

Gu Jiayu

石油工业部石油勘探开发科学研究院

Research Institute of Petroleum Exploration and Development, Ministry of Petroleum Industry

东濮凹陷随着大量油气资源的发现,对凹陷内巨厚盐层的成因及盐的来源已引起广大地质工作者的极大兴趣和关注,笔者仅就凹陷中成盐环境作尝试性的探讨,不妥之处请批评指教。

Dongpu Depression is asecond graded structure unit in Pohai Gulf Basin with thick formation of salt-sediments interbedded with dark mudstones developed during Paleogene. In this paper, the rhyme, cycle, structure and ecological properties of contained fossils in the depression are discussed and the author suggests that the salt rocks were generated in a depositional environment of still-stand deepwater and probably experienced sea water immersions in a short period expect for the salt rocks derived from surface flows. The various haloclines formed in saline lakes caused multiple dissolutions and crystal sedimentations of halogen rocks foming the saline deposits. Based on macroscopic viewpoint, the saline deposit is controlled by the highland bailt up with the marginal deep faults and is a typical example of "high mountain-deep basin" saline model.

https://doi.org/10.11781/sysydz198601022