川中古隆起的形成、发展及其油气远景

THE FORMATION AND DEVELOPMENT OF PALEO-UPLIFT IN CENTRAL SICHUAN AND ITS OIL/GAS PROSPECT

康义昌

Kang Yichang

地质矿产部西南石油地质局

Southwest Bureau of Petroleum Geology, Ministry of Geology and Mineral Resources

本文根据最新的钻井、高精度区域地震大剖面及区域地质资料,分析和研究了川中鼻状古隆起在各历史阶段的发展及特点。研究表明,读古隆起具有五套含有机质丰度达2Mt/km2的层系,主要气源岩为下古生界海相层系,占总资源量的5/8,在油气形成的高峰期(印支期)时区域封闭情况良好,在四川运动中没有遭受破坏,另外,该隆起的不同构造部位具有各类可能的储藏类型。并预测其比较含油气远景。

In this paber,the recent data from wells, regional seismic profile and regional geology have been integrated and it is concluded that the Paleo-uplift is developed through-out geological history. This nose form paleo-uplift is a structural erosion uplift with Ew trend formed during Caledo-nian movement and subsequent Devonian-Carboniferous uplifting. Thereafter, it turned to near NEE trend during Indosinian time and continued to the time of Yanshanian and Xishanian. There are plenty of gas source rocks in the uplift area and there are five sequences where the abundance of organic carbon is computed to be 2 Mt/Km2, mainly attributed to Lower Paleozoic and Tengyin Formation(Zn),and some to Permian systems.Based on the resource prediction,the resources of Lower Paleozoic marine facies sequences are of 72 percent of the total resources in the area. The regional sealing condition is excellent for the Paleo-uplift and its top erosional fault plane during the peak stage of oil/gas generation in Indosinian time without any influence of Sichuan movement. The traps in the area can be divided into four types: the reservoir related to deposition, the traps related to the control of paleo-erosional plane, gas pool formed in early stage influenced by regional paleo-uplifting and paleo-structure, and various traps formed in late stage of folding and fanlting. Finally, the possible reservoir types and their oil/gas prospects are made for different locations of the paleo-uplift.

https://doi.org/10.11781/sysydz198801012