Features and Controlling Factors of Epigenic Karstification of the Ordovician Carbonates in Akekule Arch,Tarim Basin  

作　　者：陈强路 赵永强 李国蓉 储呈林 王斌 

机构地区：[1]Wuxi Research Institute of Petroleum Geology,SINOPEC [2]State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation,Chengdu University of Technology

出　　处：《Journal of Earth Science》2012年第4期506-515,共10页地球科学学刊（英文版）

基　　金：supported by the Scientific Research Project of SINOPEC Scientific Development Department (No. P08062)

摘　　要：ABSTRACT： Tabei （塔北） uplift is an area with the highest hydrocarbon enrichment in Tarim basin, and large oilfields have been found on Akekule （阿克库勒） arch at the middle section of Tabei uplift, with Ordovician carbonate reservoirs. Storage space of the Ordovician carbonate reservoirs in the Akekule arch are mainly caves, pores and fractures resulted from dissolution and/or karstification. The Ordovician carbonate reservoirs are affected and modified by the diagenetie process in penecontemporaneous, epigenetic and burial periods and the multi-stage karstification related with deep hydrothermal activities, among which the most significant effect is from the meteoric water karstification related to the tectonic uplift from the end of Middle Ordovician to the end of Late Ordovician （end of O2-end of 03） and at the end of Middle Devonian （end of D2）. Varied palacogeologic settings and tectonic features at different geologic periods lead to different fluid flowing patterns, karstification mechanisms and transformation features in different regions, which further influence the reservoir distribution. The paleo-uplifts at different periods, such as end of O2-end of 03 and end of D2, control the dominant development zones of karstification; the paleogeomorphology and faults resulted from tectonic uplift control the flowing depth of the karst fluid; and the lithology controls the position and extent of karst development.ABSTRACT： Tabei （塔北） uplift is an area with the highest hydrocarbon enrichment in Tarim basin, and large oilfields have been found on Akekule （阿克库勒） arch at the middle section of Tabei uplift, with Ordovician carbonate reservoirs. Storage space of the Ordovician carbonate reservoirs in the Akekule arch are mainly caves, pores and fractures resulted from dissolution and/or karstification. The Ordovician carbonate reservoirs are affected and modified by the diagenetie process in penecontemporaneous, epigenetic and burial periods and the multi-stage karstification related with deep hydrothermal activities, among which the most significant effect is from the meteoric water karstification related to the tectonic uplift from the end of Middle Ordovician to the end of Late Ordovician （end of O2-end of 03） and at the end of Middle Devonian （end of D2）. Varied palacogeologic settings and tectonic features at different geologic periods lead to different fluid flowing patterns, karstification mechanisms and transformation features in different regions, which further influence the reservoir distribution. The paleo-uplifts at different periods, such as end of O2-end of 03 and end of D2, control the dominant development zones of karstification; the paleogeomorphology and faults resulted from tectonic uplift control the flowing depth of the karst fluid; and the lithology controls the position and extent of karst development.

关 键 词：epigenic karstification carbonate rock ORDOVICIAN controlling factor Akekule arch Tarim basin. 

分 类 号：P618.13[天文地球—矿床学]