Types,characteristics and geological significance of event deposits of Chang 9 Member of Triassic Yanchang Formation in southwestern Ordos Basin,NW China  

作　　者：WANG Ziye MAO Zhiguo YUAN Xuanjun DENG Xiuqin HUI Xiao ZHANG Zhongyi CUI Jingweil 

机构地区：[1]PetroChina Research Institute of Petroleum Exploration&Development,Beijing 100083,China [2]National Energy Tight Oil&Gas Research&Development Center,Beijing 100083,China [3]Key Laboratory of Oil and Gas Reservoir,CNPC,Beijing 100083,China [4]Research Institute of Exploration and Development,PetroChina Changqing Oilfield Company,Xi'an 710018,China

出　　处：《Petroleum Exploration and Development》2023年第3期588-602,共15页石油勘探与开发（英文版）

基　　金：Supported by the PetroChina Scientific Research and Technological Development Project(2021DJ0402).

摘　　要：Through core observation,thin section identification,and logging and testing data analysis,the types and characteristics of event deposits in the ninth member of Yanchang Formation of Triassic(Chang 9 Member)in southwestern Ordos Basin,China,are examined.There are 4 types and 9 subtypes of event deposits,i.e.earthquake,gravity flow,volcanic and anoxic deposits,in the Chang 9 Member in the study area.Based on the analysis of the characteristics and distribution of such events deposits,it is proposed that the event deposits are generally symbiotic or associated,with intrinsic genetic relations and distribution laws.Five kinds of sedimentary microfacies with relatively developed event deposits are identified,and the genetic model of event deposits is discussed.Seismites are mainly developed in the lake transgression stage when the basin expands episodically,and commonly affected by liquefaction flow,gravity action and brittle shear deformation.Gravity flow,mainly distributed in the high water level period,sandwiched in the fine-grained sediments of prodelta or semi-deep lake,or creates banded or lobate slump turbidite fan.It is relatively developed above the seismites strata.The volcanic event deposits are only seen in the lower part of the Chang 9 Member,showing abrupt contact at the top and bottom,which reflects the volcanic activity at the same time.Anoxic deposits are mostly formed in the late stage of lake transgression to the highstand stage.Very thick organic-rich shales are developed in the highstand stage of Chang 9 Member,and the event deposits in the depositional period of these shales are conducive to potential reservoirs.

关 键 词：event deposit SEISMITE gravity flow anoxic event Triassic Yanchang Formation Ordos Basin 

分 类 号：P618.13[天文地球—矿床学]