Genesis and development model of glutenite body at the bottom of Qingshuihe Formation, western section of southern Junggar Basin
WANG Ke1,2, ZHOU Yong1,2, WANG Jian3, GAO Chonglong4, LIU Ming3, REN Ying4
1 College of Geosciences,China University of Petroleum(Beijing),Beijing 102249,China; 2 National Key Laboratory of Petroleum Resources and Engineering,China University of Petroleum(Beijing),Beijing 102249,China; 3 Research Institute of Experiment and Detection,Xinjiang Oilfield Company,PetroChina,Xinjiang Karamay 834000,China; 4 Faculty of Petroleum,China University of Petroleum(Beijing)at Karamay,Xinjiang Karamay 834000,China
Abstract：Despite significant breakthroughs in oil and gas exploration in the glutenite section of the Qingshuihe Formation in the southern Junggar Basin,the sedimentary characteristics,genetic mechanism and controlling factors of the glutenite remain unclear,which has become a key restricting factor for hydrocarbon exploration. As such,we investigated the lower Qingshuihe Formation glutenite body in the western section of the southern Junggar Basin based on wireline logs,cores,outcrops and experimental data,with a focus on the lithofacies,lithofacies assemblage and distribution of the glutenite body,as well as their main controlling factors and genetic mechanism. Six types of lithofacies and lithofacies assemblages and genetically different glutenites are identified in the lowstand and transgression systems tracts of the Qingshuihe Formation in the western section of the southern Junggar Basin. The lowstand and transgression systems tracts of the Qingshuihe Formation in the southern Gaoquan area of the western section are dominated by alluvial fan and fan delta depositional systems,and braided river delta depositional system predominates the northern Caindic area. During the depositional period of the Qingshuihe Formation,glutenite sedimentation in the south western section of the Junggar Basin was affected by the nature of the parent rock in the provenance area,sediment supply and paleoclimate. Among them,nature of the parent rock in the provenance area and sediment supply control the sedimentary type and scale of the glutenite body. While paleoclimate affects the weathering and denudation degrees of the parent rock area and the sedimentary transport environment. Based on the controlling factors and sedimentary characteristics,a sedimentary model for the southern alluvial fan-fan delta and the northern braided river delta front of the Qingshuihe Formation lowstand and transgression systems tract in the western section of the southern Junggar Basin has been established,which can provide a geological basis to aid discrimination between different glutenite bodies and hydrocarbon exploration in similar settings.
WANG Ke,ZHOU Yong,WANG Jian et al. Genesis and development model of glutenite body at the bottom of Qingshuihe Formation, western section of southern Junggar Basin[J]. JOPC, 2024, 26(3): 600-619.
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