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Two stages of subsidence and its formation mechanisms in Mid-Late Triassic Ordos Basin,NW China

Petroleum Exploration and Development 2024年第3期51卷 576-588页

作者： DENG Xiuqin CHU Meijuan WANG Long CHEN Xiu WANG Yanxin National Engineering Laboratory for Exploration and Development of Low-Permeability Oil&Gas Fields Xi’an 710018China Exploration division of PetroChina changqing Oilfield Company Xi’an 710018China Exploration&Development Research Institute of PetroChina changqing Oilfield Company Xi’an 710018China

Based on a large number of newly added deep well data in recent years,the subsidence of the Ordos Basin in the Mid-Late Triassic is systematically studied,and it is proposed that the Ordos Basin experienced two important subsidence events during this depositional *** contrastive analysis of the two stages of tectonic subsidence,including stratigraphic characteristics,lithology combination,location of catchment area and sedimentary evolution,it is proposed that both of them are responses to the Indosinian Qinling tectonic activity on the edge of the craton *** early subsidence occurred in the chang 10 member was featured by high amplitude,large debris supply and fast deposition rate,with coarse debris filling and rapid subsidence accompanied by rapid accumulation,resulting in strata thickness increasing from northeast to southwest in *** subsidence center was located in Huanxian–Zhenyuan–Qingyang–Zhengning areas of southwestern basin with the strata thickness of 800–1300 *** subsidence center deviating from the depocenter developed multiple catchment areas,until then,unified lake basin has not been formed *** the combined action of subsidence and Carnian heavy rainfall event during the deposition period of chang 7 member,a large deep-water depression was formed with slow deposition rate,and the subsidence center coincided with the depocenter basically in the Mahuangshan–Huachi–Huangling *** deep-water sediments were 120–320 m thick in the subsidence center,characterized by fine *** are differences in the mechanism between the two stages of *** early one was the response to the northward subduction of the MianLüe Ocean and intense depression under compression in Qinling during *** later subsidence is controlled by the weak extensional tectonic environment of the post-collision stage during Late Triassic.

关键词： Ordos Basin chang 10 member chang 7 member subsidence center depocenter subsidence mechanism Qinling orogenic belt Indosinian movement

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