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Development model of sedimentary system and reservoir under valley-monadnock paleotopography during buried stage of paleouplift:Case study of 1st member of K1q  in Shinan area,hinterland of Junggar Basin

Gao Chong-long,Ji You-liang,Jin Jun,Wang Jian,Ren Ying,Zeng Li,Wang Dao-wei,Zhang Hao,Li Jin-jie   

  1. 1.College of Geosciences,China University of Petroleum (Beijing),Beijing 102249,China;
    2.State Key Laboratory of Petroleum Resource and Prospecting,China University of Petroleum (Beijing),Beijing 102249,China;
    3.Research Institute of Experiment and Detection of PetroChina Xinjiang Oilfield Company,Karamay 834000,China;
    4.Northeast Gas Plant of Sinopec Southwest Oil and Gas Company,Langzhong 637400,China;
    5.CNOOC Ener Tech-Drilling & Prodction Co.,Tianjin 300450,China;
    6.Well Logging Company,Daqing Oil Drilling Engineering Company,Daqing 163412,China
  • Received:2018-03-12 Revised:2018-06-27 Online:2018-08-10 Published:2018-08-10

Abstract: Lower Cretaceous Qingshuihe Formation (K1q) within hinterland area of Junggar Basin is a distinctive sedimentary sequence developed during the buried stage of large-scale Chemo paleouplift.In addition to Jurassic and Triassic,K1q  becomes another favorable target for hydrocarbon exploration within the basin.However,the geomorphic evolution during the buried stage of paleouplift is not fully taken into account in previous researches about sedimentary system and reservoir types of K1q,leading to the restriction of effective hydrocarbon exploration and development.Thus,using core,logging,3-D seismic data,field outcrop and assay data,this research rebuilds palaeogeomorphology of the study area based on the sequence stratigraphic classification and illustrates the sedimentary facies and distribution of depositional systems.Meanwhile,in combination with previous research results,the evolutionary model of paleogeomorphy and sedimentary system during the buried stage of paleouplift is established and its control on reservoir types is analyzed.The results show that:K1q is a whole third order sedimentary sequence,and 1st member of K1q  can be classified into LST and TST,while 2nd member of K1q is HST.Controlled by the distinctive valley-monadnockpalaeogeomorphology,LST gravelly braided rivers were confined within the valleys,moreover,slump debris flow deposits could occur around the edges of monadnocks.During the early period of TST,sedimentary system changed into shallow-water braided delta front in study area,however,shallow to semi-deep lacustrine covered the whole area in late period.Regionally,the paleouplift existed as an intrabasinal source area during the Late Jurassic due to the continuous and differential dynamics of weathering and river incision,and gradually turned into different scales of valleys and monadnocks.Whereas the intrabasinal source system of paleouplift disappeared since Early Cretaceous.During the deposition period of K1q,the paleouplift zone gradually buried and the peneplanation processes of palaeogeomorphology along with subsidence eventually turned the hinterland area into depocenter of the basin.Controlled by the valley-monadnockpalaeogeomorphology,reservoir types within the paleouplift area can be classified into monadnock reservoirs of Jurassic and stratigraphic overlap and structural reservoirs of K1q.

Key words: Chemo paleouplift, Palaeogeomorphology evolution, Depositional system, Hydrocarbon distribution, Qingshuihe Formation, Junggar Basin

CLC Number: 

  • TE121.3

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