LITHOLOGIC RESERVOIRS ›› 2015, Vol. 27 ›› Issue (5): 81-86.doi: 10.3969/j.issn.1673-8926.2015.05.013

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Sedimentary model of braided river delta of the Jurassic in Heshituoluogai Basin

Wang Yue1， Chen Shiyue1， Liang Huiyuan2， Deng Yuan1   

  1.  1. School of Geosciences ， China University of Petroleum ， Qingdao 266580 ， Shandong ， China ；2. Sinopec Shengli Oilfield Company ， Dongying 257015 ， Shandong ， China
  • Online:2015-09-26 Published:2015-09-26

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Abstract:

The braided river delta sand body is favorable oil and gas reservoir sand body, and the study of its sedimentary characteristics and sedimentary sequence has important guiding significance for the oil and gas exploration. Based on the field measurement of the braided river delta outcrop of Jurassic Sangonghe Formation in Heshituoluogai Basin, by analyzing the sedimentary characteristics of various microfacies and the types of lithofacies, this paper established sedimentary sequence and sedimentary model of the braided river delta. The results show that progradational braided river delta developed, prodelta, delta front and delta plain of the braided river delta successively developed upwards, which can be subdivided into distal bar, mouth bar, underwater distributary channel, distributary channel and swamp microfacies. Eight types of lithofacies can be identified in the braided river delta, including graded bedding conglomerate facies, lag conglomerate facies, less obvious parallel bedding conglomerate facies, parallel bedding sandstone facies, massive sandstone facies, horizontal bedding siltstone facies, horizontal bedding mudstone facies and horizontal bedding carbonaceous mudstone facies. During the sedimentary period of Sangonghe Formation, the sediment accumulation rate is greater than the basin subsidence rate, and braided river delta fan advanced towards the basin direction and superimposed on the distal side, showing coarsening upwards sedimentary characteristics.

Key words: conjugate fault, strike-slip fault, flower-like structure, paleogeomorphology, sedimentary model, Shabei structural zone, western Bohai Sea

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