HOU Mingcai; TIAN Jingchun; CHEN Hongde; CHEN Xuehua; XIAO Huanqing; QIU Quiqiang and JIA Guanghua
, 2003, 30(1): 385-0.
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In this paper, by examining cores of the Shasan intermediate section (E2s32) of the Niu30 and Niu43 wells in Niuzhuang sag and comprehensively researching their log data, tectonic setting and pore space feature, the authors of the paper think that there are two kinds of turbidite fan-the deep-water turbidite fan and delta front fluxoturbidite. Based on the above study and analysis, authors study in full their reservoir characteristics in respective microfacies type, sedimentation feature, pore genesis and controlling factor. There are four kinds of pore, such as: primary pore, secondary pore, micropore and micro-fissure. Sandbodies of inner fan main channel and middle fan braided stream are better reservoir rocks. Sandbodies of middle fan braided stream front and outer fan are worse reservoir rocks, because their grain size is smaller, mixture content is higher, primary pore is smaller. Compaction, consolidation, dissolution and recrystallization reformed obviously reservoir feature of the turbidities. Of which, compaction, consolidation and clay filling caused porosity and permeability descending, throat chocking, compaction, agglutination and metasomatism improved the reservoir feature. It is concluded that sand body of the Shasan intermediate section belongs to medium reservoir rock, which is characterized by middle to low porosity and low permeability. It is caused by deep burial, early formation times and strong diagenesis in the process of deposition to diagenism evolution.