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《Journal of Chengde Petroleum College》 2012-01
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Relationship Between Order Degree of Dolomite and Parasequence——Majiagou Formation of Ordovician in Ordos Basin

ZHANG Zhong-xin1,2,WANG Qi-zong2,WANG Nai-jun2,HU Li-zhong2,YANG Xin3(1.Yumen Oilfield Company,PetroChina,Jiuquan 735019,Gansu,China; 2.School of Oil and Gas,Xi'an Shiyou University,Xi'an 710065,Shaanxi,China; 3.Shaanxi Yanchang Petroleum Limited Liability,Yan'an 717111,Shaanxi,China)  
Applying the sequence stratigraphy theory establishes the sequence stratus frame of parasequence controls dolomitization.This paper references the data records of geochemistry and thin section analysis to discuss the relationship of the carbon and oxygen isotopes,the order degree of dolomite,and the porosity and permeability in the Ordovician Majiagou Group parasequence.The research indicates that in the research area,the rocks located on the top of the parasequence and formatted later are affected by the later rainfall,exposure and dissolution,so the order degree of dolomite is higher than the dolomite located in the bottom and firstly formed.This relationship has very good corresponding relation with the porosity in the research area;the order degree of dolomite on the top of sequence is generally higher;and the porosity of corresponding dolomite is higher too.Parasequence strongly controls the order degree of dolomite,and the relationship existed generally in the region.
【Fund】: 国家重大专项专题(大型油气田及煤层气开发):2008ZX05005-004-008HZ
【CateGory Index】: P618.13
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