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《ACTA SEDIMENTOLOGICA SINICA》 1998-01
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Study of Salinity Evolution of Geofluids during Syngenesis and Diagenesis Using Composition of Carbonate Minerals ──An Example of the Immature Source Rocks of Shasi Member in Dongying Depression

Lu Xiancai; Hu Wenxuan; Fu Qi; Zhang Wenlan; Zhou Guangjia; Hong Zhihua; Chen Zhilin(Department of Earth Sciences, Naming University, Nanjing 210093)(State Key Lab of Metallogenic Mechanism, Nanjing University 210093)(Institute of Geological Science, Sheu  
Sedimentational/syngenetic (SS),diagenetic (DG) and post-diagenetic (PD) carbonate minerals in the immature oil source rocks of the upper part of the Shasi member in Dongying Depression were identified under microscope and analyzed by EPMA (electronic probe micro-analysis). Three composition change patterns were proposed as follows: (1)The Mg/Ca atomic ratio deceases from 0. 9 in the SS carbonate to 0. 01 in the DG one; (2)the Mg/Ca ratio keeps high values in the SS and DG ones, but it becomes very low in the PS ones; and (3 ) the ratio increase largely from the SS carbonate to the DG ones. According to the relationship between salinity of pore-fluids and the Mg/Ca ratio of carbonates,the above patterns were considered as the result of different environmental evolution histories from the SS to DG,then to PS Stages. The salinity of diagenetic pore-fluid was. proved very high in the center of the depression,which was believed to have been favorable to the generation of immature oil in the area. In addition,the research methods in this paper might be useful for similar studies in other areas.
【Fund】: 中国石油天然气总公司“九五”攻关项目
【CateGory Index】: P585.3
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