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《Acta Sedimentologica Sinica》 2005-04
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Analysis of the High Resolution Sequence of Lacuatrine Carbonate

ZHAO Jun-qing1 XIA Bin1 JI You-liang2 JIANG Zai-xing3 ZHANG Shan-wen41 (Laboratory of Marginal Sea Geology,Guangzhou Institute of Geochemistry & South China Sea Institute of Oceanology, Chinese Academy of Sciences,Guangzhou 510640)2(Institute of Earth and Ocean Science,TongjiUniversity,Shanghai 200092) 3(China University Geoscience, Beijing, 100083) 4(Shengli Oil Field Limited Corporation, SINOPEC, Dongying, Shandong 257015)  
In spite of great economic sigificance, very little is known about the lacustrine carbonate rocks both at home and abroad. By the method of applying sequence stratigraphy, this paper particularly analyses the sequence developing model, sequence gradation division and controlling factors on lacustrine carbonate rocks, and put emphasis on parasequence types, distinguishing symbol, forming mechanism and correlation model. As a result, the sequence model of lacustrine carbonate rocks is summed up as steep slope model and gentle slope model. The units of high-resolution sequence are divided into sequence, tract system, parasequence sets, parasequence and microsequence. The parasequnce types are divided into steep slope type, gentle slope type and deep sag type, also divided into limestone-marl,shore,slipping and deep-water evaporate, and the controlling factor of different kinds of parasequence is different. The contrasting models of parasequence are summed up as abruptly changing model of steep slope and gradually changing model of gentle slope, parasequence can regularly charge under different models.
【Fund】: 国家十五科技攻关项目(编号:2001BA60509);; 国家重大基础研究发展规划项目(编号:G1999043304);; 中国科学院知识创新工程重要方向项目(编号:KZCX2-SW-117)联合资助.
【CateGory Index】: P539.2
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