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《Journal of Chengdu University of Technology(Science & Technology Edition)》 2007-03
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Study on diagenesis of the carbonate rocks in the Carboniferous sequence stratigraphic framework of South Guizhou

LIN Xiao-bing1,2,LI Guo-zhong3,TIAN Jing-chun1,2,CHEN Hong-de1,2,KANG Jian-wei2,Xu Sheng-lin21.State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation,Chengdu University of Technology,Chengdu 610059,China;2.Institute of Sedmentary Geology,Chengdu University of Technology,Chengdu 610059,China;3.Special School of Zhengzhou Industry & Trade,Zhengzhou 450007,China  
This paper studies the diagenesis of the Carboniferous carbonate rocks in the sequence stratigraphic framework of South Guizhou and draws the following conclusions.The main diagenesis developed during the LST period is fargoing karstification in the exposed area.The diagenetic environments with respect to TST are mainly marine and mixed-water environments,and the latter will transfer toward to the continent with the sea level continuously rising.During the highstand of sea level(HST), the platform carbonate sediments are subject to the marine(for the earlier period) and meteoric water(for the later period) diagenesis environment,in which rapid marine carbonate cementation and meteoric erosion,cementation and dolomitization will occur respectively.The diagenesis correlative toⅠ-type sequence boundary,with the characteratics of long-time process and high intensity,mainly includes erosion,cementation and dolomitization which can be correlated throughout South Guizhou area.While those diageneses correlative to Ⅱ-type sequence boundary occur relatively at a limited scale and have less ability in rebuilding the carbonate strata.The diageneses correlative to HST and Ⅰ-type sequence boundary can produce thick dolomite and large scale pore space.So they can be considered as the effective geological evidences for predicting favorable reservoirs.
【CateGory Index】: P618.13
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