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《Journal of Chengdu University of Technology(Science & Technology Edition)》 2005-03
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Study on reservoir characteristics of the Late Paleozoic reef in Youjiang basin, China

HOU Ming-cai, CHEN Hong-de, TIAN Jing-chunState Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu 610059, China  
Two stages of reef growth are recognized in Devonian, Middle and Late Permian in Youjiang basin, respectively. Reefs are widespread and exposed in west Guangxi, south Guangxi, south Guizhou, middle Guangxi, east Yunnan, and have ever been distributed along platform margins or on isolated platform. Micrograph and scanning electronic microscope show that reservoir space is of pore, fissure and solution hollow in reefal limestone. The interstice types are distinguished as intragranular corroded hollow, frame pore, intergranular pore, corroded hollow, corroded hollow associated with stylolite and micropore in matrix. Intercrystalline pore, intercrystalline corroded hollow, and corroded pore, hollow fissure, controlled by non-fabric are the main types. It is suggested that the reservoir type can be classified as fissure-pore type and pore type, and the reservoir thickenss ranges from 5 to 55 m. Reservoir rocks are dominated by either boundstone or bioclastic limestone, or biolclastic dolomicrite, or cryptalline dolomite. For the later two dolomites, textures are often diagenetically altered.
【Fund】: 四川省重点学科“构造地质学”建设基金资助项目(SZD0408)
【CateGory Index】: P618.13
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