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《Progress in Geophysics》 2011-06
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Well-logging responses and reservoir effects of rhyolite's diagenesises of Yingcheng Formation(K_1y) in the Songliao Basin

QUXue-jiao~1,WANG Pu-jun~(1*),XIU Li-jun~2,TANG Hua-feng~1,GAO You-feng~1 (1.College of Earth Science,Jilin University,Changchun 130061,China; 2.Exploration and Development Research Institute of Jilin Oil field,Songyuan 138000,China)  
Through observation of well core and thin sections and study of well-logging responses,we found that three kinds of diagenesises'well-logging responses are prominently,includes diagenetic albitization of kfeldspars, amygdules and fractures filled with quartz and matrix and/or phanerocrysts alternated by calcite,while denudation and devitrification are associated with other diagenesises in rhyolite.Diagenetic albitization of kfeldspars characterized as Na/K1 in ECS log and the stronger of the alternation the larger of the ratio,and the electrical resistivity is low, logging porosity shows a single peak in histogram.The features of amygdules and fractures filled with quartz includes high density、low logging porosity and low neutron in the cross-plots of DEN versus AC and Pige versus CN,the electrical resistivity toothly nearly to straight and mainly between 40Ω·m and 100Ω·m.Matrix and/or phanerocrysts alternated by calcite indicates the Ca curve smoothly and straightly and diverged the base line obviously,the conventional well-logging responses shows low electrical resistivity,low density,high acoustictime and high logging porosity.As a result of diagenetic albitizalion of kfeldspars,the reservoir quality improved overally, especially for the tight zone,the theoretical maximum increment of porosity is 6.8%,the actual increment of porosity is 0.15%~0.46%.Amygdules and fractures filled with quartz deteriorate the reservoir quality.The reservoir effect of matrix and/or phanerocrysts alternated by calcite mainly determined by the dissolution degree,the porosity theoretically reduced about 46%after amorphous silica in matrix alternated by calcite,the actual reduction of porosity is about 2.3%.
【Fund】: 国家“973”项日(2009CB219305);; 国家自然科学青年基金(41002038)资助;; “东北亚生物演化与环境教育部重点实验室”支持;; 吉林大学“211”工程三期建设项目和2009年教育部基本科研业务经费(“吉林大学创新团队发展计划”)多重支持
【CateGory Index】: P618.13;P631.8
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