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《Geotectonica Et Metallogenia》 2004-03
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CONSTRAINTS ON FORMATION TIME OF CO_2 FROM CENOZOIC MAGMATISM IN EASTERN CHINA

WANG Xinmou~(1,2),XIA Bin~1,CHEN Genwen~1,Yang Hanjie~2, CHEN Haiyun~2 and GUO Dong~2 (1.Key Iaboratory of Marginal Sea Geology, Guangzhou Institute of Geochemistry & South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou, GD 510640, China; 2.Shengli Oil Field Ltd., Dongying,SD 257001, China)  
There are four periods of magmatism in Eastern China, they are 65~41 Ma,41~21 Ma,21~13Ma,and 11~1Ma, respectively. The magmatic rocks for the first and second periods erupted within the rift basins. The magmatic rocks for the third and fourth periods occurred on the margins of the basins or along the Tanlu fault belt. The CO_2 derived from magma in Eastern China mainly formed in the pull-apart basins, and are consistent with the magmatic rocks formed during the first and second periods in space. The geochemical data of volcanic rocks from Jiyang depression indicate that magmatic rocks of early Teriary are mainly tholeiitic and calc-alkali. The rocks formed after Es_3 are all alkali rocks. The contents of CO_2 enclosure in volcanic rock from the Shengli Oil Field indicate that the contents of CO_2 in the volcanic rocks from Es_3 are observably higher than those from other rock units, and the CO_2 contents in the enclosures of alkali basalt are markedly higher than those of tholeiite. So the magmatism from Es_3 to Ng is the main period for the formation of CO_2.
【Fund】: 中科院重大知识创新项目 (编号 :KZCX2 -SW 117);; 胜利油田勘探管理项目部资助
【CateGory Index】: P618.13
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