INFLUENCES OF MARINE FLOOR HYDROTHERMAL ACTIVITY ON ORGANIC MATTER ABUNDANCE IN MARINE CARBONATE ROCKS——A CASE STUDY OF MIDDLE-UPPER PROTEROZOIC IN THE NORTHERN PART OF NORTH CHINA  

作　　者：WANG Jie CHEN Jianfa BAO Zhidong ZHANG Shuichang XU Yongchang WANG Darui 

机构地区：[1]Wuxi Institute of Oil Geology, Sinopec, Wuxi 214151, China [2]Geoscience Department of Zhejiang University, Hangzhou 310028, China [3]Geochemistry Department of Yangtze University, Jingzhou 434023, China [4]Chinese University of Petroleum, Beijing 102249, China [5]Research Institute of Petroleum Exploration and Development, Petro China, Beijing 100083, China [6]Lanzhou Institute of Geology, Chinese Academy of Sciences, Lanzhou 730000, China

出　　处：《Chinese Science Bulletin》2006年第5期585-593,共9页

摘　　要：Study indicates that the elements rich in marine floor hydrothermal fluids have a positive in- fluence, not only on total organic carbon (TOC), but also on the abundance of SiO2 in some Middle-Upper Proterozoic strata. The TOC bears a better positive correlation with abundance of SiO2. By the correlation analysis between organic matter and sea-floor hot fluid characterized trace elements such as P, Cu, Zn, Ni, Ba, etc in marine carbonate rocks, we conclude that organic matter enrichment of carbonate rocks were related to marine floor hydrothermal activity in a part of layers. Some thin-layered cherts, which were thought to be the indicators of hydrothermal activity, frequently occurring in Gaoyuzhuang, Wumishan, Tieling and Xiamaling formation support our conclu- sion. With the increasing of trace elements in marine carbonate rocks, the TOC and Fe/Ti ratio is creasing. In contrast, the Al/(Al+Fe+Mn) ratio is usually de- creasing.Study indicates that the elements rich in marine floor hydrothermal fluids have a positive influence, not only on total organic carbon （TOC）, but also on the abundance of SiO2 in some Middle-Upper Proterozoic strata. The TOC bears a better positive correlation with abundance of SiO2. By the correlation analysis between organic matter and sea-floor hot fluid characterized trace elements such as P, Cu, Zn, Ni, Ba, etc in marine carbonate rocks, we conclude that organic matter enrichment of carbonate rocks were related to marine floor hydrothermal activity in a part of layers. Some thin-layered cherts, which were thought to De the indicators of hydrothermal activity, frequently occurring in Gaoyuzhuang, Wumishan, Tieling and Xiamaling formation support our conclusion. With the increasing of trace elements in marine carbonate rocks, the TOC and Fe/Ti ratio is creasing. In contrast, the Al/（Al＋Fe＋Mn） ratio is usually decreasing.

关 键 词：华北北部 元古代 碳酸盐岩 有机物质 海底热流体 主要元素 微量元素 

分 类 号：P534.3[天文地球—古生物学与地层学]