| 中、新生代陆相沉积盆地生物地球化学循环、古环境与成矿 |
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| 引用本文： | 叶连俊,范璞.中、新生代陆相沉积盆地生物地球化学循环、古环境与成矿[J].地球科学进展,1995,10(5):427-431. |
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| 作者姓名： | 叶连俊 范璞 |
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| 作者单位： | 中国科学院地质研究所，中国科学院兰州地质研究所，中国石油天然气总公司石油勘探开发研究院 |
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| 摘 要： | 中新生代是地史上生物最为繁茂多样大发展和生物成矿的重要时期，陆相沉积盆地沉积岩中最为系统地保存了各种生物地化作用和过程的信息。研究中新生代陆相沉积的生物地球化学循环、古环境及成矿具有重要的意义，提出了开展该项研究的一些主要内容。
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| 关 键 词： | 生物地球化学 古环境 生物成矿 沉积盆地 |
BIOGEOCHEMICAL CIRCULATION,PALEOENVIRONMENT AND BIOMINERALIZATION OF THE MESO-CENOZOIC NON-MARINE SEDIMENTARY BASINS IN CHINA |
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| Ye Lianjun.BIOGEOCHEMICAL CIRCULATION,PALEOENVIRONMENT AND BIOMINERALIZATION OF THE MESO-CENOZOIC NON-MARINE SEDIMENTARY BASINS IN CHINA[J].Advance in Earth Sciences,1995,10(5):427-431. |
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| Authors: | Ye Lianjun |
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| Institution: | 1.Institute of Geology, Chinese Academy of Sciences, Beijing 100029;2.Lanzhou Institute of Geology, Chinese Academy of Sciences, Lanzhou 730000;3.Research Institute of Petroleum Exploration and Development, Beijing 100083 |
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| Abstract: | Meso-Cenozoic era is the most prosperous period of living cretures in geohistory,andis also an important period for biogenesis,In those Meso-Cenozoic basins,the sedimentaryrocks have systematically preserved the information of the geochemical process performedby the all sorts of living cretures at that time. Therefore,it has an important significanceto study the biogeochemical circulation,paleoenvironment and biomineralization occured inthe Meso-Cenozoic sedimentary basins. |
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| Keywords: | Biogeochelnical circulation Paleoenvironment Biomineralization |
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