BIOGEOCHEMICAL CIRCULATION, PALEOENVIRONMENT AND BIOMINERALIZATION OF THE MESO-CENOZOIC NON-MARINE SEDIMENTARY BASINS IN CHINA
Received date: 1995-05-17
Online published: 1995-10-01
Meso-Cenozoic era is the most prosperous period of living cretures in geohistory, and is also an important period for biogenesis. In those Meso-Cenozoic basins, the sedimentary rocks have systematically preserved the information of the geochemical process performed by the all sorts of living cretures at that time. Therefore, it has an important significance to study the biogeochemical circulation, paleoenvironment and biomineralization occured in the Meso-Cenozoic sedimentary basins.
Key words： Biogeochemical circulation; Paleoenvironment; Biomineralization.
Ye Lianjun, Fan Pu, Ma Baolin, Huang Difan, Cheng Keming . BIOGEOCHEMICAL CIRCULATION, PALEOENVIRONMENT AND BIOMINERALIZATION OF THE MESO-CENOZOIC NON-MARINE SEDIMENTARY BASINS IN CHINA[J]. Advances in Earth Science, 1995 , 10(5) : 427 -431 . DOI: 10.11867/j.issn.1001-8166.1995.05.0427
[1] 叶连俊，李任伟，王东安.生物成矿作用展望——沉积矿床学的新阶段.地球科学进展，1990,(3):1-4.
[2] 叶连俊.中国磷块岩.北京:科学出版社，1989.
[3] Manfred Schidlowski. The initiation of biological processes on earth summary of empirical evidence. In：Organic Geochemistry. Edited by Michael H, Engel and Stepthen A. Macho, Plenum Press, New York. 1993.
[4] IGBP Secretariat. The International Geosphere-Biosphere Programme：A Study of Global Change (The Initial Core Projects). IGBP Report No 12. Sweden.1990.
[5] 范璞，罗斌杰等.中国陆相油气的形成和运移(I )(II).中国科学.1980，(4);(6).
[6] 范璞，张彭喜，马宝林等主编.青海湖近代环境的演化和预测.北京:科学出版社，1994.
[7] 黄第落等主编.中国陆相油气生成.北京:石油工业出版社，1982.
[8] 马宝林等主编.塔里木沉积岩形成演化与油气.北京:科学出版社，1990.
[9] 程克明主编.吐哈盆地油气生成.北京:石油工业出版社，1994.
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