Microorganisms linked to Neoproterozoic microspar carbonate sedimentation in the Jilin-Liaoning area

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	Microorganisms linked to Neoproterozoic microspar carbonate sedimentation in the Jilin-Liaoning area
	Ge M ; Kuang HW ; Meng XH ; Furniss G
	2004
会议名称	32nd international geological congress on geology of china
会议日期	2004
会议地点	florence, italy
关键词	molar tooth carbonate Neoproterozoic sedimentary environment microorganisms origin PROTEROZOIC BELT SUPERGROUP TOOTH CALCITE STRUCTURES EXPANSION CRACK ORIGIN PURCELL SUPERGROUP WESTERN MONTANA GAS BUBBLE
页码	784-789
通讯作者	ge m chinese acad sci inst semicond basin xueyuan rd beijing 100083 peoples r china. 电子邮箱地址: geming@cugb.edu.cn
中文摘要	molar-tooth carbonate refers to a sort of rock that has ptygmatical folded structure comparable to the ivory. this kind of carbonate exists in a special time range (from middle to neoproterozoic). its origin and the possibility to use it in stratigraphic correlation of the paleocontinent is the key task of the igcp447, a project on proterozoic molar tooth carbonates and the evolution of the earth (2001-2005). the importance lies in that the molar-tooth structure is the key to solving problems related to precambrian biological and global geochemical events. the molar-tooth structure is associated with microorganisms. development and recession of such carbonates have relations with the evolution process of early lives and abrupt changes in sea carbonate geochemistry. in recent years, based on researches on petrology, geochemistry and sr isotope of molar-tooth carbonate in the jilin-liaoning and xuzhou-huaiyang area, the authors hold that it can be used as a marker for stratigraphic sequence and sedimentary facies analyses.
英文摘要	molar-tooth carbonate refers to a sort of rock that has ptygmatical folded structure comparable to the ivory. this kind of carbonate exists in a special time range (from middle to neoproterozoic). its origin and the possibility to use it in stratigraphic correlation of the paleocontinent is the key task of the igcp447, a project on proterozoic molar tooth carbonates and the evolution of the earth (2001-2005). the importance lies in that the molar-tooth structure is the key to solving problems related to precambrian biological and global geochemical events. the molar-tooth structure is associated with microorganisms. development and recession of such carbonates have relations with the evolution process of early lives and abrupt changes in sea carbonate geochemistry. in recent years, based on researches on petrology, geochemistry and sr isotope of molar-tooth carbonate in the jilin-liaoning and xuzhou-huaiyang area, the authors hold that it can be used as a marker for stratigraphic sequence and sedimentary facies analyses.; 于2010-10-29批量导入; made available in dspace on 2010-10-29t06:36:21z (gmt). no. of bitstreams: 1 2780.pdf: 450133 bytes, checksum: 479d7bf29659f27b331c98a1919c4ef5 (md5) previous issue date: 2004; chinese acad sci, inst semicond basin, beijing 100083, peoples r china; yangzi univ, nanjing 210000, jiangsu, peoples r china; univ montana, dept geol, missoula, mt 59812 usa
收录类别	CPCI-S
会议录	acta geologica sinica-english edition, 78 (3)
会议录出版者	geological soc china ; 26 baiwanzhuang, fuwai, beijing 100037, peoples r china
会议录出版地	26 baiwanzhuang, fuwai, beijing 100037, peoples r china
学科主题	半导体器件
语种	英语
ISSN号	1000-9515
内容类型	会议论文
源URL	[http://ir.semi.ac.cn/handle/172111/13591]
专题	半导体研究所_中国科学院半导体研究所（2009年前）
推荐引用方式 GB/T 7714	Ge M,Kuang HW,Meng XH,et al. Microorganisms linked to Neoproterozoic microspar carbonate sedimentation in the Jilin-Liaoning area[C]. 见:32nd international geological congress on geology of china. florence, italy. 2004.