SIGNIFICANCE AND CURRENT SITUATION OF STUDY ON FLUIDIZATION AND MINERALIZATION UNDER INTRACONTINENTAL COLLISION REGIME
Received date: 1994-05-16
Revised date: 1994-10-10
Online published: 1995-08-01
Since1980s, both intracontinental collision and fluidization have become the forward research fields. The upsurge and progress in these two research fields must lead to a great improvement in study of metallogenesis. Therefore, comprehensive study of collision, fluidization and mineralization will be taken on the forward trends of sciences; and it is also a most important way to trace or get ahead of the international progress in Earth sciences. Intracontinental collision orogenic belts are most universal and most complex in China, which provides unique conditions for Chinese geologists to take researching work and to get ahead knowledge on subjects related to collision orogenesis.
Reviews of the current research stage of intracontinental collision, fluidization and mineralization shows that comprehensive study of these three fields is still absent. And the absence will forbid further insighting inrelated problems. But it provides a rare chance for Chinese scientists to study and to obtain forward understanding in the research direction. Therefore, the authors appeal to initiate studying in the direction as soon as possible.
Key words： Intracontinental collision; Fluidization; Mineralization.
ChenYanjing,Yu Fang,Wei Yiying,Gao Xiouli,Chang Zhaoshan,Song Xinyu . SIGNIFICANCE AND CURRENT SITUATION OF STUDY ON FLUIDIZATION AND MINERALIZATION UNDER INTRACONTINENTAL COLLISION REGIME[J]. Advances in Earth Science, 1995 , 10(4) : 318 -322 . DOI: 10.11867/j.issn.1001-8166.1995.04.0318
[1] 陈衍景，邓健，张福勤，杨秋剑.板块理论是现代地质学的基本理论.第四届矿物岩石地质地球化学学术会议论文集.北京:地震出版社，1992.64-65.
[2] Sillitoe R H.A plate tectonic model for the origin of porphyry copper deposits. Economic Geology，1972，67:184-197.
[3] 李晓波.造山带结构、过程和动力学.当代地质科学前沿.武汉:中国地质大学出版社，1993.26-39.
[4] 李晓波.成矿作用与地球动力学.当代地质科学前沿.武汉:中国地质大学出版社，1993.49-54.
[5] 贾跃明.地壳中的流体作用.当代地质科学前沿.武汉:中国地质大学出版社，1993.54-66.
[6] 涂光炽.矿床地球化学的薄弱环节.全国第四届矿物岩石地球化学会议论文集.北京:地震出版社，1991.45-46.
[7] 张知非，郭亚曦，应思淮.到2000年的地球科学的前沿:英国的研究重点.地质科学的机会与挑战.地质矿产信息研究院，1991.165-185•
[8] Kharaka Y K and Maest A S(editors).Water-Rock Interaction.Balerma:Rotterdam，1992.1-1632.
[9] 马福臣，田兴有，刘长春，应思淮.地质科学基础研究稳定发展的几个关系.地球科学进展，1992，7(3):97-100.
[10] 陈衍景.中国绿岩带型金矿成矿的地球动力学背景和成矿模式.第五届全国矿床会议论文集.北京:地质出版社，1993.291-292.
[11] Hsu K J.Thin-skinned plate tectonice duringNeo-Alpine orogenesis.American Journal of Science，1979，279:353-366.
[12] Jamieson R A.P-T-t paths of collisional orogenesis.Geologie Rundschau，1991，180:321-332.
[13] 许靖华.中国南方大地构造的几个问题.地质科技情报，1987，(2):13-27.
[14] 胡受奚.华北与华南古板块拼合带地质与成矿.南京大学出版社，1988.558.
[15] 陈衍景，张程宁.西准噶尔地区金矿成矿模式.长春地质学院学报，1991，(1):61-66.
[16] 陈衍景，富士谷.豫西金矿成矿规律.北京:地震出版社，1992.234
[17] Kerrich R and Wyman.Gedynamic setting of mesothermal gold deposits.Geology，1990，18:882-885.
[18] Pfeifer H P and Sanchez A. In:Water-Rock Interaction.Balerma:Rotterdam，1992.1327-1331.
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