地球科学进展 ›› 1993, Vol. 8 ›› Issue (2): 40 -46. doi: 10.11867/j.issn.1001-8166.1993.02.0040

学术研究动态 上一篇    下一篇

热水喷流沉积成矿与地学思维
  1. 中国科学院地球化学研究所; 中国科学院地球化学研究所 贵阳
  • 收稿日期:1992-04-18 修回日期:1992-08-05 出版日期:1993-03-01

ORE—FORMATION OF HYDROTHERMAL EXHALATIVE SEDIMENTATION AND GEOLOGICAL THINKING

Yan Wen, Li Chaoyang   

  1. Institute of Geochemistry; Academia Sinica; Guiyang; 550002
  • Received:1992-04-18 Revised:1992-08-05 Online:1993-03-01 Published:1993-03-01

热水喷流沉积成矿是一个新的成矿思想,它弥合了地史中许多重要矿床在成因上长期存在的意见分歧。本文分析并论述了这一成矿思想的王要内容及贯穿于其产生和发展这程中的基本思维特征和思维方法,从哲学的角度概括了这一成矿思想的科学意义。

Hydrothermal exhalative sedimentation is a new thought which has healed the long divergence of genesis for many important deposits. This paper deals with the main contents of this matalligentic theory and the basic thinking way passing through the process of its development, by which the scientific significance is generalized in the sense of philosophy.

[1]A Maucher. In handbook of stratabound and stratiform ore deposotes.Edited by K H wolf.1976,7,477-504
[2]Hutchinson R W.Volcanogenic sulfide deposites and their metallogenic significance.Econ Geol.1973,68,1223-1246
[3]F J Sawkins.Massive sulfide deposits in relation to geotectonics.Geo Assoc Canada Ann Mtg(St John's) Abs.1974,8
[4]M Solomon.Volcanic massive sulfide deposits and their host rocks-a review and explanation.in handbook of stratabound and stratiform ore deposits.Edited by K H wolf.6,1976,21-55
[5]芮宗瑶.海底喷气沉积矿床研究的新进展.国外矿床地质,1989,(2):1-5
[6]哈钦森(R W Huchinson).层控矿床在地质历史中的地位,1988,(3):19-57
[7]J M Franklin et al.Volvanic-associated massive sulfide deposits.Economic Geology 75th anniversary volume.Edited by the American society of economic Geology,1981,567-573
[8]Gustafson L B and Williams N.Sediment-hosted stratiform deposits of copper,lead,and zinc.Economic Geology 75th Annibersary Volume.Edited by American society of economic Geology,1981,139-176
[9]涂光炽等.中国层控矿床地球化学(.第一卷).科学出版社,1984,10-12
[10]中共马恩列斯篇作编译局.马克思恩格斯选集(第三卷).人民出版社,1972,491-507,534-563
[11] 白屯. 魏格纳地质互补思维述评[J]. 科学技术与辩证法, 1991,(4):16-20 .
[12]拉奇(D E Large).沉积容矿中的块状硫化物铅一锌矿床一种经验模式.国外矿床地质,1989,(2):5-25
[13]H A希洛.矿床形成条件与分布规律.地质科技动态,1988,(11-12):13

[1] 姚旭, 周瑶琪, 李素, 李斗. 硅质岩与二叠纪硅质沉积事件研究现状及进展[J]. 地球科学进展, 2013, 28(11): 1189-1200.
[2] 牛向龙,李江海,冯军. 五台山新太古代块状硫化物矿床成矿作用研究——海底喷流沉积成因显微构造证据[J]. 地球科学进展, 2009, 24(9): 1009-1014.
[3] 章雨旭;吕洪波;张绮玲;乔秀夫. 微晶丘成因新认识[J]. 地球科学进展, 2005, 20(6): 693-700.
[4] 付伟;周永章;杨志军;张澄博;杨小强;何俊国;杨海生;罗春科. 现代海底热水活动的系统性研究及其科学意义[J]. 地球科学进展, 2005, 20(1): 81-088.
[5] 薛传东,刘星,杨浩,李保珠,谈树成. 昆明市地热田越流含水系统中地下热水的数值模拟[J]. 地球科学进展, 2003, 18(6): 899-905.
[6] 徐兴旺,蔡新平,肖骑彬,梁光河,张宝林,王杰. 滇西北衙地区热水岩溶作用及其伴生的地质灾害[J]. 地球科学进展, 2003, 18(6): 912-920.
[7] 曾贻善. 热水溶液地球化学[J]. 地球科学进展, 1993, 8(4): 72-73.
阅读次数
全文


摘要