地球科学进展 ›› 1991, Vol. 6 ›› Issue (2): 40 -45. doi: 10.11867/j.issn.1001-8166.1991.02.0040

干旱气候变化与可持续发展 上一篇    下一篇

成矿学及其90年代发展方向研究
林舸   
  1. 中国科学院长沙大地构造研究所  410013
  • 收稿日期:1990-06-01 出版日期:1991-03-01
  • 通讯作者: 林柯

STUDY OF THE METALLOGENY AND ITS DEVELOPMENT IN 90' S

Lin Ge   

  1. Changsha Institute of Geotectonics, Acadmia Sinica
  • Received:1990-06-01 Online:1991-03-01 Published:1991-03-01

概述了今后10年内成矿学的发展趋势在于成矿理论的不断完善和提高,成矿模式的研究和应用将向多因素的综合性的定量模式发展;并指出地幔成矿理论和行星成矿学是新的发展方向和前沿科学。

The author briefly describes the development of metallogeny which were exhibited mainly in proposing and modifying metallogenic theory continuously, and study and application metallogenic models. The crustal ore deposits, the mantle ore deposits and the mantle-crust or crust-mantle ore deposits were suggested by Diwa metallogenic theory and non-linear metallogeny, which symbolized the beginning of progress study on the mantle metallogenic theory. The development of the metallogeny in 90's related with the application of modern metallogenic theories for study and synthesized the metallogenic regularity, and exploration of mineral researces effectively. But the important subjects of the basic theory are mantle metallogenic theory and the comparative planetary metallogeny.

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[1] 肖克炎. 应用综合信息法研究成矿规律及成矿预测的进展[J]. 地球科学进展, 1994, 9(2): 18-23.
[2] 陈国达,黄瑞华. 大地构造成矿学[J]. 地球科学进展, 1991, 6(2): 60-62.
[3] 黄瑞华. 构造成矿学浅议[J]. 地球科学进展, 1990, 5(6): 84-84.
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