收稿日期: 1997-12-02
网络出版日期: 1998-04-01
基金资助
高等学校博士点专项科研基金、国家教委基金资助.
ADVANCES IN THE STUDY OF GENESIS AND METALLOGENY OF GRANITE: A BRIEF INTRODUCTION OF THE MELTING IN-SITU HYPOTHESIS AND GEOCHEMICAL FIELD OF THE ELEMENTS
Received date: 1997-12-02
Online published: 1998-04-01
陈国能 . 花岗岩成因与成矿理论研究进展——原地重熔说与元素地球化学场简介[J]. 地球科学进展, 1998 , 13(2) : 140 -144 . DOI: 10.11867/j.issn.1001-8166.1998.02.0140
The hypothesis of melting in-situ has systematically expounded the genesis of granite which constitutes an important part of the continental crust, and of the various geological and geochemical phenomena concerning the genesis of granite in the view point different from the traditional ones. The in-situ melting model of the formation of granitic magma, the metallogenic hypothesis relative to the model, and the framework of geochemical field of the elements consist of a complete logical system. This paper gives briefly an introduction to the system.
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