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

原地重熔说从与传统理论不同的角度，系统地阐述了组成大陆地壳重要部分的花岗岩以及与花岗岩有关的各种地质、地球化学现象的成因。花岗岩浆形成的原地重熔模型、与原地重熔模型相适应的成矿理论、以及在此基础上提出的元素地球化学场，三者构成了一个完整的逻辑体系。并对这一体系做了简单的介绍。

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

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 viewpoint 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.