中山大学学报(自然科学版)2001，Vol.40Issue(3)：95-99,5.
原地重熔及其地质效应
The In-situ-melting Model of Granite Origin and Its Geological Evidence
陈国能 1张珂 1邵荣松 1李榴芬 1林小明1
作者信息
摘要
Abstract
A model concerning granite origin referred to as in-situ melting has been advanced in the last several years by the first author, which regards the upper crust as a close system and the granite as the result of materials within system changing from order (protolith) to disorder (melts) and finally to new order (granite with the variations of entropy. This paper gives a brief introduction of the model, and on the basis explains the various geological phenomena resulted by the melting process, including the room of batholiths, the generation of xenoliths and enclaves, the contact relations of granite bodies and their country-rocks, the formation of granite anticlines.关键词
花岗岩/原地重熔/熔渣与熔浆/重熔界面分类
天文与地球科学引用本文复制引用
陈国能,张珂,邵荣松,李榴芬,林小明..原地重熔及其地质效应[J].中山大学学报(自然科学版),2001,40(3):95-99,5.
