igneous petrology

The Theory of Dissipative Structure and Its Significance in Igneous Petrology

耗散结构理论及其在火成岩岩石学中的意义

Crystal Optics and Igneous Petrology

晶体光学与火成岩岩石学

Open magma system : progress in igneous petrology in 1980 's

开放的岩浆体系&八十年代火成岩研究的新进展之一

A Decade of Progress and Challenges for the Future in Igneous Petrology

火成岩的10年研究进展和未来的挑战

Mantle-magma-c-h-o system progress in igneous petrology during the eighties

地幔岩浆C-H-O系统八十年代火成岩研究新进展

The integration of seismological tomography , igneous petrology , geochemistry and modeling for basin can provide basin dynamic studies with a very important way .

天然地震层析、岩浆岩石学地球化学和盆地模拟技术的综合应用提供了研究这一重要问题的手段。

This paper deals with the theory and research methods of dissipative structure , and its application in igneous petrology , which involves the following aspects : ( 1 ) Layering of basic complex ;

本文简要介绍了耗散结构理论及其研究方法，以及它在火成岩中的应用，其中包括以下几个方面：（1）基性杂岩体的层状构造；

In the study of igneous petrology , the crystallization differentiation is usually proposed , only based on the chemical variation of rock suite , and its primary mechanism is regarded as gravitational segregation of crystals in the Newtonian fluid .

火成岩石学研究中，通常仅根据岩套的化学变异来推断是否发生过结晶分异作用，而且认为结晶分异的主要机理是晶体在牛顿流体中的重力分离。