摘要
本文首次提出构造物理化学或地质构造物理化学概念。构造物理化学是研究地壳物质在受构造力作用下发生物理变化和化学变化相互关联的学科领域;是通过对构造所产生的物理化学条件差异,特别是造成局部静水压力不同而影响,制约其中化学反应、化学过程的了解来回答岩石形变与相变密切共生成因机制的一个研究途径。它属解释地壳物质结构构造地学学科类和地壳物质组成成分地学学科类,具体互相联系之物理化学条件的基础地学理论研究,亦具有具体地质找矿研究的实用价值。
This paper for the first time advances the concept of tectonophysicochemistry. It is concerned with the study of the physical and chemical changes occurring under the action of tectonic forces on crustal materials and is a way to study the intimately associated genetic mechanisms of rock deformation and facies changes through gaining a knowledge of the difference in physicochemieal conditions produced by the tectonics, particularly of the influence and control of the chemical reactions and chemical processes due to the difference in partial hydrostatic pressure produced by t e tectonics. It deals with the study of the basic geological theory that explains the physico-chemlcal conditions linking the branch of geoscience about the textures and structures of crustal materials with the branch of geoseience about the composition of crustal materials, It is of practical value in concrete mineral prospecting.
出处
《中国区域地质》
CSCD
1991年第3期254-261,253,共9页
Regional Geology of China
