摘要
归纳了地质流体力学研究中目前常用的三个基础理论,即双扩散对流理论,边界层理论和相似理论,重点总结了其在岩浆岩石学、成矿学、地球物理学及沉积岩石学等研究领域内的进展。
This paper presents a discussion of the three basic theories on which geological fluid mechanics develops: double-diffusive convection, boundary layer and simulation theories. The applications of the fluid mechanics in magmatic petrology, metallogeny, geophysics and sedimentology also summurized here.
出处
《地质科技情报》
CAS
CSCD
北大核心
1993年第3期39-44,共6页
Geological Science and Technology Information
关键词
地质体力学
双扩散对流
边界层
geological fluid mechanics, double-diffusive convection, boundary-layer theory, simulation theory, compositional zones of rock body, mineralization of sulfides, sedimentation
