摘要
热能聚散交替假说是地质学说的一个重要组成部分,是用于解析地壳演化和运动机因的新论点。本文通过实例结合研究,经实际检验,证明这一新论点不仅可以用宏观的地热异常表征加以描述,同时可以用微观的量纲给予肯定,它既有深刻的理论意义,又有重大的实际意义。
The hypothesis of geothermal energy coacervation—-diffusion alternation an important component of diwa theory, is a new used to explain the mechanism of crustal evolution and movement. Having been verified by examples and profound study, it may not only be described by macrogeothermal anomaly characters, but also be approved by micromeasurement. It is of profound theoretical and important practical significance.
出处
《大地构造与成矿学》
EI
CAS
CSCD
1991年第4期345-357,共13页
Geotectonica et Metallogenia
基金
国家自然科学基金"华北多因复成油气藏研究"成果之一
关键词
热能
聚散交替
地热
煤
矿化
hypothesis of geothermal energy coacervation-diffusion alternation, geothermal anomaly, verification of example.
