Uranium deposits, therefore, are distributed mainly in diwa.
因此，铀矿化主要分布于地洼系。
This type of ore deposits are distributed in the intersection portion between different tectonic units in diwa region.
该类型矿床均分布于地洼区的不同构造单元的交接部位。
Diwa sedimentary rhythms are of mostly continental facies and every single rhythm is several to dozens of metres thick.
地洼区的韵律通常为陆相，单个韵律一般厚几米至几十米。
There is a close relation among tectonic evolution, fluid evolution and formation of sandstonecopper deposits in diwa basins of South China.
我国南方地洼盆地构造演化、流体演化和砂岩铜矿成矿作用三者之间具有密切的关系，处于一个统一的系统之中。
Some high quality manganese ore deposits of China are found to be polygenetic compound ore deposits which are the products of diwa mineralization.
研究发现中国某些优质锰矿，属复成矿床，它们都是地洼成矿作用的产物。
The another outstanding contribution of diwa theory to metallogeny is the concept of polygenetic metallogeny and polygenetic compound ore deposits.
地洼学说对成矿学的又一突击贡献，是提出多因复成成矿论及多因复成矿床。
The late occurrence and strong block-faulting of the diwa region were the basic factors controlling the characters of diwa granites in south china.
地洼区形成的较晚性与地洼区构造型相的强烈块断性，是华南地洼型花岗岩特征形成的基本原因。
Experiment and theoretical analyses of chemical kinetics and thermodynamics on sandstone copper deposits in Meso-Cenozoic Diwa basins in South China are ptesented in this paper.
对我国南方中新生代地洼盆地中的砂岩铜矿床进行了化学动力学与热力学的理论与实验研究。
Experiment and theoretical analyses of chemical kinetics and thermodynamics on sandstone copper deposits in Meso-Cenozoic Diwa basins in South China are ptesented in this paper.
对我国南方中新生代地洼盆地中的砂岩铜矿床进行了化学动力学与热力学的理论与实验研究。
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