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.
郝家河砂岩型铜矿床产于滇中中生代陆相红色碎屑岩建造中，规模中型。
The Haojiahe sandstone copper deposit occurs in the red elastic rock formation of Mesozoic continental facies in central Yunnan, being a medium size one.
铜矿物的化学动力学和热力学制约了砂岩铜矿中以辉铜矿为主及矿床分带的形成。
Chemical kinetics and thermodynamics of copper minerals constrain that chalcocite is main and ore zoning form in sandstone copper deposits.
大姚铜矿床位于盆地北部，是滇中砂岩型铜矿最好的矿化集中区。
Dayao copper deposit locating in the north of the basin is the best mineralizing concentration area of malmstone copper in the middle of Yunnan province.
大姚铜矿床位于盆地北部，是滇中砂岩型铜矿最好的矿化集中区。
Dayao copper deposit locating in the north of the basin is the best mineralizing concentration area of malmstone copper in the middle of Yunnan province.
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