1) southern of Lanping basin
兰坪盆地南部
2) Lanping Basin
兰坪盆地
1.
Fluid dynamic processes of large-scale mineralization in the Lanping Basin,Yunnan,SW-China:evidence from fluid inclusions and basin fluid modeling;
西南三江兰坪盆地大规模成矿的流体动力学过程——流体包裹体和盆地流体模拟证据
2.
A Discussion on the Helium and Argon Isotopic Evidences for Genesis of the Baiyangping Copper—Cobalt Deposit in the Lanping Basin;
论兰坪盆地白秧坪铜(钴)矿床成因的氦氩同位素证据
3.
THE SYNTHETIC ANALYSIS OF REMOTE SENSING AND GEO-ANOMALY ON ORE-FORMING PREDICTION--Taking the Lanping basin as an example;
成矿预测中遥感与地质异常的综合分析——以兰坪盆地为例
3) Lanping-Simao Basin
兰坪-思茅盆地
1.
Lead and sulfur isotope geochemistry and the ore sources of the vein-type copper deposits in Lanping-Simao Basin, Yunnan province.;
云南兰坪-思茅盆地脉状铜矿床铅、硫同位素地球化学与成矿物质来源研究
4) Lanping Simao basin
兰坪-思茅盆地
1.
In Mesozoic era, the formation and evolution of the Mesozoic Lanping Simao basin were controlled by the Tethys tectonic zone.
兰坪-思茅盆地位于澜沧江缝合线与金沙江缝合线之间,它是在澜沧江洋和金沙江洋消亡后发展起来的一个中新生代陆内盆地。
5) the western border of Lanping basin
兰坪盆地西缘
6) series of deposit evolution
兰坪-思茅盆地呵叻盆地
补充资料:南部县大坪中学
四川省南部县大坪中学,创办于 1957 年。学校现有高、中级教师 50人,有全国、省、市、县明星教师、优秀教师 30 人。 目前有学生近 2000 人。
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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