首页> 外文期刊>地质学报(英文版) >SHRIMP Zircon U-Pb and Molybdenite Re-Os Datings of the Superlarge Donggou Porphyry Molybdenum Deposit in the East Qinling, China,and Its Geological Implications
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SHRIMP Zircon U-Pb and Molybdenite Re-Os Datings of the Superlarge Donggou Porphyry Molybdenum Deposit in the East Qinling, China,and Its Geological Implications

机译:东秦岭超大型东沟斑岩钼矿床的SHRIMP锆石U-Pb和辉钼矿Re-Os年代及其地质意义

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摘要

Located in the eastern part of the East Qinling molybdenum belt, the Donggou deposit is a superlarge porphyry molybdenum deposit discovered in recent years. The authors performed highly precise dating of the mineralized porphyry and ores in the Donggou molybdenum deposit. A SHRIMP U-Pb zircon dating of the Donggou aluminous A-type granite-porphyry gave a rock-forming age of 112±1 Ma, and the ICP-MS Re-Os analyses of molybdenite from the molybdenum deposit yielded Re-Os model ages ranging from 116.5±1.7 to 115.5±1.7 Ma for the deposit. The ages obtained by the two methods are quite close, suggesting that the rocks and ores formed approximately at the same time. The Donggou molybdenum deposit formed at least 20 Ma later than the Jinduicheng, Nannihu,Shangfanggou and Leimengou porphyry molybdenum deposits in the same molybdenum belt, implying that these deposits were formed in different tectonic settings.
机译:东沟矿床位于东秦岭钼带的东部,是近年来发现的超大型斑岩钼矿床。作者对东沟钼矿床中的斑岩和矿石进行了高精度测年。东沟铝质A型花岗岩斑岩的SHRIMP U-Pb锆石测年年龄为112±1 Ma,钼矿床中辉钼矿的ICP-MS Re-Os分析得出Re-Os模型年龄沉积物范围从116.5±1.7到115.5±1.7 Ma。通过这两种方法获得的年龄非常接近,这表明岩石和矿石大约同时形成。东沟钼矿床比金堆城,南泥湖,上房沟和雷门沟斑岩型钼矿床晚至少20Ma,这表明这些矿床是在不同构造背景下形成的。

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