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Geochemistry of Volcanic Rocks at Zhaokalong Iron-Copper-Polymetallic Ore Deposit, Qinghai Province, China: Implications for the Tectonic Background

机译:Zhaokalong铁铜 - 多金属矿床,中国青海省火山岩地球化学:构造背景的影响

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In order to investigate the tectonic metallogenic background of Zhaokalong deposit, major elements and trace elements of volcanic rocks at Zhaokalong deposit were analyzed. The volcanic rocks of Zhaokalong deposit are andes ite - island arc tholeiitic basalt, showing high AI, Na and low K content, with deep magma source originalfeatures. Trace elements analysis show that the volcanic rocks have high Cu, Pb and Zn, indicating the close relationship between volcanic and mineralization. Based on the results, Zhaokalong deposit can be classified as sedimentary-exhalative ore deposit. We conclude Zhaokalong polymetallic deposit was located in the Chesuo-Shengda graben, northwest part of Jiangda island arc uplift. The tectonic metallogenic background of Zhaokalong deposit was the Paleo-Tethyan archipelago oceanic basin in the Mesozoic. The oceanic basin may be formed after back-arc spreading.
机译:为了研究Zhaokalong沉积物的构造成分背景,分析了Zhaokalong矿床的主要元素和微量元素。 Zhaokalong押金的火山岩是Andes Ite-Island Arc Tholeitis玄武岩,显示出高AI,NA和低k含量,深岩浆源原创性优势。痕量元素分析表明,火山岩具有高Cu,Pb和Zn,表明火山和矿化之间的密切关系。基于结果,Zhaokalong矿床可归类为沉积呼气矿床。我们得出结论Zhaokalong Moveretallic Deposit,位于江达岛西北部的Chesuo-Shengda Graben arc隆起。 Zhaokalong矿床的构造成矿背景是中生代古茶山群岛海洋盆地。可以在后弧涂布后形成海洋盆地。

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