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首页> 外文期刊>Ore Geology Reviews: Journal for Comprehensive Studies of Ore Genesis and Ore Exploration >Comment on 'Geochronology and geochemistry of submarine volcanic rocks in the Yamansu iron deposit, Eastern Tianshan Mountains, NW China: Constraints on the metallogenesis' by Tong Hou, Zhaochong Zhang, M. Santosh, John Encarnacion, Jiang Zhu, Wenjuan Luo [Ore Geology Review, 56(2014):487-502]
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Comment on 'Geochronology and geochemistry of submarine volcanic rocks in the Yamansu iron deposit, Eastern Tianshan Mountains, NW China: Constraints on the metallogenesis' by Tong Hou, Zhaochong Zhang, M. Santosh, John Encarnacion, Jiang Zhu, Wenjuan Luo [Ore Geology Review, 56(2014):487-502]

机译：侯彤，张兆冲，桑托什，约翰·恩卡纳西翁，姜柱，罗文娟[评论]“关于中国西北天山东部雅曼苏铁矿床海底火山岩的年代学和地球化学：对成矿的限制”评论，56（2014）：487-502]

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摘要

In a recent paper, Hou et al. (2014) presented their study on the Yamansu iron deposit in eastern Tianshan Mountains, NW China. Hou et al. (2014) proposed a genetic model for the iron mineralization in Yamansu, which was based on geochronology and geochemistry study on volcanic rocks and skarns. In their paper, they gave an excellent discussion on the geochemistry data of basalt. However, we would like to address the following arguments:(1) What are meanings of zircon U-Pb ages derived from the basalt and skarn?(2) Did the Yamansu basalts provide the source of iron for the skarn mineralization?
机译：侯等人在最近的一篇论文中。 （2014）介绍了他们对中国西北天山东部Yamansu铁矿床的研究。侯等人。 （2014）提出了Yamansu铁矿化的遗传模型，该模型基于火山岩和矽卡岩的年代学和地球化学研究。他们在论文中对玄武岩的地球化学数据进行了很好的讨论。但是，我们想提出以下论点：（1）源自玄武岩和矽卡岩的锆石U-Pb年龄的含义是什么？（2）Yamansu玄武岩是否为矽卡岩矿化提供铁源？

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