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- W2347589428 abstract "Hypo-thermal tungsten deposits came into being after intrusion of ore-bearing Yanshanian granite in the Wumushan area.These mineralized vein bodies are usually distributed within fractures of regional fault with medium or low dip angle near surface and high angle bellow or their alternating occarrences.The preminerogenic and syn-minerogenic fractures are defined by measurement and statistics of the ore-bearig fractures.The NE fractures host ore thus the ore-searching direction is pointed out." @default.
- W2347589428 created "2016-06-24" @default.
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- W2347589428 date "2008-01-01" @default.
- W2347589428 modified "2023-09-23" @default.
- W2347589428 title "ORE-BEARING STRUCTURES AND PROSPECTTING DIRECTION ABOUT TUNGSTEN DEPOSITS IN THE WUMUSHAN AREA OF ZHEJIANG PROVINCE" @default.
- W2347589428 hasPublicationYear "2008" @default.
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