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- W2390261832 abstract "All gold deposits in North-Eastern Hunan are of vein type, and hosted by the low grade metamorphic rocks of Lengjiaxi Group of the Middle Proterozoic Era. Their geochemical characteristics show that the ore-forming materials came from their host rocks. Oreforming fluids are rich in CO2 and SO2-4,with high Na+/K+ ratio, low Cl - and varied δ18O and δD values, showing that they are from multisources. These gold deposits were formed by a series of tectonic-thermal events which reworked the Lengjiaxi Group. There are two main stages of tectonic-thermal events: the Wulingian Period forming the auriferous quartz veins by syntectonic metamorphic differentiation, and the Indosinian-Yanshanian peroid causing re formation and enrichment of the former auriferous quartz veins." @default.
- W2390261832 created "2016-06-24" @default.
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- W2390261832 date "1996-01-01" @default.
- W2390261832 modified "2023-09-27" @default.
- W2390261832 title "TECTONIC-THERMAL EVOLUTION AND GOLD MINERALIZATION IN NORTH-EASTERN HUNAN, CHINA" @default.
- W2390261832 hasPublicationYear "1996" @default.
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