2018
DOI: 10.1111/rge.12185
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Ore Genesis and Tectonic Significance of the Xiaojiashan Tungsten Deposit, Eastern Tianshan, Xinjiang, China: Evidence from Geology, Fluid Inclusions, and Stable Isotope Geochemistry

Abstract: The Xiaojiashan tungsten deposit is located about 200 km northwest of Hami City, the Eastern Tianshan orogenic belt, Xinjiang, northwestern China, and is a quartz vein-type tungsten deposit. Combined fluid inclusion microthermometry, host rock geochemistry, and H-O isotopic compositions are used to constrain the ore genesis and tectonic setting of the Xiaojiashan tungsten deposit. The orebodies occur in granite intrusions adjacent to the metamorphic crystal tuff, which consists of the second lithological secti… Show more

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“…Tin-tungsten deposits form in association with magmatic intrusions, and magmatic hydrothermal fluids are the most probable source for the deposits [1][2][3][4]. Oxygen isotopes are used to constrain the ore genesis [1], and magmatic fluid evolution by meteoric water incorporation was discussed [2]. Japan is divided into two metallogenic provinces, molybdenum and tin-tungsten.…”
Section: Introductionmentioning
confidence: 99%
“…Tin-tungsten deposits form in association with magmatic intrusions, and magmatic hydrothermal fluids are the most probable source for the deposits [1][2][3][4]. Oxygen isotopes are used to constrain the ore genesis [1], and magmatic fluid evolution by meteoric water incorporation was discussed [2]. Japan is divided into two metallogenic provinces, molybdenum and tin-tungsten.…”
Section: Introductionmentioning
confidence: 99%