Fluid evolution and ore genesis of the Lianhuashan lode gold deposit, northern North China Craton: evidence from fluid inclusions and H–O–C–S–Pb isotopes
Abstract:The Lianhuashan Au deposit, located in the northern margin of North China Craton, is hosted in the metamorphic rocks of Neoarchean Wulashanyan Group along NNW-to N-trending faults, with pyrite as the predominant ore mineral. The mineralization process can be divided into four stages, involving stage I quartz-pyrite, stage II quartz-magnetite-chalcopyrite, stage III quartz-marcasite-pyrite, and stage IV quartz-calcite. Three types of fluid inclusions (FIs) have been identified, namely, pure carbonic inclusions … Show more
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