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Hydrothermal Zircon from a Newly Found Porphyritic Granite in the Dongping Gold Deposit in Northern Hebei, China: Evidence from Petrography and Hf Isotope Composition

Hydrothermal Zircon from a Newly Found Porphyritic Granite in the Dongping Gold Deposit in Northern Hebei, China: Evidence from Petrography and Hf Isotope Composition
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摘要 Objective Hydrothermal zircon is altered by hydrothermal fluids and sometimes shows"hydrothermal mineral"characteristics.Studying hydrothermal zircon in gold deposits can help understand the origins of the gold mineralization.The Hf isotope composition of zircon can be used to determine the properties of the original rock.
出处 《Acta Geologica Sinica(English Edition)》 SCIE CAS CSCD 2019年第6期1985-1986,共2页 地质学报(英文版)
基金 funded by the National Nature Science Foundation of China (grant No. 41672070) Hebei key R & D project (grants No. 19224205D) Hebei Hydraulic Science and technology program (grants No. 2018-68)
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