Hydrothermal evolution and origin of the Suixian molybdenum deposit in the Tongbai orogenic belt, China: Constraints from geology, fluid inclusions and multiple isotopes (H O C S Pb)

Author:

Niu Pan-PanORCID,Jiang Shao-YongORCID,Li Wen-Tian,Cui Pei-Long,Chen Yi-Chun,Muñoz ManuelORCID

Funder

National Natural Science Foundation of China

China University of Geosciences, Wuhan

State Key Laboratory of Geological Processes and Mineral Resources

Publisher

Elsevier BV

Subject

Economic Geology,Geochemistry and Petrology,Geology

Reference93 articles.

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2. Interpretation of microthermometric data for H2O-NaCl fluid inclusions;Bodnar,1994

3. Solubility of molybdenite and the transport of molybdenum in hydrothermal solutions;Cao,1989

4. Diverse and multistage Mo, Au, Ag-Pb-Zn and Cu deposits in the Xiong'er terrane. East Qinling: from Triassic Cu mineralization;Cao;Ore Geol. Rev.,2016

5. O and H isotopic evidence for a mantle source of water in appinite magma: An example from the late Neoproterozoic Greendale Complex, Nova Scotia;Cawood;Lithos,2021

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