In-situ LA–ICP–MS U–Pb geochronology and trace elements analysis of polygenetic titanite from the giant Beiya gold–polymetallic deposit in Yunnan Province, Southwest China-Reference-Cited by-同舟云学术

In-situ LA–ICP–MS U–Pb geochronology and trace elements analysis of polygenetic titanite from the giant Beiya gold–polymetallic deposit in Yunnan Province, Southwest China

Published:2016-09 Issue: Volume:77 Page:43-56
ISSN:0169-1368
Container-title:Ore Geology Reviews
language:en
Short-container-title:Ore Geology Reviews

Author:

Fu Yu,Sun Xiaoming,Zhou Haoyang,Lin Hai,Yang Tianjian

Funder

National Natural Science Foundation of China

China Postdoctoral Science Foundation

Ministry of Science and Technology of the People's Republic of China

Higher School Specialized Research Fund for the Doctoral Program Funding Issue

Guangdong Province Universities and Colleges Pearl River Scholar Funded Scheme

Publisher

Elsevier BV

Subject

Economic Geology,Geochemistry and Petrology,Geology

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3. Formation of magmatic titanite and titanite–ilmenite phase relations during granite alteration in the Tribeč Mountains, Western Carpathians, Slovakia;Broska;Lithos,2007

4. In situ LA-(MC)-ICP-MS trace element and Nd isotopic compositions and genesis of polygenetic titanite from the Baogutu reduced porphyry Cu deposit, Western Junggar, NW China;Cao;Ore Geol. Rev.,2015

5. Complexly zoned niobian titanite from hedenbergite skarn at Písek, Czech Republic, constrained by substitutions Al(Nb,Ta)Ti−2, Al(F,OH)(TiO)−1 and SnTi−1;Cempírek;Mineral. Mag.,2008

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