Chemical and boron isotope composition of tourmaline from Koktokay pegmatite, Altay Orogenic Belt, Northwest China: Implications for metallogenic mechanism and prospecting indicator for rare-metal pegmatites

Author:

Zheng Beiqi,Chen Meihua,Zhang Yuyang

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geophysics

Reference131 articles.

1. Characterization and mineralization potentials of granitic pegmatites of Komu area, southwestern Nigeria;Adetunji;Resour. Geol.,2010

2. In-situ elemental and boron isotopic variations of tourmaline from the Koktokay pegmatitic rare-metal deposit, China: insights into external contamination and the source of the granitic pegmatite;Bai;Ore Geol. Rev.,2023

3. Significant Li isotope fractionation in geochemically evolved rare element-bearing pegmatites from the little Nahanni pegmatite group, NWT, Canada;Barnes;Lithos,2012

4. Geological Memoirs, Series, Vol.1, No.32;BGMRX (Bureau of Geology and Mineral Resources of Xinjiang Uygur Autonomous Region),1993

5. Pegmatite dykes and quartz veins with tourmaline: an example of partial melting in the contact aureole of the Chandman massif intrusion, SW Mongolia;Buriánek;Geosci. J.,2012

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