What is it about?
Application of Pb-isotope signatures on VHMS deposit to constraint the source region and tectonic setting.
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Why is it important?
Our finding reveal a new information regarding the tectonic evolution of Peninsular Malaysia.
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This page is a summary of: Pb-isotope compositions of the Tasik Chini volcanic-hosted massive sulfide deposit, Central Belt of Peninsular Malaysia: Implication for source region and tectonic setting, Island Arc, February 2017, Wiley,
DOI: 10.1111/iar.12177.
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