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Abstract
Zircons separated from an meta-granite dyke sample in the Bo Xinh complex area were dated to determine the protolith age for the complex. Nine LA-ICP-MS U-Pb zircon analyses give concordant ages concentrated at 278 Ma (weighted mean). These results indicated the protolith age of the metagranite dyke (primary magma crystallization age). These meta-granite dyke penetrated the mafic rocks of Bo Xinh complex, therefore it can be confirmed that the crystallization age of the mafic rocks of Bo Xinh complex must be older than 278 Ma (early Permian).
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Article Details
Issue: Vol 17 No 4 (2014)
Page No.: 42-48
Published: Dec 31, 2014
Section: Natural Sciences - Research article
DOI: https://doi.org/10.32508/stdj.v17i4.1555
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Copyright: The Authors. This is an open access article distributed under the terms of the Creative Commons Attribution License CC-BY 4.0., which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.
How to Cite
Pham, H. (2014). 278 Ma U-Pb zircon age of metagranite in Bo Xinh complex area of song Ma structural zone and its significances. Science and Technology Development Journal, 17(4), 42-48. https://doi.org/https://doi.org/10.32508/stdj.v17i4.1555
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