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Abstract
Results of analyzing U – Pb isotopic age for zircon in biotite granite, fine granite, monzodiorite, syenite diorite are 88±1,7 Ma, 86±1,7 Ma, 108±0,63 Ma 101±1,5 Ma,. These confirmed that they are Cretaceous age. Through this paper, many thanks to Professor Tony Crawford and Master Dinh Quang Sang (Tasmania University, Australia) for helping us to analyze these isotopic samples.
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Article Details
Issue: Vol 14 No 4 (2011)
Page No.: 46-56
Published: Dec 30, 2011
Section: Natural Sciences - Research article
DOI: https://doi.org/10.32508/stdj.v14i4.2026
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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
Tran, H., & Trinh, V. (2011). U – Pb ISOTOPIC AGE IN ZIRCON OF THE GRANITOID ROCKS AT CAM MOUNTAIN – ANGIANG PROVINCE. Science and Technology Development Journal, 14(4), 46-56. https://doi.org/https://doi.org/10.32508/stdj.v14i4.2026
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