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U – Pb ISOTOPIC AGE IN ZIRCON OF THE GRANITOID ROCKS AT CAM MOUNTAIN – ANGIANG PROVINCE

Hung Phu Tran 1, *
Vy Nguyen Hung Trinh 1
  1. University of Science, VNU-HCM
Correspondence to: Hung Phu Tran, University of Science, VNU-HCM. Email: pvphuc@hcmuns.edu.vn.
Volume & Issue: Vol. 14 No. 4 (2011) | Page No.: 46-56 | DOI: 10.32508/stdj.v14i4.2026
Published: 2011-12-30

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Copyright The Author(s) 2023. This article is published with open access by Vietnam National University, Ho Chi Minh city, Vietnam. This article is distributed under the terms of the Creative Commons Attribution License (CC-BY 4.0) which permits any use, distribution, and reproduction in any medium, provided the original author(s) and the source are credited. 

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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