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U-Pb zircon age of the pegmatoid of the Muong Lat complex

Tran Van Thanh 1
Pham Trung Hieu 2, *
  1. North Vietnam Geological Mapping Division
  2. University of Science, VNU-HCM
Correspondence to: Pham Trung Hieu, University of Science, VNU-HCM. Email: pthieu@hcm.edu.vn.
Volume & Issue: Vol. 2 No. 1 (2018) | Page No.: 96-101 | DOI: 10.32508/stdjns.v2i1.681
Published: 2019-01-06

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This article is published with open access by Viet Nam National University Ho Chi Minh City, Viet Nam. 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

Muong Lat granitoid complex located in Thanh Hoa province. It is composed of two mica granite, aplite and pegmatoid. Rock forming minerals include mainly K-feldspar, quartz biotite and muscovite. Crystallization age of pegmatite in Muong Lat body is determined by U-Pb zircon LA-ICP-MS method. Most of the analytical results 206Pb age / 238U ranged from 217–238 Ma, average 230 ± 7 Ma. Age results indicate, the existence magma activity in the study area. Three inherited zircon core gaves age of ~2.8Ga, ~2.4Ga, ~1.8Ga, ~400Ma and ~750 Ma, suggesting that the continental crust of the study area including material composition of the Neoarchean, Paleoproterozoic, Paleozoic and Neoproterozoic

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