Open Access

Downloads

Download data is not yet available.

Abstract

The Late Mesozoic igneous rocks of Da Lat Zone include variety of rocks of which composition ranges from mafic (even Fe-ultramafic) to very felsic one. Among them, a small part is product of non-differentiation magmatism and the rest is mainly of a differentiation crystallization process. The Late Mesozoic igneous rocks of Da Lat Zone are derived from enriched mantle at different grades, characterized by isotopic geochemistry and petrochemistry. The Da Lat Zone magmatism is product of active continental margin of Paleo East Asian type in which there exist at the same time compression due to subduction and extension upon magmatic arc.



Author's Affiliation
Article Details

Issue: Vol 6 No 11 (2003)
Page No.: 74-83
Published: Nov 30, 2003
Section: Article
DOI: https://doi.org/10.32508/stdj.v6i11.3380

 Copyright Info

Creative Commons License

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
Van Long, T., & Thi Chich, L. (2003). THE LATE MESOZOIC MAGMATIC EVOLUTION OF DALAT ZONE. Science and Technology Development Journal, 6(11), 74-83. https://doi.org/https://doi.org/10.32508/stdj.v6i11.3380

 Cited by



Article level Metrics by Paperbuzz/Impactstory
Article level Metrics by Altmetrics

 Article Statistics
HTML = 934 times
Download PDF   = 578 times
Total   = 578 times