Tectonic Implication of the Permo-Triassic Khao Yai Mafic Volcanic Rocks in Nakhon Nayok Province, Thailand: Evidence from Geochemistry and Rare Earth Elements (REEs)

Authors

  • Patcharin Kosuwan Jundee Department of Geological Sciences, Faculty of Science, Chiang Mai University, Chiang Mai 50200, Thailand
  • Yuenyong Panjasawatwong Department of Geological Sciences, Faculty of Science, Chiang Mai University, Chiang Mai 50200, Thailand
  • Phisit Limtrakun Department of Geological Sciences, Faculty of Science, Chiang Mai University, Chiang Mai 50200, Thailand
  • Sirot Salyapongse Division of Geoscience, Mahidol University, Kanchanaburi Campus, Kanchanaburi 71150, Thailand

DOI:

https://doi.org/10.48048/tis.2023.6582

Keywords:

Khao Yai mafic volcanic rocks, calc-alkalic magma, volcanic arc, REEs, active continental margin

Abstract

The Permo-Triassic Khao Yai Volcanics in Nakhon Nayok Province, Thailand, is a part of the Loei-Phetchabun-Nakhon Nayok Volcanic Belt. The purpose of this study is to clarify the geochemistry and REEs characteristic of Khao Yai Volcanics that is useful for identifying the paleo-environment or tectonic setting eruption in this area. The least-altered, mafic volcanic rocks from the Permo-Triassic Khao Yai volcanics, are seriate-textured to porphyritic, with variable amounts of phenocrysts/microphenocrysts. The mineral compositions include plagioclase, clinopyroxene, orthopyroxene, olivine, minor Fe-Ti oxide mineral, amphibole, apatite, biotite/phlogopite, monazite/zircon, glassy, and quartz. The geochemical characteristic of the Khao Yai Volcanics informed that the rocks had the same parental magma with different degrees of crystal fractionation. Most of the mafic volcanic rocks are subalkalic andesite on the basis of their Zr/TiO2 and Nb/Y ratios and calc-alkalic on diagrams Ti-Zr, Ti-Zr-Y, Hf-Th-Ta and Y-La-Nb. The least-altered mafic volcanic rocks have (La/Sm)cn and (Sm/Yb)cn ranging from 2.41 to 2.71 and 1.86 to 2.22, respectively.  The studied calc-alkalic andesite are analogous to the Quaternary calc-alkalic dacite and andesite from Maca Volcano, Patagonian Andes and the Middle Eocene andesite from Shimokoh cauldron, SW Japan in terms of chondrite-normalized REEs and N-MORB normalized patterns. Accordingly, the studied Khao Yai volcanics have been developed in an active continental margin, formed by eastward underthrusting Paleo-Tethys, the leading edge of Shan-Thai, beneath Indochina in the Late Permian to Early Triassic.

HIGHLIGHTS

  • New tectonic model of the Permo-Triassic Khao Yai mafic volcanic rocks in Nakhon Nayok Province, Thailand
  • The geochemistry and rare earth elements (REEs) analysis by XRF and ICP-MS
  • The REEs analog to modern volcanic rock
  • The classification of pre-Jurassic volcanic belt in Thailand


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Published

2023-03-18

How to Cite

Jundee, P. K., Panjasawatwong, Y. ., Limtrakun, P. ., & Salyapongse, S. . (2023). Tectonic Implication of the Permo-Triassic Khao Yai Mafic Volcanic Rocks in Nakhon Nayok Province, Thailand: Evidence from Geochemistry and Rare Earth Elements (REEs). Trends in Sciences, 20(7), 6582. https://doi.org/10.48048/tis.2023.6582