Petrochemistry of granitic rocks in Tha Pai area, Mae Hi sub-district,Pai district, Mae Hong Son province, Northern Thailand
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Creator 1. Patcharin Kosuwan Jundee
2. Supanida Phanbuppha
3. Thisanabordee Jamsai
4. Burapha Phajuy
Title Petrochemistry of granitic rocks in Tha Pai area, Mae Hi sub-district,Pai district, Mae Hong Son province, Northern Thailand
Publisher Research and Development Office, Prince of Songkla University
Publication Year 2565
Journal Title Songklanakarin Journal of Science an Technology (SJST)
Journal Vol. 44
Journal No. 6
Page no. 1427-1433
Keyword Tha Pai granite, S-type, high K-calc alkaline, orogenic environment
URL Website https://sjst.psu.ac.th/
ISSN 0125-3395
Abstract Granitic rocks in the Ban Tha Pai area, Mae Hi sub-district, Pai district, Mae Hong Son province, are located in thewestern line of the Central Granitic Belt in northern Thailand. These granitic rocks are in N-S orientation and have a Triassic age.Petrographic investigation of the granitic rocks indicates that they are monzogranite with medium to coarse-grained porphyritictexture. Mineral compositions of them mainly consist of quartz, K-feldspar, and plagioclase, with minor biotite and smallamounts of muscovite, apatite, zircon, titanite, and opaque minerals. Geochemical investigation of the granitic rocks indicatesthat they are in sub alkaline series and almost totally of high-K calc-alkaline affinity. Furthermore, the granitic rock samples wereS-type granite and peraluminous rock. According to tectonic discrimination diagrams, the granitic rocks might have formed in anorogenic environment.
Songklanakarin Journal of Science and Technology (SJST)

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