Geochemical Characteristics and U–Pb Dating of Granites in the Western Granitoid Belt of Thailand

• Published in: Geosciences (Basel) Vol. 14; no. 5; p. 135
• Main Authors: Uchida, Etsuo, Yokokura, Takumi, Niki, Sota, Hirata, Takafumi
• Format: Journal Article
• Language: English
• Published: Basel MDPI AG 01-05-2024
• Subjects: Ablation; Carbon; Chemical properties; Continental crust; Electron microscopes; Environmental aspects; geochemical signature; Geochemistry; Geological research; Granite; Ilmenite; Isotope ratios; Lasers; Lead; Magnetic permeability; Magnetic susceptibility; Magnetite; Methods; Nd–Sr initial isotopic ratios; Oceanic crust; Radiometric dating; Ratios; Sensors; Subduction; tectonic setting; Thailand; Tin; Uranium; Uranium-lead dating; U–Pb dating; Western Granitoid Belt; Zircon; Thailand; Southeast Asia; Myanmar (Burma); United Kingdom > UK; United States > US; Indochina; Japan; Phuket Thailand
• ISSN: 2076-3263; 2076-3263
• DOI: 10.3390/geosciences14050135

This paper presents the integration of magnetic susceptibility measurements and whole-rock geochemical compositional and Nd–Sr isotopic ratio analyses for granite samples collected from the Ranong, Lam Pi, Ban Lam Ru, and Phuket granite bodies in the Western Granitoid Belt of Thailand. In addition, U–Pb dating was performed on zircons extracted from the samples. All samples are proper granites based on their mineralogical and geochemical characteristics. Two samples collected from the Lam Pi granite body were classified as magnetite-series and I-type. The remaining granite samples were classified as ilmenite-series and S- or A-type. Furthermore, all granites were classified as syn-collision granites. Excluding the magnetite-series samples from the Lam Pi granite body, the other samples exhibit enrichment in incompatible elements, such as Nb, Sn, Ta, Pb, Bi, Th, U, Ce, Rb, and Cs. Zircon U–Pb dating yielded ages of ca. 60 Ma for the magnetite-series granites from the Lam Pi granite body, whereas ages of 88–84 Ma were obtained for the other granite bodies. Initial Nd–Sr isotopic ratios indicate a higher contribution of mantle material in the Lam Pi magnetite-series granites and a higher contribution of continental crust material in the other granites. Based on these compositional and zircon U–Pb age data, it is inferred that the 88–84 Ma granites formed as a result of the thickening of the continental crust owing to the collision between the Sibumasu and the West Burma blocks. In contrast, the ca. 60 Ma Lam Pi magnetite-series granites are thought to have been generated via partial melting of the mantle wedge associated with the subduction of the Neo-Tethyan oceanic crust beneath the West Burma Block.