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- W2011673677 abstract "40Ar/39Ar radiometric age-dating results together with petrochemical studies of granitoid rocks from nearly all parts of Thailand strongly indicate that the granitoid belts (i.e. Eastern, Central and Western) form in different geological and geotectonic environments and show marked contrast in geochronological evolution. The new 40Ar/39Ar dating results differ markedly from those previously reported by other methods. The Eastern Granite Belt formed in Early to Late Triassic (245-210 Ma), the Central Belt in Late Triassic (220-180 Ma) to Middle Jurassic, and the Western Belt in Late Cretaceous to Middle Tertiary (80-50 Ma). Granitoid rocks of the S-type which are considered to be related to Sn-W-REE mineralization are widely present in the Western and Central belts as a result of Shan-Thai/Indo-China and Shan-Thai/Western Burma microcontinental plate collisions, respectively. On the other hand, I-type granitoid rocks are inferred to be related to CuFeAuSb mineralization and are largely limited to the Eastern belt, formed as a result of subduction of oceanic lithospheric plates beneath the Shan-Thai and Indo-China microcontinents." @default.
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- W2011673677 date "1993-01-01" @default.
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- W2011673677 title "Granite belts in Thailand: evidence from the 40Ar/39Ar geochronological and geological syntheses" @default.
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- W2011673677 doi "https://doi.org/10.1016/0743-9547(93)90014-g" @default.
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