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Geochemistry and geochronology of Late Triassic volcanic rocks in the Chiang Khong region, northern Thailand


Srichan, W and Crawford, AJ and Berry, RF, Geochemistry and geochronology of Late Triassic volcanic rocks in the Chiang Khong region, northern Thailand, The Island Arc, 18, (1) pp. 32-51. ISSN 1038-4871 (2009) [Refereed Article]

DOI: doi:10.1111/j.1440-1738.2008.00660.x


The Chiang Khong segment of the Chiang Khong-Lampang-Tak Volcanic Belt is composed of three broadly meridional sub-belts of mafic to felsic volcanic, volcaniclastic, and associated intrusive rocks. Associated sedimentary rocks are largely non-marine red beds and conglomerates. Three representative Chiang Khong lavas have Late Triassic (223-220 Ma) laser ablation inductively coupled mass-spectroscopy U-Pb zircon ages. Felsic-dominated sequences in the Chiang Khong Western and Central Sub-belts are high-K calc-alkaline rocks that range from basaltic to dominant felsic lavas with rare mafic dykes. The Western Sub-belt lavas have slightly lower high field strength element contents at all fractionation levels than equivalent rocks from the Central Sub-belt. In contrast, the Eastern Sub-belt is dominated by mafic lavas and dykes with compositions transitional between E-mid-oceanic ridge basalt and back-arc basin basalts. The Eastern Sub-belt rocks have higher FeO* and TiO2 and less light rare earth element enrichment than basalts in the high-K sequences. Basaltic and doleritic dykes in the Western and Central sub-belts match the composition of the Eastern Sub-belt lavas and dykes. A recent geochemical study of the Chiang Khong rocks concluded that they were erupted in a continental margin volcanic arc setting. However, based on the dominance of felsic lavas and the mainly non-marine associated sediments, we propose an alternative origin, in a post-collisional extensional setting. A major late Middle to early Late Triassic collisional orogenic event is well documented in northern Thailand and Yunnan. We believe that the paucity of radiometric dates for arc-like lavas in the Chiang Khong-Lampang-Tak Volcanic Belt that precede this orogenic event, coupled with the geochemistry of the Chiang Khong rocks, and strong compositional analogies with other post-collisional magmatic suites, are features that are more typical of volcanic belts formed in a rapidly evolving post-collisional, basin-and range-type extensional setting.

Item Details

Item Type:Refereed Article
Keywords:Thailand, geology, Chiang Kong-Lampang volcanic belt, Late Triassic volcanism, tectonics
Research Division:Earth Sciences
Research Group:Geology
Research Field:Structural geology and tectonics
Objective Division:Mineral Resources (Excl. Energy Resources)
Objective Group:Mineral exploration
Objective Field:Mineral exploration not elsewhere classified
UTAS Author:Srichan, W (Mr Weerapan Srichan)
UTAS Author:Crawford, AJ (Professor Anthony Crawford)
UTAS Author:Berry, RF (Associate Professor Ron Berry)
ID Code:62079
Year Published:2009
Web of Science® Times Cited:35
Deposited By:Centre for Ore Deposit Research - CODES CoE
Deposited On:2010-03-09
Last Modified:2010-04-15

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