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Lithofacies and Fossils of Carboniferous and Permian Carbonate Rocks from the Chiang Dao Area, Northern Thailand


Paper Type 
Contributed Paper
Title 
Lithofacies and Fossils of Carboniferous and Permian Carbonate Rocks from the Chiang Dao Area, Northern Thailand
Author 
Sutee Jongautchariyakul and Wutti Uttamo
Email 
sutee.kittymail.com
Abstract:
Based on 150 thin-sections, the Carboniferous-Permian carbonate rocks in the Chiang Dao area were classified into eight microfacies: oosparite, pelsparite, cortoidsparite, oncoidsparite, biosparite, biomicrite, intrasparite, and dolostone. These microfacies occur in tidal flat, tidal inlet, tidal bar, and lagoonal depositional environments. The tectonic setting of the Chiang Dao carbonate rocks is different from that of the carbonate rocks in peninsular Thailand. These northern Thailand rocks were deposits of  a warm tropical environment rather than of the cold glacial environment that existed in southern Thailand during Carboniferous and Permian time.
Start & End Page 
294 - 310
Received Date 
2007-09-10
Revised Date 
Accepted Date 
2007-10-20
Full Text 
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Keyword 
microfacies, carbonate rocks, Chiang Dao area, Carboniferous-Permian boundary
Volume 
Vol.35 No.2 (MAY 2008)
DOI 
Citation 
Jongautchariyakul S. and Uttamo W., Lithofacies and Fossils of Carboniferous and Permian Carbonate Rocks from the Chiang Dao Area, Northern Thailand, Chiang Mai J. Sci., 2008; 35(2): 294-310.
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Chiang Mai Journal of Science

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