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Petrography and Estimation of Depositional Environment on Thitsipin Formation of Naung Wo Area, Pinlaung Township, Southern Shan State
http://hdl.handle.net/20.500.12678/0000007887
http://hdl.handle.net/20.500.12678/0000007887557cbd4d-cc89-4eab-a000-e2bc6c09298f
9e49c739-8dc8-408d-a829-9ebdcea9f435
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Than Htoo Aung, Dr.pdf (28.7 MB)
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Publication type | ||||||
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Journal article | ||||||
Upload type | ||||||
Publication | ||||||
Title | ||||||
Title | Petrography and Estimation of Depositional Environment on Thitsipin Formation of Naung Wo Area, Pinlaung Township, Southern Shan State | |||||
Language | en | |||||
Publication date | 2020-08-31 | |||||
Authors | ||||||
Than Htoo Aung | ||||||
Nyan Win | ||||||
Aye Sis Thu | ||||||
Description | ||||||
The study area occupies southern part of Kawlaw-Pinlaung Basin and it is a region covering the southern continuation of the Eastern Highlands. It forms as a part of the western marginal zone of Shan Plateau. Kalaw – Pinlaung Basin. The major stratigraphic units occured in the study area are Thitsipin Formation and Thigaungtaung Formation of Plateau Limestone Group (Late Permian to Early Triassic), Loi-an Group (Middle Jurassic – Early Cretaceous), Kalaw Formation (Cretaeous) and Legaing Limestone Formation (Late Cretaceous). Lithologically, Thitsipin Formation mainly composed of slightly dolomitized gray coloured calcitic limestone, silt laminated limestone and whitish grey coloured limestone containing some chert nodules. These limestones are commonly dolomitized but some organic remains such as algae, bryozoan and hashes of bivalves, brachiopods, gastropods and corals are not uncommon. Petrographically, the Thitsipin Formation can be classified as (1) Ooidal Packstone - Grainstone, (2) Bioclastic Packstone – Grainstone, (3) Dolomitized Peloidal Wackestone, (4) Bioclastic Wackstone, and (5) Mudstone. In facts, the occurrence of early dolomitization and low fauna content are indicating tidal-flat origin. The bioclasts present and dominance of grainstones indicate shallow – water condition with relatively strong wave and current action, and the sediment represents the accumulation in current washed shoal conditions. The present of ooids with may be deposited in the oxygenated water and form above to below wave base. Marine ooids originate in warm, high energy, shallow-water environment; particularly in tidal bars. | ||||||
Keywords | ||||||
Petrography, Depositional environment, Thitsipin Formation, Naung Wo area | ||||||
Journal articles | ||||||
I | ||||||
Meiktila University Research Journal, 2020, Vol.XI, No.1 | ||||||
371-376 | ||||||
XI |