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Petrology of Devonian Strata in Naungcho Area, Naungcho Township
http://hdl.handle.net/20.500.12678/0000002511
http://hdl.handle.net/20.500.12678/000000251195bba791-a48e-4cd1-9f91-21da98768389
faf1630e-0c59-450f-9429-6f03998c4b30
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Journal article | ||||||
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Publication | ||||||
Title | ||||||
Title | Petrology of Devonian Strata in Naungcho Area, Naungcho Township | |||||
Language | en | |||||
Publication date | 2008 | |||||
Authors | ||||||
Thein Htike Swe | ||||||
Yan Naing Htun | ||||||
Nyan Win | ||||||
Description | ||||||
The present work deals with the systematic classification of the Paleozoic sequence in Naungcho area, situated about 30 miles north-east of Pyinoo- Lwin, in Naungcho Township. The Devonian strata of the study area can be differentiated into two lithostratigraphic units of formation rank, viz., Maymyo Dolomite Formation (Middle-Late Devonian) and Zebingyi Formation (Early Devonian). In the view of petrology, the sedimentary sequences of the present area can be classified into two microfacies; (i) biomicrite/ bioclastic-wackestone and (ii) laminated micrite/ mudstone in the Zebingyi Formation. Furthermore, there can also be classified into two microfacies, such as (i) micritic dolomite/ muddy dolomite and dolomitized sandy pelmicrite/ dolomitized sandy peloidal wackestone-packstone in the Maymyo Dolomite Formation. According to lithology, faunal content, and sedimentary structure, the depositional environments of all these units, can be concluded as follow; the restricted shallow lagoon environment for the Zebingyi Formation, and warm, slightly agitated shallow marine environment for the Maymyo Dolomite Formation. |
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Keywords | ||||||
Zibingyi Formation | ||||||
Identifier | https://uyr.uy.edu.mm/handle/123456789/570 | |||||
Journal articles | ||||||
2 | ||||||
Universities Research Journal (URJ) | ||||||
Conference papaers | ||||||
Books/reports/chapters | ||||||
Thesis/dissertations |