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Permalink :
http://hdl.handle.net/20.500.12678/0000000389
0228248b-cdc5-41bd-8d38-353a5954236b
7823019b-23db-4f37-b5bd-28500867ad65
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![]() sha256: 75eeb29982066a14ccc19e4e355258a3f3f0eba0187aa2174dc469b27452693a |
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Publication type | Journal article | |||||
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Upload Type | Publication | |||||
Title | ||||||
Facies and sedimentary environment of the Nwabangyi dolomite formation exposed in Napeng-Namon Area, Northern Shan State | ||||||
en | ||||||
Publication date | 2017 | |||||
Authors | ||||||
Dr.Cho Cho Lwin | ||||||
Description | ||||||
Napeng-Namon area is situated about 7 miles south-east of Kayukme, located in the southwestern part of the Lashio basin, on the Shan Plateau. The main objectives of this research were focused on description of facies and their distribution and the paleoenvironmental construction of Nwabangyi Dolomite Formation, in Napeng- Namon area. The Nwabangyi Dolomite Formation is thick, carbonate succession of the Late Permian to Middle Triassic age in northern Shan State. Twelve different microfacies types have been recognized by field observation, petrographic studies, identification of facies and facies association. Based on the typical characteristics features such as high dolomite content, high micrite content, desiccation cracks, algal mats, calcisphere, aggregate grains of many peloids, fairly rich in bivalves, gastropods, ostracods, and foraminiferas and other bioclasts, these carbonate microfacies can be divided into five major subenvironments, supratidal , tidal flat, lagoon, shoal and fore slope. The depositional environment of the Nwabangyi Dolomite Formation can be interpreted as a rimmed shelf, carbonate platform environments. | ||||||
Keywords | ||||||
microfacies | ||||||
Files | 560 Kb Available 2020-05-05 application/pdf preview application/pdf open_access Cho Cho Lwin.pdf |
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Journal articles | ||||||
1 | ||||||
Yadanabon University Research Journal | ||||||
8 | ||||||
Conference papaers | ||||||
Books/reports/chapters | ||||||
Thesis/dissertations |