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  1. Yadanabon University
  2. Department of Geology

Facies and sedimentary environment of the Nwabangyi dolomite formation exposed in Napeng-Namon Area, Northern Shan State

http://hdl.handle.net/20.500.12678/0000000389
http://hdl.handle.net/20.500.12678/0000000389
0228248b-cdc5-41bd-8d38-353a5954236b
7823019b-23db-4f37-b5bd-28500867ad65
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Cho Cho Cho Lwin.pdf (560 Kb)
Publication type
Journal article
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Publication
Title
Title Facies and sedimentary environment of the Nwabangyi dolomite formation exposed in Napeng-Namon Area, Northern Shan State
Language 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
Identifier https://oar.ydbu.edu.mm/handle/123456789/204
Journal articles
1
Yadanabon University Research Journal
8
Conference papaers
Books/reports/chapters
Thesis/dissertations
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