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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

Permalink : http://hdl.handle.net/20.500.12678/0000000389
0228248b-cdc5-41bd-8d38-353a5954236b
7823019b-23db-4f37-b5bd-28500867ad65
Preview
Name / File License Actions
Cho Cho Cho Lwin.pdf (560.4 kB)
sha256: 75eeb29982066a14ccc19e4e355258a3f3f0eba0187aa2174dc469b27452693a
Publication type Journal article
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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