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Stratigraphy of the Napeng-Namon Area, Northern Shan State
http://hdl.handle.net/20.500.12678/0000000511
http://hdl.handle.net/20.500.12678/0000000511ea884dfc-c71d-4088-a5c8-90118b0129cc
8a82527d-de97-400c-979b-cff666dd1999
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Title | ||||||
Title | Stratigraphy of the Napeng-Namon Area, Northern Shan State | |||||
Language | en | |||||
Publication date | 2018 | |||||
Authors | ||||||
Cho Cho Lwin | ||||||
Description | ||||||
Napeng-Namon area is situated about 7 miles south-east of Kayukme, northern Shan State. This area lies between North Latitudes 22º 28′ and 22º 31′ and East Longitudes 97º 02′ and 97º 12′ and occupies parts of one-inch topographic map of 93 F/2 and 93 F/3. It covers about 36 square miles. The stratigraphic successions of the study area are Nwabangyi Dolomite Formation (?Late Permian-Middle Triassic), and Napeng Formation (Late Triassic, Rhaetic). The beds are trending generally NE-SW, dipping towards SE with the amounts of 30º- 40º. Nwabangyi Dolomite Formation consists of whitish grey to grey, medium- to thickbedded, highly brecciated dolomite, dolomitic limestone, clastic limestone (calcarenite and calcirudite), and locally developed oolitic limestones. Napeng Formation overlies on the Nwabangyi Dolomite Formation unconformably and contains yellow to buff siltstones, highly fossiliferous siltstones (pelecypods and gastropods) variegated clays, shales and arenaceous limestones, calcareous mudstones, argillaceous limestones intercalated with shales. Based on the lithologic characters, faunal contents and their stratigraphic positions, Nwabangyi Dolomite Formation is deposited in the slope apron to shallow marine with agitated water, Napeng Formation in tidal flat. |
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Keywords | ||||||
Napeng-Namon area | ||||||
Identifier | https://oar.ydbu.edu.mm/handle/123456789/249 | |||||
Journal articles | ||||||
1 | ||||||
Yadanabon University Research Journal | ||||||
9 | ||||||
Conference papaers | ||||||
Books/reports/chapters | ||||||
Thesis/dissertations |