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Item

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Stratigraphy of the Rock Units Exposed in Taungkyun Area, Pyin 00 Lwin Township, Mandalay Region

http://hdl.handle.net/20.500.12678/0000007992
44f01e50-716a-47cf-a398-af9b2801e40e
d4e7743c-45b6-4a27-aefd-80b743dec11d
None
Name / File License Actions
Maw Maw Maw Myint (4).pdf (4.5 MB)
Publication type
Journal article
Upload type
Publication
Title
Title Stratigraphy of the Rock Units Exposed in Taungkyun Area, Pyin 00 Lwin Township, Mandalay Region
Language en
Publication date 2019-12-01
Authors
Hnin Hnin Swe
Maw Maw Myint
Description
The Taungkyun area is situated in Pyin 00 Lwin Township, Mandalay Region. The Paleozoic strata are exposed in the study area. They are generally trending nearly N-S direction and dipping toward the east. The rock units exposed in the study area are the Sitha Formation, the Kunlein Formation, the Nyaungbaw Formation, the Zebingyi Formation, and the Plateau Limestone Group. The Sitha Formation comprises stromatolites and biogenic laminated structures. The age of the Sitha Formation is regarded as the Middle Ordovician age on the basis of stratigraphic position and lithologic characters. The age of the Kunlein Formation is regarded as Late Ordovician by comparing the presence of the abundant brachiopods, echinoderms and biogenic structures (trace fossils or ichnofossil) and the lithologic similarity with the type area. The age of the Nyaungbaw Formation may indicate the Silurian by the presence of microfossil content, lithological character and relative stratigraphic position. The Zebingyi Formation may indicate the Early-Middle Devonian age by the occurrences of the diverse fauna assemblages including Trilobites, Cephalopods and Pteropods fossils (Tentaculites elegan and styliolina sp.). The Plateau Limestone Group may be regarded as the Permian age by the occurrences of coral and relative stratigraphic position.
Keywords
Stratigraphy, Sitha Formation, Kunlein Formation, Nyaungbaw Formation, Zebingyi Formation, Plateau Limestone Group
Journal articles
2
Taunggyi University Research Journal, 20 19, Vol. 1 1 .NO:2
345-351
11
814
1350
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