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  1. Yadanabon University
  2. Department of Geology

"Sedimentary Facies Analysis of Irrawaddy Formation in the Migyaungye- Kunon Area, Magway Township, Magway Region"

https://meral.edu.mm/records/8408
https://meral.edu.mm/records/8408
819c9922-0cee-43c2-956a-f2bfd25d3889
8001cf7f-0190-4450-ba09-9af79bcc9bf5
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Warr Warr Warr Thidar Swam.pdf (1.1 MB)
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Title
Title "Sedimentary Facies Analysis of Irrawaddy Formation in the Migyaungye- Kunon Area, Magway Township, Magway Region"
Language en
Publication date 2022-08-12
Authors
Warr Warr Thidar Swam
Khin San
Zin Maung Maung Thein
Soe Myint
Description
"Migyaungye- Kunon area is situated far about 40 miles from the eastern bank of the
Ayeyarwaddy River in the southeast of Magway Township,. It is located between the
latitudes 19º 53' N and 19º 59' N and between the longitudes 95º 06' E and 95º 14'E,
referring to UTM topographic map 1995-01 (85 M-1). The sedimentary rocks found in the
study area are subdivided into two formation based on the lithologic and faunal
characteristics. They are Irrawaddy Formation (Late Miocene to Early Pleistocene) and
Obogon Formation (Middle Miocene). Section measurements were particularly made in
detailed along the well exposed sections which are perpendicular to structural trend. In
the present study area, the Irrwaddy Formation is well exposed along the Ye Ngan Chaung,
Sadaung Chaung and Kun on Chaung section. At least (9) lithofacies can be recognized
and there are grouped into (3) lithofacies association of the Irrwaddy Formation,
according to the feature of lithology, texture, sedimentary structures, fossil contents, etc.
They are (1) Channel facies association, (2) Overbank facies association and (3) Flood
plain facies association. According to the facies association and sedimentary characters,
the Irrwaddy Formation is assigned to be deposited under meandering river dominated
fluvial environment."
Keywords
facies, facies association, fluvial environment
Journal articles
2022
Yadanabon University Research Journal
184-193
Vol.12, No.2
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