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An Integrated Stratigraphic and Biostratigraphic Analysis of Southern Part of Ayeyarwady Delta Basin
http://hdl.handle.net/20.500.12678/0000007097
http://hdl.handle.net/20.500.12678/0000007097bd122576-6111-45d0-b58c-c657728b28f5
00903e08-ab9f-4071-93d6-077ed3d81195
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3 Thet Htar Aung, Tin Myint Oo.pdf (1.5 MB)
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Publication type | ||||||
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Journal article | ||||||
Upload type | ||||||
Publication | ||||||
Title | ||||||
Title | An Integrated Stratigraphic and Biostratigraphic Analysis of Southern Part of Ayeyarwady Delta Basin | |||||
Language | en | |||||
Publication date | 2020-12-01 | |||||
Authors | ||||||
Thet Htar Aung | ||||||
Tin Myint Oo | ||||||
Khaing Zin Phyu | ||||||
Lynn Myint | ||||||
Description | ||||||
Ayeyarwady Delta Basin occupies southernmost part of Central lowlands of Myanmar located between latitudes15°44'00"-17°59'00"N and longitudes 94°15'00"-96°20'00"E covering 3.418x105 Km2. In the present study an integrated lithostratigraphic and biostratigraphic analysis of southern part of the Ayeyarwady Delta Basin was conducted based on outcrops, seismic and well data. During the February 2019 a geological field checking was carried out in three areas; Myaungmya, Purian Point and Mawdin. The outcrop stratigraphy of these areas are examined and collected rock samples for petrological and paleontological analysis. The stratigraphic succession of the areas from older to younger is; Mawdin Fm, Kanbala Fm, Taunggale Fm , Tumyaung Fm, Kwingyaung Fm, Kathabaung Fm and Irrawaddy Fm. The seismic sequence stratigraphic analysis of the Ayeryarwady Delta Basin was conducted by MOGE and eight overall traceable unconformities and important reflectors were identified and correlated as far as possible with the data from the drilled wells and the outcrops. The electrofacies analysis was attempted by using electrical log motif and SP curve of the wells to define boundaries of the formations. Biostratigraphy of the Tumyaung, Kwingyaung and Kathabaung formations are analyzed in conjunction with of the results of MOGE. Paleogene /Neogene unconformity is greatly evident by a remarkable foraminiferal onset. The general marine record is of Lower Miocene age and begins with a relatively rapid basinal deepening characterized by rich planktonic foraminiferal microfaunas. The Oligocene larger benthonic foraminiferal assemblage were not found in the Ayeyarwady Delta area. |
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Keywords | ||||||
Lithostratigraphic, Biostratigraphic, Petrological, Paleontological, Electrofacies | ||||||
Journal articles | ||||||
Maubin University Research Journal | ||||||
p. 365 - 373 | ||||||
Vol.11 |