SEQUENCE STRATIGRAPHY OF EAST AIR KOMERING, SOUTH PALEMBANG SUB-BASIN
The purpose of this study is to establish the sequence stratigraphy of Early to Middle Miocene sediments of Talang Akar Formation, Baturaja Formation, Gumai Formation, Air Benakat Formation, and Muara Enim Formation in East Air Komering area, South Sumatra. Method used in this study is strat...
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Format: | Theses |
Language: | Indonesia |
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Online Access: | https://digilib.itb.ac.id/gdl/view/16393 |
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Institution: | Institut Teknologi Bandung |
Language: | Indonesia |
Summary: | The purpose of this study is to establish the sequence stratigraphy of Early to
Middle Miocene sediments of Talang Akar Formation, Baturaja Formation,
Gumai Formation, Air Benakat Formation, and Muara Enim Formation in East
Air Komering area, South Sumatra.
Method used in this study is stratigraphic facies analysis utilizing GR and SP
wireline log data from three wells, which are AR-1, CM-1, and JG-1.
The study area resided at the southern edge of South Palembang Sub-basin, South
Sumatra Basin. Currently, South Sumatera Basin is one of the Tertiary back-arc
basins, which spread across the southern part of Sumatra land bearing north west
– south east.
Sequence stratigraphy analysis divides the Early to Middle Miocene sediments in
the study area into nine sequence stratigraphy units bounded by nine sequence
boundaries. Those nine units area, respectively from older to younger, are
Sequence Unit 9, Sequence Unit 8, Sequence Unit 7, Sequence Unit 6, Sequence
Unit 5, Sequence Unit 4, Sequence Unit 3, Sequence Unit 2, and Sequence Unit 1.
Sequence Unit 9 deposited in inner neritic environment. Sequence Unit 8
deposited in shallow marine environment. Sequence Unit 7 deposited in shallow
marine to swamp. Sequence Unit 6, 5, 4, and 3 deposited in inner to outer neritic.
Sequence Unit 2 and 1 deposited in swampy to tidal mud flat.
In general, the Early to Middle Miocene sediments were deposited in relatively
shallow marine environment. There is tendency of shallow up and deepening
upward from middle neritic to transitional (tidal) environment.
The study area has undergone repeated changes of environment, which are
insignificant. During Early Miocene to Middle Miocene, the study area was still in
range of tidal to outer neritic environment.
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