(UUID : dc8f8e93-a976-41bf-9938-6ce0fc9bf46f)
Rock
Lava flow
MM_Rock_28_2024
Rock
Geological Survey in Lay Thar taung area, Singu township, Mandalay division
Lava flow occurs in Lay Thar tarung (mountain) area, Singu township.
0.0118 ~ 5.332
Million Years (Ma)
Pliocene to Pleistocene
Singu Basalt
Manual
Mineral Database
Geological Survey in Lay Thar taung area, Singu township, Mandalay division. (DGSE and Shwe Lin Kar Industrial Co., Ltd.
Field report
300 ~ 520
GPS
Plain
Geological Survey in Lay Thar taung (mountain) area, Singu township, Mandalay division
Lay Thar taung area, Singu township, Mandalay division
Tertiary age, Singu basalt is mostly occur in the study area. And the gravel bed of Irrawaddy formation (Plistocene) is also occur as an underlinning bed. Singu basalt has verious characters, Pumiceous, Amygdoloidal and Tortoise shell. At Singu, syn-tectonic Pleistocene basalts, possibly vented through the active fault strands, form a low elliptical plateau. The basalts overlie the upper part of the Plio-Quaternary Irrawaddy Group and straddle the fault trace (Chhibber 1934; Bender 1983; Bertrand et al. 1998).
Myanmar (Burma)
Mandalay division
Singu township
Aung Pe (Assistant Geologist) DGSE and Geologists of Shwe Lin Kar Industrial Co., Ltd.
2022-02-17 ~ 2022-05-31
Database
Database
JPEG
Lava flow_MM_Rock_28_2024
CC BY-NC - The author is free to use, but not for profit.
The copyright of this data is held by CCOP.
2024-07-25