Latkhat Fm
Period:
Neogene
Age Interval:
Late Oligocene-Early Miocene
Province:
Myanmar Central Basins
Type Locality and Naming
Chindwin Basin, [Original Publication: Barber, A. J., Khin Zaw & Crow, M. J. (eds) 2017. Myanmar: Geology, Resources and Tectonics. Geological Society, London, Memoirs, 48, 219–260]
[Figure: Map showing location of sub-basins of the Central Myanmar Basin (after Myint Thein and M. Maung 2017)]
Lithology and Thickness
Sandstone. Latkhat Fm is characterized by basal, quartz conglomerates interbedded with light grey, fine- to coarse-grained sandstone and mottled clay beds. Thick: 2400 m
Synonyms: Also called Letkan Fm (Wandrey, C.J. 2006)
[Figure: Stratigraphic succession of the Chindwin Basin (after Than Htut, 2017)]
Lithology Pattern:
Sandstone
Relationships and Distribution
Lower contact
Unconformable with Tonhe Fm
Upper contact
Conformable with Natma Fm
GeoJSON
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Fossils
Age
Late Oligocene-Early Miocene
Age Span:
Beginning stage:
Chattian
Fraction up in beginning stage:
0.0
Beginning date (Ma):
27.29
Ending stage:
Aquitanian
Fraction up in the ending stage:
1.0
Ending date (Ma):
20.45
Depositional setting
Under fluvial to lacustrine conditions.
Depositional pattern:  
Additional Information
Compiler:
Than Htut, Kapesa Lokho, D.S.N.Raju and Ravi Misra (Than Htut, Myanmar petroleum systems, including the offshore area, Chapter 11 in Barber, A. J., Khin Zaw & Crow, M. J. (eds) 2017. Myanmar: Geology, Resources and Tectonics. Geological Society, London, Memoirs, 48, 219–260)