Tilin Fm
Type Locality and Naming
Chindwin Basin, In the road section, between 75 and 81 milestone, on the Pakokku-Tilin road, the horizon, where Cotter and first described in 1913-14 is well marked. In Minbu-Salin Basin, Tilin area. [Original Publication: Barber, A. J., Khin Zaw & Crow, M. J. (eds) 2017. Myanmar: Geology, Resources and Tectonics. Geological Society, London, Memoirs, 48, 219–260]
Synonym: Tilin Sandstones
[Figure: Map showing location of sub-basins of the Central Myanmar Basin (after Myint Thein and M. Maung 2017)]
Lithology and Thickness
Sandstone. Consists mainly of sandstones, grey-green, moderately hard, fine- to coarse-grained, intercalated with silty clay beds. The Tilin Sandstones show considerable variation in lithology and thick and cannot everywhere be differentiated. Thickness is 3000 m. In Minbu-Salin Basin and Pyay Embayment, Clayey sandstone. This Fm contains sandstones, interbedded with carbonaceous shale beds. The sandstones are light yellow-brown to light grey, thinly bedded, fine- to medium-grained, fairly sorted, composed of quartz, feldspar, mica and carbonaceous materials. Shales are bluegrey, moderately hard, thinly laminated, slightly micaceous and fairly carbonaceous.
[Figure: Stratigraphic succession of the Chindwin Basin (after Than Htut, 2017)]
Relationships and Distribution
Lower contact
Conformable with Laungshe Fm
Upper contact
Conformable with Tabyin Fm
GeoJSON
Fossils
In Minbu-Salin Basin and Pyay Embayment, contains few fossils, but some burrowing structures are recorded.
Age
Depositional setting
Deposited under nearshore marine conditions in Chindwin Basin, deposited under outer shoreface to abyssal conditions in Minbu-Salin Basin and Pyay Embayment.
Additional Information