Panlaung Fm
Type Locality and Naming
Shan mid-Plateau (Pyin Oo Lwin). The Panlaung Fm was first described by Garson et al. (1976). [Original Publication: Barber, A. J., Khin Zaw & Crow, M. J. (eds) 2017. Myanmar: Geology, Resources and Tectonics. Geological Society, London, Memoirs, 48, 143-167]
Lithology and Thickness
Sandy claystone. First described by Garson et al. (1976) as an alternating sand and shale sequence. However, later investigation of the Panlaung Fm reveals a wide range of lithologies such as red beds, turbidites and allochemical limestone facies (Myint Thein & Bo San 1984; Myint Thein 2004).
Relationships and Distribution
Lower contact
Unconformable with Plateau Limestone Gr
Upper contact
Conformable contact with Alluvium.
Regional extent
This Fm is developed in Shan mid-Plateau (Pyin Oo Lwin).
GeoJSON
Fossils
containing abundant fossils: foraminifera: Pseudocyclammina, Caskizolinoides, Lucanzella, Ammobaculites, Gaudryna, Nautiloculina, Givanella and Cordiacian; algae: Halimeda Algal Oncolites (Turbiphytes) and Oligostegina; gastropoda: Narenea and Narinella; corals: Montivaltia and Peresphinctid ammonites.
Age
Depositional setting
Shallow-marine environment
Additional Information