Malekhu Limestone Fm
Type Locality and Naming
Katmandu region (Lesser Himalayan succession)
Lithology and Thickness
The Malekhu Limestone is one of the conspicuous units of the Upper Nawakot Group. It is constituted of thin-bedded, platy dolomitic and siliceous limestones of pale-yellow color. It is microcrystalline to dense, and hard with green sericite–chlorite partings and thin intercalations. Especially, its lower and upper parts comprise platy limestone, whereas the middle portion is rather thick-bedded dark gray dolomite or dolomitic limestone with bands of black chert and intercalations of black siliceous and carbonaceous slates. Frequently, there is an approximately 50 m thick basal limestone zone and it is separated by about 150 m thick black slates from the main limestone body. The Malekhu Limestone assumes a thickness of about 800 m at its type locality (Stöcklin and Bhattarai 1977, p. 20) and is presumably older than 1.3 Ga (Martin et al. 2011).
Relationships and Distribution
Lower contact
The Malekhu Limestone exhibits perfectly gradational contacts with the underlying slate bands of the Benighat Slates Fm. The transition is generally marked by an approximately 20–30 m thick alternation of calcareous and argillaceous rocks.
Upper contact
The Malekhu Limestone exhibits perfectly gradational contacts with the overlying slate bands of the Robang Fm. The transition is generally marked by an approximately 20–30 m thick alternation of calcareous and argillaceous rocks.
Regional extent
GeoJSON
Fossils
At Malekhu, sporadic domed stromatolites are observed in its middle part.
Age
Depositional setting
Additional Information