Langmaria Fm
Type Locality and Naming
The type section is lies from the south slope of Deriangma Mt. to Xiala Mt., 6 km northeast of Yunzhug Township, Xianza (Shenzha), Tibet. It was named by Yang Shipu and Fan Yingnian in 1982.
Lithology and Thickness
Sandstone and Limestone. Light-gray and gray-green thin- to moderately thick-bedded medium- and coarse-grained feldspar-quartz pebbly sandstone, glacial-till conglomerate, fine-grained sandstone and siltstone, intercalated with thin-bedded sandy-clayey limestone, compact limestone and calcareous siltstone. Thickness reaching 877.4 m
Relationships and Distribution
Lower contact
Conformable contact with the underlying Angjie Fm
Upper contact
Conformable contact with the overlying Permian Xiala Fm
Regional extent
Distributed at Yunzhug Township of Xianza County, Yangwei Mt. of the Shiquan River, both banks of the Zhanjin River north of Jipu Village, Cameng and Tuotala of Rutog County, et al.
GeoJSON
Fossils
Containing Brachiopods Trigonatreta sp., Stepanoviella sp., Neospirifer fasciger paucicostulata, Spiriferellina cristata; Corals Wannerophyllum rianense, Plerophyllum ngangjiense, Lophophyllidium sp., Paralleyia yunzhugensis, Amplexus romanovskyi, Amplexocarinia sp., etc.,
Age
Depositional setting
It is interpreted as glacial-marine to neritic
Additional Information
This following entry was in the Carboniferous Lexicon suite, for some reason. Difficult to reconcile with age span of Angjie Fm as indicated by Shuzhong Shen et al (2019; Permian integrated stratigraphy and time scale), who did not have this unit on their Lhasa regional summary.