Liangquan Fm
Type Locality and Naming
The type section is located on the hill ridge, east of Liangquan of Nyalam County, Xizang; the reference section is nearby Kede of Pazhu Township in Tingri (XĂȘgar) County, Xizang (Tibet) Autonomous Region. It was named by Wang Yigang et al. in 1974.
Lithology and Thickness
Shale, limestone. It is composed of interbeds between grayish-white shale and gray thin-bedded limestone, and also of light-gray silty mudstone which may change into grayish-green or grayish-white in color after weathering.
It is 40 m in thickness.
Relationships and Distribution
Lower contact
The Formation has a conformable contact to the light- to dark-gray limestone of the Pulu Fm of the Upper Silurian. [NOTE: Lexicon chart had indicated a fault contact at the reference section; and therefore base- Liangquam Fm is base-Pragian, and Lochkovian is unknown.]
Upper contact
The Formation is overlain by the light-gray feldspathic quartz sandstone of the Poqu Fm (see Boqu Gr).
Regional extent
It is mainly distributed in Burang, Zanda (Toling) and Zhongba counties, at Yali of Nyalam County, at Kede of Pazhu in Tingri County, and at Yadong County in southern Xizang. Eastward and westward from Nyalam, the thickness of the formation may reach approximately 400 m.
GeoJSON
Fossils
The formation contains a large number of tentaculites of Nowakia acuaria Zone, graptolites of Monograptus Yukonensis Zone, belonging to Pragian in age.
Age
Depositional setting
It is interpreted as a deep-water basin facies deposits.
Additional Information