Qigaisu Gr
Type Locality and Naming
The type section is located at west of Qigaisu River of northern slope of Kunlun Mts., Gelmu County of Qinghai Province. It was named by No. 8 Team of Qinghai Petroleum Survey in 1958 and was published in Qinghai Compiling Group for Regional Stratigraphical Scale.
Lithology and Thickness
Volcanics, Sandstone and Claystone. Lower part (volcanics) is composed of grayish dark and purplish-red volcanic rocks of andesite, rhyolite and lamprophyre. Middle part is composed of grayish-green and purplish-red medium-fine-grained sandstone, siltstone and sandy slate intercalated with a few beds of conglomerate. Upper part is purplish-red slate. In the type area, the Group recorded an incomplete thickness of 2194 m.
Relationships and Distribution
Lower contact
Its lower boundary is not exposed.
Upper contact
The upper boundary is a disconformable contact with the overlying Lower Carboniferous. In a nearby region (same generalized column 17) are the Late Devonian volcanics of the Harza Fm.
Regional extent
Eastward to Tuolahe River, it is 1982 m thick, and mainly consists of feldspar sandstone intercalated with volcanic breccia.
At Jucheshan, it consists of feldspar sandstone, pebbly sandstone, siltstone and basalt, is 881 m in thickness, and its upper part is dominated by volcanic lava intercalated with clastics that can be divided into several cycles, from basic to acidic, of volcanic eruptions and sedimentation.
GeoJSON
Fossils
Fossils of chitinozoans and spore have been found in the middle part, and fragments of Asterolepiformis and ?Protolepidodendron in the upper part.
Age
Depositional setting
Additional Information