Xiaorequanzi Fm
Type Locality and Naming
The type section is lies at Aqikebulak and Shuiquangou of Xinjiang. It was named by Zhang Zhongxiu in 1966, and formally cited in Regional Stratigraphic Scale of Xinjiang in 1981.
Lithology and Thickness
Volcanics and Volcaniclastics. At Aqikebulake and Shuiquangou, it is dominated by green plagioclase-rich porphyrite, felsite, gray-green andesitic porphyrite, dacite-porphyrite, dacite-porphyritic tuff, tuff sandstone, tuff siltstone, tuff conglomerate, etc. Exposed thickness over 4000 m. At the Yamansu gully, it is Na-rich with exposed thickness of 1600 m. and the basal limestone contains Corals.
Relationships and Distribution
Lower contact
Unknown: The underlying stratum is unseen
Upper contact
Conformable contact with the overlying Yamansu Fm
Regional extent
Distributed at Qoltag Mt., extending NW-SE
GeoJSON
Fossils
At the Yamansu gully, the basal limestone contains Corals Dibunophyllum sp. and Carcinophyllum sp.
Age
Depositional setting
It is interpreted as eruptive volcanics into a neritic setting
Additional Information