Yinping Fm
Type Locality and Naming
Sichuan south of Gansu. The Yinping Fm was named by the Second Team of the Second Geological Survey Party of the Sichuan Bureau of Geology (1977), which was quoted in the Sichuan Regional Geology of Sichuan Province (1991). The type section is located in Yinping-Wugongkou, Mupi, Pingwu County, Sichuan Province. Uppermost formation of Bikou Gr in this region.
Synonym: (阴平组)
Lithology and Thickness
The Yinping Fm consists mainly of a series of metamorphosed clastic rocks with metamorphosed volcanic rocks. The lithological character is light gray, gray thin- to medium-bedded banded metamorphosed sandstone (garnet-mica-quartz schist or biotite sericite quartz schist) and gray, light gray-green metamorphosed siltstone (biotite sericite micrite schist and sericite quartz phyllite), the interbedded volcanic rocks are mainly gray, gray-green and purple basic volcanics, meta-acidic volcanics and tuffaceous microcrystalline schist. It is 1828-3536 m thick.
Relationships and Distribution
Lower contact
The formation is disconformable or unconformable with underlying Baiyang Fm of the middle Bikou Gr, then Dashaba Fm of lower Bikou Gr.
Upper contact
The top of the Yinping Fm is conformable with the overlying Muzuo Fm (glaciomarine)
Regional extent
Sichuan south of Gansu. The Yinping Fm is distributed in Motian Mt. area, Pingwu, and is well developed from Yinping to Nijiagou, Qingchuan County, Sichuan Province.
GeoJSON
Fossils
Age
Depositional setting
Additional Information