Shexing Fm
Type Locality and Naming
South Lhasa Block - Linzhou Basin. The Shexing Formation was erected by Wang Naiwen et al in 1983. The section for the designation is to the southeast of the Shexing Village south of Maqu of the Doilungdêgên County, Xizang. The reference section is in Dianzhong-Nama and Liangang- the breeding stock farm of the Lhunzhub County, Xizang (Wang Sien et al, 1989).
[Figure: Shexing Formation in type section at Shexing Village south of Maqu of Doilungdêgên County]
Lithology and Thickness
The Shexing Formation is mainly represented by purple, purple red, gray purple, gray and gray green siltstone, mudstone, shale, silty mudstone and shale and fine sandstone with thin-bedded limestone. The Shexing Formation is 981.4 m thick.
Relationships and Distribution
Lower contact
The base marked by dark purple red mudstone, siltstone and gray green shale lies conformably on the underlying Takna Fm.
Upper contact
The top of the formation shows an angular discordance with the overlying Linzizong Fm consisting of dark purple tuffaceous sandstone, sandy conglomerate and andesite.
Regional extent
The present formation occurs in Shexing and Langbagou (Kaiji) of the Doilungdêgên County and the Pengbo farm, Dianzhong, Nama, Liangang and the breeding stock farm of the Lhunzhub County, Xizang. It is persistent in lithology and 980-2400 m or more in thickness.
[Figure: Unconformity between Shexing Formation (lower) and Linzizong Formation (upper) in Maqu of Doilungdêgên County]
Fossils:
None listed
GeoJSON
Fossils
None listed
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Fossils:
In the Lhunzhub area, the upper part of the formation bears ostracods Altanicypris aff. bispinofera, Scabriculocypris ?ingenicus, Cypridopsis aff. bugintsavicus, etc.; and sporopollen grains Retitrilcopites geogensis, Tricopites spp., Cyathidites minor, C. australis, Undulatisporites spp., Piceaepollenites spp., Densiosporites spp., Araucariacites spp., Classopollis spp., Cerebropollenites mesozoicus, Biredisporites spp., etc.
Age
Depositional setting
Additional Information