Home Multi-Country Search About Admin Login
Cenozoic
Cretaceous
Jurassic
Triassic
Permian
Carboniferous
Devonian
Silurian
Ordovician
Cambrian
Neoproterozoic
Mesoproterozoic

Search by
Select Region(s) to search
Hold Ctrl (Windows/Linux) or Command (Mac) to select multiple
Quanyagou Gr
Click to display on map of the Ancient World at:
Quanyagou Gr base reconstruction

Quanyagou Gr


Period: 
Cretaceous

Age Interval: 
Early Cretaceous, (13b) K1qG


Province: 
Qinghai

Type Locality and Naming

The Qinghai Petroleum Administration erected the Quanyagou Group in the report on the Mesozoic strata of the Qaidam basin (unpublished). The type locality for the designation is at Quanyagou on the western margin of the Qaidam basin of Qinghai. The reference section is at Quanyagou of the Mangya Town of the west Qaidam basin.


Lithology and Thickness

The Quanyagou Group is mainly represented by a set of tangerine sandstone and is represented by brown red sandstone, siltstone and brown gray sandy conglomerate and its lower part is built up by gray white conglomerate with tangerine and yellow gray sandy mudstone, bearing ostracods and sporopollen grains. It is 852.01 m thick.


Lithology Pattern: 
Sandstone


Relationships and Distribution

Lower contact

Its base is a disconformity marked by tangerine and yellow gray sandy mudstone with abundant Cretaceous faunas is distinguished from the Hongshuigou Fm marked by dark brown sandstone.

Upper contact

Its top is an unconformity bounded by the appearance of gray and gray yellow sandy conglomerate interbedded with sandy mudstone under the Lulehe Fm (or, the higher Ganchaigou Fm).

Regional extent

The present group occurs in the Qaidam basin, which varies considerably both in lithology and thickness. In the Quanyagou area it is quite coarse in lithology and 852.61 m thick. In the Lenghu area, only the lower part of the formation is composed of sandy mudstone with a thickness of 55 m. In the Lulehe area, it is mainly represented by tangerine and purple gray sandy conglomerate, with a thickness of 571.4 m. In the Kushuiquan and Dahonggou areas, it becomes fine in lithology and there appear multiple layers of dark brown and blue gray mudstone, except tangerine and gray white sandy conglomerate, with a thickness of 1173 m.


GeoJSON

{"type":"Feature","geometry":{"type":"MultiPolygon","coordinates":[[[[94.2,38.81],[94.58,38.8],[94.79,38.72],[95.09,38.49],[95.61,38.15],[96.01,37.94],[95.95,37.84],[95.55,37.75],[94.69,37.84],[94.09,37.89],[93.33,38.02],[92.44,38.22],[91.96,38.35],[91.9,38.45],[92.01,38.53],[92.25,38.55],[93.03,38.65],[94.2,38.81]]]]}}

Fossils

This formation yields ostracods Latonia onerusa, Darwinula sp., D. contracta, Timiriasevia sp., Clinocypris sp.; sporopollen grains Cicatricosisporites sp., Cyathidites minor. In Dahonggou and Ruoshuiquan it contains ostracods Cypridea unicostata, Cypridea vitmensiis, Rhinocypris cirrita, D. jungarica sp., Theriosynoecum sp.; estherias Dachaidanestheria loxoquadrata; Charophytes Mesochara stipitata, Minchechara xiaoxiensis; sporopollen grains Toroisporis, Iygodiumsporites, Cicatricosisporites.


Age 


Age Span: 

    Beginning stage: 
Valanginian

    Fraction up in beginning stage: 
0.75

    Beginning date (Ma): 
133.88

    Ending stage: 
Cenomanian

    Fraction up in the ending stage: 
0.25

    Ending date (Ma):  
98.85

Depositional setting

It belongs to piedmont-diluvial-fluvial deposition.


Depositional pattern:  


Additional Information


Compiler:  

Wan Xiaoqiao