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Yacheng Formation

Yacheng Fm


Period: 
Paleogene

Age Interval: 
Eocene, (28a)


Province: 
Hainan

Type Locality and Naming

Hainan-offshore SW. The naming section is located in well Ya13-1-1 in the Yacheng rise, ca. 100 km slightly west of Sanya City, Hainan. Named by Western South Sea Branch, China National Offshore Oil Corp. in 1983.


Lithology and Thickness

This formation refers to clastic coal measures below the Lingshui Formation. The formation, lithologically coarse below and fine above, may be divided into two members: Lower member, repeatedly alternating beds of coarse clastic rocks such as purplish gray, thick-bedded conglomerate, sandy conglomerate and sandstone and brownish red, thin-bedded mudstone, ~450 m thick. Upper member, mainly thick-bedded, dark mudstone, with gray or dark gray, multi-bedded sandy conglomerate, sandstone and coal beds, ~460 m thick. The total thickness is 0–900 m. The deposits are thick in the deep part of the basin and thin and even absent on the basin margins. At the seismic section this formation is equivalent to the reflector group between T7 and T8.


Lithology Pattern: 
Clayey sandstone


Relationships and Distribution

Lower contact

The lower part of the formation is not penetrated.

Upper contact

It has an unconformable contact with the overlying Oligocene Lingshui Fm.

Regional extent

It is distributed in the Yinggehai basin and Qiongdongnan basin.


GeoJSON

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Fossils

The upper part of the formation contains some planktic foraminifera such as Globigerina ciperoensis and Globorotalia opima and benthic foraminifera; the calcareous nannofossils include Sphenolithus ciperoensis, Dictyococcites bisectus and Zygrhablithus bijugatus etc.; the sporopollen is represented by the Verrucatosporites-Leiotrilletes-Trilobapollis assemblage. In addition, there are also the dinoflagellates Homotryblium floripes and Hystrichokolpoma rigaudiae etc.


Age 

Its age was previously considered to be Late Eocene to Early Oligocene (Zheng et al., 1999). Recent study assigns this formation to whole Eocene (National Commission on Stratigraphy of China, 2018).

Age Span: 

    Beginning stage: 
Ypresian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
56.00

    Ending stage: 
Priabonian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
33.90

Depositional setting

This formation consists dominantly of continental strata with marine intercalations, belonging to littoral-swampy and estuarine deposits. It is the most important source rock in the Qiongdongnan basin.


Depositional pattern:  

Additional Information


Compiler:  

Tao Deng, Yuanqing Wang, Qian Li, et al.