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Chumphon Redbeds Formation
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Chumphon Redbeds Fm base reconstruction

Chumphon Redbeds Fm


Period: 
Cretaceous

Age Interval: 
Early Cretaceous (4)


Province: 
Sibumasu: Upper Peninsula

Type Locality and Naming

Type area:

Chumphon basin in Chumphon province

Synonym: หมวดหินสีแดงชุมพร


Lithology and Thickness

Red sandstone interbedded with siltstone and shale, few bivalves and plant remains. Thickness: 350 m


Lithology Pattern: 
Sandstone


Relationships and Distribution

Lower contact

Implied to be unconformable on the Khao Lak Fm of middle Jurassic in this Chumphon Basin.

Upper contact

Need clarification. Might be the Sam Chom Fm conglomerates of mid-Cretaceous if it is the same succession as in the in the Thung Yai Gr in the nearby Nakhon Si Thammarat Basin.

Regional extent

Chumphon Basin


GeoJSON

{"type":"Feature","geometry":{"type":"MultiPolygon","coordinates":[[[[99.56,11.61],[99.53,12.18],[99.22,12.82],[99.08,13.85],[99.83,13.27],[100.04,12.96],[99.77,10.5],[99.75,10.11],[99.57,9.48],[99.12,8.96],[98.76,8.35],[98.66,8.2],[98.51,7.96],[98.34,7.55],[98.26,7.61],[98.27,7.95],[98.22,8.26],[98.21,9.05],[98.53,9.72],[98.93,10.56],[99.56,11.61]]]]}}

Fossils

Few bivalves and plant remains


Age 

It is thought by Raksaskulwong (1994) to correlate with and be synonymous with the Lam Thap Fm of early Cretaceous in the Nakhon Si Thammarat Basin (nearby in the Lower Peninsula region); therefore the same age span is applied here.

Age Span: 

    Beginning stage: 
Berriasian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
145.73

    Ending stage: 
Barremian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
126.30

Depositional setting


Depositional pattern:  


Additional Information

Parent unit: Trang Gr (Thung Yai Gr)

Compiler


Compiler:  

Compiler Wen Du - modified from Lexicon of Stratigraphic Names of Thailand of 2013; Assanee Meesook, 2011, Chapter 8 Cretaceous in Ridd, M.F., Barber, A.J., and Grow, M.J., editors, The Geology of Thailand, Geol. Soc. of London.