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Phra That Formation
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Phra That Fm base reconstruction

Phra That Fm


Period: 
Triassic

Age Interval: 
Early Triassic (Upper Griesbachian to Lower Anisian) (11)


Province: 
Sukhothai Fold Belt

Type Locality and Naming

Phra That Muang Kham, 11 km southeast of Lampang province. Parent unit: lowermost formation in Lampang Gr.

Synonym: หมวดหินพระธาต


Lithology and Thickness

Red beds in the lower part, often upward to grey beds of mudstone, siltstone, sandstone with occasional intercalated limestone. Thickness:100-840 m, 90 m at the type section.


Lithology Pattern: 
Sandy claystone


Relationships and Distribution

Lower contact

Ngao Gr (Unconformable?)

Upper contact

Pha Kan Fm (conformable)

Regional extent

Lampang-Phrae basin, west part of the Northern Region of Sukhothai Fold Belt.: Lampang and Sukhothai provinces


GeoJSON

{"type":"Feature","geometry":{"type":"MultiPolygon","coordinates":[[[[99.59,20.42],[99.77,20.62],[100.02,20.62],[100.29,20.58],[100.56,20.32],[100.65,20.21],[100.86,20.03],[100.99,19.79],[101.06,19.55],[101.01,18.73],[100.44,17.98],[100.3,17.46],[100.3,17.2],[100.08,17.12],[99.93,16.92],[99.9,16.86],[99.64,16.65],[99.6,16.65],[99.3,16.91],[98.84,17.53],[98.8,17.99],[98.9,18.74],[99.29,19.31],[99.59,20.42]]]]}}

Fossils

The formation contains bivalves which indicate an age range from Late Griesbachian (Earliest Triassic) to Early Anisian. (Geology of Thailand, 2011)


Age 

Early Triassic in Fig. 6.2 of Chonglakmani, C.P., 2011.

Age Span: 

    Beginning stage: 
Induan

    Fraction up in beginning stage: 
0.25

    Beginning date (Ma): 
251.38

    Ending stage: 
Anisian

    Fraction up in the ending stage: 
0

    Ending date (Ma):  
246.80

Depositional setting

Near shore to continental deposits


Depositional pattern:  


Additional Information


Compiler:  

Wen Du - modified from- Chonglakmani, C.P., 2011, Chapter 6 Triassic in Ridd, M.F., Barber, A.J., and Grow, M.J., editors, The Geology of Thailand, Geol. Soc. of London.;Lexicon of Stratigraphic Names of Thailand of 2013.