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Takua Pa Formation
Click to display on map of the Ancient World at:
Takua Pa Fm base reconstruction

Takua Pa Fm


Period: 
Quaternary

Age Interval: 
Pliocene – Pleistocene to recent (1,2)


Province: 
Andaman Sea: Mergui Basin

Type Locality and Naming

At the A-1 well between interval <2,250-3,320 feet; named after Takua Pa Town of Phuket province. The Takua Pa Fm was first named by Nakanart and Mantajit (1983) for Pliocene-Pleistocene sediments. Parent unit: Mergui Gr.

Synonym: หมวดหินตะกัว่ป่า

[Figure 1: Map of the Mergui Basin showing the main structural features including basin depocentres, based on an extensive grid of 2D seismic reflection data. (From C K Morley & A Racey, 2011)]


Lithology and Thickness

Grey, calcareous, glauconitic shales containing abundant foraminifera, and occasional siltstones. Thickness: 320 m.

[Figure 2: Stratigraphy and cross-section through the Mergui Basin, Andaman Sea, based on data in Polachan & Racey (1994) and Andreason et al. (1997). (a) Oligocene–Recent stratigraphy of the Mergui Basin; (b) stratigraphy of the syn-rift section (Oligocene–early Miocene) schematically illustrating the east–west variation in stratigraphy across the basin and the effect of rift-basin highs (e.g. Central High horst block) on large-scale distribution of sedimentary facies, modified from Andreason et al. (1997); (c) east–west cross-section through the Mergui Basin illustrating the typical half-graben geometries of the basin (modified from Polachan & Racey 1994). (From C K Morley & A Racey, 2011)]


Lithology Pattern: 
Pelagic marl


Relationships and Distribution

Lower contact

Thalang Fm (unconformable)

Upper contact

Unnamed Quaternary

Regional extent

Andaman Sea: Mergui Basin. Correlation: Seurula and Julu Rayeu Formations of North Sumatra Basin.


GeoJSON

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Fossils


Age 

Pliocene – Pleistocene to recent

Age Span: 

    Beginning stage: 
Zanclean

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
5.34

    Ending stage: 
Holocene

    Fraction up in the ending stage: 
0.0

    Ending date (Ma):  
0.01

Depositional setting

Lower bathyal, basin plain deposits


Depositional pattern:  


Additional Information


Compiler:  

Wen Du - modified from- C. K. Morley & A. Racey, 2011, Chapter 10 Tertiary 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.