Home Multi-Country Search About Admin Login
Cenozoic
Cretaceous
Jurassic
Triassic
Permian
Carboniferous
Devonian
Early Paleozoic

Search by
Select Region(s) to search
Hold Ctrl (Windows/Linux) or Command (Mac) to select multiple
Doi Chiang Dao Limestone Formation
Click to display on map of the Ancient World at:
Doi Chiang Dao Limestone Fm base reconstruction

Doi Chiang Dao Limestone Fm


Period: 
Carboniferous, Permian

Age Interval: 
Upper Carboniferous to basal Triassic (Visean to Dienerian) (10)


Province: 
NW Thailand – Inthanon Zone – PaleoTethys domain

Type Locality and Naming

Named after Doi Chiang Dao (a 2194 m high karst mountain west of Chiang Dao) where the type locality is located, Chiang Dao district, Chiang Mai province.

Synonym: หมวดหินปูนดอยเชียงดาว

[Figure: Distribution of Carboniferous and Permian strata in Northern Thailand. Data mainly based on 1:1 million scale geological map of Thailand (DMR 1999) with minor modifications (Ueno K. & Charoentitirat T., 2011, page 75.)]


Lithology and Thickness

Seamount. "Pale-grey massive limestone but partly more dark-colored and moderately bedded particularly in its lower part, with frequent dolomitic levels, and free from siliciclastic materials throughout the thick succession. The dominant microfacies are bioclastic grainstone, ooid grainstone, oncoidal rudstone and bioclastic packstone, suggesting an open shallow-marine setting. … It is important to note the occurrence of basalt, sometimes showing pillow texture, in what is possibly the basal part of the succession." (Ueno & Charoentitrat, 2011). Thickness: More than 1000 m (rough estimate).


Lithology Pattern: 
Reef limestone


Relationships and Distribution

Lower contact

Not given

Upper contact

Not given. Drowning of Paleo-Tethyan seamounts occurred at end of Early Triassic.

Regional extent

Chiang Mai and Mae Hong Son provinces of North Region of Sibumasu - Inthanon Zone; Paratethys domain. "Huge carbonate bodies, generally with spectacular karst topography, are extensively distributed in northernmost Thailand, such as the Pai and Soppong areas in northern Mae Hong Son Province and the Wiang Haeng, Chai Prakan and Chiang Dao areas in northern Chiang Mai Province.


GeoJSON

{"type":"Feature","geometry":{"type":"MultiPolygon","coordinates":[[[[99.44,20.54],[99.56,20.49],[99.55,20.38],[99.52,20.12],[99.41,19.81],[99.28,19.33],[99.08,19.01],[98.86,18.55],[98.85,18.7],[98.91,19.06],[98.9,19.64],[98.92,19.97],[99.09,20.34],[99.44,20.54]]]]}}

Fossils

Various fossils, mostly foraminifers, minor corals and conodonts, have been reported from the Doi Chiang Dao Limestone since the first fusuline and coral records by Japanese student .. Although the data are still fragmentary and from many isolated localities, almost continu- ous Carboniferous – Permian foraminiferal faunas have been recognized from the Doi Chiang Dao Limestone (Fig. 5.5) (Ueno et al. 2008). They have essentially palaeotropical Tethyan affinities." (Ueno & Charoentitrat, 2011)


Age 

Carboniferous-Permian (Visean – Induan). "The basal basalt is probably Visean or slightly older judging from the age of the overlying carbonates. … Based on foraminifers, the Doi Chiang Dao Limestone ranges from the Visean (Mississippian/Early Carboniferous) to the Changhsingian (latest Permian), resting upon Tournaisian – Visean basalt." (Ueno & Charoentitrat, 2011).

Age Span: 

    Beginning stage: 
Tournaisian

    Fraction up in beginning stage: 
0.5

    Beginning date (Ma): 
352.84

    Ending stage: 
Olenekian

    Fraction up in the ending stage: 
0

    Ending date (Ma):  
249.81

Depositional setting

Mid-oceanic carbonates formed upon seamounts, open shallow-marine origin. "Ueno (1999) concluded that their unusually long and continuous deposition without any siliciclastic input in a stable tectonic setting can only be accomplished in a mid-oceanic setting as isolated build-ups such as seamount or oceanic plateau-top carbonates. Ueno & Hisada (1999) also interpreted the carbonates as seamount-capping shallow-marine build- ups probably resting upon a base of oceanic island basal." (Ueno & Charoentitrat, 2011)


Depositional pattern:  


Additional Information


Compiler:  
Wen Du - modified from Katsumi Ueno & Thasinee Charoentitrat, 2011, Chapter 5 Carboniferous and Permian in: Ridd, M.F., Barber, A.J., and Grow, M.J., editors, The Geology of Thailand, Geol. Soc. of London.; and Lexicon of Stratigraphic Names of Thailand of 2013.