Nam Phong Formation

The Nam Phong Formation, which correlates to the Indosinian III Unconformity, is a geological formation in Thailand. It underlies the Khorat Group. It consists of resistant, red-brown micaceous sandstones, conglomerates, siltstones and mudstones of mainly fluvial origin. The sandstones are medium to very fine-grained and are usually calcareous. The conglomerates contain pebbles of quartz, brown and grey chert, and reddish brown siltstone. Cross bedding and plane-bed stratification are common in the sandstones and conglomerates. The sandstones and conglomerates make up approximately 30% of the formation. This sedimentary rock formation is found in Khon Kaen Province, Thailand. It is of Norian to Rhaetian age (Upper Triassic) to (Lower Jurassic) age, and is notable for its fossils of early dinosaurs.

Nam Phong Formation
Stratigraphic range: Late Triassic-Late Jurassic
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TypeGeological formation
UnderliesPhu Kradung Formation
OverliesIndosinian II Unconformity
Thickness1,465 m (4,806 ft)
Lithology
PrimarySandstone
OtherConglomerate, siltstone, mudstone
Location
Coordinates16.3°N 102.0°E / 16.3; 102.0
Approximate paleocoordinates20.9°S 93.0°E / -20.9; 93.0
RegionIsan
Country Thailand
ExtentKhorat Plateau
Type section
Named byWard & Bunnag
Year defined1964
Nam Phong Formation (Thailand)
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