- Nam Phong Formation
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Nam Phong Formation
Stratigraphic range: Upper TriassicType Geological formation Unit of Khorat Group Underlies Phu Kradung Fm Overlies Indosinian II Uncomformity Lithology Primary Sandstones Other Conglomerates, Siltstones Location Region Khorat Plateau Basin Country Thailand The Nam Phong Formation is the basal unit of the Khorat Group. It consists of resistant, red-brown micaceous sandstones, conglomerates, siltstone and mudstone 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 redish 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 Changwat Khon Kaen, Thailand. It is of Norian to Rhaetian age (Upper Triassic) to (Lower Jurrasic) age, and is notable for its fossils of early dinosaurs.[1]
Vertebrate fauna
Indeterminate prosauropod remains are present in Khon Kaen Province.[1]
Color key
Taxon Reclassified taxon Taxon falsely reported as present Discredited taxon Ichnotaxon Ootaxon Morphotaxon Notes
Uncertain or tentative data are in small text;crossed outdata are discredited.Vertebrates reported from the Nam Phong Formation Genus Species Location Stratigraphic position Material Notes Images I. attavipachi[1]
Geographically present in Khon Kaen Province.[1]
"Associated fragmentary vertebrae, ribs, chevrons, scapula, sternal, femur."[2]
See also
References
- ^ a b c d e Weishampel, David B; et al. (2004). "Dinosaur distribution (Late Triassic, Asia)." In: Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. Pp. 525–527. ISBN 0-520-24209-2.
- ^ "Table 13.1," in Weishampel, et al. (2004). Page 261.
Categories:- Geology of Thailand
- Triassic paleontological sites of Asia
- Geologic formation stubs
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