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Khao Noi, Nakhon Sawan Province, Thailand
| Lat/Long (Decimal) | 15.318,100.433 |
|---|---|
| Co-ordinates Derivation | estimated from map |
| Mindat.org Region (for given coordinates) | Nakhon Sawan Province, Thailand |
Collections
| Collection | Reference | Stratigraphic Name | Comments | Lithology | Age |
|---|---|---|---|---|---|
| Khao Noi, block A | Ketwetsuriya C., Nützel A., et al (2016) | Tak Fa | Yanagida (1964, 1988) reported the presence of the fusulinid Verbeekina verbeeki. However, Fontaine et al. (1994) suggested that the Tak Fa formation has a late Middle Permian (Murghabian) age based on bryozoans, brachiopods and the coral fauna. Verbeekina verbeeki Suggests a Wordian age. | packstone | 268.8 - 265.1 Ma Permian |
| Khao Noi, block B | Ketwetsuriya C., Nützel A., et al (2016) | Tak Fa | Yanagida (1964, 1988) reported the presence of the fusulinid Verbeekina verbeeki. However, Fontaine et al. (1994) suggested that the Tak Fa formation has a late Middle Permian (Murghabian) age based on bryozoans, brachiopods and the coral fauna. Verbeekina verbeeki Suggests a Wordian age. | packstone | 268.8 - 265.1 Ma Permian |
| Khao Noi, block C | Ketwetsuriya C., Nützel A., et al (2016) | Tak Fa | Yanagida (1964, 1988) reported the presence of the fusulinid Verbeekina verbeeki. However, Fontaine et al. (1994) suggested that the Tak Fa formation has a late Middle Permian (Murghabian) age based on bryozoans, brachiopods and the coral fauna. Verbeekina verbeeki Suggests a Wordian age. | packstone | 268.8 - 265.1 Ma Permian |
| Khao Noi, block D | Ketwetsuriya C., Nützel A., et al (2016) | Tak Fa | Yanagida (1964, 1988) reported the presence of the fusulinid Verbeekina verbeeki. However, Fontaine et al. (1994) suggested that the Tak Fa formation has a late Middle Permian (Murghabian) age based on bryozoans, brachiopods and the coral fauna. Verbeekina verbeeki Suggests a Wordian age. | packstone | 268.8 - 265.1 Ma Permian |
| Khao Noi, block E | Ketwetsuriya C., Nützel A., et al (2016) | Tak Fa | Yanagida (1964, 1988) reported the presence of the fusulinid Verbeekina verbeeki. However, Fontaine et al. (1994) suggested that the Tak Fa formation has a late Middle Permian (Murghabian) age based on bryozoans, brachiopods and the coral fauna. Verbeekina verbeeki Suggests a Wordian age. | packstone | 268.8 - 265.1 Ma Permian |
| Khao Noi, block F | Ketwetsuriya C., Nützel A., et al (2016) | Tak Fa | Yanagida (1964, 1988) reported the presence of the fusulinid Verbeekina verbeeki. However, Fontaine et al. (1994) suggested that the Tak Fa formation has a late Middle Permian (Murghabian) age based on bryozoans, brachiopods and the coral fauna. Verbeekina verbeeki Suggests a Wordian age. | packstone | 268.8 - 265.1 Ma Permian |
| Khao Noi, block G | Ketwetsuriya C., Nützel A., et al (2016) | Tak Fa | Yanagida (1964, 1988) reported the presence of the fusulinid Verbeekina verbeeki. However, Fontaine et al. (1994) suggested that the Tak Fa formation has a late Middle Permian (Murghabian) age based on bryozoans, brachiopods and the coral fauna. Verbeekina verbeeki Suggests a Wordian age. | packstone | 268.8 - 265.1 Ma Permian |
| Khao Noi, block H | Ketwetsuriya C., Nützel A., et al (2016) | Tak Fa | Yanagida (1964, 1988) reported the presence of the fusulinid Verbeekina verbeeki. However, Fontaine et al. (1994) suggested that the Tak Fa formation has a late Middle Permian (Murghabian) age based on bryozoans, brachiopods and the coral fauna. Verbeekina verbeeki Suggests a Wordian age. | packstone | 268.8 - 265.1 Ma Permian |
| Khao Noi, unspecified block | Ketwetsuriya C., Nützel A., et al (2016) | Tak Fa | Yanagida (1964, 1988) reported the presence of the fusulinid Verbeekina verbeeki. However, Fontaine et al. (1994) suggested that the Tak Fa formation has a late Middle Permian (Murghabian) age based on bryozoans, brachiopods and the coral fauna. Verbeekina verbeeki Suggests a Wordian age. | packstone | 268.8 - 265.1 Ma Permian |
Recorded Fossils
References
Data courtesy of: PBDB: The Paleobiology Database, Creative Commons CC-BY licenced. , GBIF: the Global Biodiversity Information Facility, various licences, iDigBio, various licences, and EOL: The Encyclopedia of Life (Open Data Public Domain). Because fossils are made of minerals too!
