Indosinian II Unconformity
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| Indosinian II Unconformity Stratigraphic range: Permian-Late Triassic | |
|---|---|
| Type | Geological formation |
| Underlies | Indosinian I Unconformity |
| Overlies | Nam Phong Formation |
| Area | Kuchinarai Group |
| Thickness | 200 m (660 ft) |
| Lithology | |
| Primary | Sandstone |
| Other | Conglomerate |
| Location | |
| Coordinates | 16°18′N 102°00′E / 16.3°N 102.0°ECoordinates: 16°18′N 102°00′E / 16.3°N 102.0°E ⧼validator-fatal-error⧽ |
| Approximate paleocoordinates | 20°54′S 93°00′E / 20.9°S 93.0°E ⧼validator-fatal-error⧽ |
| Region | Isan |
| Country |  Thailand |
| Extent | Khorat Plateau |
  Indosinian II Unconformity (Thailand) | |
The Indosinian II Unconformity is an unconformity located in the Khorat Plateau, Thailand. It has been dated to the Permian-Late Triassic and the formation is made up of conglomerate and sandstone.[1] The Indosinian II Unconformity separates the Kuchinarai Group from the Nam Phong Formation. The Indosinian II Event (late Triassic; Rhaetian) led to the creation of the overlying Nam Phong Formation.[1][2]
References[edit]
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