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Geologic formation in Thailand From Wikipedia, the free encyclopedia
The Early Cretaceous Phra Wihan Formation is the second lowest member of the Mesozoic Khorat Group which outcrops in Northeast Thailand.
Phra Wihan Formation | |
---|---|
Stratigraphic range: Berriasian-Valanginian ~ | |
Type | Geological formation |
Unit of | Khorat Group |
Underlies | Sao Khua Formation |
Overlies | Phu Kradung Formation |
Thickness | 150 m (490 ft) |
Lithology | |
Primary | Sandstone |
Other | Siltstone, mudstone, conglomerate |
Location | |
Coordinates | 16.1°N 103.9°E |
Approximate paleocoordinates | 14.3°N 111.4°E |
Region | Northeast Thailand (Khorat Basin) |
Country | Thailand |
Extent | Khorat Plateau |
Type section | |
Named for | Khao Phra Wihan, an 11th-century Khmer Temple (Khao Phra Wihan National Park) |
Named by | Ward & Bunnag |
Year defined | 1964 |
Comprises fine- to coarse-grained sheet and channelled sandstone beds and rarer variegated siltstone and mudstone. Intermittent conglomerate beds.
Deposited in a fluvial environment dominated by high-energy, shallow braided rivers with subordinate lower energy meandering river systems and associated flood plains.
The Phra Wihan Formation is considered to be Berriasian-Valanginian in age based on palynological analysis.[1][2][3]
Sauropod (fossil) tracks have been recorded from this formation.[4]
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