Phra Wihan Formation | |
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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°06′N 103°54′E / 16.1°N 103.9°E |
Approximate paleocoordinates | 14°18′N 111°24′E / 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 |
The Early Cretaceous Phra Wihan Formation is the second lowest member of the Mesozoic Khorat Group which outcrops in Northeast Thailand.
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]