Loei Gr
Type Locality and Naming
Pha Nok Khao Platform (Loei region): Defined by Ueno K. & Charoentitirat T., 2011 to incorporate the upward succession of the Wang Saphung Fm, Nam Mahoran Fm, E-Let Fm and Pha Dua Fm. The upper three had been conventionally placed in the Saraburi Gr, which is more appropriate for the southern (Saraburi) region of the Loei-Phetchabun Range. In the Khon San area to the south, they applied the Loei Gr to the upward succession of the Huai Som Fm, Pha Nok Hao Fm and Hua Na Kham Fm.
Synonym:
[Figure: Late Paleozoic major facies subdivisions on the western margin of the Indochina Block by Ueno and Charoentitirat (2011). (Slightly modified from Wielchowsky & Young 1985).]
Lithology and Thickness
See individual formations.
Relationships and Distribution
Lower contact
An emergence at around the Mississippian-Pennsylvanian boundary separates the underlying Ban Sa Ngao Fm from the Wang Saphung Fm at the base of the Loei Gr.
Upper contact
Terminated by the Indosinian I Event (latest Permian); Next higher regional unit is the Hua Hin Lat Fm of late Triassic.
Regional extent
Loei region.
[Figure: Distribution of Carboniferous and Permian in NE Thailand. Data mainly based on 1:1 million scale geological map of Thailand (DMR 1999) with minor modifications (Ueno and Charoentitirat 2011).]
GeoJSON
Fossils
See individual formations.
Age
Depositional setting
Additional Information