Spillway Fm
Type Locality and Naming
Named after the spillway of Kaeng Krachan Dam, Phetchaburi province, where the type section is located. Originally defined by Raksaskulwong & Wongwanich (1993). Chaodumrong et al. (2004, 2007) suggest that the Spillway Formation is the lateral equivalent of the upper part of their Laem Mai Phai Fm. Lower-middle formation in the Kaeng Krachan Gr.
Synonym: หมวดหินสปิลเวย์
Lithology and Thickness
Sequence of laminated mudstone and thin to medium bedded sandstone. Ripple marks, load cast, slump structure and hummocky cross stratification are present. 120 m thick.
Relationships and Distribution
Lower contact
Laem Mai Phai Fm (conformable) by Chaodumrong et al. (2004, 2007); or equivalent Khao Wang Kradat Fm (subdivisions of Kaeng Krachan Gr by Rakaskulwong & Wongwanich, 1993).
Upper contact
Conformably overlain by Ko He Fm (glacial-marine).
Regional extent
Upper Peninsula: Phetchaburi province
GeoJSON
Fossils
Age
Depositional setting
Interpreted as Stormy shelf deposits by Chaodumrong et al. (2004, 2007). Aternatively, partly Glacial-marine?
Additional Information