Ban Pa Kha Fm
Type Locality and Naming
Li Basin (NW Thailand, Inthanon Zone), Lamphun province. Type locality: Pa Kha coal mine, Li district, Lamphun province (Ratanashien, 1990)
Synonym: หมวดหินบ้านป่าคา
[Figure: Map showing the Tertiary basins of Thailand, with Phetchabun basin highlighted. The solid black lines onshore are the principal rivers draining Northern and Central Thailand and the Khorat Plateau (Morley and Racey, 2011, page 224).]
Lithology and Thickness
Coarsening-upward succession of coarse alluvial fan sediments overlain by lacustrine deposits including coals, oil shales and marls (mined at Ban Pu and Ban Pa Kha), interbedded with coarser grained fluvio-alluvial sediments. 250 m. Coal seams are present in both the Ban Pa Kha Fm and the Mae Long Fm and may be up to 20 m thick, frequently with recognizable tree trunks; they are exploited at the Ban Pu and Ban Pa Kha mines. (Morley and Racey, 2011)
Relationships and Distribution
Lower contact
Not given. Basin is "bounded by hills of pre-Tertiary (commonly Paleozoic – Triassic) sedimentary and igneous rocks" (Morley and Racey, 2011)
Upper contact
Transitional into the lacustrine and coal deposits of the Mae Long Fm.
Regional extent
Present day surface
GeoJSON
Fossils
"The section immediately above the coal in the Ban Pu Mine has yielded an Early Miocene palynoflora (Fig. 10.4e, Morley 2001) supporting the view that the Ban Pa Kha Formation is of Late Oligocene–Early Miocene age. The pollen from this for- mation is predominantly from warm temperate species and the coals have a low ash content (up to 4%)." (Morley and Racey, 2011).
Age
Depositional setting
Additional Information