Pattani Sequence IV Fm
Type Locality and Naming
Pattani Basin (central Gulf of Thailand). 4th upward) of the 5 sequences
Synonym: Upper Red-beds
[Figure: Map showing the Tertiary basins of Thailand. The solid black lines onshore are the principal rivers draining Northern and Central Thailand and the Khorat Plateau (Morley C. K. &Racey A., 2011, page 224).]
Lithology and Thickness
The unit comprises variegated dark-brown to reddish-brown claystones, grey to pale yellow sandstones and a few coals. It also contains important reservoir sandstone units for hydrocarbons.
Relationships and Distribution
Lower contact
On seismic data the base of the sequence may be conformably or disconformably overly Pattani Sequence III Fm. This boundary marks the Middle Miocene unconformity which may be erosional but tends, on seismic data, to be of low-amplitude expression and a subtle feature.
Upper contact
Overlain by Pattani Sequence V Fm
Regional extent
Pattani Basin (central Gulf of Thailand); but the succession is similar to adjacent basins (Fig. 10.16 in Morley and Racey, 2011)
GeoJSON
Fossils
Age
Depositional setting
"Fluvial-deltaic, with sands accumulating in point bars and channels. The sequence was deposited during a regression; hence, deposition occurred primarily in a fluvial floodplain environment." (Morley & Racey, 2011)
Additional Information