Hadatu Fm
Type Locality and Naming
Erlian Basin. "The Bayanhua Gr, consisting of the Aershan Fm, Tenggeer Fm and Saihan Fm in ascending order, was deposited during the Early Cretaceous, is widely preserved in the basin, and constitutes the chief part of the basin-fill deposits." However, an uppermost Hadatu Fm is present in portions of the basin as described by Jingeng Sha (in Kosenko et al., 2021).
Lithology and Thickness
" It mainly comprises alternating grey to off-white sandstones, conglomerates, grits and siltstones, and grey, greyish-green and brownish-red mudstones rarely intercalated with thin-bedded coals or carbonaceous clays"
Relationships and Distribution
Lower contact
Rests unconformably on the Saihantala Fm (= Saihan Fm).
Upper contact
"After the deposition of the Saihan Fm [or locally the Hadatu Fm], a significant sedimentary hiatus occurred in most regions of the Erlian Basin. The Upper Cretaceous Erlian Fm was locally deposited in a few sub-basins in the northwestern basin, and … unconformity between … is named as T2 in seismic reflection sections" (see entry in Saihan Fm for more details).
Regional extent
GeoJSON
Fossils
It yields spores and pollen grains, a Porusphaera erenensis acritarch assemblage, and the rare brackish-water dinocyst Paucibucina pylophora (Sha, 2007a).
Age
Depositional setting
Additional Information