Abstract Qom Formation (Oligo-Miocene marine deposits, Central Iran) in the South of
Kashan, was studied in order to determine its microfacies and depositional environment …

Clastic sediments of Oligocene to Lower Miocene age form a major thick and widespread
sequence in the Tatau-Nyalau province of the north Sarawak Miri Zone. New light and heavy …

The aim of this research is to shed light on the distribution of Rupelian (Early Oligocene) and
evaporate deposits as evidences for timing and trending of opening and closure of the …

Abstract Qom Formation in the Sanandaj–Sirjan fore-arc and Central Iran back-arc basins
was studied in order to determine its accurate age. Larger benthic foraminifera (mainly …

The study presents a detailed record of foraminiferal faunas from CK2 core, a 928.75 m long
core drilled in the center of Xisha Islands, South China Sea, for biostratigraphy and …

This study focuses on an Oligocene succession dominated by larger foraminifera and
coralline algae in the Benitatxell Range (Prebetic Domain, southeastern Iberian Peninsula) …

Although carbonate ramps are widely described from the geological record, there is still a
debate on the relative influence of water temperature, trophic conditions and type of …

Facies characterization of Piacenzian (late Pliocene) carbonate sediments of the Guitar
Formation in Car Nicobar Island, India and the subsequent integration of paleoecological …

Abstract Qom Formation (Oligo-Miocene marine deposits of Middle Iran) is deposited at the
northeastern margin of the Tethyan Seaway. The Qom Formation in northern Abadeh …

Biofacies analysis is used to understand the palaeoenvironmental implications of late
middle Miocene (Serravallian) algal-foraminiferal assemblages and carbonate deposition …