In this study, based on a multidisciplinary approach (biostratigraphy, cyclostratigraphy, and
facies analysis), the Asmari carbonate successions were evaluated across two platform-to …

The Asmari Formation deposited in the Zagros foreland basin during the Oligocene-
Miocene. Four different measured sections were studied in this area in order to interpret the …

Oligocene carbonate ramps and platforms are widespread and though they are important
carbonate reservoirs, detailed studies on the facies organization, platform type and internal …

Photozoan and heterozoan skeletal assemblages are controlled by their trophic
requirements (ie light-based photosynthesis versus other sources) and temperature …

Here, the larger foraminifera found in Middle Eocene-Early Miocene rocks from Dhofar
(Oman) and Socotra Island (Yemen) are studied in detail. The architectural analysis leads to …

Chattian mixed carbonate-siliciclastic deposits from two palaeogeographic units of Southern
Alps, the Lessini Shelf and Venetian foreland basin of northeast Italy, are studied with …

The definition of the type species of the genus Globoreticulina Rahaghi, 1978, G. iranica
Rahaghi, 1978, is emended and its age discussed in relation to those of 17 associated taxa …

Abstract The Asmari Formation is a thick carbonate succession of the Oligo-Miocene in
Zagros Mountains (southwest Iran). In order to interpret the facies and depositional …

The Cenozoic tectonic evolution of Central Europe was governed over long periods of time
by far-field stresses resulting from continent collision in the Alps (which is still ongoing) ridge …

Over the last 65 Ma, our world assumed its modern shape. This timespan is divided into the
Palaeogene Period, lasting from 65 to 23 Ma and the Neogene, which extends up to the …