[HTML][HTML] The Tethyan Seaway during the early to middle Miocene–New data and a review
Abstract The Tethyan Seaway was the connection between the Eastern and Western Tethys
which became restricted and finally closed during the Early and Middle Miocene. The …
which became restricted and finally closed during the Early and Middle Miocene. The …
Biostratigraphy of the nummulitids and lepidocyclinids bearing Qom Formation based on larger benthic foraminifera (Sanandaj–Sirjan fore-arc basin and Central Iran …
E Mohammadi, MR Vaziri, M Dastanpour - Arabian Journal of Geosciences, 2015 - Springer
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 …
was studied in order to determine its accurate age. Larger benthic foraminifera (mainly …
Timing and forcing mechanism of the final Neotethys seawater retreat from Central Iran in response to the Arabia-Asia collision in the late early Miocene
Abstract The Iranian Plateau lies in the middle of the Neotethys tectonic domain; to the east it
connects with the Tibetan Plateau, and to the west with the Anatolian Plateau and the Alpine …
connects with the Tibetan Plateau, and to the west with the Anatolian Plateau and the Alpine …
Microfacies and depositional environments of the Qom Formation in Barzok area, SW Kashan, Iran
E Mohammadi, M Hasanzadeh-Dastgerdi… - Carbonates and …, 2019 - Springer
Abstract Qom Formation (Oligo-Miocene marine deposits of Middle Iran) in the southwestern
Kashan was studied to determine its microfacies and depositional environments. Outcrops of …
Kashan was studied to determine its microfacies and depositional environments. Outcrops of …
Late Chattian larger foraminifera from the Prebetic domain (SE Spain): new data on shallow benthic zone 23
C Ferrandez-Canadell, T Bover-Arnal - Palaios, 2017 - pubs.geoscienceworld.org
This study focuses on an Oligocene succession dominated by larger foraminifera and
coralline algae in the Benitatxell Range (Prebetic Domain, southeastern Iberian Peninsula) …
coralline algae in the Benitatxell Range (Prebetic Domain, southeastern Iberian Peninsula) …
[HTML][HTML] Foraminiferal paleoecology and paleoenvironmental reconstructions of the lower Miocene deposits of the Qom Formation in Northeastern Isfahan, Central …
The early Miocene Qom Formation is exposed in the Bagh section, northeast Isfahan,
Central Iran, where it unconformably overlies Oligocene deposits and is unconformably …
Central Iran, where it unconformably overlies Oligocene deposits and is unconformably …
An upper Paleogene shallowing-upward sequence in the southern Sandino Forearc Basin (NW Costa Rica): response to tectonic uplift
G Andjić, C Baumgartner-Mora, PO Baumgartner - Facies, 2016 - Springer
Abstract The Sandino Forearc Basin of western Nicaragua and northwestern Costa Rica
(Central America) provides a Campanian to Pliocene sedimentary record. The study of the …
(Central America) provides a Campanian to Pliocene sedimentary record. The study of the …
Benthic foraminiferal events of the Qom Formation in the north Central Iran Zone
J Daneshian, LR Dana - Paleontological research, 2019 - BioOne
In order to recognize and verify the lower Miocene deposits and the Aquitanian-Burdigalian
boundary, benthic foraminifera from different localities in the north of the Central Iran Zone …
boundary, benthic foraminifera from different localities in the north of the Central Iran Zone …
Late Chattian platform carbonates with benthic foraminifera and coralline algae from the SE Iberian plate
T Bover-Arnal, C Ferràndez-Cañadell, J Aguirre… - …, 2017 - pubs.geoscienceworld.org
The carbonate system studied represents an under-investigated sedimentary record formed
in the western end of the Tethys during the Chattian relatively warm climate regime. These …
in the western end of the Tethys during the Chattian relatively warm climate regime. These …
Foraminiferal biostratigraphy of the Miocene Qom Formation, northwest of the Qom, Central Iran
J Daneshian, L Ramezani Dana - Frontiers of earth science, 2018 - Springer
Near Dochah, in the type area of the Qom Formation, Central Iran, the Miocene is partly
developed in pelagic facies. From the 894.1 meter thick,'a to e'members of this section, 152 …
developed in pelagic facies. From the 894.1 meter thick,'a to e'members of this section, 152 …