Results 171 to 180 of about 1,836 (211)
Some of the next articles are maybe not open access.
The Neotethys suture in the eastern Bulgarian Rhodopes
2020<p>Following a tectonic scheme proposed by Jan&#225;k et al. (2011; Journal of Metamorphic Geology 29, 317-332) and Pleuger et al. (2011; Zeitschrift der Deutschen Gesellschaft f&#252;r Geowissenschaften 162, 171-192), the Rhodopes are composed of four nappe complexes, from bottom to top the Lower, Middle, and ...
Jan Pleuger +12 more
openaire +1 more source
The Andaman and Nicobar ophiolites, in the forearc of the western Sunda subduction zone, underwent enigmatic, rapid Cenozoic vertical motions: shallow-water sediments with abundant arc debris characterize the middle Paleocene–middle Eocene and are under- and overlain by significantly deeper sediments.
Eldert L. Advokaat +2 more
exaly +5 more sources
Cretaceous carbonate deposits of Neotethys Ocean in the northwest of Iran
Journal of Earth Science, 2017Cretaceous carbonate deposits are considerably extensively distributed in the northwest of Iran and form most of the paleohighs of the region and different Cenozoic sedimentary units have deposited over these units with angular unconformity. Cretaceous stratigraphic units of northwestern Iran can be divided into three main categories: clastic, shallow ...
Rahim Mahari, Somaieh Sadigh Janbehan
openaire +1 more source
Propagating Neotethys Slab Break-Off Beneath Iran Following Arabia-Eurasia Collision
The closure of the Paleo- and Neotethys resulted in a long history of subduction of oceanic crust and production of a large variety of Phanerozoic magmatic rocks in the region occupied by present day Iran.
Niknam, Ali +10 more
exaly +3 more sources
Palaeogeography, Palaeoclimatology, Palaeoecology, 2003
Abstract New stratigraphic, petrographic and paleontological data from the Lower Permian of southeastern Arabia help to elucidate the still debated timing of Neotethys rifting and the climatic evolution following the Gondwanan glaciation. The transition from the Al Khlata to the Saiwan Formation, here described in detail, is interpreted to record ...
Angiolini L. +4 more
openaire +2 more sources
Abstract New stratigraphic, petrographic and paleontological data from the Lower Permian of southeastern Arabia help to elucidate the still debated timing of Neotethys rifting and the climatic evolution following the Gondwanan glaciation. The transition from the Al Khlata to the Saiwan Formation, here described in detail, is interpreted to record ...
Angiolini L. +4 more
openaire +2 more sources
2023
Modern global warming is proven to affect shallow water calcifiers among which are symbiont-bearing larger foraminifera (LF). To better understand the possible effects on modern faunas, we can explore the response of LF to past global events, referring to the last greenhouse megacycle terminated near the end of the Paleogene.
Cesare Andrea Papazzoni +1 more
openaire +1 more source
Modern global warming is proven to affect shallow water calcifiers among which are symbiont-bearing larger foraminifera (LF). To better understand the possible effects on modern faunas, we can explore the response of LF to past global events, referring to the last greenhouse megacycle terminated near the end of the Paleogene.
Cesare Andrea Papazzoni +1 more
openaire +1 more source
The Carbonate Platforms of Neotethys: a Comparison Study between Apulia and Eratosthenes Platforms
Second EAGE Eastern Mediterranean Workshop, 2019Summary Apulian Platform has been developed on the passive margin of Africa, the Adria or Apulia margin. It is characterised by platforms and deep-sea basins controlled by the Norian-Liassic rifting phase of the Tethyan rifting (Bertottti, 1993). The Eratosthenes carbonate platform sits on top of a thicker continental block (Moho depths of 32–35 km ...
V. Kosmidou, N. Papadimitriou
openaire +1 more source
Endemic foraminifera of the LateMaastrichtian from the northern branch of the Neotethys, NE Turkey
Micropaleontology, 2009The study of benthic foraminifera from the upper Maastrichtian intraplatform open shelf limestones in northeastern (Eastern Pontides) and central (Anatolides parts of Turkey reveals the presence of some benthic foraminiferal taxa,which appear to characterize the northern branch of the Neo-Tethys.
Nurdan Inan, Selim Inan
openaire +1 more source
A new Miscellanea (Foraminiferida) from the Selandian of the central Neotethys [PDF]
We present a new species of Miscellanea from a Selandian clast of the Mt. Vrachionas succession conglomerate (Zakynthos, Greece; Dermitzakis, 1978). This species occurs also in various coeval deposits from central and southern Italy: Mattinata (Gargano), Rio Arno (Gran Sasso), Conca di Cittareale (Rieti).
DI CARLO, MASSIMO, PIGNATTI, Johannes
openaire
Sedimentary Geology, 2018
Abstract We integrate stratigraphic, petrographic and geochemical analysis of subsurface data (wells) together with field surveys to study the sedimentation of a marginal Miocene sub-basin of the Southeastern Anatolian Foreland Basin (SEAFB; SE Turkey).
Yeşilova, Çetin +2 more
openaire +3 more sources
Abstract We integrate stratigraphic, petrographic and geochemical analysis of subsurface data (wells) together with field surveys to study the sedimentation of a marginal Miocene sub-basin of the Southeastern Anatolian Foreland Basin (SEAFB; SE Turkey).
Yeşilova, Çetin +2 more
openaire +3 more sources

