Structural evolution of the Kopeh Dagh fold-and-thrust belt (NE Iran) and interactions with the South Caspian Sea Basin and Amu Darya Basin
We present a detailed stratigraphic and structural study of the Kopeh Dagh fold-and-thrust
belt in NE Iran, which is an investigation of the complex polyphased tectonic history of this …
belt in NE Iran, which is an investigation of the complex polyphased tectonic history of this …
Environmental significance of trace fossil assemblages in a tide‒wave-dominated shallow-marine carbonate system (Lower Cretaceous), northern Neo-Tethys margin …
This study integrates ichnological and sedimentological data to interpret depositional
environments of the carbonate sediments of the Tirgan Formation (Lower Cretaceous) in the …
environments of the carbonate sediments of the Tirgan Formation (Lower Cretaceous) in the …
Progressive opening of a shallow-marine bay (Oliete Subbasin, Spain) and the record of possible eustatic fall events near the Barremian-Aptian boundary
In this paper, we analyse the upper Barremian-lowermost Aptian Alacón Formation (Oliete
subbasin, Maestrazgo Basin) of Spain to understand the progressive opening of a shallow …
subbasin, Maestrazgo Basin) of Spain to understand the progressive opening of a shallow …
[HTML][HTML] Bioturbation enhanced petrophysical properties in the Ordovician carbonate reservoir of the Tahe oilfield, Tarim Basin, NW China
Bioturbation plays an important role in enhancing the reservoir capacity of tight reservoirs.
This study aims to understand the alteration mechanism and effects of bioturbation on oil …
This study aims to understand the alteration mechanism and effects of bioturbation on oil …
Syn-depositional continental rifting of the Southeastern Neo-Tethys margin during the Albian–Cenomanian: evidence from stratigraphic correlation
ABSTRACT Albian–Cenomanian successions (Kazhdumi and Sarvak formations) represent
remarkable variations in thickness, facies, fauna, and environments throughout the Zagros …
remarkable variations in thickness, facies, fauna, and environments throughout the Zagros …
Palaeogeographic reconstruction and sequence architecture of the middle‐upper Jurassic successions of Hawraman Basin (NW Iran): Implications for tectono …
The middle‐upper Jurassic successions (Sargelu, Najmah, and Gotnia formations) of the
NW sector of the Zagros Mountain belt are studied to generate a sequence stratigraphic …
NW sector of the Zagros Mountain belt are studied to generate a sequence stratigraphic …
Ichnological analysis of the Kheneg el Aatène Formation (Floian-Da**ian) at its type locality (Saoura Valley, Ougarta Range, southwestern Algeria)
ABSTRACT The Early-Mid Ordovician Kheneg el Aatène Formation of the Ougarta Range is
here divided into two members:(i) the Aatène Micaceous Sandstone Member and (ii) the …
here divided into two members:(i) the Aatène Micaceous Sandstone Member and (ii) the …
[HTML][HTML] Geosites of Northern Mountainous Adygeya (Southwestern Russia): A Novel Vision
AV Mikhailenko, DA Ruban - Geosciences, 2024 - mdpi.com
Territorial inventories of geosites remain on the international agenda, and they can help in
acquiring information for solving pure geological research tasks. New field investigations in …
acquiring information for solving pure geological research tasks. New field investigations in …
Ichnology of tidal ravinement omission surfaces in siliciclastic transgressive deposits from the Puesto El Moro formation (Upper Cretaceous), Southern Patagonia …
Omission surfaces represent a gap in the sedimentary record on a particular environment,
constituting an important tool for basin analyses. Nevertheless, not always these surfaces …
constituting an important tool for basin analyses. Nevertheless, not always these surfaces …
Ichnology in oceanic islands; case studies from the Cape Verde Archipelago
Miocene and Pleistocene marine deposits in the Cape Verde Archipelago are represented
by a series of thin, transgressive sandy-bioclastic limestones that typically occur between …
by a series of thin, transgressive sandy-bioclastic limestones that typically occur between …