International audienceThe continental carbonate deposits of the Zarand Basin were deposited within an intra-continental strike-slip basin situated in the northwestern corner of central Iran. They consist of distal alluvial mudstones to marlstones, carbonate pond deposits, carbonate and siliciclastic-infilled channels, and lacustrine carbonates deposited within a distal alluvial-lacustrine-palustrine complex. Both sedimentological and palaeontological evidence suggest that these sediments mostly formed within an open hydrological system. The common presence of root traces, greyish green mudstones, calcareous nodulisation, mottling, and desiccation breccias indicate a palustrine setting. The carbonate deposits of the Zarand Basin were formed ...
Major global events during the Oligocene epoch included a climatic change from warm “greenhouse” to ...
In the Getic of the Carpatho-Balcanides (eastern Serbia) and the Tirgan Formation of the Kopet-Dagh ...
International audienceThe Paleogene carbonate deposits of Pabdeh and Jahrum formations are widesprea...
International audienceThe continental carbonate deposits of the Zarand Basin were deposited within a...
The continental carbonate deposits of the Zarand Basin were deposited within an intra-continental st...
The continental carbonate deposits of the Zarand Basin were deposited within an intra-continental st...
Palustrine carbonates are frequently found with active and dried karstic springs in the foothills of...
International audienceMirak is a Palaeolithic site in Iran comprising several localities ("mounds") ...
Alluvial fans are one of the most important landforms in geomorphological and paloenvironmental stud...
The Fahliyan Formation (Lower Cretaceous) is composed of carbonate rocks and is composed of carbonat...
International audienceCore sediments from the dry lake bed of Hamoun were subdivided into 3 main sed...
Three stratigraphic sections of the Early Carboniferous Gachal Formation in the Kalmard area, centra...
Major global events during the Oligocene epoch included a climatic change from warm “greenhouse” to ...
In the Getic of the Carpatho-Balcanides (eastern Serbia) and the Tirgan Formation of the Kopet-Dagh ...
International audienceThe Paleogene carbonate deposits of Pabdeh and Jahrum formations are widesprea...
International audienceThe continental carbonate deposits of the Zarand Basin were deposited within a...
The continental carbonate deposits of the Zarand Basin were deposited within an intra-continental st...
The continental carbonate deposits of the Zarand Basin were deposited within an intra-continental st...
Palustrine carbonates are frequently found with active and dried karstic springs in the foothills of...
International audienceMirak is a Palaeolithic site in Iran comprising several localities ("mounds") ...
Alluvial fans are one of the most important landforms in geomorphological and paloenvironmental stud...
The Fahliyan Formation (Lower Cretaceous) is composed of carbonate rocks and is composed of carbonat...
International audienceCore sediments from the dry lake bed of Hamoun were subdivided into 3 main sed...
Three stratigraphic sections of the Early Carboniferous Gachal Formation in the Kalmard area, centra...
Major global events during the Oligocene epoch included a climatic change from warm “greenhouse” to ...
In the Getic of the Carpatho-Balcanides (eastern Serbia) and the Tirgan Formation of the Kopet-Dagh ...
International audienceThe Paleogene carbonate deposits of Pabdeh and Jahrum formations are widesprea...