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Maastrichtian Rudist Fauna from Tarbur Formation (Zagros Region, SW Iran): Preliminary Observations
Tarbur Formation Preliminary Observations
2010/12/20
The uppermost Cretaceous Tarbur Formation of the Zagros region (SW Iran) is mainly siliciclastic in composition, though it also incorporates some carbonate units including several rudist lithosomes.
Oligocene history of the Çardak - Dazkırı subbasin (Denizli, SW Turkey): Integrated molluscan and planktonic foraminiferal biostratigraphy
Oligocene history of the Ç ardak Integrated molluscan planktonic foraminiferal biostratigraphy
2010/10/14
The detailed analysis of molluscan and planktonic foraminiferal fauna in the Oligocene Çardak-Dazkırı sub-basin, in northeastern Denizli provin ce (western Turkey) allowed accurate da...
Testing Miocene Remagnetization of Bey Dağları: Timing and Amount of Neogene Rotations in SW Turkey
Aegean orocline palaeomagnetism IRM component analysis remagnetization
2010/10/14
Here we reassess the timing and amount of rotation of the eastern limb of the Aegean orocline, located in SW Turkey. The current model for this orocline involves a 25-30° counterclockwise (CCW) rotati...
Distributed power-law seismicity changes and crustal deformation in the SW Hellenic ARC
power-law seismicity changes crustal deformation SW Hellenic ARC
2009/12/11
A region of definite accelerating seismic release rates has been identified at the SW Hellenic Arc and Trench system, of Peloponnesus, and to the south-west of the island of Kythera (Greece). The iden...
Palaeoecology of the Late Badenian foraminifera and ostracoda from the SW Central Paratethys (Medvednica Mt.,Croatia)
Benthic foraminifera Ostracoda Palaeoecology Biostratigraphy Late Badenian
2009/12/8
The quantitative study of microfossil communities from the Late Badenian marls at the Sveta Barbara (eastern Medvednica Mt.) enabled reconstruction of three different palaeoenvironments: middle shelf,...
Calcareous algae,foraminifera and sequence stratigraphy of the Fahliyan Formation at Kuh-e-Surmeh (Zagros Basin,SW of Iran)
Iran Zagros Mountains Fahliyan Formation Gadvan Formation Dasycladales foraminifers Cretaceous
2009/12/7
Palaeontological, environmental and sequence stratigraphic studies were carried out on the shallow carbonate platform facies of the Berriasian – Hauterivian, Fahliyan Formation and the lower part of t...
Kinematics and timing of polyphase post-Caledonian deformation in the Bergen area,SW Norway
Kinematics timing polyphase post-Caledonian deformation Bergen area
2009/12/3
Polyphase semi-brittle to brittle deformation of the basement rocks of the Øygarden Complex commenced shortly after Caledonian ESE-directed thrusting and followed ductile W-directed shearing. T...
Weichselian interstadial sediments on Jæren (SW Norway)–paleoenvironments and implications for ice sheet configuration
Weichselian interstadial sediments paleoenvironments implications ice sheet configuration
2009/12/3
Interstadial glaciomarine sediments at Jæren in south-western Norway have been investigated for their composition, distribution and age, and a model for the depositional environment is proposed....
Timing of continental building in the Sveconorwegian orogen,SW Scandinavia
Timing continental building Sveconorwegian orogen
2009/12/3
The timing of continental building in the Sveconorwegian orogen of SW Scandinavia is evaluated with zircon U-Pb geochronology. ID-TIMS,LA-ICPMS and SIMS data are reported for 21 samples of orthogneiss...
Age constraints on the late Caledonian (Scandian) deformation in the Major Bergen Arc,SW Norway
Age constraints late Caledonian deformation Major Bergen Arc
2009/12/3
The Ulven Syncline in the Bergen Arcs contains some of the youngest rocks involved in Caledonian orogenic deformation in West Norway. The pelitic Vaktdal Formation contains a Middle Llandovery (439-43...
A four-phase model for the Sveconorwegian orogeny,SW Scandinavia
Afour-phase model Sveconorwegian orogeny SW Scandinavia
2009/12/2
The Sveconorwegian orogenic belt resulted from collision between Fennoscandia and another major plate, possibly Amazonia, at the end of the Mesoproterozoic. The belt divides, from east to west, into a...