نتایج جستجو برای: Tectonosedimentary
تعداد نتایج: 14 فیلتر نتایج به سال:
This review and analysis work presents the Campos Basin, in its geological aspects, such as tectonosedimentary evolution petroleum systems exploratory plays, history of exploration production, post-salt pre-salt reservoirs, panorama current production well future perspectives for basin, context national medium long-term forecasts.
Evidence of at least ten different tectonic- controlled sedimentary basins can be recognized in the central part of the Alborz Mountains in the Middle part of the Alpine-Himalayan belt. They formed from Neoprotrozoic to recent time as the results of the relative plate motion in southwest of Asia in Tethyan realm. The basins include: (1) Prototethys Late Neo-Proterozoic to Early Ordovician epi-c...
The forearc of south-central Chile (36°30?-42°S) is characterized by the presence a Coastal Cordillera and low lying area known as Central Depression. origin these morphostructural units has been largely debated. They have ascribed to different ages between Cretaceous Pliocene, tectonic causes that involve extensional or contractional deformation related Andean evolution accretionary processes ...
The Eşen Basin is a ca. 30 km long and 15 km wide, NNE-SSW trending young graben which is located in SW Turkey between the Isparta Angle and the Western Anatolian Extensional Province (Fig. 3). The basin has a key position in the south-western part of the Fethiye-Burdur Fault Zone (FBFZ), which is a presumed strike-slip zone with faults that run through numerous small cities and villages. There...
Abstract Coupled U–Pb and Lu–Hf LA-ICP-MS detrital igneous zircon data were obtained from metasedimentary sequences (Kaserer Formation, Schmirntal Quartzite, Seidlwinkel Bündnerschiefer Basin, Riffler Basin) of the western Tauern Window (Eastern Alps). Results show maximum deposition ages between Late Permian Triassic, indicating protracted sedimentation magmatism Paleozoic Mesozoic. The finger...
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