Search
CSV
RISPetrography and geochemistry of Silurian Niur sandstones, Derenjal Mountains, East Central Iran: implications for tectonic setting, provenance and weathering
Petrographical and geochemical studies of Silurian Niur sandstones, Derenjal Mountains, Central
Iran, were carried out to infer their provenance and tectonic setting. Modal analysis data of 37 medium sand size and well-sorted samples revealed...
Petrography, Major and Trace Elemental Geochemistry of the Ordovician-Silurian Siliciclastics in North of Tabas Block, Central Iran: Implications for Provenance and Paleogeography
and transitional continent were interpreted as a tectonic setting for
UPS and LPN formations, respectively. Furthermore, the geochemical analysis revealed
active continental margin and mostly passive margin during deposition of these two...
Detrital mode and geochemistry of the Shurijeh Formation (Late Jurassic-Early Cretaceous) in the central and western parts of the Intracontinental Kopet-Dagh Basin, Northeastern Iran: Implications for provenance, tectonic setting and weathering processes
studies of siliciclastic rocks can be used for the provenance, tectonic setting and paleoweathering studies in the source area....
Geochemistry of Carboniferous Sandstones (Sardar Formation), East-Central Iran: Implication for Provenance and Tectonic Setting
Geochemical analysis of sandstones from the Sardar Formation (from two stratigraphic successions) in east-central Iran were used for identification of geochemical characterization of sandstones, provenance and tectonic setting. Sandstones in the two...
Sandstone petrography and geochemistry of the Nayband Formation -Upper Triassic, Central Iran-: Implications for provenance and tectonic setting
to high-grade metamorphic provenance area. The major elements and modal analyses of the Nayband Formation sandstone samples suggest an active continental margin tectonic settings. The palaeoclimatic conditions were sub-humid to humid with relatively low...
Sandstone petrography and geochemistry of the Oligo-Miocene Zivah Formation, NW Iran: implications on provenance and tectonic setting.
Sandstone petrography and geochemistry of the Oligo-Miocene Zivah Formation, NW Iran: implications on provenance and tectonic setting....
Provenance and tectonic setting of Upper Devonian sandstones from Ilanqareh Formation (NW Iran)
Provenance and tectonic setting of the Upper Devonian sandstones in NW Iran have been interpreted
on the basis of petrography and trace-element analysis of samples from two different stratigraphic
sections. Modal analysis data of 27...
Petrography and geochemistry of sandstones succession of the Qal'eh Dokhtar Formation (Middle-Upper Jurassic), east central Iran: Implications for provenance, tectonic setting and palaeoweathering
rocks and tectonic setting. This formation is composed mainly of alternating marine sandstones,
laminated greenish to light gray shales with well bedded gray limestones. Texturally, these sandstones are fine
grained, subangular...
U-Pb zircon geochronology, geochemistry, and petrogenesis of the Hamech intrusions in the Kuh-e-Shah volcano-plutonic complex, Eastern Iran
The Hamech area is located in the west of Kuh-e-Shah volcano-plutonic complex, close to the boundary between the Lut Block
and Sistan Suture Zone -SSZ-, and is composed of monzonite to diorite porphyries and rare ...