Search
CSV
RISGeochemical constraints on the provenance of Oligocene– Miocene siliciclastic deposits (Zivah Formation) of NW Iran: implications for the tectonic evolution of the Caucasus
In this study, the whole-rock geochemistry of 35 Oligocene–Miocene sandstone and shale samples from the Zivah Formation, Moghan area (NW Iran) were collected and analyzed for evaluation of their provenance, tectonic setting and the intensity...
Geochemistry of shales of the Qadir Member (Nayband Formation; Upper Triassic), East Central Iran (Tabas Block): Implications for provenance and paleogeography
The Upper Triassic shale of the Qadir Member of the Nayband Formation, East Central Iran has been analyzed geochemically to evaluate provenance and paleogeography. The Qadir Member in the Parvadeh Coal Mine section is 450 meters thick, and includes...
Designing a Step-by-Step User Interface for Finding Provenance Information over Linked Data
their required data easily, a good user interface is needed. Also, as
users want to reach trustworthy or more up-to-date information in Linked Data,
they would like to have access to the provenance data, as well. In this paper, a
new method...
PROVENANCE AND TECTONIC SETTING OF MIOCENE SEDIMENTS, BINALOOD MOUNTAIN, NE IRAN
Binalood Mountain, Iran, active continental margin, Provenance...
Provenance of Rayen River sediments based on trace element geochemistry, Southeast of Kerman
Provenance, Trace elements, geochemistry, Rayen River...
Geochemistry of Carboniferous shales of the Sardar Formation, east central Iran: Implication for provenance, paleoclimate and paleo-oxygenation conditions at a passive continental margin
The Sardar Formation (Carboniferous) has a lithological variation that is characterized by sandstone, shale and limestone members. Shales of the Sardar Formation from the east central Iran have been analyzes for major ...
A study on innovation investing effectiveness of automobile listed companies
Multiuser frequency allocation with wideband power amplifier models
Triassic sedimentation and postaccretionary crustal evolution along the Solonker suture zone in Inner Mongolia, China
Geochemistry of the Late Jurassic–Early Cretaceous shales (Shurijeh Formation) in the intracontinental Kopet-Dagh Basin, northeastern Iran: implication for provenance, source weathering, and paleoenvironments
Abstract In the present study, the geochemical data were used to investigate the provenance, weathering history, and paleoenvironmental studies of the Shurijeh Shales, Kopet-Dagh Basin. The X-ray diffraction and X-ray fluorescence spectrometry...