Sanandaj-sirjan zone - Open Access .click

Results 201 to 210 of about 1,221,168 (223)

Some of the next articles are maybe not open access.

Gaw-Khuni Basin: An active stepover structure in the Sanandaj-Sirjan zone, Iran

Geological Society of America Bulletin, 2011
The Gaw-Khuni Basin is located in the central part of the Sanandaj-Sirjan zone, on the northeastern margin of the Zagros orogen. This basin is one of the continuous zones of Sanandaj-Sirjan zone basins that is filled by Pliocene–Holocene sediments. The Gaw-Khuni Basin is surrounded by an en echelon to parallel arrangement of active faults in dextral ...
A. Nadimi, A. Konon
openaire +1 more source

Petrology and Geochemistry of the Granitoid Complex of Boroujerd, Sanandaj-Sirjan Zone, Western Iran

Journal of Asian Earth Sciences, 2007
Abstract The Middle Jurassic Boroujerd Granitoid Complex of the Sanandaj-Sirjan Zone (with a U–Pb zircon age of 169–172 Ma) was emplaced in an active continental margin setting. This complex consists of three main units: an elongate NW–SE extending granodioritic unit (SiO2 = 58–71 wt%), which is widespread throughout the area, a quartz-dioritic unit (
Hossain Rahimpour-Bonab, Dariush Esmaeily +1 more
exaly +2 more sources

Strike-Slip Faulting in the Central Part of the Sanandaj-Sirjan Zone, Zagros Orogen, Iran

Journal of Structural Geology, 2012
Abstract The Sanandaj-Sirjan Zone (SSZ) is one of the main basement tectonic blocks located close to the northeastern margin of the Zagros Orogenic Belt. New observations in the central part of the zone indicate that the fault pattern is dominated by NW-trending longitudinal faults.
Andrzej Konon, Alireza Nadimi
exaly +2 more sources

Deep basin Sanandaj- Sirjan Zone

2023
openaire +1 more source

LAVAS OF THE NORTHERN SANANDAJ-SIRJAN ZONE, IRAN: FRACTIONATION OF MULTIPLE PARENTAL MELTS