Correlation of lineaments and groundwater quality in Dasht-e-Arjan Fars, SW of Iran
R Sarikhani, Z Kamali, AG Dehnavi… - Environmental earth …, 2014 - Springer
The NE-oriented Dasht-e-Arjan graben is located 65 km west of Shiraz and has resulted
from the active Kare-e-Bas fault segmentations. This extensional graben bounded by two …
from the active Kare-e-Bas fault segmentations. This extensional graben bounded by two …
Facies analysis and depositional environment of the Oligocene–Miocene Asmari Formation, in Interior Fars (Zagros Basin, Iran)
S Karami, V Ahmadi, H Sarooe, M Bahrami - Carbonates and Evaporites, 2020 - Springer
The present study deals with depositional environment and microfacies analysis of the
Asmari Formation in the Nasr–Abad section of Zagros basin in SW of Iran. The thickness of …
Asmari Formation in the Nasr–Abad section of Zagros basin in SW of Iran. The thickness of …
NEW CONSTRAINTS OF INTERIOR FARS SEDIMENTARY BASIN ANALYSIS DURING ASMARI FORMATION (OLIGOCENE-LOWER MIOCENE) DEPOSITION …
MYT Sohrabi, YTS Maryam… - Russian Journal of …, 2024 - journals.rcsi.science
Interior Fars region is an important geological province of Zagros basin due to historical
events. The present paper focused on the time span of the Asmari deposition (Oligo-Lower …
events. The present paper focused on the time span of the Asmari deposition (Oligo-Lower …