Sructural analysis of Ipek(south of Eshtehard to South Of Booin Zahra)
| Category | Tectonic & Seismotectonic |
|---|---|
| Group | GSI.IR |
| Location | 21th symposium on geosciences |
| Holding Date | 24 May 2008 |
Abstract:
The area of study is closed between longitude (50?,00 to 50?,25?) , and latitude (35?,30? to 35?, 50?). This region is effected by Alpine Phases .That is caused the main structure to be created . These structures are including , faults , folds , dykes. and joints.
The analysis of these structures leads us to get the direction of main stress . For example, the direction of stress in this area, and we can realized the relationship of (R,R? and P ) fractures and (D) main foult . We can recognize the compression and shear forces in this area too.
General:
The area of study is closed between longitude (50? ,00 to 50? ,52?), and latitude (35? ,30' to 35? ,50?). This region is effected by Alpine Phases. That is caused the main structure to be created. These structures are including, faults, folds, dykes. And foints.
The analysis of these structures lesds us to get the direction of main stress. For example, the direction of stress in this area, and we can realized the relationship of (R,R? and p) fractures and (D) main foult. We can recognize the compression and shear forces in this area too.