Persian
Home | News | Articles | Gallery | FAQ | Contact us | Sitemap | About us
Menu
Geology
Exploration
Geomatics
Chemistry lab
Geology Museum
geological maps
Main Projects
Finance & Official
Publication and Library
Articles
Thesises Index
Environment
Innovation and dehiscence year
uses of Geology
Geotourism
Quarterly Journal Geosciences Index
Geology of Khorassan
mines of Khorasan
book introduction
About us
services and products
Knowledges of Geology
The Eastern sun
Famous geoscientist of Iran
seminars
mashad
Geology and mine laws
Park Museum
Hot Links
Khorassan Geotourism
Khorassan's warm springs
GSINET project
Subsidence in Mashhad plate
Geology Museum
Home » Articles

Articles

Refference : The 25th Symposium on Geoscience;Tehran
Publishing Year : 1385

Abstract :

Folding in Quaternary and Neogen deposition the north of the Birjand has made by blinde thrust. Resulting field evidence show fold is in the B group with low slop in the north limb(7°) and high slop(42°) in the south limb. Fault scarp andfault plane which it has been measured in Hjiabad show 270-280N trend for the main fault. Tension joint show N- NE trend for pressure stress. Axial surface, fault and joint all illustrate this trend.
Axial surface of the fold and fault plane, both, have the northern slop and show southern movement in material.


Subject List : Kinetic model

E-mail : info [at] gsinet [dot] ir
Last Update: 2010/09/26
Copyright © 2002-2007 GSINET , All rights reserverd.
P.B. : 91735-1166
18 Str. Sarafrazan Blv. Hour Sq., Mashhad - Iran
Tel: + 98 511 8218146-8 / Fax; +98 511 821 6044