Geomorphic Signatures of Active Tectonics of Darian Area, Northeast of Shiraz, Iran

Paper Details

Research Paper 01/07/2015
Views (244) Download (9)
current_issue_feature_image
publication_file

Geomorphic Signatures of Active Tectonics of Darian Area, Northeast of Shiraz, Iran

Mahdi Azadmanesh, Mohsen Pour kermani, Abdolmajid Asadi, Manouchehr Ghorashi, Ali Solgi
J. Bio. Env. Sci.7( 1), 572-578, July 2015.
Certificate: JBES 2015 [Generate Certificate]

Abstract

This paper examines both the relative Active Tectonics of Gadvan anticline based on morphometric parameters and their application in morphology and topography evolution in northeast of Shiraz. In the present study, the analysis including line ament mapping, length density mapping, intersection and the counts of lineaments and also the calculation of three geomorphic parameters (Smf, facet% and Vf) have been conducted. Some of which can be used in the study of morphology. According to the classification of geomorphic indicators, the study area was tectonically detected as an area within tense activity. Therefore, the uplift rate in this area is over the front of the mountain which is estimated about 1/5 to 4 mm per year. In the study, for the extraction of lineaments, automatic and semi-automatic methods along with manual one werealso conducted. Area lineament maps and length density, counts not only specifies areas with anomalous fracture but also can contribute in determining the location of drilling water wells of Darian plains.

VIEWS 13

Berberian M. 1995. Master blind thrust faults hidden under the zagros folds: Active basement tectonics and surface morph tectonics, Tectonics and surface morph tectonic, tectonophysics 241, 193-224. A.

Bull WB, Mcfadden LD. 1977. Tectonic geomorp-hology north and south of the Garlock fault, proceeding of the 8th Annual geomorphology symposium, New York.

Bull WB. 1978. Geomorphic tectonic classes of the south front of the San Gabried Mountains, California, U.S. Geological survey contract Report 14-08-001-G-394, office of Earthquakes, Volcanoes & Engineering: Menlo park CA.

Kocal A. 2004. A methodology for detection and evaluation of lineament from satellite imagery, Ms. Thesis, Middle East Technical University, 121 p.

Lee ST, Yu TT, Wang CL, Peng WF. 2007. Automatic Geological Lineaments Extraction from Digital Elevation Model of Airborne LiDAR, Geophysical Research Abstracts, 9, SRef-ID: 1607-7962/ European Geosciences Union.

Naylor, MA. 1986. Fault geometries in basement in duced wrench faulting under different initial stress states, Jur. Struct. Geol 8, 737-752.

Oliver D. 1987. The development of structural patterns above reactivated basement faults, in: Price, 1990, Analysis of geological structures, Cambridge university Press.

Ragan DM. 1985. structural geology, John Wiley and sons Inc.

Ramsay JC, Huber M. 1987. The techniques of modern structural geology, Vol. 2, Folds and fractures, Academic press London.

Stewart IS, Hancock PL. 1994. geotectonic. In: continental deformation (Edited by P.L. Hancock), Pergamum press.

Wells SG. 1988. Regional variation in tectonic geomorphology along a segmented convergent plate boundary pacific coast of coastal Rica, Geomorphology 1, 239-265.

Zamani A, Malek A. 1987. The application of morphometric parameters in Neo-tectonic studies of the southern parts of Central Alborz, Master’s thesis in tectonics, Shiraz University.