TECTONICS, VOL. 25, TC1003, doi:[removed]2005TC001831, 2006 Late Cenozoic and modern stress fields in the western Fars (Iran): Implications for the tectonic and kinematic evolution of central Zagros O. Lacombe and F. Mou

First Page		Document Content
Date: 2007-10-03 11:25:52 Fault Inversion Focal mechanism Earthquake Thrust fault Décollement Shear Fold Detachment fold Geology Structural geology Zagros Mountains		TECTONICS, VOL. 25, TC1003, doi:[removed]2005TC001831, 2006 Late Cenozoic and modern stress fields in the western Fars (Iran): Implications for the tectonic and kinematic evolution of central Zagros O. Lacombe and F. Mou Add to Reading List Source URL: bmeyer2.free.fr Download Document from Source Website File Size: 2,92 MB Share Document on Facebook

	Earth-Science Reviews – 138 www.elsevier.com/locate/earscirev The Black Mountains turtlebacks: Rosetta stones of Death Valley tectonics Marli B. Miller a,*, Terry L. Pavlis b DocID: 1qKav - View Document
	SummerInvestigations • Service • Information Vol. 19, No. 2 DocID: 1pG7p - View Document
	Analytical and Numerical Investigation of 3D Multilayer Detachment Folding Naiara Fernández and Boris Kaus 1 Introduction Folding is a common mode of deformation in geology when mechanically layered DocID: 1laHk - View Document
	Reprinted from Journal of Structural Geology, 2014, in press Quantifying the geometry, displacements, and subresolution deformation in thrust-ramp anticlines with growth and erosion: From models to seismic-reflection pr DocID: 1g4LI - View Document
	Reprinted from Journal of Structural Geology Bed length does not remain constant during deformation: Recognition and why it matters Richard H. Groshong, Jr.a, Martha Oliver Withjackb, Roy W. Schlischeb, DocID: 1fDKq - View Document