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Lithospheric deformation on Earth is localized under both brittle and ductile deformation conditions. As high-temperature ductile rheologies are fundamentally strain-rate hardening, the formation of localized ductile shear zones must involve a structural or ...
Reference: Journal of Structural Geology xxx (2013) 1e13
<p>A GPS-derived velocity field is presented from a dense geodetic network (~5km distance between stations) established in the broader area of Athens. It shows significant local variations of strain rates across a major inactive tectonic boundary separating ...
Reference: ANNALS OF GEOPHYSICS, 56, 6, 2013
<p>We present a tectonic map of the Tauern Window and surrounding units (Eastern Alps, Austria), combined with a series of crustal-scale cross-sections parallel and perpendicular to the Alpine orogen. This compilation, largely based on literature data and ...
Reference: Swiss J Geosci (2013) 106:1–32
In this contribution, is presented evidence for ductile E-W extension in the Kung Co area of southern Tibet that took place at ~19 Ma and is associated with a major N-S trending normal fault.
Reference: Earth and Planetary Science Letters 325-326 (2012), 10-20
<p>The East Anatolian fault system (EAFS) is the 80-km-wide, 700-km-long, NE trending sinistral strike-slip fault system forming a seismically very active intracontinental transfom fault boundary. It is located between Karlıova County in the northeast and ...
Reference: Turkish Journal of Earth Sciences (Turkish J. Earth Sci.), Vol. 21, 2012, pp. 547–570.
In this paper the structural relationships and their interpretations were investigated and analyzed in detail with the aim of unravelling the tectonic evolution of the Nigerian basement.
Reference: Journal of Engineering and Technology Research Vol. 3(4), pp. 133-138, April 2011
This paper presents the results of a structural-kinematic and petrographic analysis of the Novillo Gneiss (Trainor, 2010), which is combined with published age data in order to establish a tectonothermal history.
Reference: Revista Mexicana de Ciencias Geol?gicas, v. 28, num. 3, 2011, p. 580-592
<p>The East Anatolian fault system (EAFS) is the 80-km-wide, 700-km-long, NE trending sinistral strike-slip fault system forming a seismically very active intracontinental transfom fault boundary. It is located between Karlıova County in the northeast and ...
Reference: Turkish Journal of Earth Sciences (Turkish J. Earth Sci.), Vol. 21, 2012, pp. 1–. Copyright ©TÜBİTAK First published online 16 August 2011
<p>Crustal deformation is the study of active geophysical processes that occur within he earth&rsquo;s lithosphere. Geodesy provides facilities to investigate the earth&rsquo;s crust ovements and shares these data with the other disciplines. The various sources ...
Reference: Scientific Research and Essays Vol. 5 (9), pp. 911-916, 4 May, 2010
The authors present a numerical modeling study that examines the deformational response of western North America to Baja California and/or Sierra Nevada microplate motion. In particular we study if, and under what condition of microplate motion, shear strain ...
Reference: Tectonophysics 485 (2010) 78-84