Late Pan-African granite emplacement during regional deformation, evidence from magnetic fabric and structural studies in the Hammamat–Atalla area, Central Eastern Desert of Egypt
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R. Greiling | M. Sadek | C. Dietl | H. Wall
[1] T. Kusky,et al. Orogen styles in the East African Orogen: A review of the Neoproterozoic to Cambrian tectonic evolution , 2013, Journal of African earth sciences.
[2] Atef A. Qaddah,et al. Three-dimensional structure of Conrad and Moho discontinuities in Egypt , 2013 .
[3] A. Fowler,et al. Sedimentation and inversion history of three molasse basins of the western Central Eastern Desert of Egypt: Implications for the tectonic significance of Hammamat basins , 2013 .
[4] K. Burke,et al. Tectonic Escape in the Evolution of the Continental Crust , 2013 .
[5] J. Nzenti,et al. Strain partitioning along the Neoproterozoic Central Africa Shear Zone system: structures and magnetic fabrics (AMS) from the Meiganga area, Cameroon , 2012 .
[6] R. Greiling,et al. Rocks, fabrics and magnetic anisotropy: an introduction to the issue in honour of František Hrouda , 2012, International Journal of Earth Sciences.
[7] T. Kusky,et al. Late Cryogenian-Ediacaran history of the Arabian-Nubian Shield: A review of depositional, plutonic, structural, and tectonic events in the closing stages of the northern East African Orogen , 2011 .
[8] S. Fishwick,et al. Towards a better understanding of African topography: a review of passive-source seismic studies of the African crust and upper mantle , 2011 .
[9] G. Y. Boghdady,et al. Structural constraints on the evolution of the Meatiq Gneiss Dome (Egypt), East-African Orogen , 2010 .
[10] M. El-Wahed. The role of the Najd Fault System in the tectonic evolution of the Hammamat molasse sediments, Eastern Desert, Egypt , 2010 .
[11] J. Nzenti,et al. Pan-African strike–slip tectonics in eastern Cameroon—Magnetic fabrics (AMS) and structure in the Lom basin and its gneissic basement , 2009 .
[12] F. Corfu,et al. U–Pb TIMS age constraints on the evolution of the Neoproterozoic Meatiq Gneiss Dome, Eastern Desert, Egypt , 2009 .
[13] A. Tryggvason,et al. Mountain building processes during continent-continent collision in the Uralides , 2008 .
[14] D. Bernoulli,et al. The Alpine-Carpathian-Dinaridic orogenic system: correlation and evolution of tectonic units , 2008 .
[15] A. Fowler,et al. El Sibai gneissic complex, Central Eastern Desert, Egypt: Folded nappes and syn-kinematic gneissic granitoid sheets – not a core complex , 2007 .
[16] Ahmed Akawy. Geometry and texture of quartz veins in Wadi Atalla area, Central Eastern Desert, Egypt , 2007 .
[17] H. Koyi,et al. Centrifuge modelling of plutons intruding shear zones: application to the Fürstenstein Intrusive Complex (Bavarian Forest, Germany) , 2006 .
[18] R. Greiling,et al. Granite emplacement and its relation with regional deformation in the Aravalli Mountain Belt (India)—inferences from magnetic fabric , 2005 .
[19] R. Greiling,et al. A Quantitative structural study of late pan-african compressional deformation in the central eastern desert (Egypt) during Gondwana assembly , 2005 .
[20] R. Gayer,et al. Thrustbelts: Structural Architecture, Thermal Regimes and Petroleum Systems , 2005 .
[21] B. E. Kalioubi,et al. Gravitational collapse origin of shear zones, foliations and linear structures in the Neoproterozoic cover nappes, Eastern Desert, Egypt , 2004 .
[22] J. Dewey,et al. Changing Silurian–Devonian relative plate motion in the Caledonides: sinistral transpression to sinistral transtension , 2003, Journal of the Geological Society.
[23] H. Fritz,et al. Neoproterozoic tectonothermal evolution of the Central Eastern Desert, Egypt: a slow velocity tectonic process of core complex exhumation , 2002 .
[24] P. Barbey,et al. Role of magma pressure, tectonic stress and crystallization progress in the emplacement of syntectonic granites. The A-type Estrela Granite Complex (Carajás Mineral Province, Brazil) , 2001 .
[25] J Loizenbauer,et al. Structural geology, single zircon ages and fluid inclusion studies of the Meatiq metamorphic core complex: Implications for Neoproterozoic tectonics in the Eastern Desert of Egypt , 2001 .
[26] T. Fowler,et al. Gneiss-cored interference dome associated with two phases of late Pan-African thrusting in the Central Eastern Desert, Egypt , 2001 .
[27] T. Fowler. Pan-African granite emplacement mechanisms in the Eastern Desert, Egypt , 2001 .
[28] A. Kontny,et al. Case Studies on the Use of Temperature-Dependent Susceptibility for the Characterisation of Magneto-Mineralogical Changes During Metamorphism , 2000 .
[29] A. Sinha. Basement Tectonics 13 , 1999 .
[30] J. Cuevas,et al. The Los Pedroches Batholith (Southern Spain): Polyphase Interplay between Shear Zones in Transtension and Setting of Granites , 1997 .
[31] H. Fritz,et al. Formation of Neoproterozoic metamorphic complex during oblique convergence (Eastern Desert, Egypt) , 1996 .
[32] R. Greiling,et al. A structural synthesis of the Proterozoic Arabian-Nubian Shield in Egypt , 1994 .
[33] F. Hrouda. A technique for the measurement of thermal changes of magnetic susceptibility of weakly magnetic rocks by the CS-2 apparatus and KLY-2 Kappabridge , 1994 .
[34] H. Walther. The Turin Papyrus - The oldest geological and mineral map in the world , 1994 .
[35] R. Stern. ARC Assembly and Continental Collision in the Neoproterozoic East African Orogen: Implications for the Consolidation of Gondwanaland , 1994 .
[36] J. Bouillin,et al. Granite emplacement in an extensional setting: an AMS study of the magmatic structures of Monte Capanne (Elba, Italy) , 1993 .
[37] D. H. Tarling,et al. The magnetic anisotropy of rocks , 1993 .
[38] R. Holdsworth,et al. Sinistral transpression and the Silurian closure of Iapetus , 1992, Journal of the Geological Society.
[39] P. Rochette,et al. Rock magnetism and the interpretation of anisotropy of magnetic susceptibility , 1992 .
[40] M. Brown,et al. Granite magma generation, ascent and emplacement within a transpressional orogen , 1992, Journal of the Geological Society.
[41] J. A. Harrell,et al. The World's Oldest Surviving Geological Map: The 1150 B.C. Turin Papyrus from Egypt , 1992, The Journal of Geology.
[42] G. Borradaile. Correlation of strain with anisotropy of magnetic susceptibility (AMS) , 1991 .
[43] G. Borradaile. Magnetic susceptibility, petrofabrics and strain , 1988 .
[44] Raymond E. Arvidson,et al. Extension of the Najd Shear System from Saudi Arabia to the central eastern desert of Egypt based on integrated field and LANDSAT observations , 1988 .
[45] G. Draper. Geological strain analysis—a manual for the Rf/φ technique: by Richard J. Lisle. Pergamon Press, Oxford, 1985, viii + 99 pp. $15 hard cover/$8.95 soft cover , 1986 .
[46] L. Brown,et al. Reflection seismology : the continental crust , 1986 .
[47] R. Stern. The Najd Fault System, Saudi Arabia and Egypt: A Late Precambrian rift‐related transform system? , 1985 .
[48] R. Stern,et al. Geochronologic and isotopic constraints on late Precambrian crustal evolution in the Eastern Desert of Egypt , 1985 .
[49] M. Sultan,et al. Geology and origin of Meatiq Dome, Egypt: A Precambrian metamorphic core complex? , 1983 .
[50] A. Ries,et al. Pan-African structures, ophiolites and mélange in the Eastem Desert of Egypt: a traverse at 26°N , 1983, Journal of the Geological Society.
[51] M. F. Ramly,et al. A proposed new classification of the granites of egypt , 1982 .
[52] F. Hrouda. Magnetic anisotropy of rocks and its application in geology and geophysics , 1982 .
[53] V. Jelínek. Characterization of the magnetic fabric of rocks , 1981 .
[54] D. Flinn. Construction and computation of three-dimensional progressive deformations , 1978, Journal of the Geological Society.
[55] A. Arzi. Critical phenomena in the rheology of partially melted rocks , 1978 .
[56] G. Knetsch. Überschiebungs-Tiefbau, Magmatismus und Lagerstätten-tradition in einem präkambrischen Molassebereich Ägyptens , 1959 .