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This book focuses on the structural setting of the well known "El Qaa Fault Block" which is a NE-dipping block in the eastern side of the Gulf of Suez rift, Sinai Peninsula, Egypt. The Gulf of Suez rift is the northwestern arm of the Oligo-Miocene Red Sea rift. The structural model presented in this study involves the young age of the oblique faults relative to the rift-parallel (Clysmic) faults and their relation to the movement on the Dead Sea transform.

Produktbeschreibung
This book focuses on the structural setting of the well known "El Qaa Fault Block" which is a NE-dipping block in the eastern side of the Gulf of Suez rift, Sinai Peninsula, Egypt. The Gulf of Suez rift is the northwestern arm of the Oligo-Miocene Red Sea rift. The structural model presented in this study involves the young age of the oblique faults relative to the rift-parallel (Clysmic) faults and their relation to the movement on the Dead Sea transform.
Autorenporträt
Assoc. Prof. of Structural Geology and Head of Geological Applications and Mineral Resources Division at the Egyptian National Authority for Remote Sensing and Space Sciences in Cairo.Born in 1959 in Cairo, EgyptB.Sc. & M.Sc. in Geology, 1981 & 1988, Ain Shams University, Cairo. PhD in Structural Geology, 1995 at Heidelberg University,Germany