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The AAPG/Datapages Combined Publications Database

AAPG Bulletin

Abstract


Volume: 50 (1966)

Issue: 9. (September)

First Page: 1890

Last Page: 1898

Title: General Outlines of Epeirogenesis and Sedimentation in Region Between Safaga, Quseir, and Southern Wadi Qena Area, Eastern Desert, Egypt

Author(s): El-Sayed El-Tarabili (2)

Abstract:

The Egyptian region of the Red Sea depression attained its present configuration primarily as a result of a series of epeirogenic movements. The area between Quseir, Safaga, and the southern part of Wadi Qena was subjected to a series of alternations between major faulting and regional uplift. Structurally, the basement complex of the Red Sea mountain range (west side of Red Sea) constitutes a major horst with a general Erythrean structural direction (northwest-southeast). East of the horst, toward the Red Sea coast, is a group of step faults, ranging in age from post-early Eocene to Pleistocene-Recent. These main faults were shoreline zones during periods of marine sedimentation. The whole area was subjected to successive uplifts, forming an anteclise whose axis parallel d the present Red Sea mountain range.

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