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The AAPG/Datapages Combined Publications Database
AAPG Bulletin
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The Wadi Khaboba-Gebel Nukhul high, in the Um Bogma area of southwestern Sinai, underwent a small-scale uplift-subsidence cycle during the Paleozoic. The trend of this structure is close to and almost parallel with the Suez rift, indicating that the young rift is related to older structures.
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