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Chordata
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Reptilia
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Archosauria
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Lepidosauria
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Plesiosauria (1)
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Invertebrata
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Protista
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isotopes
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Mediterranean region (2)
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Mediterranean Sea
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Mesozoic
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Precambrian
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upper Precambrian
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GeoRef Categories
Era and Period
Epoch and Age
Book Series
Date
Availability
Sudr Chalk
Figure 1. Location (inset) and geology of Gebel El Minshera, modified from ... Available to Purchase
Early Maastrichtian-Early Eocene Biostratigraphy of El Hasana Area, Central Sinai, Egypt Available to Purchase
RECENT LITERATURE ON FORAMINIFERA Available to Purchase
Geology and hydrocarbon habitat in a rift setting: southern Gulf of Suez, Egypt Available to Purchase
Geology and hydrocarbon habitat in rift setting: northern and central Gulf of Suez, Egypt Available to Purchase
Sinai hinge belt: a major crustal boundary in NE Africa Available to Purchase
Carbonate Platform to Basin Transition along an Upper Cretaceous to Lower Tertiary Syrian Arc Uplift, Galala Plateaus, Eastern Desert of Egypt Open Access
Microfacies Analysis and Cyclostratigraphy of the Upper Cretaceous-Lower Paleogene Succession of Bir Dakhl Section, North Eastern Desert, Egypt Available to Purchase
A Common Source Rock for Egyptian and Saudi Hydrocarbons in the Red Sea Available to Purchase
Control of compressional transfer zones on syntectonic and post-tectonic sedimentation: implications for hydrocarbon exploration Available to Purchase
Spatial and temporal variation of Syrian Arc structures in the onshore and offshore Eastern Mediterranean region Available to Purchase
A new Palaeocene albulid (Teleostei: Elopomorpha) from the Ouled Abdoun phosphatic basin, Morocco Available to Purchase
Petroleum geology and potential hydrocarbon plays in the Gulf of Suez rift basin, Egypt Available to Purchase
A Middle–Late Eocene vertebrate fauna (marine fish and mammals) from southwestern Morocco; preliminary report: age and palaeobiogeographical implications Available to Purchase
RECENT LITERATURE ON FORAMINIFERA Available to Purchase
The Paleocene/Eocene boundary in Egypt: An overview Available to Purchase
The structure of the Gulf of Suez (Clysmic) rift, with special reference to the eastern side Available to Purchase
Tectonic Framework of Egypt and Its Influence on Distribution of Foraminifera Available to Purchase
Magnetostratigraphy Susceptibility Used for High-Resolution Correlation Among Santonian (Upper Cretaceous) Marine Sedimentary Sequences in the U.S. Western Interior Seaway and the Western Sinai Peninsula, Egypt Available to Purchase
Abstract Magnetic susceptibility (MS) measurements of marine rocks provide an underutilized but powerful high-resolution tool in stratigraphy. In ideal circumstances and when combined with other stratigraphic techniques, the method can yield resolution to 10,000 years or less. This paper applies the MS method to solving a Cretaceous global correlation problem. Because of the active global processes that drove significant evolutionary changes during this time, the Upper Cretaceous is important in Earth history. However, correlations among geological sequences are difficult, in part because Earth’s magnetic polarity was essentially non-varying from the Aptian to the Santonian. Here we present high-resolution correlations for Upper Cretaceous marine sedimentary successions spanning all or part of the Santonian Stage from the Western Interior Seaway (U.S.A.) and the Western Sinai Peninsula (Egypt). To do this we have integrated the results of magnetic susceptibility (MS) measurements of unoriented samples from lithified marine rocks (in outcrop and from core) and biostratigraphic data sets from these sequences. In this study a MS zonation for the Santonian Stage has been developed and graphic comparison has been used for correlation. In the main, correlation between the U.S. and Egyptian sequences is excellent. Third order T/ R cycles (> 100 kyr) observed in this high-resolution data set for the Santonian Stage indicate significant similarities between the U.S. and Egyptian sections and allow correlation among sequences. We interpret these correlations to result from cyclicities caused by climate-controlled continental erosion and deposition of detrital components, mainly clay, in the marine realm. Second-order cycles (> 1 Myr) are also observed in these data sets but show distinctive differences between the U.S. and Egyptian sequences. We interpret these second-order differences to result from local synsedimentary tectonic controls on sediment erosion and deposition. Also observed are two distinct, short-term MS marker events that can be correlated globally. Application of Modern Stratigraphic Techniques: Theory and Case Histories SEPM Special Publication No. 94, Copyright © 2010 SEPM (Society for Sedimentary Geology), ISBN 978-1-56576-199-5, p. 155–166.