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Hot Brines and Recent Heavy Metal Deposits in the Red Sea
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“In contrast, only two brine pools are classified as type I: the Oceanographer deep (26°17.2′N, 35°01.0′E)37 and the Kebrit deep (24°43.1′N, 36°17′E)38.”
From The Red Sea Deep Water is a potent source of atmospheric ethane and propane (2020) · cites this paper as [37]
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“…these structural trends are initiated in the Precambrian time and rejuvenated several times in other geologic periods as indicated by the affected rocks in the Red Sea area and other parts through North Africa (AbdelGawad 1969; Girdler 1969; Meshref 1990; Guiraud et al. 2001; Issawi 2002).”
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“Manganese and Fe concentrations in sediments were plotted as a function of distance from the Deep, together with the background values of these elements in normal Red Sea sediments.”
BackgroundInfluential
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- Venue
- Springer eBooks
- Publisher
- Springer Berlin Heidelberg
- Published
- 1969
- OpenAlex
- W2486748790
- Cited by
- 480
- References
- 0
- Citations by year
- 2026: 2 · 2025: 4 · 2024: 1 · 2023: 2 · 2022: 4 · 2021: 1 · 2020: 3 · 2019: 3 · 2018: 6 · 2017: 3 · 2016: 3 · 2015: 18 · 2014: 8 · 2013: 7 · 2012: 7
- FWCI
- 16.73
- Type
- book
- Language
- de
- Open access
- closed
- Licence
- www.springer.com/tdm (tdm)
- Locations
- Springer eBooks (publishedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Physical Sciences › Earth and Planetary Sciences › Oceanography › Marine and environmental studies
- Keywords
- hot brines, Red Sea, hydrothermal deposits, metal mineralization
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