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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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BackgroundInfluential
Metadata
- 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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