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author Kuptsov, Vladimir M
Palkina, Alla M
author_facet Kuptsov, Vladimir M
Palkina, Alla M
collection Datos científicos de ciencias marinas y ambientales
contents Sedimentation rates (SR) for metalliferous and ore sediments containing ore material in 15 depressions of the Red Sea rift zone are discussed. SR for normal sediments was ca. 3.2 cm/ka in the second half of Holocene, 14.3 cm/ka yrs in the first half of Holocene, and 21.3 cm/ka in Late Würmian. Accumulation of metalliferous and ore sediments requires considerable accumulation of hydrothermal matter. Ore sediments have been found primarily in the Atlantis II and Chain Deeps; average sedimentation rate in these depressions is 90.0 cm/ka. In other depressions geothermal activity during considered time intervals was lower, and ore material occurs as admixture or in layers.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_756799
institution PANGAEA
language en
publishDate 1987
publisher PANGAEA
record_format pangaea
spellingShingle Radiocarbon ages of bottom sediments and sedimentation rates in depressions of the Red Sea rift zone
Kuptsov, Vladimir M
Palkina, Alla M
Archive of Ocean Data; ARCOD; GC; Grab; GRAB; Gravity corer; PIKAR; PS-223; PS-224; PS-225; PS-361; PS-362; PS-363; PS-364; PS-365; PS-366; PS-368; PS-383; PS-385; PS-387; PS-391; PS-398; PS-399; PS-400; PS-402; PS-406; PS-408; PS-410; PS-411; PS-412; PS-413; PS-414; Red Sea; Red Sea, Albatros Deep; Red Sea, Atlantis II Deep; Red Sea, Discovery Deep; Red Sea, Erba Deep; Red Sea, Gipsum Deep; Red Sea, Hadarba Deep; Red Sea, Kebrit Deep; Red Sea, Nereus Deep; Red Sea, Port Sudan Deep; Red Sea, Shagara Deep; Red Sea, Suakin Deep; Red Sea, Tethis Deep; Red Sea, Valdivia Deep; Red Sea, Vema Deep
Sedimentation rates (SR) for metalliferous and ore sediments containing ore material in 15 depressions of the Red Sea rift zone are discussed. SR for normal sediments was ca. 3.2 cm/ka in the second half of Holocene, 14.3 cm/ka yrs in the first half of Holocene, and 21.3 cm/ka in Late Würmian. Accumulation of metalliferous and ore sediments requires considerable accumulation of hydrothermal matter. Ore sediments have been found primarily in the Atlantis II and Chain Deeps; average sedimentation rate in these depressions is 90.0 cm/ka. In other depressions geothermal activity during considered time intervals was lower, and ore material occurs as admixture or in layers.
title Radiocarbon ages of bottom sediments and sedimentation rates in depressions of the Red Sea rift zone
topic Archive of Ocean Data; ARCOD; GC; Grab; GRAB; Gravity corer; PIKAR; PS-223; PS-224; PS-225; PS-361; PS-362; PS-363; PS-364; PS-365; PS-366; PS-368; PS-383; PS-385; PS-387; PS-391; PS-398; PS-399; PS-400; PS-402; PS-406; PS-408; PS-410; PS-411; PS-412; PS-413; PS-414; Red Sea; Red Sea, Albatros Deep; Red Sea, Atlantis II Deep; Red Sea, Discovery Deep; Red Sea, Erba Deep; Red Sea, Gipsum Deep; Red Sea, Hadarba Deep; Red Sea, Kebrit Deep; Red Sea, Nereus Deep; Red Sea, Port Sudan Deep; Red Sea, Shagara Deep; Red Sea, Suakin Deep; Red Sea, Tethis Deep; Red Sea, Valdivia Deep; Red Sea, Vema Deep
url https://doi.org/10.1594/PANGAEA.756799