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Main Authors: Shimkus, Kazimir M, Rozanov, Alexander G
Format: Dataset Open Access
Language:en
Published: PANGAEA 2000
Subjects:
Online Access:https://doi.org/10.1594/PANGAEA.784907
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author Shimkus, Kazimir M
Rozanov, Alexander G
author_facet Shimkus, Kazimir M
Rozanov, Alexander G
collection Datos científicos de ciencias marinas y ambientales
contents An investigation of recent bottom sediments between the Cyprus Island and the Syrian seacoast during Cruise 27 of R/V Vityaz-2 (1993) gave comprehensive field data significantly complementing our understanding of the sedimentation process in this part of the Mediterranean Sea. Mineralogical and geochemical indicators testify to different input into sedimentation of the Syrian and Nile River sources. The Nile River plays a leading role in terrigenous sedimentation in the southeastern Mediterranean Sea, especially in deep-sea areas. In contrast, contribution of weathering products of basalts and ophiolites from the Syrian drainage area (hornblende, monoclinic and rhombic pyroxenes, olivine, spinel, palagonite, and epidote) are particularly detectable in sediments of the near-coast zone. During Late Quaternary contribution of terrigenous material both from the Syrian and Nile sources was irregular in time.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_784907
institution PANGAEA
language en
publishDate 2000
publisher PANGAEA
record_format pangaea
spellingShingle Composition of bottom sediments from the Mediterranean Sea off Syria
Shimkus, Kazimir M
Rozanov, Alexander G
Archive of Ocean Data; ARCOD; GC; Gravity corer; Mediterranean Sea; MULT; Multiple investigations; Vy27-3856; Vy27-3866; Vy27-3867; Vy27-3869; Vy27-3870; Vy27-3941; Vy27-3942; Vy27-3943; Vy27-3944; Vy27-3947; Vy27-3953; Vy27-3960; Vy27-4007
An investigation of recent bottom sediments between the Cyprus Island and the Syrian seacoast during Cruise 27 of R/V Vityaz-2 (1993) gave comprehensive field data significantly complementing our understanding of the sedimentation process in this part of the Mediterranean Sea. Mineralogical and geochemical indicators testify to different input into sedimentation of the Syrian and Nile River sources. The Nile River plays a leading role in terrigenous sedimentation in the southeastern Mediterranean Sea, especially in deep-sea areas. In contrast, contribution of weathering products of basalts and ophiolites from the Syrian drainage area (hornblende, monoclinic and rhombic pyroxenes, olivine, spinel, palagonite, and epidote) are particularly detectable in sediments of the near-coast zone. During Late Quaternary contribution of terrigenous material both from the Syrian and Nile sources was irregular in time.
title Composition of bottom sediments from the Mediterranean Sea off Syria
topic Archive of Ocean Data; ARCOD; GC; Gravity corer; Mediterranean Sea; MULT; Multiple investigations; Vy27-3856; Vy27-3866; Vy27-3867; Vy27-3869; Vy27-3870; Vy27-3941; Vy27-3942; Vy27-3943; Vy27-3944; Vy27-3947; Vy27-3953; Vy27-3960; Vy27-4007
url https://doi.org/10.1594/PANGAEA.784907