(Table 1) Major and trace elements at DSDP Leg 57 Holes

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Main Author: Nohara, Masato
Format: Dataset Open Access
Language:en
Published: PANGAEA 1980
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author Nohara, Masato
author_facet Nohara, Masato
collection Datos científicos de ciencias marinas y ambientales
contents Several papers have recently appeared concerning the metalliferous sediments on the active oceanic ridges. The geochemistry of such sediments is reasonably well understood and the deposits generally considered to be products of volcanic processes (Boström and Peterson, 1969; Boström et al., 1969; Horowitz, 1970, 1974; Cronan et al., 1972; Cronan and Garrett, 1973; Piper, 1973). The geochemistry of trench sediments, however, is less well known. There is a great need for studies of trench inner slope sediments, particularly in view of the significance of such sediments as a record of the effects of oceanic plate subduction under the continental crust. Sampling by Glomar Challenger in the trench inner slope was therefore of utmost importance in determining the origin of trench inner slope deposits.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_823013
institution PANGAEA
language en
publishDate 1980
publisher PANGAEA
record_format pangaea
spellingShingle (Table 1) Major and trace elements at DSDP Leg 57 Holes
Nohara, Masato
57-438; 57-438A; 57-438B; 57-439; 57-440; 57-440A; 57-440B; 57-441; 57-441A; 57-441B; Aluminium; Atomic absorption spectrometry (AAS); Chromium; Cobalt; Copper; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Elevation of event; Event label; Glomar Challenger; Iron; Latitude of event; Leg57; Lithium; Longitude of event; Manganese; Nickel; North Pacific/BASIN; North Pacific/TRENCH; Sample code/label; Strontium; Titanium; Zinc
Several papers have recently appeared concerning the metalliferous sediments on the active oceanic ridges. The geochemistry of such sediments is reasonably well understood and the deposits generally considered to be products of volcanic processes (Boström and Peterson, 1969; Boström et al., 1969; Horowitz, 1970, 1974; Cronan et al., 1972; Cronan and Garrett, 1973; Piper, 1973). The geochemistry of trench sediments, however, is less well known. There is a great need for studies of trench inner slope sediments, particularly in view of the significance of such sediments as a record of the effects of oceanic plate subduction under the continental crust. Sampling by Glomar Challenger in the trench inner slope was therefore of utmost importance in determining the origin of trench inner slope deposits.
title (Table 1) Major and trace elements at DSDP Leg 57 Holes
topic 57-438; 57-438A; 57-438B; 57-439; 57-440; 57-440A; 57-440B; 57-441; 57-441A; 57-441B; Aluminium; Atomic absorption spectrometry (AAS); Chromium; Cobalt; Copper; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Elevation of event; Event label; Glomar Challenger; Iron; Latitude of event; Leg57; Lithium; Longitude of event; Manganese; Nickel; North Pacific/BASIN; North Pacific/TRENCH; Sample code/label; Strontium; Titanium; Zinc
url https://doi.org/10.1594/PANGAEA.823013