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author Presley, Bobby J
Kaplan, Isaac R
author_facet Presley, Bobby J
Kaplan, Isaac R
collection Datos científicos de ciencias marinas y ambientales
contents The interstitial water received at UCLA from Leg 7 (Guam to Hawaii) consisted of forty-two samples of approximately 5 milliliters each, three samples of approximately 10 milliliters each, and three samples of approximately 100 milliliters each. These pore waters had been squeezed from sediments consisting primarily of biogenic ooze, and had been collected at five different drilling sites along the route. High cobalt value were observed at Site 66 and were accompanied by a relatively high manganese concentration, but more normal iron, nickel and copper concentrations. This apparent cobalt enrichment could not be explained at the time of procedure. The line Islands area were Site 66 is situated was later notoriously known for its high Co values in manganese crust deposits (see, He, G., Ma, W., Song, C., Yang, S., Zhu, B., Yao, H., Jiang, X., Cheng, Y., 2011. Distribution characteristics of seamount cobalt-rich ferromanganese crusts and the determination of the size of areas for exploration and exploitation. Acta Oceanologica Sinica 30, 63–75. doi:10.1007/s13131-011-0120-9).
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_868503
institution PANGAEA
language en
publishDate 1971
publisher PANGAEA
record_format pangaea
spellingShingle (Table 2, page 887) Trace constituents of interstitial water, DSDP Leg 7, from large volume ( about 100 ml) squeezing (Cores 62A-12, 65-9, 66-7)
Presley, Bobby J
Kaplan, Isaac R
7-62A; 7-65; 7-66; Atomic absorption spectrometry (AAS); Cobalt; Comment; Copper; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Iron; Leg7; Manganese; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Pacific/BASIN; North Pacific/RIDGE; Sample code/label; Sediment type; Silicon
The interstitial water received at UCLA from Leg 7 (Guam to Hawaii) consisted of forty-two samples of approximately 5 milliliters each, three samples of approximately 10 milliliters each, and three samples of approximately 100 milliliters each. These pore waters had been squeezed from sediments consisting primarily of biogenic ooze, and had been collected at five different drilling sites along the route. High cobalt value were observed at Site 66 and were accompanied by a relatively high manganese concentration, but more normal iron, nickel and copper concentrations. This apparent cobalt enrichment could not be explained at the time of procedure. The line Islands area were Site 66 is situated was later notoriously known for its high Co values in manganese crust deposits (see, He, G., Ma, W., Song, C., Yang, S., Zhu, B., Yao, H., Jiang, X., Cheng, Y., 2011. Distribution characteristics of seamount cobalt-rich ferromanganese crusts and the determination of the size of areas for exploration and exploitation. Acta Oceanologica Sinica 30, 63–75. doi:10.1007/s13131-011-0120-9).
title (Table 2, page 887) Trace constituents of interstitial water, DSDP Leg 7, from large volume ( about 100 ml) squeezing (Cores 62A-12, 65-9, 66-7)
topic 7-62A; 7-65; 7-66; Atomic absorption spectrometry (AAS); Cobalt; Comment; Copper; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Iron; Leg7; Manganese; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Pacific/BASIN; North Pacific/RIDGE; Sample code/label; Sediment type; Silicon
url https://doi.org/10.1594/PANGAEA.868503