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Hauptverfasser: Andrews, Anthony J, Dollase, W A, Fleet, M E
Format: Dataset Open Access
Sprache:en
Veröffentlicht: PANGAEA 1983
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Online-Zugang:https://doi.org/10.1594/PANGAEA.816466
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author Andrews, Anthony J
Dollase, W A
Fleet, M E
author_facet Andrews, Anthony J
Dollase, W A
Fleet, M E
collection Datos científicos de ciencias marinas y ambientales
contents Mössbauer analyses were conducted on a sample of saponite selected from DSDP Leg 69 basalt core. The sample was initially placed within a nitrogen-purged container on-board Glomar Challenger approximately three hours after recovery, where it remained until analysis. The Mössbauer data revealed an original, in situ Fe2O3/FeO ratio of 0.46, with both Fe**2+ and Fe**3+ in octahedral coordination. With controlled exposure to air under ambient laboratory storage conditions, the proportion of Fe**3+ increased from an original 30% to 51% over a period of about 11.5 months. The Fe**3+ thus produced remained in octahedral coordination, and no observable changes occurred in the physical appearance of the sample.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_816466
institution PANGAEA
language en
publishDate 1983
publisher PANGAEA
record_format pangaea
spellingShingle Sample descriptions, d-spacing and geochemistry at DSDP Holes 68-501 and 69-504B
Andrews, Anthony J
Dollase, W A
Fleet, M E
68-501; 69-504B; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Leg68; Leg69; North Pacific/FLANK
Mössbauer analyses were conducted on a sample of saponite selected from DSDP Leg 69 basalt core. The sample was initially placed within a nitrogen-purged container on-board Glomar Challenger approximately three hours after recovery, where it remained until analysis. The Mössbauer data revealed an original, in situ Fe2O3/FeO ratio of 0.46, with both Fe**2+ and Fe**3+ in octahedral coordination. With controlled exposure to air under ambient laboratory storage conditions, the proportion of Fe**3+ increased from an original 30% to 51% over a period of about 11.5 months. The Fe**3+ thus produced remained in octahedral coordination, and no observable changes occurred in the physical appearance of the sample.
title Sample descriptions, d-spacing and geochemistry at DSDP Holes 68-501 and 69-504B
topic 68-501; 69-504B; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Leg68; Leg69; North Pacific/FLANK
url https://doi.org/10.1594/PANGAEA.816466