Element oxides in basaltic glass fragments from ODP Hole 203-1243B

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Hauptverfasser: Moberly, Ralph, Ishii, Teruaki, Garcia, M O, Ross, K, Artita, Kimberly
Format: Dataset Open Access
Sprache:en
Veröffentlicht: PANGAEA 2006
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author Moberly, Ralph
Ishii, Teruaki
Garcia, M O
Ross, K
Artita, Kimberly
author_facet Moberly, Ralph
Ishii, Teruaki
Garcia, M O
Ross, K
Artita, Kimberly
collection Datos científicos de ciencias marinas y ambientales
contents Sand-sized basaltic glass fragments were recovered in the liner of Core 203-1243B-19R, the deepest recovery from Hole 1243B. Microprobe analysis of 582 glassy cuttings cluster into five compositionally distinct groups, most of which are unlike the lithologic units described on board ship. Drilling operations intended to sweep cuttings from the caving hole and differences between the cuttings and geochemically distinct lithologic units of the upper part of the basement indicate that the cuttings came mainly, if not entirely, from the lower part of the hole. They give information about the part of Hole 1243B that had poor core recovery. Enriched mid-ocean-ridge basalt (MORB) from the upper part of the hole and transitional MORB from two groups of cuttings from sources low in the hole may be a trace of the Galápagos plume on the Pacific plate or may be a normal consequence of eruptions from two distinct magmas on fast-spreading crust.
format Dataset Open Access
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institution PANGAEA
language en
publishDate 2006
publisher PANGAEA
record_format pangaea
spellingShingle Element oxides in basaltic glass fragments from ODP Hole 203-1243B
Moberly, Ralph
Ishii, Teruaki
Garcia, M O
Ross, K
Artita, Kimberly
203-1243B; DRILL; Drilling/drill rig; Joides Resolution; Leg203; North Pacific Ocean; Ocean Drilling Program; ODP
Sand-sized basaltic glass fragments were recovered in the liner of Core 203-1243B-19R, the deepest recovery from Hole 1243B. Microprobe analysis of 582 glassy cuttings cluster into five compositionally distinct groups, most of which are unlike the lithologic units described on board ship. Drilling operations intended to sweep cuttings from the caving hole and differences between the cuttings and geochemically distinct lithologic units of the upper part of the basement indicate that the cuttings came mainly, if not entirely, from the lower part of the hole. They give information about the part of Hole 1243B that had poor core recovery. Enriched mid-ocean-ridge basalt (MORB) from the upper part of the hole and transitional MORB from two groups of cuttings from sources low in the hole may be a trace of the Galápagos plume on the Pacific plate or may be a normal consequence of eruptions from two distinct magmas on fast-spreading crust.
title Element oxides in basaltic glass fragments from ODP Hole 203-1243B
topic 203-1243B; DRILL; Drilling/drill rig; Joides Resolution; Leg203; North Pacific Ocean; Ocean Drilling Program; ODP
url https://doi.org/10.1594/PANGAEA.774362