Chemical composition of hydrogarnet and celadonite from ODP Hole 206-1256D

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Autore principale: Laverne, Christine
Natura: Dataset Open Access
Lingua:en
Pubblicazione: PANGAEA 2006
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author Laverne, Christine
author_facet Laverne, Christine
collection Datos científicos de ciencias marinas y ambientales
contents Mid-ocean-ridge basalts recovered from Hole 1256D during Ocean Drilling Program Leg 206 exhibit the effects of various low-temperature (<100°C) alteration processes, including the formation of black or dark green alteration halos adjacent to celadonite-bearing veins. In several samples from the deepest basalts, a Ti-rich hydrogarnet occurs. To our knowledge, such a mineral has never been reported in the oceanic crust. This report presents a brief description and microprobe analyses of this hydrogarnet and associated celadonite. More detailed characterizations of this mineral and a description of its relationship to other secondary minerals will be undertaken in a future study, in an attempt to determine the mineral's formation conditions and its place in the general alteration history of the Hole 1256D basalts.
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institution PANGAEA
language en
publishDate 2006
publisher PANGAEA
record_format pangaea
spellingShingle Chemical composition of hydrogarnet and celadonite from ODP Hole 206-1256D
Laverne, Christine
206-1256D; DRILL; Drilling/drill rig; Joides Resolution; Leg206; North Pacific Ocean; Ocean Drilling Program; ODP
Mid-ocean-ridge basalts recovered from Hole 1256D during Ocean Drilling Program Leg 206 exhibit the effects of various low-temperature (<100°C) alteration processes, including the formation of black or dark green alteration halos adjacent to celadonite-bearing veins. In several samples from the deepest basalts, a Ti-rich hydrogarnet occurs. To our knowledge, such a mineral has never been reported in the oceanic crust. This report presents a brief description and microprobe analyses of this hydrogarnet and associated celadonite. More detailed characterizations of this mineral and a description of its relationship to other secondary minerals will be undertaken in a future study, in an attempt to determine the mineral's formation conditions and its place in the general alteration history of the Hole 1256D basalts.
title Chemical composition of hydrogarnet and celadonite from ODP Hole 206-1256D
topic 206-1256D; DRILL; Drilling/drill rig; Joides Resolution; Leg206; North Pacific Ocean; Ocean Drilling Program; ODP
url https://doi.org/10.1594/PANGAEA.775746