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Gose, Jürgen; Schmädicke, Esther; Stachel, Thomas (2025): Water in eclogite and pyroxenite xenoliths from the bottom 100 km of the Slave Craton (Canada) mantle root [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.975214

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Published: 2025-02-12DOI registered: 2025-02-12

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Abstract:
Significant amounts of water can be stored in the mantle in nominally anhydrous minerals (NAMs) such as garnet, olivine, clino- and orthopyroxene as structural OH− ions. Water or, more precisely, hydrogen is incorporated as a trace element in the mineral structure. Subduction is the only conceivable mode to transport water into the mantle. The main goal of this study is to evaluate the water storage and transport capacity of garnet-clinopyroxene xenoliths (eclogite and pyroxenite, built by metamorphic processes during subduction of oceanic crust) and, in turn, the potential of subducted oceanic crust to recycle water into the mantle. For this purpose, 20 kimberlite-hosted xenoliths from the Diavik diamond mine, Canada, were investigated. The location is known for its abundance of well-preserved xenoliths. Previous studies have shown that the composition of garnet and clinopyroxene is highly variable (e.g., Aulbach et al., 2007), which is favorable for our study. Sample parameters, mineral composition, trace elements, and infrared data are listed in the attached tables.
Keyword(s):
Diavik diamond mine (Canada); eclogite; FTIR spectroscopy; pyroxenite; structural water
Supplement to:
Schmädicke, Esther; Gose, Jürgen; Stachel, Thomas (2025): Water in Eclogite and Pyroxenite Xenoliths From the Bottom 100 km of the Slave Craton (Canada) Mantle Root. Geochemistry, Geophysics, Geosystems, 26(3), e2024GC011922, https://doi.org/10.1029/2024GC011922
References:
Aulbach, Sonja; Pearson, Norman J; O'Reilly, Suzanne Y; Doyle, Buddy J (2007): Origins of Xenolithic Eclogites and Pyroxenites from the Central Slave Craton, Canada. Journal of Petrology, 48(10), 1843-1873, https://doi.org/10.1093/petrology/egm041
Coverage:
Latitude: 64.500000 * Longitude: -110.230000
Event(s):
DDM (Diavik Diamond Mine) * Latitude: 64.500000 * Longitude: -110.230000 * Location: Lac de Gras, Canada * Method/Device: Outcrop sample (OUTCROP) * Comment: Eclogite and peridotite xenoliths from lower continental crust
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1File contentContentGose, Jürgen
2Office Open XML WorkbookXLSXGose, Jürgen
3Office Open XML Workbook (File Size)XLSX (Size)BytesGose, Jürgen
Status:
Curation Level: Basic curation (CurationLevelB)
Size:
8 data points

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