Geochemistry of Kerguelen-Heard Plateau basalts

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Main Authors: Salters, Vincent J M, Storey, Michael, Sevigny, James H, Whitechurch, Hubert
Format: Dataset Open Access
Language:en
Published: PANGAEA 1992
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author Salters, Vincent J M
Storey, Michael
Sevigny, James H
Whitechurch, Hubert
author_facet Salters, Vincent J M
Storey, Michael
Sevigny, James H
Whitechurch, Hubert
collection Datos científicos de ciencias marinas y ambientales
contents During Leg 120 basalts were recovered at four drill holes on the Kerguelen-Heard Plateau. This paper reports the trace element and Sr, Nd, Hf, and Pb isotopic characteristics of these basalts and compares these basalts with Indian Ocean basalts and Kerguelen and Heard island volcanics. Kerguelen-Heard Plateau basalts are extremely heterogeneous in character. Intersite variations are larger than intrasite variations. Part of the chemical variations of the plateau volcanics overlap with those characteristics of Kerguelen Island volcanics, which indicates tapping of the same mantle source during the two different periods of activity. The estimates of the degree of melting for the plateau basalts (smaller degree of melting than for mid-ocean ridge basalts) and the heterogeneous character of the plateau exclude an origin that requires large degrees of melting or more rigorous convection than at ocean ridges. However, all characteristics indicate an oceanic origin for the Kerguelen-Heard Plateau.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_758553
institution PANGAEA
language en
publishDate 1992
publisher PANGAEA
record_format pangaea
spellingShingle Geochemistry of Kerguelen-Heard Plateau basalts
Salters, Vincent J M
Storey, Michael
Sevigny, James H
Whitechurch, Hubert
120-747C; 120-748C; 120-749C; 120-750B; DRILL; Drilling/drill rig; Joides Resolution; Leg120; Ocean Drilling Program; ODP; South Indian Ridge, South Indian Ocean
During Leg 120 basalts were recovered at four drill holes on the Kerguelen-Heard Plateau. This paper reports the trace element and Sr, Nd, Hf, and Pb isotopic characteristics of these basalts and compares these basalts with Indian Ocean basalts and Kerguelen and Heard island volcanics. Kerguelen-Heard Plateau basalts are extremely heterogeneous in character. Intersite variations are larger than intrasite variations. Part of the chemical variations of the plateau volcanics overlap with those characteristics of Kerguelen Island volcanics, which indicates tapping of the same mantle source during the two different periods of activity. The estimates of the degree of melting for the plateau basalts (smaller degree of melting than for mid-ocean ridge basalts) and the heterogeneous character of the plateau exclude an origin that requires large degrees of melting or more rigorous convection than at ocean ridges. However, all characteristics indicate an oceanic origin for the Kerguelen-Heard Plateau.
title Geochemistry of Kerguelen-Heard Plateau basalts
topic 120-747C; 120-748C; 120-749C; 120-750B; DRILL; Drilling/drill rig; Joides Resolution; Leg120; Ocean Drilling Program; ODP; South Indian Ridge, South Indian Ocean
url https://doi.org/10.1594/PANGAEA.758553