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The geochemistry and petrogenesis of basalts from the Taupo Volcanic Zone and Kermadec Island Arc, S.W. Pacific

Identifieur interne : 002295 ( Main/Exploration ); précédent : 002294; suivant : 002296

The geochemistry and petrogenesis of basalts from the Taupo Volcanic Zone and Kermadec Island Arc, S.W. Pacific

Auteurs : J. A. Gamble [Nouvelle-Zélande] ; I. E. M. Smith ; M. T. Mcculloch ; I. J. Graham ; B. P. Kokelaar

Source :

RBID : Pascal:93-0246325

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English descriptors

Abstract

Basalts from the Taupo Volcanic Zone (TVZ), New Zealand, the Kermadec Island Arc (KA) and its back-arc basin, the Havre Trough show systematic variations in trace-element and isotope geochemistry which are attributed to differences in tectonic setting and source heterogeneity along a more or less continuous plate boundary. Basalts from the Kermadec Arc are characterised by low abundances of high field strength elements (HFSE) such as Ti, Zr, Nb, Ta and Hf and have high ratios of Ti/Zr and low ratios of Ti/Sc and Ti/V relative to typical MORB. Basalts from TVZ also show low abundances of the HFS elements relative to MORB but show lower Ti/Zr, higher Ti/V and Ti/Se ratios and generally higher Zr abundances than KA most basalts


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Le document en format XML

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<term>Kermadec Islands</term>
<term>Mid Ocean Ridge Basalt</term>
<term>Nd-144/Nd-143</term>
<term>North Island</term>
<term>Southwest Pacific</term>
<term>Sr-87/Sr-86</term>
<term>Taupo volcanic zone</term>
<term>alkali basalts</term>
<term>back-arc basins</term>
<term>chemical composition</term>
<term>contamination</term>
<term>depleted mantle</term>
<term>enrichment</term>
<term>heterogeneity</term>
<term>island arcs</term>
<term>lithophile elements</term>
<term>plate boundaries</term>
<term>rare earths</term>
<term>subduction</term>
<term>tholeiitic basalt</term>
<term>upper mantle</term>
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<term>Zone volcanique Taupo</term>
<term>Nouvelle Zélande Ile Nord</term>
<term>Arc insulaire</term>
<term>Iles Kermadec</term>
<term>Pacifique Sud Ouest</term>
<term>Bassin arrière arc</term>
<term>Limite plaque</term>
<term>Hétérogénéité</term>
<term>Manteau sup</term>
<term>Basalte tholéitique</term>
<term>Basalte alcalin</term>
<term>MORB</term>
<term>Analyse chimique</term>
<term>Terre rare</term>
<term>Sr 87-Sr 86</term>
<term>Nd 143-Nd 144</term>
<term>Contamination</term>
<term>Manteau appauvri</term>
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<div type="abstract" xml:lang="en">Basalts from the Taupo Volcanic Zone (TVZ), New Zealand, the Kermadec Island Arc (KA) and its back-arc basin, the Havre Trough show systematic variations in trace-element and isotope geochemistry which are attributed to differences in tectonic setting and source heterogeneity along a more or less continuous plate boundary. Basalts from the Kermadec Arc are characterised by low abundances of high field strength elements (HFSE) such as Ti, Zr, Nb, Ta and Hf and have high ratios of Ti/Zr and low ratios of Ti/Sc and Ti/V relative to typical MORB. Basalts from TVZ also show low abundances of the HFS elements relative to MORB but show lower Ti/Zr, higher Ti/V and Ti/Se ratios and generally higher Zr abundances than KA most basalts</div>
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