AustralieFrV1, Main, Exploration, bibRecord, 00D885

Regional setting of a complex backarc: New Hebrides Arc, northern Vanatu-eastern Solomon Islands

Identifieur interne : 00D885 ( Main/Exploration ); précédent : 00D884; suivant : 00D886

Regional setting of a complex backarc: New Hebrides Arc, northern Vanatu-eastern Solomon Islands

Auteurs : D. P. Johnson [Australie] ; P. C. Maillet [France] ; R. Price [Australie]

Source :

Geo-Marine Letters [ 0276-0460 ] ; 1993-06-01.

RBID : ISTEX:F3DC2D27936F94DFB6CFE19ABDB91CA293D8A030

Descripteurs français

Wicri :
- geographic : Fidji.
- topic : Ressource minérale.

English descriptors

Abstract

Abstract: New GLORIA imagery over the complex backarc area of the northern New Hebrides Arc clearly outlines the deeply faulted Jean Charcot Troughs. The troughs are 2400–3000 m deep and are not magmatically active. They appear to be fragmented older crust and are not backarc basins in the usual sense. Horst and graben structures on the Hazel Holme Fracture Zone (HHFZ) cut obliquely across the trend of the Zone, which therefore is not a simple transform. The enechelon ridges may form a relay, but Y-shaped grabens could be remnant spreading zones, formed earlier in the history of the western part of the North Fiji Basin.

Url:

https://api.istex.fr/document/F3DC2D27936F94DFB6CFE19ABDB91CA293D8A030/fulltext/pdf

DOI: 10.1007/BF01204549

Affiliations:

Links toward previous steps (curation, corpus...)

to stream Istex, to step Corpus: 002D92
to stream Istex, to step Curation: 002D92
to stream Istex, to step Checkpoint: 002A00
to stream Main, to step Merge: 00EB06
to stream Main, to step Curation: 00D885

Le document en format XML

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<profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Backarc</term>
<term>Backarc basins</term>
<term>Backarc troughs</term>
<term>Banks islands</term>
<term>Basin</term>
<term>Basin formation</term>
<term>Bright zones</term>
<term>Central basin</term>
<term>Central chain</term>
<term>Charcot</term>
<term>Charvis</term>
<term>Comptes rendus</term>
<term>Coriolis troughs</term>
<term>Crust</term>
<term>Earth science series</term>
<term>Earthquake mechanism solutions</term>
<term>Eastern flank</term>
<term>Eastern solomon islands</term>
<term>Extensional features</term>
<term>Fiji</term>
<term>Fiji basin</term>
<term>Fiji plateau</term>
<term>Geological society</term>
<term>Gloria</term>
<term>Gloria data show</term>
<term>Gloria image</term>
<term>Gloria imagery</term>
<term>Graben structures</term>
<term>Hazel</term>
<term>Hazel holme facture zone</term>
<term>Hazel holme fracture zone</term>
<term>Heat flow</term>
<term>Hebrides</term>
<term>Hebrides island</term>
<term>Hhfz</term>
<term>Holme</term>
<term>Impacting zone</term>
<term>Individual troughs</term>
<term>Jean charcot troughs</term>
<term>Kroenke</term>
<term>Louat</term>
<term>Marginal basin</term>
<term>Marginal basins</term>
<term>Mineral resources</term>
<term>Northern part</term>
<term>Northern side</term>
<term>Oceanologica acta</term>
<term>Offshore resources</term>
<term>Pacific island region</term>
<term>Pelletier</term>
<term>Platform levels</term>
<term>Recent extension</term>
<term>Regional bathymetry</term>
<term>Ridge crest processes</term>
<term>Seabed</term>
<term>Study area</term>
<term>Torres islands</term>
<term>Triple junction</term>
<term>Trough</term>
<term>Vanikoro trough</term>
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<term>Backarc basins</term>
<term>Backarc troughs</term>
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<term>Basin formation</term>
<term>Bright zones</term>
<term>Central basin</term>
<term>Central chain</term>
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<term>Charvis</term>
<term>Comptes rendus</term>
<term>Coriolis troughs</term>
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<term>Earth science series</term>
<term>Earthquake mechanism solutions</term>
<term>Eastern flank</term>
<term>Eastern solomon islands</term>
<term>Extensional features</term>
<term>Fiji</term>
<term>Fiji basin</term>
<term>Fiji plateau</term>
<term>Geological society</term>
<term>Gloria</term>
<term>Gloria data show</term>
<term>Gloria image</term>
<term>Gloria imagery</term>
<term>Graben structures</term>
<term>Hazel</term>
<term>Hazel holme facture zone</term>
<term>Hazel holme fracture zone</term>
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<term>Hebrides</term>
<term>Hebrides island</term>
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<term>Impacting zone</term>
<term>Individual troughs</term>
<term>Jean charcot troughs</term>
<term>Kroenke</term>
<term>Louat</term>
<term>Marginal basin</term>
<term>Marginal basins</term>
<term>Mineral resources</term>
<term>Northern part</term>
<term>Northern side</term>
<term>Oceanologica acta</term>
<term>Offshore resources</term>
<term>Pacific island region</term>
<term>Pelletier</term>
<term>Platform levels</term>
<term>Recent extension</term>
<term>Regional bathymetry</term>
<term>Ridge crest processes</term>
<term>Seabed</term>
<term>Study area</term>
<term>Torres islands</term>
<term>Triple junction</term>
<term>Trough</term>
<term>Vanikoro trough</term>
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<front><div type="abstract" xml:lang="en">Abstract: New GLORIA imagery over the complex backarc area of the northern New Hebrides Arc clearly outlines the deeply faulted Jean Charcot Troughs. The troughs are 2400–3000 m deep and are not magmatically active. They appear to be fragmented older crust and are not backarc basins in the usual sense. Horst and graben structures on the Hazel Holme Fracture Zone (HHFZ) cut obliquely across the trend of the Zone, which therefore is not a simple transform. The enechelon ridges may form a relay, but Y-shaped grabens could be remnant spreading zones, formed earlier in the history of the western part of the North Fiji Basin.</div>
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Regional setting of a complex backarc: New Hebrides Arc, northern Vanatu-eastern Solomon Islands

Regional setting of a complex backarc: New Hebrides Arc, northern Vanatu-eastern Solomon Islands

Source :

Descripteurs français

English descriptors

Abstract

Links toward previous steps (curation, corpus...)

Le document en format XML

Pour manipuler ce document sous Unix (Dilib)

Pour mettre un lien sur cette page dans le réseau Wicri