Regional setting of a complex backarc: New Hebrides Arc, northern Vanatu-eastern Solomon Islands
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 sens...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Johnson, D. P. [verfasserIn] |
|---|
| Format: |
Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
1993 |
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| Schlagwörter: |
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| Anmerkung: |
© Springer-Verlag 1993 |
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| Übergeordnetes Werk: |
Enthalten in: Geo-marine letters - Springer-Verlag, 1981, 13(1993), 2 vom: Juni, Seite 82-89 |
|---|---|
| Übergeordnetes Werk: |
volume:13 ; year:1993 ; number:2 ; month:06 ; pages:82-89 |
| Links: |
|---|
| DOI / URN: |
10.1007/BF01204549 |
|---|
| Katalog-ID: |
OLC2036167950 |
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| 520 | |a 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. | ||
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10.1007/BF01204549 doi (DE-627)OLC2036167950 (DE-He213)BF01204549-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Johnson, D. P. verfasserin aut Regional setting of a complex backarc: New Hebrides Arc, northern Vanatu-eastern Solomon Islands 1993 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1993 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. Fracture Zone Usual Sense Solomon Island Backarc Basin Regional Setting Maillet, P. C. aut Price, R. aut Enthalten in Geo-marine letters Springer-Verlag, 1981 13(1993), 2 vom: Juni, Seite 82-89 (DE-627)129932140 (DE-600)381526-2 (DE-576)015466973 0276-0460 nnns volume:13 year:1993 number:2 month:06 pages:82-89 https://doi.org/10.1007/BF01204549 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_21 GBV_ILN_40 GBV_ILN_62 GBV_ILN_70 GBV_ILN_600 GBV_ILN_612 GBV_ILN_2018 GBV_ILN_4012 GBV_ILN_4082 AR 13 1993 2 06 82-89 |
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10.1007/BF01204549 doi (DE-627)OLC2036167950 (DE-He213)BF01204549-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Johnson, D. P. verfasserin aut Regional setting of a complex backarc: New Hebrides Arc, northern Vanatu-eastern Solomon Islands 1993 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1993 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. Fracture Zone Usual Sense Solomon Island Backarc Basin Regional Setting Maillet, P. C. aut Price, R. aut Enthalten in Geo-marine letters Springer-Verlag, 1981 13(1993), 2 vom: Juni, Seite 82-89 (DE-627)129932140 (DE-600)381526-2 (DE-576)015466973 0276-0460 nnns volume:13 year:1993 number:2 month:06 pages:82-89 https://doi.org/10.1007/BF01204549 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_21 GBV_ILN_40 GBV_ILN_62 GBV_ILN_70 GBV_ILN_600 GBV_ILN_612 GBV_ILN_2018 GBV_ILN_4012 GBV_ILN_4082 AR 13 1993 2 06 82-89 |
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10.1007/BF01204549 doi (DE-627)OLC2036167950 (DE-He213)BF01204549-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Johnson, D. P. verfasserin aut Regional setting of a complex backarc: New Hebrides Arc, northern Vanatu-eastern Solomon Islands 1993 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1993 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. Fracture Zone Usual Sense Solomon Island Backarc Basin Regional Setting Maillet, P. C. aut Price, R. aut Enthalten in Geo-marine letters Springer-Verlag, 1981 13(1993), 2 vom: Juni, Seite 82-89 (DE-627)129932140 (DE-600)381526-2 (DE-576)015466973 0276-0460 nnns volume:13 year:1993 number:2 month:06 pages:82-89 https://doi.org/10.1007/BF01204549 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_21 GBV_ILN_40 GBV_ILN_62 GBV_ILN_70 GBV_ILN_600 GBV_ILN_612 GBV_ILN_2018 GBV_ILN_4012 GBV_ILN_4082 AR 13 1993 2 06 82-89 |
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10.1007/BF01204549 doi (DE-627)OLC2036167950 (DE-He213)BF01204549-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Johnson, D. P. verfasserin aut Regional setting of a complex backarc: New Hebrides Arc, northern Vanatu-eastern Solomon Islands 1993 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1993 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. Fracture Zone Usual Sense Solomon Island Backarc Basin Regional Setting Maillet, P. C. aut Price, R. aut Enthalten in Geo-marine letters Springer-Verlag, 1981 13(1993), 2 vom: Juni, Seite 82-89 (DE-627)129932140 (DE-600)381526-2 (DE-576)015466973 0276-0460 nnns volume:13 year:1993 number:2 month:06 pages:82-89 https://doi.org/10.1007/BF01204549 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_21 GBV_ILN_40 GBV_ILN_62 GBV_ILN_70 GBV_ILN_600 GBV_ILN_612 GBV_ILN_2018 GBV_ILN_4012 GBV_ILN_4082 AR 13 1993 2 06 82-89 |
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10.1007/BF01204549 doi (DE-627)OLC2036167950 (DE-He213)BF01204549-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Johnson, D. P. verfasserin aut Regional setting of a complex backarc: New Hebrides Arc, northern Vanatu-eastern Solomon Islands 1993 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1993 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. Fracture Zone Usual Sense Solomon Island Backarc Basin Regional Setting Maillet, P. C. aut Price, R. aut Enthalten in Geo-marine letters Springer-Verlag, 1981 13(1993), 2 vom: Juni, Seite 82-89 (DE-627)129932140 (DE-600)381526-2 (DE-576)015466973 0276-0460 nnns volume:13 year:1993 number:2 month:06 pages:82-89 https://doi.org/10.1007/BF01204549 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_21 GBV_ILN_40 GBV_ILN_62 GBV_ILN_70 GBV_ILN_600 GBV_ILN_612 GBV_ILN_2018 GBV_ILN_4012 GBV_ILN_4082 AR 13 1993 2 06 82-89 |
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regional setting of a complex backarc: new hebrides arc, northern vanatu-eastern solomon islands |
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Regional setting of a complex backarc: New Hebrides Arc, northern Vanatu-eastern Solomon Islands |
| 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. © Springer-Verlag 1993 |
| abstractGer |
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. © Springer-Verlag 1993 |
| abstract_unstemmed |
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. © Springer-Verlag 1993 |
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Regional setting of a complex backarc: New Hebrides Arc, northern Vanatu-eastern Solomon Islands |
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