Bathymetry and Canyons of the western Solomon Sea
Abstract The floor of the western Solomon Sea (for new bathymetric map see inside back cover of this issue) is dominated by the arched and ridged basement of the Solomon Sea Basin, the partly-sediment-filled New Britain Trench, and a more completely filled trench, the Trobriand Trough. There is a de...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Davies, H. L. [verfasserIn] |
|---|
| Format: |
Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
1986 |
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| Schlagwörter: |
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| Anmerkung: |
© Springer-Verlag New York Inc. 1987 |
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| Übergeordnetes Werk: |
Enthalten in: Geo-marine letters - Springer-Verlag, 1981, 6(1986), 4 vom: Dez., Seite 181-191 |
|---|---|
| Übergeordnetes Werk: |
volume:6 ; year:1986 ; number:4 ; month:12 ; pages:181-191 |
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| DOI / URN: |
10.1007/BF02239579 |
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| 520 | |a Abstract The floor of the western Solomon Sea (for new bathymetric map see inside back cover of this issue) is dominated by the arched and ridged basement of the Solomon Sea Basin, the partly-sediment-filled New Britain Trench, and a more completely filled trench, the Trobriand Trough. There is a deep basin where the trenches join (149° Embayment), and a silled basin west of the New Britain Trench (Finsch Deep). Submarine canyons descend from the west and south to the 149° Embayment. Abyssal fans and plains are structurally defined and locally disturbed by young faults. Probable submerged pinnacle reefs stand in water depths as great as 1,200 m. | ||
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| 700 | 1 | |a Hashimoto, K. |4 aut | |
| 700 | 1 | |a Joshima, M. |4 aut | |
| 700 | 1 | |a Stuart, J. E. |4 aut | |
| 700 | 1 | |a Tiffin, D. L. |4 aut | |
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10.1007/BF02239579 doi (DE-627)OLC2036166024 (DE-He213)BF02239579-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Davies, H. L. verfasserin aut Bathymetry and Canyons of the western Solomon Sea 1986 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag New York Inc. 1987 Abstract The floor of the western Solomon Sea (for new bathymetric map see inside back cover of this issue) is dominated by the arched and ridged basement of the Solomon Sea Basin, the partly-sediment-filled New Britain Trench, and a more completely filled trench, the Trobriand Trough. There is a deep basin where the trenches join (149° Embayment), and a silled basin west of the New Britain Trench (Finsch Deep). Submarine canyons descend from the west and south to the 149° Embayment. Abyssal fans and plains are structurally defined and locally disturbed by young faults. Probable submerged pinnacle reefs stand in water depths as great as 1,200 m. Trench Abyssal Plain Submarine Canyon Central Ridge Canyon Floor Keene, J. B. aut Hashimoto, K. aut Joshima, M. aut Stuart, J. E. aut Tiffin, D. L. aut Enthalten in Geo-marine letters Springer-Verlag, 1981 6(1986), 4 vom: Dez., Seite 181-191 (DE-627)129932140 (DE-600)381526-2 (DE-576)015466973 0276-0460 nnns volume:6 year:1986 number:4 month:12 pages:181-191 https://doi.org/10.1007/BF02239579 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_21 GBV_ILN_40 GBV_ILN_70 GBV_ILN_267 GBV_ILN_612 GBV_ILN_2018 GBV_ILN_4012 AR 6 1986 4 12 181-191 |
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10.1007/BF02239579 doi (DE-627)OLC2036166024 (DE-He213)BF02239579-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Davies, H. L. verfasserin aut Bathymetry and Canyons of the western Solomon Sea 1986 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag New York Inc. 1987 Abstract The floor of the western Solomon Sea (for new bathymetric map see inside back cover of this issue) is dominated by the arched and ridged basement of the Solomon Sea Basin, the partly-sediment-filled New Britain Trench, and a more completely filled trench, the Trobriand Trough. There is a deep basin where the trenches join (149° Embayment), and a silled basin west of the New Britain Trench (Finsch Deep). Submarine canyons descend from the west and south to the 149° Embayment. Abyssal fans and plains are structurally defined and locally disturbed by young faults. Probable submerged pinnacle reefs stand in water depths as great as 1,200 m. Trench Abyssal Plain Submarine Canyon Central Ridge Canyon Floor Keene, J. B. aut Hashimoto, K. aut Joshima, M. aut Stuart, J. E. aut Tiffin, D. L. aut Enthalten in Geo-marine letters Springer-Verlag, 1981 6(1986), 4 vom: Dez., Seite 181-191 (DE-627)129932140 (DE-600)381526-2 (DE-576)015466973 0276-0460 nnns volume:6 year:1986 number:4 month:12 pages:181-191 https://doi.org/10.1007/BF02239579 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_21 GBV_ILN_40 GBV_ILN_70 GBV_ILN_267 GBV_ILN_612 GBV_ILN_2018 GBV_ILN_4012 AR 6 1986 4 12 181-191 |
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10.1007/BF02239579 doi (DE-627)OLC2036166024 (DE-He213)BF02239579-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Davies, H. L. verfasserin aut Bathymetry and Canyons of the western Solomon Sea 1986 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag New York Inc. 1987 Abstract The floor of the western Solomon Sea (for new bathymetric map see inside back cover of this issue) is dominated by the arched and ridged basement of the Solomon Sea Basin, the partly-sediment-filled New Britain Trench, and a more completely filled trench, the Trobriand Trough. There is a deep basin where the trenches join (149° Embayment), and a silled basin west of the New Britain Trench (Finsch Deep). Submarine canyons descend from the west and south to the 149° Embayment. Abyssal fans and plains are structurally defined and locally disturbed by young faults. Probable submerged pinnacle reefs stand in water depths as great as 1,200 m. Trench Abyssal Plain Submarine Canyon Central Ridge Canyon Floor Keene, J. B. aut Hashimoto, K. aut Joshima, M. aut Stuart, J. E. aut Tiffin, D. L. aut Enthalten in Geo-marine letters Springer-Verlag, 1981 6(1986), 4 vom: Dez., Seite 181-191 (DE-627)129932140 (DE-600)381526-2 (DE-576)015466973 0276-0460 nnns volume:6 year:1986 number:4 month:12 pages:181-191 https://doi.org/10.1007/BF02239579 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_21 GBV_ILN_40 GBV_ILN_70 GBV_ILN_267 GBV_ILN_612 GBV_ILN_2018 GBV_ILN_4012 AR 6 1986 4 12 181-191 |
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10.1007/BF02239579 doi (DE-627)OLC2036166024 (DE-He213)BF02239579-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Davies, H. L. verfasserin aut Bathymetry and Canyons of the western Solomon Sea 1986 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag New York Inc. 1987 Abstract The floor of the western Solomon Sea (for new bathymetric map see inside back cover of this issue) is dominated by the arched and ridged basement of the Solomon Sea Basin, the partly-sediment-filled New Britain Trench, and a more completely filled trench, the Trobriand Trough. There is a deep basin where the trenches join (149° Embayment), and a silled basin west of the New Britain Trench (Finsch Deep). Submarine canyons descend from the west and south to the 149° Embayment. Abyssal fans and plains are structurally defined and locally disturbed by young faults. Probable submerged pinnacle reefs stand in water depths as great as 1,200 m. Trench Abyssal Plain Submarine Canyon Central Ridge Canyon Floor Keene, J. B. aut Hashimoto, K. aut Joshima, M. aut Stuart, J. E. aut Tiffin, D. L. aut Enthalten in Geo-marine letters Springer-Verlag, 1981 6(1986), 4 vom: Dez., Seite 181-191 (DE-627)129932140 (DE-600)381526-2 (DE-576)015466973 0276-0460 nnns volume:6 year:1986 number:4 month:12 pages:181-191 https://doi.org/10.1007/BF02239579 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_21 GBV_ILN_40 GBV_ILN_70 GBV_ILN_267 GBV_ILN_612 GBV_ILN_2018 GBV_ILN_4012 AR 6 1986 4 12 181-191 |
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10.1007/BF02239579 doi (DE-627)OLC2036166024 (DE-He213)BF02239579-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Davies, H. L. verfasserin aut Bathymetry and Canyons of the western Solomon Sea 1986 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag New York Inc. 1987 Abstract The floor of the western Solomon Sea (for new bathymetric map see inside back cover of this issue) is dominated by the arched and ridged basement of the Solomon Sea Basin, the partly-sediment-filled New Britain Trench, and a more completely filled trench, the Trobriand Trough. There is a deep basin where the trenches join (149° Embayment), and a silled basin west of the New Britain Trench (Finsch Deep). Submarine canyons descend from the west and south to the 149° Embayment. Abyssal fans and plains are structurally defined and locally disturbed by young faults. Probable submerged pinnacle reefs stand in water depths as great as 1,200 m. Trench Abyssal Plain Submarine Canyon Central Ridge Canyon Floor Keene, J. B. aut Hashimoto, K. aut Joshima, M. aut Stuart, J. E. aut Tiffin, D. L. aut Enthalten in Geo-marine letters Springer-Verlag, 1981 6(1986), 4 vom: Dez., Seite 181-191 (DE-627)129932140 (DE-600)381526-2 (DE-576)015466973 0276-0460 nnns volume:6 year:1986 number:4 month:12 pages:181-191 https://doi.org/10.1007/BF02239579 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_21 GBV_ILN_40 GBV_ILN_70 GBV_ILN_267 GBV_ILN_612 GBV_ILN_2018 GBV_ILN_4012 AR 6 1986 4 12 181-191 |
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bathymetry and canyons of the western solomon sea |
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Bathymetry and Canyons of the western Solomon Sea |
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Abstract The floor of the western Solomon Sea (for new bathymetric map see inside back cover of this issue) is dominated by the arched and ridged basement of the Solomon Sea Basin, the partly-sediment-filled New Britain Trench, and a more completely filled trench, the Trobriand Trough. There is a deep basin where the trenches join (149° Embayment), and a silled basin west of the New Britain Trench (Finsch Deep). Submarine canyons descend from the west and south to the 149° Embayment. Abyssal fans and plains are structurally defined and locally disturbed by young faults. Probable submerged pinnacle reefs stand in water depths as great as 1,200 m. © Springer-Verlag New York Inc. 1987 |
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Abstract The floor of the western Solomon Sea (for new bathymetric map see inside back cover of this issue) is dominated by the arched and ridged basement of the Solomon Sea Basin, the partly-sediment-filled New Britain Trench, and a more completely filled trench, the Trobriand Trough. There is a deep basin where the trenches join (149° Embayment), and a silled basin west of the New Britain Trench (Finsch Deep). Submarine canyons descend from the west and south to the 149° Embayment. Abyssal fans and plains are structurally defined and locally disturbed by young faults. Probable submerged pinnacle reefs stand in water depths as great as 1,200 m. © Springer-Verlag New York Inc. 1987 |
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Abstract The floor of the western Solomon Sea (for new bathymetric map see inside back cover of this issue) is dominated by the arched and ridged basement of the Solomon Sea Basin, the partly-sediment-filled New Britain Trench, and a more completely filled trench, the Trobriand Trough. There is a deep basin where the trenches join (149° Embayment), and a silled basin west of the New Britain Trench (Finsch Deep). Submarine canyons descend from the west and south to the 149° Embayment. Abyssal fans and plains are structurally defined and locally disturbed by young faults. Probable submerged pinnacle reefs stand in water depths as great as 1,200 m. © Springer-Verlag New York Inc. 1987 |
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Bathymetry and Canyons of the western Solomon Sea |
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Keene, J. B. Hashimoto, K. Joshima, M. Stuart, J. E. Tiffin, D. L. |
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