Matches in Nanopublications for { ?s ?p <https://doi.org/10.18710/DWOUPL> ?g. }
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- A%20total%20of%2011%20new%20contourite%20drifts%2C%20named%20I%E2%80%93XI%2C%20have%20been%20defined%20in%20the%20Kai%20and%20Naust%20formations. obtainsSupportFrom DWOUPL assertion.
- These%20drifts%20are%20up%20to%20280%20km%20long%2C%20150%20km%20wide%20and%20960%20ms%20TWT%20thick. obtainsSupportFrom DWOUPL assertion.
- Contourite%20drifts%20in%20the%20Kai%20Formation%20on%20the%20mid-Norwegian%20margin%20commenced%20in%20the%20mid-Miocene%20%28slightly%20before%2011%20Ma%29. obtainsSupportFrom DWOUPL assertion.
- The%20Molo%20Formation%20initiated%20on%20the%20mid-Norwegian%20shelf%20in%20the%20late%20Miocene%20%288.8%20Ma%29. obtainsSupportFrom DWOUPL assertion.
- Coastal%20progradation%20of%20the%20Molo%20Formation%20interfingered%20with%20drift%20growth%20on%20the%20slope%20in%20the%20Kai%20Formation%2C%20showing%20contemporaneous%20deposition%20of%20the%20two%20formations%20up%20until%202.7%20Ma. obtainsSupportFrom DWOUPL assertion.
- The%20Naust%20Formation%20in%20the%20mid-Norwegian%20region%20mainly%20built%20out%20as%20a%20glacigenic%20progradational%20wedge%20throughout%20the%20Quaternary%20%282.7%E2%80%930%20Ma%29%2C%20but%20it%20also%20included%20significant%20intervals%20of%20contourite%20sedimentation. obtainsSupportFrom DWOUPL assertion.
- Previously%20described%20Lofoten%20and%20Vester%C3%A5len%20drifts%20started%20to%20accumulate%20in%20the%20early%20Quaternary%2C%20not%20in%20the%20mid-Miocene. obtainsSupportFrom DWOUPL assertion.
- Structurally-controlled%20drifts%20formed%20due%20to%20accumulation%20in%20bathymetric%20lows%20created%20by%20complex%20underlying%20relief%2C%20including%20highs%2C%20ridges%2C%20and%20domes. obtainsSupportFrom DWOUPL assertion.
- The%20distinct%20difference%20in%20margin%20construction%20between%20the%20mid-Norwegian%20and%20Lofoten%E2%80%93Vester%C3%A5len%20segments%20results%20from%20differences%20in%20hinterland%20and%20basin%20topography. obtainsSupportFrom DWOUPL assertion.
- The%20Neogene%E2%80%93Quaternary%20sedimentation%20patterns%20were%20influenced%20by%20ocean%20currents%20that%20redistributed%20sediments%20from%20the%20south%20to%20both%20margin%20segments. obtainsSupportFrom DWOUPL assertion.
- The%20Neogene-Quaternary%20continental%20margin%20offshore%20mid-north%20Norway%20shows%20contrasting%20evolution%20patterns%20between%20Neogene%20and%20Quaternary%20periods. obtainsSupportFrom DWOUPL assertion.
- Submarine%20canyons%20offshore%20mid-north%20Norway%20evolved%20significantly%20during%20the%20Quaternary%20period%20due%20to%20glacial%20processes. obtainsSupportFrom DWOUPL assertion.
- The%20Lofoten-Vester%C3%A5len%20margin%20features%20a%20contourite%20drift%20system%20influenced%20by%20bottom%20currents%20predominantly%20during%20the%20Quaternary. obtainsSupportFrom DWOUPL assertion.
- Source-to-sink%20sediment%20delivery%20to%20the%20continental%20margin%20offshore%20mid-north%20Norway%20was%20substantially%20higher%20during%20Quaternary%20glacial%20periods%20compared%20to%20the%20Neogene. obtainsSupportFrom DWOUPL assertion.
- The%20mid-Norwegian%20continental%20slope%20exhibits%20multiple%20large-scale%20submarine%20landslides%20primarily%20initiated%20during%20the%20Quaternary%20period. obtainsSupportFrom DWOUPL assertion.
- Along-slope%20bottom%20current%20deposits%20%28contourites%29%20are%20volumetrically%20more%20significant%20on%20the%20mid-Norwegian%20margin%20compared%20to%20down-slope%20glacial%20deposits%20during%20the%20Neogene. obtainsSupportFrom DWOUPL assertion.
- The%20slope%20morphology%20offshore%20Lofoten-Vester%C3%A5len%20transitioned%20from%20a%20predominantly%20aggradational%20to%20erosional%20regime%20at%20the%20onset%20of%20the%20Quaternary%20glaciations. obtainsSupportFrom DWOUPL assertion.
- The%20Naust%20Formation%2C%20representing%20Quaternary%20deposits%20offshore%20mid-Norway%2C%20records%20intense%20glacial%20erosion%20and%20sediment%20delivery%20not%20observed%20in%20Neogene%20formations. obtainsSupportFrom DWOUPL assertion.