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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Cascade Range (1)
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Chama Basin (1)
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Coast Ranges (1)
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Europe
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Alps
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Swiss Alps (1)
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Western Alps (1)
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Central Europe
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Switzerland
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Swiss Alps (1)
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Southern Europe
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Italy (1)
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Western Europe
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France (1)
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North America
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Skagit Valley (1)
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San Pedro Basin (1)
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South America
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Andes
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Venezuelan Andes (1)
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Venezuela
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Venezuelan Andes (1)
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United States
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Washington
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Chelan County Washington (1)
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King County Washington (1)
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Skagit County Washington (1)
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Snohomish County Washington (1)
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Whatcom County Washington (1)
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geochronology methods
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(U-Th)/He (1)
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fission-track dating (2)
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He/He (1)
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thermochronology (2)
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geologic age
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Cenozoic
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Quaternary
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Cordilleran ice sheet (1)
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Tertiary
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Neogene
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Miocene
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upper Miocene (1)
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Pliocene (2)
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minerals
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phosphates
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apatite (2)
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Primary terms
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Cenozoic
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Quaternary
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Cordilleran ice sheet (1)
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Tertiary
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Neogene
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Miocene
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upper Miocene (1)
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Pliocene (2)
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climate change (1)
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Europe
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Alps
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Swiss Alps (1)
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Western Alps (1)
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Central Europe
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Switzerland
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Swiss Alps (1)
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Southern Europe
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Italy (1)
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Western Europe
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France (1)
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faults (1)
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geochronology (1)
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geomorphology (2)
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hydrology (1)
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isostasy (1)
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North America
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Skagit Valley (1)
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sediments (1)
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South America
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Andes
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Venezuelan Andes (1)
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Venezuela
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Venezuelan Andes (1)
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tectonics (1)
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United States
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Washington
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Chelan County Washington (1)
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King County Washington (1)
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Skagit County Washington (1)
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Snohomish County Washington (1)
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Whatcom County Washington (1)
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sediments
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sediments (1)
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Low-temperature thermochronologic signature of range-divide migration and breaching in the North Cascades
Strong tectonic and weak climatic control on exhumation rates in the Venezuelan Andes
Spatial correlation between long-term exhumation rates and present-day forcing parameters in the western European Alps
Abstract Postrift domal uplift patterns are a distinct feature of northern North Atlantic margins. On the basis of apatite fission-track data, offshore seismic stratigraphy, geomorphology, gravity and seismic tomography, we argue that southern Norway is characterized by predominantly Neogene domal uplift. The uplift is tectonically driven and estimated at around 1.5 km. Low flexural rigidity ( c. 10 22 Nm) and corresponding equivalent elastic thickness T e ( c. 15 km) values for the southern Norwegian lithosphere indicate that the lithosphere is relatively weak. Additionally, high temperature estimates derived from low-velocity mantle P- and S-wave seismic tomography below the dome suggest a thermal anomaly at depth. Therefore, the observed topography is most plausibly explained by mantle upwelling. This would supercede other previously proposed primary mechanisms such as eustasy, isostatic readjustment to glacial erosion, magmatic underplating and intraplate compression. Currently available data suggest similar processes for other uplifted regions such as Spitsbergen, northern Norway, the British Isles and parts of East Greenland.