Global and Planetary Change

fission track analyses of samples from a deep borehole on Nuussuaq (reported elsewhere). The difference between a reconstruction of the upper planation surface across the entire area and the present topography was used as an estimate of erosion of basement rock The relationships between uplift, eros...

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Bibliographic Details
Main Author: Peter Japsen
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 2004
Subjects:
palaeosurface
West Greenland
uplift
tectonic movements
differential erosion
Neogene
planation surface
etch surface
hilly relief
Landform analysis
Greenland
Nuussuaq
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.533.5892
http://www.geus.dk/publications/extern/bonow_et_al_gpc_2006_pp21_in_press.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.533.5892 2023-05-15T16:27:32+02:00 Global and Planetary Change Peter Japsen The Pennsylvania State University CiteSeerX Archives 2004 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.533.5892 http://www.geus.dk/publications/extern/bonow_et_al_gpc_2006_pp21_in_press.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.533.5892 http://www.geus.dk/publications/extern/bonow_et_al_gpc_2006_pp21_in_press.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.geus.dk/publications/extern/bonow_et_al_gpc_2006_pp21_in_press.pdf palaeosurface West Greenland uplift tectonic movements differential erosion Neogene planation surface etch surface hilly relief Landform analysis text 2004 ftciteseerx 2016-01-08T10:43:15Z fission track analyses of samples from a deep borehole on Nuussuaq (reported elsewhere). The difference between a reconstruction of the upper planation surface across the entire area and the present topography was used as an estimate of erosion of basement rock The relationships between uplift, erosion and sedimentation along the elevated passive continental Text Greenland Nuussuaq Unknown Greenland Nuussuaq ENVELOPE(-51.918,-51.918,66.626,66.626)
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
topic palaeosurface
West Greenland
uplift
tectonic movements
differential erosion
Neogene
planation surface
etch surface
hilly relief
Landform analysis
spellingShingle palaeosurface
West Greenland
uplift
tectonic movements
differential erosion
Neogene
planation surface
etch surface
hilly relief
Landform analysis
Peter Japsen
Global and Planetary Change
topic_facet palaeosurface
West Greenland
uplift
tectonic movements
differential erosion
Neogene
planation surface
etch surface
hilly relief
Landform analysis
description fission track analyses of samples from a deep borehole on Nuussuaq (reported elsewhere). The difference between a reconstruction of the upper planation surface across the entire area and the present topography was used as an estimate of erosion of basement rock The relationships between uplift, erosion and sedimentation along the elevated passive continental
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Peter Japsen
author_facet Peter Japsen
author_sort Peter Japsen
title Global and Planetary Change
title_short Global and Planetary Change
title_full Global and Planetary Change
title_fullStr Global and Planetary Change
title_full_unstemmed Global and Planetary Change
title_sort global and planetary change
publishDate 2004
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.533.5892
http://www.geus.dk/publications/extern/bonow_et_al_gpc_2006_pp21_in_press.pdf
long_lat ENVELOPE(-51.918,-51.918,66.626,66.626)
geographic Greenland
Nuussuaq
geographic_facet Greenland
Nuussuaq
genre Greenland
Nuussuaq
genre_facet Greenland
Nuussuaq
op_source http://www.geus.dk/publications/extern/bonow_et_al_gpc_2006_pp21_in_press.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.533.5892
http://www.geus.dk/publications/extern/bonow_et_al_gpc_2006_pp21_in_press.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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