The rifted volcanic margin of East Greenland has remained a major area for field studies and the devel-opment of models for the dynamics of plume-related continental break-up since the start of the Danish Lithosphere Centre (DLC) in 1994. The studies cover a range of disciplines and geological proce...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.607.780 2023-05-15T16:03:31+02:00 Statens Naturvidenskabelige Forskningsråd (snf The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.607.780 http://www.geus.dk/publications/review-greenland-00/gsb189p83-98.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.607.780 http://www.geus.dk/publications/review-greenland-00/gsb189p83-98.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.geus.dk/publications/review-greenland-00/gsb189p83-98.pdf text ftciteseerx 2016-01-08T14:20:44Z The rifted volcanic margin of East Greenland has remained a major area for field studies and the devel-opment of models for the dynamics of plume-related continental break-up since the start of the Danish Lithosphere Centre (DLC) in 1994. The studies cover a range of disciplines and geological processes from the early development of pre-break-up basin formation and sedimentation over the main phase of basaltic mag-matism to the late stages of alkaline magmatism and structural re-equilibration. The East Greenland field activities in the summer of 2000, collectively referred to as EG 2000, were facili-tated by a logistic platform provided by support from Text East Greenland Greenland Unknown Greenland |
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English |
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The rifted volcanic margin of East Greenland has remained a major area for field studies and the devel-opment of models for the dynamics of plume-related continental break-up since the start of the Danish Lithosphere Centre (DLC) in 1994. The studies cover a range of disciplines and geological processes from the early development of pre-break-up basin formation and sedimentation over the main phase of basaltic mag-matism to the late stages of alkaline magmatism and structural re-equilibration. The East Greenland field activities in the summer of 2000, collectively referred to as EG 2000, were facili-tated by a logistic platform provided by support from |
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The Pennsylvania State University CiteSeerX Archives |
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Text |
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Statens Naturvidenskabelige Forskningsråd (snf |
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Statens Naturvidenskabelige Forskningsråd (snf |
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Statens Naturvidenskabelige Forskningsråd (snf |
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Statens Naturvidenskabelige Forskningsråd (snf |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.607.780 http://www.geus.dk/publications/review-greenland-00/gsb189p83-98.pdf |
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Greenland |
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Greenland |
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East Greenland Greenland |
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East Greenland Greenland |
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http://www.geus.dk/publications/review-greenland-00/gsb189p83-98.pdf |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.607.780 http://www.geus.dk/publications/review-greenland-00/gsb189p83-98.pdf |
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