The Skaergaard intrusion (Fig. 1) is probably the most stud- ied layered gabbro intrusion in the world (Wager & Deer
2004). The intrusion is c. 54.5 Ma old and was formed dur-ing the Palaeogene opening of the North Atlantic Ocean, intruding into the base of the East Greenland flood basalts. The intrusion is relatively small with a volume of c. 300 km3 (Nielsen 2004). Spectacular magmatic layering and system-atic e...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.631.5904 2023-05-15T16:03:44+02:00 The Skaergaard intrusion (Fig. 1) is probably the most stud- ied layered gabbro intrusion in the world (Wager & Deer The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.631.5904 http://www.geus.dk/publications/bull/nr17/nr17_p61-64.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.631.5904 http://www.geus.dk/publications/bull/nr17/nr17_p61-64.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.geus.dk/publications/bull/nr17/nr17_p61-64.pdf text ftciteseerx 2016-01-08T15:30:34Z 2004). The intrusion is c. 54.5 Ma old and was formed dur-ing the Palaeogene opening of the North Atlantic Ocean, intruding into the base of the East Greenland flood basalts. The intrusion is relatively small with a volume of c. 300 km3 (Nielsen 2004). Spectacular magmatic layering and system-atic evolution in the compositions of liquidus phases and esti-mated melt compositions (e.g. Wager & Brown 1968) have made the intrusion the most studied example of the develop-ment of the ‘Fenner trend ’ of iron enrichment in basaltic liquids (e.g. Thy et al. in press; Veksler in press). The identification in the late 1980s of significant plat-inum-group elements (PGE) and gold (Au) occurrences in the intrusion (e.g. Bird et al. 1991; Nielsen et al. 2005) has led to continued investigation and exploration drilling. The Skaergaard intrusion is suggested to hold c. 33 million ounces Text East Greenland Greenland North Atlantic Unknown Greenland |
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Open Polar |
collection |
Unknown |
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ftciteseerx |
language |
English |
description |
2004). The intrusion is c. 54.5 Ma old and was formed dur-ing the Palaeogene opening of the North Atlantic Ocean, intruding into the base of the East Greenland flood basalts. The intrusion is relatively small with a volume of c. 300 km3 (Nielsen 2004). Spectacular magmatic layering and system-atic evolution in the compositions of liquidus phases and esti-mated melt compositions (e.g. Wager & Brown 1968) have made the intrusion the most studied example of the develop-ment of the ‘Fenner trend ’ of iron enrichment in basaltic liquids (e.g. Thy et al. in press; Veksler in press). The identification in the late 1980s of significant plat-inum-group elements (PGE) and gold (Au) occurrences in the intrusion (e.g. Bird et al. 1991; Nielsen et al. 2005) has led to continued investigation and exploration drilling. The Skaergaard intrusion is suggested to hold c. 33 million ounces |
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The Pennsylvania State University CiteSeerX Archives |
format |
Text |
title |
The Skaergaard intrusion (Fig. 1) is probably the most stud- ied layered gabbro intrusion in the world (Wager & Deer |
spellingShingle |
The Skaergaard intrusion (Fig. 1) is probably the most stud- ied layered gabbro intrusion in the world (Wager & Deer |
title_short |
The Skaergaard intrusion (Fig. 1) is probably the most stud- ied layered gabbro intrusion in the world (Wager & Deer |
title_full |
The Skaergaard intrusion (Fig. 1) is probably the most stud- ied layered gabbro intrusion in the world (Wager & Deer |
title_fullStr |
The Skaergaard intrusion (Fig. 1) is probably the most stud- ied layered gabbro intrusion in the world (Wager & Deer |
title_full_unstemmed |
The Skaergaard intrusion (Fig. 1) is probably the most stud- ied layered gabbro intrusion in the world (Wager & Deer |
title_sort |
skaergaard intrusion (fig. 1) is probably the most stud- ied layered gabbro intrusion in the world (wager & deer |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.631.5904 http://www.geus.dk/publications/bull/nr17/nr17_p61-64.pdf |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
East Greenland Greenland North Atlantic |
genre_facet |
East Greenland Greenland North Atlantic |
op_source |
http://www.geus.dk/publications/bull/nr17/nr17_p61-64.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.631.5904 http://www.geus.dk/publications/bull/nr17/nr17_p61-64.pdf |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766399431881523200 |