CT and MH were supported by a Royal Society International Joint Project grant, and by the Carlsberg Foundation. CT was also supported by the Danish Council of Independent Research and the Danish National Research Foundation. The project was supported by the Natural Environment Research Council [grant number NE/F020325/1]. ON acknowledges support from Magdalene College (University of Cambridge) and the von Humboldt Foundation (Germany; University of Hannover)
Abstract The Skaergaard Intrusion of East Greenland solidified as a closed system, wi...
Volatiles can have a substantial influence on the constrains and genesis of ore deposit, but are not...
This paper presents a new high-precision zircon U-Pb geochronological view on the crystallization an...
The Cambridge Drill Core provides a continuous sample of the lower part of the floor cumulates of th...
The Cambridge Drill Core provides a continuous sample of the lower part of the floor cumulates of th...
The Skaergaard Intrusion of East Greenland is cut by several generations of dykes, the earliest of w...
AbstractThe Skaergaard Intrusion of East Greenland is cut by several generations of dykes, the earli...
The Palaeogene Skaergaard intrusion, East Greenland, has since its first description by Wager & ...
The Skaergaard intrusion is a layered, ferrobasaltic intrusion emplaced during the Early Eocene into...
This is the final version of the article. Available from Springer verlag via the DOI in this record....
This is the author accepted manuscript. The final version is available from Oxford University Press ...
The Skaergaard intrusion (Fig. 1) is probably the most studied layered gabbro intrusion in the world...
The upper parts of the floor cumulates of the Skaergaard Intrusion, East Greenland, contain abundant...
The Eocene Skaergaard intrusion, part of the East Greenland flood basalt province, is the type examp...
Oxygen isotope analyses have been obtained on rocks and coexisting minerals, principally plagioclase...
Abstract The Skaergaard Intrusion of East Greenland solidified as a closed system, wi...
Volatiles can have a substantial influence on the constrains and genesis of ore deposit, but are not...
This paper presents a new high-precision zircon U-Pb geochronological view on the crystallization an...
The Cambridge Drill Core provides a continuous sample of the lower part of the floor cumulates of th...
The Cambridge Drill Core provides a continuous sample of the lower part of the floor cumulates of th...
The Skaergaard Intrusion of East Greenland is cut by several generations of dykes, the earliest of w...
AbstractThe Skaergaard Intrusion of East Greenland is cut by several generations of dykes, the earli...
The Palaeogene Skaergaard intrusion, East Greenland, has since its first description by Wager & ...
The Skaergaard intrusion is a layered, ferrobasaltic intrusion emplaced during the Early Eocene into...
This is the final version of the article. Available from Springer verlag via the DOI in this record....
This is the author accepted manuscript. The final version is available from Oxford University Press ...
The Skaergaard intrusion (Fig. 1) is probably the most studied layered gabbro intrusion in the world...
The upper parts of the floor cumulates of the Skaergaard Intrusion, East Greenland, contain abundant...
The Eocene Skaergaard intrusion, part of the East Greenland flood basalt province, is the type examp...
Oxygen isotope analyses have been obtained on rocks and coexisting minerals, principally plagioclase...
Abstract The Skaergaard Intrusion of East Greenland solidified as a closed system, wi...
Volatiles can have a substantial influence on the constrains and genesis of ore deposit, but are not...
This paper presents a new high-precision zircon U-Pb geochronological view on the crystallization an...