Bulk Liquid for the Skaergaard Intrusion and Its PGE-Au Mineralization: Composition, Correlation, Liquid Line of Descent, and Timing of Sulphide Saturation and Silicate–Silicate Immiscibility

Autor: C. Kent Brooks, Troels F.D. Nielsen, Jakob K. Keiding

Publikováno v: Journal of Petrology. 60:1853-1880

Preferred and modelled bulk composition of the Skaergaard intrusion are compared to coeval basaltic compositions in East Greenland and found to relate to the second evolved cycle of Geikie Plateau Formation lavas and coeval Skaergaard-like dikes in m

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::9d5f3c493d32f32d259a3d9f6aba4177
https://doi.org/10.1093/petrology/egz055

On the Skaergaard intrusion and forward modeling of its liquid line of descent: A reply to 'Principles of applied experimental igneous petrology' by Morse, 2008, Lithos 105, pp. 395−399

Autor: Charles E. Lesher, C. Kent Brooks, Peter Thy, Troels F.D. Nielsen

Publikováno v: Lithos. 105:401-411

Forward modeling based on an experimental investigation successfully duplicated main features of the gabbros in the Skaergaard layered series [Thy, P., Lesher, C.E., Nielsen, T.F.D., and Brooks, C.K. 2006. Experimental constraints on the Skaergaard l

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::f1629f6de8781c94849e6fa0fc5dde41
https://doi.org/10.1016/j.lithos.2008.04.007

Formation of low-δ18O magmas of the Kangerlussuaq Intrusion by addition of water derived from dehydration of foundered basaltic roof rocks

Autor: Chris Harris, Christian Tegner, Morten S. Riishuus, C. Kent Brooks, David W. Peate, J. Richard Wilson

Publikováno v: Riishuus, M S, Harris, C, Peate, D W, Tegner, C, Wilson, J R & Brooks, C K 2015, ' Formation of low-δ 18 O magmas of the Kangerlussuaq Intrusion by addition of water derived from dehydration of foundered basaltic roof rocks ', Contributions to Mineralogy and Petrology, vol. 169, no. iss. 5,, Art.no. 41 . https://doi.org/10.1007/s00410-015-1134-7

The Kangerlussuaq Intrusion in East Greenland is concentrically zoned from quartz nordmarkite (quartz syenite) at the margin, through pulaskite, to foyaite (nepheline syenite) in the centre, with no apparent intrusive contacts. The δ18O values of co

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6def8819837d18b73f3d3bc0806f7fe0
https://doi.org/10.1007/s00410-015-1134-7

Ultra-depleted, shallow cratonic mantle beneath West Greenland: dunitic xenoliths from Ubekendt Ejland

Autor: Peter B. Kelemen, Karen Hanghøj, Stefan Bernstein, C. Kent Brooks

Publikováno v: Contributions to Mineralogy and Petrology. 152:335-347

Dunitic xenoliths from late Palaeogene, alkaline basalt flows on Ubekendt Ejland, West Greenland contain olivine with 100 × Mg/(Mg + Fe), or Mg#, between 92.0 and 93.7. Orthopyroxene has very low Al2O3 and CaO contents (0.024–1.639 and 0.062–0.2

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::3e91f413364824df30b254088d264765
https://doi.org/10.1007/s00410-006-0109-0

Magma plumbing systems in large igneous provinces: Inferences from cyclical variations in Palaeogene East Greenland basalts

Autor: C. Kent Brooks, David W. Peate, Rasmus Andreasen

Publikováno v: Contributions to Mineralogy and Petrology. 147:438-452

We present compositional data on a 1,250-m-thick sequence of sparsely porphyritic lavas that comprise the Geikie Plateau Formation, part of the ~55-Ma break-up-related flood basalts in East Greenland. Major element compositions are relatively restric

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::828773714adfe5743980cc822869feea
https://doi.org/10.1007/s00410-004-0566-2