Zobrazeno 1 - 10
of 14
pro vyhledávání: '"T F D Nielsen"'
Publikováno v:
Pilbeam, L H, Rasmussen, T M, Waight, T E & Nielsen, T F D 2023, ' Inverse Modeling to Constrain Composition of CO 2-Rich Parental Melt of Kimberlite : Model Development and Application to the Majuagaa Dyke, Southern West Greenland ', Journal of Petrology, vol. 64, no. 2, 127 . https://doi.org/10.1093/petrology/egac127
A model is developed to test the hypothesis that kimberlites can form by low-degree melting of asthenospheric mantle followed by entrainment and assimilation of lithospheric mantle. The developed model uses inversion calculations based upon rare eart
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::afdf17e33858ac7fb1a6d7e511f81a6d
https://curis.ku.dk/portal/da/publications/inverse-modeling-to-constrain-composition-of-co2rich-parental-melt-of-kimberlite(362b44c1-c14d-4318-b29e-8b871e9ec212).html
https://curis.ku.dk/portal/da/publications/inverse-modeling-to-constrain-composition-of-co2rich-parental-melt-of-kimberlite(362b44c1-c14d-4318-b29e-8b871e9ec212).html
Autor:
C. K. Brooks, T. F. D. Nielsen
Publikováno v:
Economic Geology. 90:1911-1917
A survey of precious metals, Ni and Cu levels, and their mutual relationships in several magma suites of the East Greenland volcanic passive margin shows that the magma type which was parental to the Skaergaard intrusion was markedly enriched in Pt,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::88a0bce706e244f31197788e5fc157e7
https://doi.org/10.2113/gsecongeo.90.7.1911
https://doi.org/10.2113/gsecongeo.90.7.1911
Autor:
C. K. Brooks, T. F. D. Nielsen
Publikováno v:
Contributions to Mineralogy and Petrology. 104:244-247
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0d2423e77ccb6eb84394f0a666c120c1
https://doi.org/10.1007/bf00306448
https://doi.org/10.1007/bf00306448
Publikováno v:
Frontiers in Mineral Sciences 2007 (Cambridge, UK 2007)
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::e35b281d9cd8190c6df58f7828c72048
https://gfzpublic.gfz-potsdam.de/pubman/item/item_235437
https://gfzpublic.gfz-potsdam.de/pubman/item/item_235437
Publikováno v:
European Union of Geosciences-EUG XI Meeting (Strasbourg 2001)
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::aa931a79a7656671167d3ab18d03dd5f
https://gfzpublic.gfz-potsdam.de/pubman/item/item_228771
https://gfzpublic.gfz-potsdam.de/pubman/item/item_228771
Publikováno v:
Geology. 21:857
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0285748474c322569c8d157c2db440c7
https://doi.org/10.1130/0091-7613(1993)021<0857:trodif>2.3.co
https://doi.org/10.1130/0091-7613(1993)021<0857:trodif>2.3.co
Autor:
T. F. D. Nielsen
Publikováno v:
Contributions to Mineralogy and Petrology. 76:60-72
The ultramafic cumulate series of the ultramafic, alkaline and carbonatite bearing Gardiner complex in East Greenland is divided in: 1) Contact zone of plagio-clase-bearing alkaline rocks chilled to the surrounding gneisses and alkaline lavas; 2) a b
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bcbdf99b345d2095d2e1da95b7cd0f3f
https://doi.org/10.1007/bf00373684
https://doi.org/10.1007/bf00373684
Autor:
C. K. Brooks, T. F. D. Nielsen
Publikováno v:
Journal of the Geological Society. 139:265-275
The E Greenland continental margin differs from typical margins in having a superimposed regional uplift which has exposed the early rift products for direct examination. Most of the igneous rocks in this region find counterparts in the oceanic setti
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6476c1bce4fd747d9b9cd6afec2ab505
https://doi.org/10.1144/gsjgs.139.3.0265
https://doi.org/10.1144/gsjgs.139.3.0265
Autor:
T. F. D. Nielsen
Publikováno v:
Contributions to Mineralogy and Petrology. 69:235-244
The formation and stabilities of Fe2+-NAT (NaTi1/2Fe2+ 1/2Si2O6) and Mg-NAT (NaT1/2Mg1/2 Si2O6) clinopyroxene end-members in peralkaline nepheline syenites of a shonkinite-nepheline syenite suite in the Tertiary ultramafic alkaline Gardiner complex,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7b8ef8e0cc89fe0bdd282accbf2538ef
https://doi.org/10.1007/bf00372325
https://doi.org/10.1007/bf00372325
Autor:
C. K. Brooks, T. F. D. Nielsen
Publikováno v:
Journal of the Geological Society. 138:559-568
The structure of the E Greenland coastal flexure, a major structure developed during continental break-up, is interpreted on the basis of field observations. An earlier model, which involves normal inland-dipping, antithetic faulting and seaward rota
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6c4e3486bc823caf54f85f698569ff8b
https://doi.org/10.1144/gsjgs.138.5.0559
https://doi.org/10.1144/gsjgs.138.5.0559