Trace elements in ilmenite, titanomagnetite and apatite unravel the petrogenesis of Fe-Ti-P-(+/-Zr) rich rocks and associated nelsonite from the Raftsund intrusion, Vesterålen-Lofoten AMCG suite, Northern Norway-Reference-Cited by-同舟云学术

Trace elements in ilmenite, titanomagnetite and apatite unravel the petrogenesis of Fe-Ti-P-(+/-Zr) rich rocks and associated nelsonite from the Raftsund intrusion, Vesterålen-Lofoten AMCG suite, Northern Norway

Published:2023-12 Issue: Volume:460-461 Page:107389
ISSN:0024-4937
Container-title:Lithos
language:en
Short-container-title:Lithos

Author:

Coint Nolwenn,Mansur Eduardo T.,Keiding Jakob K.,Skår Øyvind

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference78 articles.

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3. Most granitoid rocks are cumulates: deductions from hornblende compositions and zircon saturation;Barnes;J. Petrol.,2019

4. The Lofoten-Vesterålen continental margin: a multiphase Mesozoic-Palaeogene rifted shelf as shown by offshore-onshore brittle fault-fracture analysis;Bergh;Nor. J. Geol.,2007

5. Stable and metastable silicate liquid immiscibility in ferrobasalts;Charlier;Am. Mineral.,2015

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1. Multi-stage evolution of the monzonitic Larvik Plutonic Complex (Oslo Rift, Norway) and its implications for the formation of the Kodal Fe-Ti-P(−REE) deposit;Lithos;2024-11

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3. Corrigendum to “Trace elements in ilmenite, titanomagnetite and apatite unravel the petrogenesis of Fe-Ti-P (+/-Zr) rich rocks and associated nelsonite from the Raftsund intrusion, Vesterålen-Lofoten AMCG suite, Northern Norway” [Lithos 460–461 (2023) 107389];Lithos;2023-12