Investigation of the Fe-Ti-HFSE enrichment in the Raftsund intrusion, Årsteinen, Lofoten-Vesterålen archipelago, Northern Norway
Iron+Ti±P±HFSE enriched rocks are found in a variety of localities worldwide, including some that are temporally and spatially related to Proterozoic AMCG (Anorthosite-Mangerite-Charnokite-Granite) suites. The origin of these enriched rocks has been widely debated and petrogenetic models such as liq...
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fttexastechuniv:oai:ttu-ir.tdl.org:2346/85033 2023-05-15T17:08:16+02:00 Investigation of the Fe-Ti-HFSE enrichment in the Raftsund intrusion, Årsteinen, Lofoten-Vesterålen archipelago, Northern Norway Maute, Donald Barnes, Calvin G. Coint, Nolwenn Hetherington, Callum J. 2019-08-02T16:40:08Z application/pdf https://hdl.handle.net/2346/85033 eng eng https://hdl.handle.net/2346/85033 Unrestricted. Iron Titanium Oxides High field strength elements HFSE Raftsund intrusion Årsteinen Zircon Apatite Clinopyroxene Olivine Magnetite Ilmenite Norway Lofoten Vesterålen Mineral accumulation Liquid immiscibility Hydrothermal enrichment Residual liquids LA-ICPMS EPMA XRF Thesis text 2019 fttexastechuniv 2023-01-04T07:25:31Z Iron+Ti±P±HFSE enriched rocks are found in a variety of localities worldwide, including some that are temporally and spatially related to Proterozoic AMCG (Anorthosite-Mangerite-Charnokite-Granite) suites. The origin of these enriched rocks has been widely debated and petrogenetic models such as liquid-liquid immiscibility, fractional crystallization and mineral accumulation, hydrothermal fluid enrichment, and residual liquids concentrated by filter pressing have all been proposed to explain occurrences of these rocks associated with AMCG suites. This locality is particularly distinct for two reasons, 1) abundant and large (>2.5mm) zircon, which contrasts with many Fe+Ti±P±HFSE enriched rocks where apatite is the main REE carrier 2) the mineralized zones are located as thin veins (up to 3 cm wide) located at the contact between two rock-types – an equigranular olivine-clinopyroxene-monzonite and a porphyritic orthopyroxene-clinopyroxene monzonite. Field relationships down to the microscale suggest the mineralization is related to the equigranular monzonite - the mineralized zones show planar contacts with the porphyritic monzonite, while it protrudes in between mesoperthitic feldspar grains of the equigranular monzonite. The mineralized zones likely developed from the equigranular monzonite, while the porphyritic monzonite served as a boundary where the mineralization was concentrated. Mg# and Fo% in clinopyroxene and olivine, respectively, are highest in phases of the mineralization (35.0 and 6.17) compared to the equigranular monzonite (22.2 and 2.50) and are can be suggested to be early-forming. Magnetite in the mineralization also has relatively elevated V and Al, which are known to behave as fractionation indices, and indicates earlier forming magnetite compared to magnetite in the equigranular monzonite. Strontium content and Eu/Eu* of apatite in the mineralization indicate a contradicting relationship – having more evolved signature compared to apatite of both the equigranular monzonite indicating ... Thesis Lofoten Northern Norway Vesterålen Texas Tech University: TTU DSpace Repository Årsteinen ENVELOPE(15.000,15.000,68.280,68.280) Lofoten Norway Vesterålen ENVELOPE(14.939,14.939,68.754,68.754) |
institution |
Open Polar |
collection |
Texas Tech University: TTU DSpace Repository |
op_collection_id |
fttexastechuniv |
language |
English |
topic |
Iron Titanium Oxides High field strength elements HFSE Raftsund intrusion Årsteinen Zircon Apatite Clinopyroxene Olivine Magnetite Ilmenite Norway Lofoten Vesterålen Mineral accumulation Liquid immiscibility Hydrothermal enrichment Residual liquids LA-ICPMS EPMA XRF |
spellingShingle |
Iron Titanium Oxides High field strength elements HFSE Raftsund intrusion Årsteinen Zircon Apatite Clinopyroxene Olivine Magnetite Ilmenite Norway Lofoten Vesterålen Mineral accumulation Liquid immiscibility Hydrothermal enrichment Residual liquids LA-ICPMS EPMA XRF Maute, Donald Investigation of the Fe-Ti-HFSE enrichment in the Raftsund intrusion, Årsteinen, Lofoten-Vesterålen archipelago, Northern Norway |
topic_facet |
Iron Titanium Oxides High field strength elements HFSE Raftsund intrusion Årsteinen Zircon Apatite Clinopyroxene Olivine Magnetite Ilmenite Norway Lofoten Vesterålen Mineral accumulation Liquid immiscibility Hydrothermal enrichment Residual liquids LA-ICPMS EPMA XRF |
description |
Iron+Ti±P±HFSE enriched rocks are found in a variety of localities worldwide, including some that are temporally and spatially related to Proterozoic AMCG (Anorthosite-Mangerite-Charnokite-Granite) suites. The origin of these enriched rocks has been widely debated and petrogenetic models such as liquid-liquid immiscibility, fractional crystallization and mineral accumulation, hydrothermal fluid enrichment, and residual liquids concentrated by filter pressing have all been proposed to explain occurrences of these rocks associated with AMCG suites. This locality is particularly distinct for two reasons, 1) abundant and large (>2.5mm) zircon, which contrasts with many Fe+Ti±P±HFSE enriched rocks where apatite is the main REE carrier 2) the mineralized zones are located as thin veins (up to 3 cm wide) located at the contact between two rock-types – an equigranular olivine-clinopyroxene-monzonite and a porphyritic orthopyroxene-clinopyroxene monzonite. Field relationships down to the microscale suggest the mineralization is related to the equigranular monzonite - the mineralized zones show planar contacts with the porphyritic monzonite, while it protrudes in between mesoperthitic feldspar grains of the equigranular monzonite. The mineralized zones likely developed from the equigranular monzonite, while the porphyritic monzonite served as a boundary where the mineralization was concentrated. Mg# and Fo% in clinopyroxene and olivine, respectively, are highest in phases of the mineralization (35.0 and 6.17) compared to the equigranular monzonite (22.2 and 2.50) and are can be suggested to be early-forming. Magnetite in the mineralization also has relatively elevated V and Al, which are known to behave as fractionation indices, and indicates earlier forming magnetite compared to magnetite in the equigranular monzonite. Strontium content and Eu/Eu* of apatite in the mineralization indicate a contradicting relationship – having more evolved signature compared to apatite of both the equigranular monzonite indicating ... |
author2 |
Barnes, Calvin G. Coint, Nolwenn Hetherington, Callum J. |
format |
Thesis |
author |
Maute, Donald |
author_facet |
Maute, Donald |
author_sort |
Maute, Donald |
title |
Investigation of the Fe-Ti-HFSE enrichment in the Raftsund intrusion, Årsteinen, Lofoten-Vesterålen archipelago, Northern Norway |
title_short |
Investigation of the Fe-Ti-HFSE enrichment in the Raftsund intrusion, Årsteinen, Lofoten-Vesterålen archipelago, Northern Norway |
title_full |
Investigation of the Fe-Ti-HFSE enrichment in the Raftsund intrusion, Årsteinen, Lofoten-Vesterålen archipelago, Northern Norway |
title_fullStr |
Investigation of the Fe-Ti-HFSE enrichment in the Raftsund intrusion, Årsteinen, Lofoten-Vesterålen archipelago, Northern Norway |
title_full_unstemmed |
Investigation of the Fe-Ti-HFSE enrichment in the Raftsund intrusion, Årsteinen, Lofoten-Vesterålen archipelago, Northern Norway |
title_sort |
investigation of the fe-ti-hfse enrichment in the raftsund intrusion, årsteinen, lofoten-vesterålen archipelago, northern norway |
publishDate |
2019 |
url |
https://hdl.handle.net/2346/85033 |
long_lat |
ENVELOPE(15.000,15.000,68.280,68.280) ENVELOPE(14.939,14.939,68.754,68.754) |
geographic |
Årsteinen Lofoten Norway Vesterålen |
geographic_facet |
Årsteinen Lofoten Norway Vesterålen |
genre |
Lofoten Northern Norway Vesterålen |
genre_facet |
Lofoten Northern Norway Vesterålen |
op_relation |
https://hdl.handle.net/2346/85033 |
op_rights |
Unrestricted. |
_version_ |
1766063996592455680 |