IRON ISOTOPE GEOCHEMISTRY OF BULK ROCKS AND Fe-Ti OXIDES FROM THE SKAERGAARD LAYERED MAFIC INTRUSION, SE GREENLAND
Small, but significant fractionation of Fe isotopes occurs in high-temperature igneous rocks. Despite increasing study, the exact causes of this fractionation are still debated. Therefore, a systematic study of a complete igneous intrusive system is presented to evaluate the extent and causes of Fe...
Main Author: | |
---|---|
Other Authors: | , |
Format: | Master Thesis |
Language: | English |
Published: |
East Carolina University
2019
|
Subjects: | |
Online Access: | http://hdl.handle.net/10342/7487 |
id |
fteastcaroluni:oai:TheScholarship.intra.ecu.edu:10342/7487 |
---|---|
record_format |
openpolar |
spelling |
fteastcaroluni:oai:TheScholarship.intra.ecu.edu:10342/7487 2023-05-15T16:26:48+02:00 IRON ISOTOPE GEOCHEMISTRY OF BULK ROCKS AND Fe-Ti OXIDES FROM THE SKAERGAARD LAYERED MAFIC INTRUSION, SE GREENLAND Hammerstrom, Alex Joseph Heimann, Adriana Geological Sciences 2019-08-19T17:41:16Z application/pdf http://hdl.handle.net/10342/7487 en eng East Carolina University http://hdl.handle.net/10342/7487 Fe isotopes Magnetite and ilmenite MC-ICP-MS Gabbros Layered mafic intrusion Igneous rocks--Greenland Skærgården Channel (Greenland) Analytical geochemistry--Greenland Master's Thesis text 2019 fteastcaroluni 2022-07-11T11:40:10Z Small, but significant fractionation of Fe isotopes occurs in high-temperature igneous rocks. Despite increasing study, the exact causes of this fractionation are still debated. Therefore, a systematic study of a complete igneous intrusive system is presented to evaluate the extent and causes of Fe isotope fractionation. The Eocene Skaergaard layered mafic intrusion, SE Greenland has a relatively simple magmatic history and localized superimposed alteration, which makes it a good setting to study Fe isotope fractionation. High-precision Fe isotope compositions ([delta]Fe��, relative to igneous rocks, in ‰) are presented for bulk rocks and bulk Fe-Ti oxides (magnetite-ilmenite) from a suite of 26 gabbros and ferrodiorites that encompasses the magmatic/alteration history of the Skaergaard intrusion. The [delta]Fe�� values of bulk rocks differ only by 0.074‰ (-0.043±0.013‰ to +0.031±0.027; avg. = -0.007±0.012‰, 2-SE; n = 11) and show a lack of or a slight variation with magmatic evolution as measured by plagioclase compositions and bulk-rock geochemistry. These bulk-rock [delta]Fe�� values remain within the 2-SE of the average mafic-intermediate composition of the Earth's crust (0.00±0.08‰ ). The lack of clear measurable trends in [delta]Fe�� values of Skaergaard bulk rocks as a function of magmatic evolution outside of analytical error is consistent with data from other mafic and ultramafic intrusions in that [delta]Fe�� values do not vary as much as in high-silica igneous rocks. In contrast, [delta]Fe�� values of Fe-Ti oxides throughout the evolution vary significantly, up to 0.69‰ (-0.179±0.010‰ to +0.508±0.012‰ , 2-SE; n = 26). A positive correlation between [delta]Fe�� values and Fe3+:Fe2+ ratios for bulk Fe-Ti oxides shows that their Fe isotope compositions are controlled by their Fe3+:Fe2+ ratio. Similar trends of [delta]Fe�� variations in Fe-Ti oxides and previously modeled fO2 values through the Layered Series seem to suggest that Fe isotope ... Master Thesis Greenland East Carolina University: The ScholarShip at ECU Greenland |
institution |
Open Polar |
collection |
East Carolina University: The ScholarShip at ECU |
op_collection_id |
fteastcaroluni |
language |
English |
topic |
Fe isotopes Magnetite and ilmenite MC-ICP-MS Gabbros Layered mafic intrusion Igneous rocks--Greenland Skærgården Channel (Greenland) Analytical geochemistry--Greenland |
spellingShingle |
Fe isotopes Magnetite and ilmenite MC-ICP-MS Gabbros Layered mafic intrusion Igneous rocks--Greenland Skærgården Channel (Greenland) Analytical geochemistry--Greenland Hammerstrom, Alex Joseph IRON ISOTOPE GEOCHEMISTRY OF BULK ROCKS AND Fe-Ti OXIDES FROM THE SKAERGAARD LAYERED MAFIC INTRUSION, SE GREENLAND |
topic_facet |
Fe isotopes Magnetite and ilmenite MC-ICP-MS Gabbros Layered mafic intrusion Igneous rocks--Greenland Skærgården Channel (Greenland) Analytical geochemistry--Greenland |
description |
Small, but significant fractionation of Fe isotopes occurs in high-temperature igneous rocks. Despite increasing study, the exact causes of this fractionation are still debated. Therefore, a systematic study of a complete igneous intrusive system is presented to evaluate the extent and causes of Fe isotope fractionation. The Eocene Skaergaard layered mafic intrusion, SE Greenland has a relatively simple magmatic history and localized superimposed alteration, which makes it a good setting to study Fe isotope fractionation. High-precision Fe isotope compositions ([delta]Fe��, relative to igneous rocks, in ‰) are presented for bulk rocks and bulk Fe-Ti oxides (magnetite-ilmenite) from a suite of 26 gabbros and ferrodiorites that encompasses the magmatic/alteration history of the Skaergaard intrusion. The [delta]Fe�� values of bulk rocks differ only by 0.074‰ (-0.043±0.013‰ to +0.031±0.027; avg. = -0.007±0.012‰, 2-SE; n = 11) and show a lack of or a slight variation with magmatic evolution as measured by plagioclase compositions and bulk-rock geochemistry. These bulk-rock [delta]Fe�� values remain within the 2-SE of the average mafic-intermediate composition of the Earth's crust (0.00±0.08‰ ). The lack of clear measurable trends in [delta]Fe�� values of Skaergaard bulk rocks as a function of magmatic evolution outside of analytical error is consistent with data from other mafic and ultramafic intrusions in that [delta]Fe�� values do not vary as much as in high-silica igneous rocks. In contrast, [delta]Fe�� values of Fe-Ti oxides throughout the evolution vary significantly, up to 0.69‰ (-0.179±0.010‰ to +0.508±0.012‰ , 2-SE; n = 26). A positive correlation between [delta]Fe�� values and Fe3+:Fe2+ ratios for bulk Fe-Ti oxides shows that their Fe isotope compositions are controlled by their Fe3+:Fe2+ ratio. Similar trends of [delta]Fe�� variations in Fe-Ti oxides and previously modeled fO2 values through the Layered Series seem to suggest that Fe isotope ... |
author2 |
Heimann, Adriana Geological Sciences |
format |
Master Thesis |
author |
Hammerstrom, Alex Joseph |
author_facet |
Hammerstrom, Alex Joseph |
author_sort |
Hammerstrom, Alex Joseph |
title |
IRON ISOTOPE GEOCHEMISTRY OF BULK ROCKS AND Fe-Ti OXIDES FROM THE SKAERGAARD LAYERED MAFIC INTRUSION, SE GREENLAND |
title_short |
IRON ISOTOPE GEOCHEMISTRY OF BULK ROCKS AND Fe-Ti OXIDES FROM THE SKAERGAARD LAYERED MAFIC INTRUSION, SE GREENLAND |
title_full |
IRON ISOTOPE GEOCHEMISTRY OF BULK ROCKS AND Fe-Ti OXIDES FROM THE SKAERGAARD LAYERED MAFIC INTRUSION, SE GREENLAND |
title_fullStr |
IRON ISOTOPE GEOCHEMISTRY OF BULK ROCKS AND Fe-Ti OXIDES FROM THE SKAERGAARD LAYERED MAFIC INTRUSION, SE GREENLAND |
title_full_unstemmed |
IRON ISOTOPE GEOCHEMISTRY OF BULK ROCKS AND Fe-Ti OXIDES FROM THE SKAERGAARD LAYERED MAFIC INTRUSION, SE GREENLAND |
title_sort |
iron isotope geochemistry of bulk rocks and fe-ti oxides from the skaergaard layered mafic intrusion, se greenland |
publisher |
East Carolina University |
publishDate |
2019 |
url |
http://hdl.handle.net/10342/7487 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Greenland |
genre_facet |
Greenland |
op_relation |
http://hdl.handle.net/10342/7487 |
_version_ |
1766015780419272704 |