Supplementary files for: Petrology of the Skaergaard Layered Series ...
The Skaergaard intrusion is a layered, ferrobasaltic intrusion emplaced during the Early Eocene into the rifting volcanic margin of East Greenland. The magma chamber crystallised in response to cooling from the roof and margins upwards and inward, forming upper, marginal and bottom series, the latte...
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ftdatacite:10.22008/fk2/utfjp4 2024-03-31T07:52:30+00:00 Supplementary files for: Petrology of the Skaergaard Layered Series ... Thy, Peter Tegner, Christian Lesher, Charles E. 2023 https://dx.doi.org/10.22008/fk2/utfjp4 https://dataverse.geus.dk/citation?persistentId=doi:10.22008/FK2/UTFJP4 unknown GEUS Dataverse https://dx.doi.org/10.22008/fk2/utfjp4/tvibzw https://dx.doi.org/10.22008/fk2/utfjp4/pf3qqv https://dx.doi.org/10.22008/fk2/utfjp4/tg5uvo https://dx.doi.org/10.22008/fk2/utfjp4/l52bht https://dx.doi.org/10.22008/fk2/utfjp4/indgej https://dx.doi.org/10.22008/fk2/utfjp4/tjkdpq https://dx.doi.org/10.22008/fk2/utfjp4/6doaqd https://dx.doi.org/10.22008/fk2/utfjp4/xbjyru https://dx.doi.org/10.22008/fk2/utfjp4/vybs0m https://dx.doi.org/10.22008/fk2/utfjp4/bwjg6y https://dx.doi.org/10.22008/fk2/utfjp4/3o3p5f https://dx.doi.org/10.22008/fk2/utfjp4/hjjwqr https://dx.doi.org/10.22008/fk2/utfjp4/uevy9k https://dx.doi.org/10.22008/fk2/utfjp4/ibhbav https://dx.doi.org/10.22008/fk2/utfjp4/pfcmfa https://dx.doi.org/10.22008/fk2/utfjp4/pbgdsh https://dx.doi.org/10.22008/fk2/utfjp4/qvnqsz https://dx.doi.org/10.22008/fk2/utfjp4/w3cbqx https://dx.doi.org/10.22008/fk2/utfjp4/ugyfnr https://dx.doi.org/10.22008/fk2/utfjp4/kxruv2 dataset Dataset 2023 ftdatacite https://doi.org/10.22008/fk2/utfjp410.22008/fk2/utfjp4/tvibzw10.22008/fk2/utfjp4/pf3qqv10.22008/fk2/utfjp4/tg5uvo10.22008/fk2/utfjp4/l52bht10.22008/fk2/utfjp4/indgej10.22008/fk2/utfjp4/tjkdpq10.22008/fk2/utfjp4/6doaqd10.22008/fk2/utfjp4/xbjyru10.22008/fk2 2024-03-04T12:33:26Z The Skaergaard intrusion is a layered, ferrobasaltic intrusion emplaced during the Early Eocene into the rifting volcanic margin of East Greenland. The magma chamber crystallised in response to cooling from the roof and margins upwards and inward, forming upper, marginal and bottom series, the latter referred to as the Layered Series. The phase layering in the bottom series suggests an evolved, olivine-normative tholeiitic melt saturated in plagioclase and olivine, followed by augite, and then simultaneously by ilmenite and magnetite forming primocrysts. Pigeonite appears in the lower parts and continues until the centre of the series. Apatite appears in the upper part concurrently with liquid immiscibility. Cryptic variations of the individual primocrysts record a systematic upward increase in iron and decrease in magnesium for the mafic minerals and a systematic increase in sodium and decrease in calcium for plagioclase. The appearance of pigeonite is caused by reactions and crystallisation in the trapped ... Dataset East Greenland Greenland DataCite Metadata Store (German National Library of Science and Technology) Greenland |
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Open Polar |
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DataCite Metadata Store (German National Library of Science and Technology) |
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ftdatacite |
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description |
The Skaergaard intrusion is a layered, ferrobasaltic intrusion emplaced during the Early Eocene into the rifting volcanic margin of East Greenland. The magma chamber crystallised in response to cooling from the roof and margins upwards and inward, forming upper, marginal and bottom series, the latter referred to as the Layered Series. The phase layering in the bottom series suggests an evolved, olivine-normative tholeiitic melt saturated in plagioclase and olivine, followed by augite, and then simultaneously by ilmenite and magnetite forming primocrysts. Pigeonite appears in the lower parts and continues until the centre of the series. Apatite appears in the upper part concurrently with liquid immiscibility. Cryptic variations of the individual primocrysts record a systematic upward increase in iron and decrease in magnesium for the mafic minerals and a systematic increase in sodium and decrease in calcium for plagioclase. The appearance of pigeonite is caused by reactions and crystallisation in the trapped ... |
format |
Dataset |
author |
Thy, Peter Tegner, Christian Lesher, Charles E. |
spellingShingle |
Thy, Peter Tegner, Christian Lesher, Charles E. Supplementary files for: Petrology of the Skaergaard Layered Series ... |
author_facet |
Thy, Peter Tegner, Christian Lesher, Charles E. |
author_sort |
Thy, Peter |
title |
Supplementary files for: Petrology of the Skaergaard Layered Series ... |
title_short |
Supplementary files for: Petrology of the Skaergaard Layered Series ... |
title_full |
Supplementary files for: Petrology of the Skaergaard Layered Series ... |
title_fullStr |
Supplementary files for: Petrology of the Skaergaard Layered Series ... |
title_full_unstemmed |
Supplementary files for: Petrology of the Skaergaard Layered Series ... |
title_sort |
supplementary files for: petrology of the skaergaard layered series ... |
publisher |
GEUS Dataverse |
publishDate |
2023 |
url |
https://dx.doi.org/10.22008/fk2/utfjp4 https://dataverse.geus.dk/citation?persistentId=doi:10.22008/FK2/UTFJP4 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
East Greenland Greenland |
genre_facet |
East Greenland Greenland |
op_relation |
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