(Table 1) Apatite fission track (AFT) data of the Eisenhower Range ...
The Transantarctic Mountains (TAM) were one of the first regions where apatite fission track (AFT) thermochronology was applied routinely to study exhumation processes and long term landscape evolution. Pioneering publications from the region introduced or refined interpretation concepts of thermoch...
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ftdatacite:10.1594/pangaea.868499 2023-10-01T03:51:20+02:00 (Table 1) Apatite fission track (AFT) data of the Eisenhower Range ... Prenzel, Jannis Lisker, Frank Balestrieri, Maria Laura Läufer, Andreas Spiegel, Cornelia 2016 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.868499 https://doi.pangaea.de/10.1594/PANGAEA.868499 en eng PANGAEA https://dx.doi.org/10.1016/j.chemgeo.2013.06.005 Creative Commons Attribution Non Commercial Share Alike 3.0 Unported https://creativecommons.org/licenses/by-nc-sa/3.0/legalcode cc-by-nc-sa-3.0 Event label Latitude of event Longitude of event Elevation of event Area/locality Number Standard deviation Fission-tracks, density, counted in stan Fission-tracks Fission-tracks, spontaneous, density Fission-tracks, spontaneous Fission-tracks, induced, density Fission-tracks, induced Percentage Grains, counted/analyzed Age, dated Age, dated standard deviation Fission-track length, mean Fission-track length, mean, standard deviation Number of observations Goodness of fit Diameter Rock sample GANOVEX_IX Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas SPP1158 Dataset Supplementary Dataset dataset 2016 ftdatacite https://doi.org/10.1594/pangaea.86849910.1016/j.chemgeo.2013.06.005 2023-09-04T14:52:34Z The Transantarctic Mountains (TAM) were one of the first regions where apatite fission track (AFT) thermochronology was applied routinely to study exhumation processes and long term landscape evolution. Pioneering publications from the region introduced or refined interpretation concepts of thermochronological data such as the break in slope in vertical age profiles as qualitative marker for the onset of accelerated rock cooling. New AFT data were compiled from vertical profiles in the Eisenhower Range, northern TAM, and compared with published data. Samples originally examined by population technique were re-analysed via the external detector technique. AFT ages increase from 32±2 Ma at an elevation of 220 m to 175±14 Ma at 2380 m. Geological evidence and thermal history modeling of the AFT data require Jurassic to Late Eocene reheating of the samples and an onset of cooling at ~35 - 30 Ma. This requires the deposition of a ~3 to 3.5 km thick sedimentary sequence on the granitic basement subsequent to ... : Supplement to: Prenzel, Jannis; Lisker, Frank; Balestrieri, Maria Laura; Läufer, Andreas; Spiegel, Cornelia (2013): The Eisenhower Range, Transantarctic Mountains: Evaluation of qualitative interpretation concepts of thermochronological data. Chemical Geology, 352, 176-187 ... Dataset Antarc* Antarctic Arctic Sea ice DataCite Metadata Store (German National Library of Science and Technology) Andreas ENVELOPE(-60.729,-60.729,-64.008,-64.008) Antarctic Arctic Eisenhower Range ENVELOPE(162.250,162.250,-74.250,-74.250) Transantarctic Mountains |
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Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
Event label Latitude of event Longitude of event Elevation of event Area/locality Number Standard deviation Fission-tracks, density, counted in stan Fission-tracks Fission-tracks, spontaneous, density Fission-tracks, spontaneous Fission-tracks, induced, density Fission-tracks, induced Percentage Grains, counted/analyzed Age, dated Age, dated standard deviation Fission-track length, mean Fission-track length, mean, standard deviation Number of observations Goodness of fit Diameter Rock sample GANOVEX_IX Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas SPP1158 |
spellingShingle |
Event label Latitude of event Longitude of event Elevation of event Area/locality Number Standard deviation Fission-tracks, density, counted in stan Fission-tracks Fission-tracks, spontaneous, density Fission-tracks, spontaneous Fission-tracks, induced, density Fission-tracks, induced Percentage Grains, counted/analyzed Age, dated Age, dated standard deviation Fission-track length, mean Fission-track length, mean, standard deviation Number of observations Goodness of fit Diameter Rock sample GANOVEX_IX Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas SPP1158 Prenzel, Jannis Lisker, Frank Balestrieri, Maria Laura Läufer, Andreas Spiegel, Cornelia (Table 1) Apatite fission track (AFT) data of the Eisenhower Range ... |
topic_facet |
Event label Latitude of event Longitude of event Elevation of event Area/locality Number Standard deviation Fission-tracks, density, counted in stan Fission-tracks Fission-tracks, spontaneous, density Fission-tracks, spontaneous Fission-tracks, induced, density Fission-tracks, induced Percentage Grains, counted/analyzed Age, dated Age, dated standard deviation Fission-track length, mean Fission-track length, mean, standard deviation Number of observations Goodness of fit Diameter Rock sample GANOVEX_IX Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas SPP1158 |
description |
The Transantarctic Mountains (TAM) were one of the first regions where apatite fission track (AFT) thermochronology was applied routinely to study exhumation processes and long term landscape evolution. Pioneering publications from the region introduced or refined interpretation concepts of thermochronological data such as the break in slope in vertical age profiles as qualitative marker for the onset of accelerated rock cooling. New AFT data were compiled from vertical profiles in the Eisenhower Range, northern TAM, and compared with published data. Samples originally examined by population technique were re-analysed via the external detector technique. AFT ages increase from 32±2 Ma at an elevation of 220 m to 175±14 Ma at 2380 m. Geological evidence and thermal history modeling of the AFT data require Jurassic to Late Eocene reheating of the samples and an onset of cooling at ~35 - 30 Ma. This requires the deposition of a ~3 to 3.5 km thick sedimentary sequence on the granitic basement subsequent to ... : Supplement to: Prenzel, Jannis; Lisker, Frank; Balestrieri, Maria Laura; Läufer, Andreas; Spiegel, Cornelia (2013): The Eisenhower Range, Transantarctic Mountains: Evaluation of qualitative interpretation concepts of thermochronological data. Chemical Geology, 352, 176-187 ... |
format |
Dataset |
author |
Prenzel, Jannis Lisker, Frank Balestrieri, Maria Laura Läufer, Andreas Spiegel, Cornelia |
author_facet |
Prenzel, Jannis Lisker, Frank Balestrieri, Maria Laura Läufer, Andreas Spiegel, Cornelia |
author_sort |
Prenzel, Jannis |
title |
(Table 1) Apatite fission track (AFT) data of the Eisenhower Range ... |
title_short |
(Table 1) Apatite fission track (AFT) data of the Eisenhower Range ... |
title_full |
(Table 1) Apatite fission track (AFT) data of the Eisenhower Range ... |
title_fullStr |
(Table 1) Apatite fission track (AFT) data of the Eisenhower Range ... |
title_full_unstemmed |
(Table 1) Apatite fission track (AFT) data of the Eisenhower Range ... |
title_sort |
(table 1) apatite fission track (aft) data of the eisenhower range ... |
publisher |
PANGAEA |
publishDate |
2016 |
url |
https://dx.doi.org/10.1594/pangaea.868499 https://doi.pangaea.de/10.1594/PANGAEA.868499 |
long_lat |
ENVELOPE(-60.729,-60.729,-64.008,-64.008) ENVELOPE(162.250,162.250,-74.250,-74.250) |
geographic |
Andreas Antarctic Arctic Eisenhower Range Transantarctic Mountains |
geographic_facet |
Andreas Antarctic Arctic Eisenhower Range Transantarctic Mountains |
genre |
Antarc* Antarctic Arctic Sea ice |
genre_facet |
Antarc* Antarctic Arctic Sea ice |
op_relation |
https://dx.doi.org/10.1016/j.chemgeo.2013.06.005 |
op_rights |
Creative Commons Attribution Non Commercial Share Alike 3.0 Unported https://creativecommons.org/licenses/by-nc-sa/3.0/legalcode cc-by-nc-sa-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.86849910.1016/j.chemgeo.2013.06.005 |
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1778534987094556672 |