id ftdatacite:10.1594/pangaea.868499
record_format openpolar
spelling 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
institution 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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