Apatite fission crack data from the Eisenhauer Range, Antarctica
The Eisenhower Range is a N-S trending mountain range in the Transantarctic Mountains (TAM) adjacent to the NW Ross Sea Embayment. New AFT and apatite (U-Th-Sm)/He (AHe) data from vertical basement profiles supplemented by paleotemperature and pressure estimates derived from Beacon sandstones provid...
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.868481 2024-09-15T17:48:07+00:00 Apatite fission crack data from the Eisenhauer Range, Antarctica Prenzel, Jannis Lisker, Frank Elsner, Martin Schöner, Robert Balestrieri, Maria Laura Läufer, Andreas Berner, Ulrich Spiegel, Cornelia MEDIAN LATITUDE: -74.151439 * MEDIAN LONGITUDE: 162.179140 * SOUTH-BOUND LATITUDE: -74.710000 * WEST-BOUND LONGITUDE: 161.457000 * NORTH-BOUND LATITUDE: -73.909000 * EAST-BOUND LONGITUDE: 162.784000 2016 application/zip, 2 datasets https://doi.pangaea.de/10.1594/PANGAEA.868481 https://doi.org/10.1594/PANGAEA.868481 en eng PANGAEA Original files of Prenzel et al. (2014) in xls format (URI: https://store.pangaea.de/Publications/Prenzel-etal_2014/Prenzel-al2014.xlsx) https://doi.pangaea.de/10.1594/PANGAEA.868481 https://doi.org/10.1594/PANGAEA.868481 CC-BY-NC-SA-3.0: Creative Commons Attribution-NonCommercial-ShareAlike 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess Supplement to: Prenzel, Jannis; Lisker, Frank; Elsner, Martin; Schöner, Robert; Balestrieri, Maria Laura; Läufer, Andreas; Berner, Ulrich; Spiegel, Cornelia (2014): Burial and exhumation of the Eisenhower Range, Transantarctic Mountains, based on thermochronological, sedimentary rock maturity and petrographic constraints. Tectonophysics, 630, 113-130, https://doi.org/10.1016/j.tecto.2014.05.020 Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas SPP1158 dataset publication series 2016 ftpangaea https://doi.org/10.1594/PANGAEA.86848110.1016/j.tecto.2014.05.020 2024-07-24T02:31:21Z The Eisenhower Range is a N-S trending mountain range in the Transantarctic Mountains (TAM) adjacent to the NW Ross Sea Embayment. New AFT and apatite (U-Th-Sm)/He (AHe) data from vertical basement profiles supplemented by paleotemperature and pressure estimates derived from Beacon sandstones provide new quantitative results on regional burial evolution and first regional constraints on basin inversion and exhumation processes. AFT ages between 32 ± 2 and 259 ± 18 Ma and AHe ages of 37 ± 3-173 ± 16 Ma correlate positively with sample elevations. Thermal history modeling of these data and complementary thermal indications detect heating of the paleosurface on the Eisenhower Range to temperatures >= 80 °C subsequent to Ferrar magmatism, and constrain Late Eocene rapid cooling. Regression of modeled paleotemperatures against sample elevations refers to a high Jurassic (~ 45 °C/km) and a moderate Cretaceous-Eocene (28 ± 8 °C/km) geothermal gradient. The texture of Beacon sandstones supports strong mechanical compaction that requires a higher overburden than preserved in the stratigraphic record. Modeled paleotemperatures and pressures suggest basement burial that increases from Late Jurassic (0.7-1.1 km) to Eocene (1.8-2.1 km). The overburden comprises 0.7-1.1 km cumulative Beacon/Ferrar rocks and 0.7-1.4 km of post-Ferrar sediments. Rapid cooling of the whole sample suite between ~ 35 and 30 Ma implies fast erosion of the post-Ferrar sediments and (re-) exposure of underlying magmatic rocks. Subsequent differential sample cooling to present-day surface temperature infers ongoing exhumation by glacial incision enhanced by isostatic response to basin inversion. Decreasing amounts of exhumation from the coast (> 3 km) toward the interior (1.5-2.2 km) point to backstepping incision along the fault controlled Priestley Glacier. Substantial exhumation of the Eisenhower Range since the Late Eocene is hence triggered by both tectonic and climatic factors, superimposed by considerable lithological influence during the ... Other/Unknown Material Antarc* Antarctic Antarctica Priestley Glacier Ross Sea Sea ice PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(161.457000,162.784000,-73.909000,-74.710000) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas SPP1158 |
spellingShingle |
Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas SPP1158 Prenzel, Jannis Lisker, Frank Elsner, Martin Schöner, Robert Balestrieri, Maria Laura Läufer, Andreas Berner, Ulrich Spiegel, Cornelia Apatite fission crack data from the Eisenhauer Range, Antarctica |
topic_facet |
Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas SPP1158 |
description |
The Eisenhower Range is a N-S trending mountain range in the Transantarctic Mountains (TAM) adjacent to the NW Ross Sea Embayment. New AFT and apatite (U-Th-Sm)/He (AHe) data from vertical basement profiles supplemented by paleotemperature and pressure estimates derived from Beacon sandstones provide new quantitative results on regional burial evolution and first regional constraints on basin inversion and exhumation processes. AFT ages between 32 ± 2 and 259 ± 18 Ma and AHe ages of 37 ± 3-173 ± 16 Ma correlate positively with sample elevations. Thermal history modeling of these data and complementary thermal indications detect heating of the paleosurface on the Eisenhower Range to temperatures >= 80 °C subsequent to Ferrar magmatism, and constrain Late Eocene rapid cooling. Regression of modeled paleotemperatures against sample elevations refers to a high Jurassic (~ 45 °C/km) and a moderate Cretaceous-Eocene (28 ± 8 °C/km) geothermal gradient. The texture of Beacon sandstones supports strong mechanical compaction that requires a higher overburden than preserved in the stratigraphic record. Modeled paleotemperatures and pressures suggest basement burial that increases from Late Jurassic (0.7-1.1 km) to Eocene (1.8-2.1 km). The overburden comprises 0.7-1.1 km cumulative Beacon/Ferrar rocks and 0.7-1.4 km of post-Ferrar sediments. Rapid cooling of the whole sample suite between ~ 35 and 30 Ma implies fast erosion of the post-Ferrar sediments and (re-) exposure of underlying magmatic rocks. Subsequent differential sample cooling to present-day surface temperature infers ongoing exhumation by glacial incision enhanced by isostatic response to basin inversion. Decreasing amounts of exhumation from the coast (> 3 km) toward the interior (1.5-2.2 km) point to backstepping incision along the fault controlled Priestley Glacier. Substantial exhumation of the Eisenhower Range since the Late Eocene is hence triggered by both tectonic and climatic factors, superimposed by considerable lithological influence during the ... |
format |
Other/Unknown Material |
author |
Prenzel, Jannis Lisker, Frank Elsner, Martin Schöner, Robert Balestrieri, Maria Laura Läufer, Andreas Berner, Ulrich Spiegel, Cornelia |
author_facet |
Prenzel, Jannis Lisker, Frank Elsner, Martin Schöner, Robert Balestrieri, Maria Laura Läufer, Andreas Berner, Ulrich Spiegel, Cornelia |
author_sort |
Prenzel, Jannis |
title |
Apatite fission crack data from the Eisenhauer Range, Antarctica |
title_short |
Apatite fission crack data from the Eisenhauer Range, Antarctica |
title_full |
Apatite fission crack data from the Eisenhauer Range, Antarctica |
title_fullStr |
Apatite fission crack data from the Eisenhauer Range, Antarctica |
title_full_unstemmed |
Apatite fission crack data from the Eisenhauer Range, Antarctica |
title_sort |
apatite fission crack data from the eisenhauer range, antarctica |
publisher |
PANGAEA |
publishDate |
2016 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.868481 https://doi.org/10.1594/PANGAEA.868481 |
op_coverage |
MEDIAN LATITUDE: -74.151439 * MEDIAN LONGITUDE: 162.179140 * SOUTH-BOUND LATITUDE: -74.710000 * WEST-BOUND LONGITUDE: 161.457000 * NORTH-BOUND LATITUDE: -73.909000 * EAST-BOUND LONGITUDE: 162.784000 |
long_lat |
ENVELOPE(161.457000,162.784000,-73.909000,-74.710000) |
genre |
Antarc* Antarctic Antarctica Priestley Glacier Ross Sea Sea ice |
genre_facet |
Antarc* Antarctic Antarctica Priestley Glacier Ross Sea Sea ice |
op_source |
Supplement to: Prenzel, Jannis; Lisker, Frank; Elsner, Martin; Schöner, Robert; Balestrieri, Maria Laura; Läufer, Andreas; Berner, Ulrich; Spiegel, Cornelia (2014): Burial and exhumation of the Eisenhower Range, Transantarctic Mountains, based on thermochronological, sedimentary rock maturity and petrographic constraints. Tectonophysics, 630, 113-130, https://doi.org/10.1016/j.tecto.2014.05.020 |
op_relation |
Original files of Prenzel et al. (2014) in xls format (URI: https://store.pangaea.de/Publications/Prenzel-etal_2014/Prenzel-al2014.xlsx) https://doi.pangaea.de/10.1594/PANGAEA.868481 https://doi.org/10.1594/PANGAEA.868481 |
op_rights |
CC-BY-NC-SA-3.0: Creative Commons Attribution-NonCommercial-ShareAlike 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1594/PANGAEA.86848110.1016/j.tecto.2014.05.020 |
_version_ |
1810289241893109760 |