Table 1: Station data for the entire survey, including coordinates and description of BPBASE ...

During GANOVEX VI new gravity data were collected along an east-west profile in North Victoria Land south of the Drygalski Ice Tongue, extending 150 km across the Transantarctic Mountains, and comprising 21 data points. Thirty five additional data points were collected over a small area near Brimsto...

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Bibliographic Details
Main Authors: Redfield, Tim, Behrendt, John, Damaske, Detlef, Delisle, Georg, Möller, Dieter, Sievers, Joachim
Format: Dataset
Language:English
Published: PANGAEA 2011
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.763366
https://doi.pangaea.de/10.1594/PANGAEA.763366
id ftdatacite:10.1594/pangaea.763366
record_format openpolar
spelling ftdatacite:10.1594/pangaea.763366 2024-09-15T18:35:30+00:00 Table 1: Station data for the entire survey, including coordinates and description of BPBASE ... Redfield, Tim Behrendt, John Damaske, Detlef Delisle, Georg Möller, Dieter Sievers, Joachim 2011 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.763366 https://doi.pangaea.de/10.1594/PANGAEA.763366 en eng PANGAEA Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Event label Station label LATITUDE LONGITUDE ELEVATION Sea ice thickness Correction Bouguer anomaly Gravimetry dataset Supplementary Dataset Dataset 2011 ftdatacite https://doi.org/10.1594/pangaea.763366 2024-08-01T11:01:17Z During GANOVEX VI new gravity data were collected along an east-west profile in North Victoria Land south of the Drygalski Ice Tongue, extending 150 km across the Transantarctic Mountains, and comprising 21 data points. Thirty five additional data points were collected over a small area near Brimstone Peak, near the western end of the regional profile. The survey south of the Drygalski has been connected to northern gravity data (GANOVEX V) by a survey line of 12 points. All data have been terrain corrected, and are further constrained by satellite elevation (GPS) and radar ice-thickness measurements. A pronounced regional Bouguer gravity gradient decreasing to the west by approximately 3 mgal/km is superimposed over a coast-parallel belt of granitoid basement rock. West of this belt the local gravity fields become mote variable. Over Beta Peak (Ferrar dolerite) a 50 mgal spike is obser- ved. Within this area, the Ferrar sills are exposed at the surface. West of Brimstone Peak (Ferrar/Kirk patrick ... : Supplement to: Redfield, Tim; Behrendt, John; Damaske, Detlef; Delisle, Georg; Möller, Dieter; Sievers, Joachim (1992): 21. Gravity transect across the Transantarctic Mountains South of the Drygalski lce Tongue. Polarforschung, 60(2), 143-151 ... Dataset Sea ice Victoria Land DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Event label
Station label
LATITUDE
LONGITUDE
ELEVATION
Sea ice thickness
Correction
Bouguer anomaly
Gravimetry
spellingShingle Event label
Station label
LATITUDE
LONGITUDE
ELEVATION
Sea ice thickness
Correction
Bouguer anomaly
Gravimetry
Redfield, Tim
Behrendt, John
Damaske, Detlef
Delisle, Georg
Möller, Dieter
Sievers, Joachim
Table 1: Station data for the entire survey, including coordinates and description of BPBASE ...
topic_facet Event label
Station label
LATITUDE
LONGITUDE
ELEVATION
Sea ice thickness
Correction
Bouguer anomaly
Gravimetry
description During GANOVEX VI new gravity data were collected along an east-west profile in North Victoria Land south of the Drygalski Ice Tongue, extending 150 km across the Transantarctic Mountains, and comprising 21 data points. Thirty five additional data points were collected over a small area near Brimstone Peak, near the western end of the regional profile. The survey south of the Drygalski has been connected to northern gravity data (GANOVEX V) by a survey line of 12 points. All data have been terrain corrected, and are further constrained by satellite elevation (GPS) and radar ice-thickness measurements. A pronounced regional Bouguer gravity gradient decreasing to the west by approximately 3 mgal/km is superimposed over a coast-parallel belt of granitoid basement rock. West of this belt the local gravity fields become mote variable. Over Beta Peak (Ferrar dolerite) a 50 mgal spike is obser- ved. Within this area, the Ferrar sills are exposed at the surface. West of Brimstone Peak (Ferrar/Kirk patrick ... : Supplement to: Redfield, Tim; Behrendt, John; Damaske, Detlef; Delisle, Georg; Möller, Dieter; Sievers, Joachim (1992): 21. Gravity transect across the Transantarctic Mountains South of the Drygalski lce Tongue. Polarforschung, 60(2), 143-151 ...
format Dataset
author Redfield, Tim
Behrendt, John
Damaske, Detlef
Delisle, Georg
Möller, Dieter
Sievers, Joachim
author_facet Redfield, Tim
Behrendt, John
Damaske, Detlef
Delisle, Georg
Möller, Dieter
Sievers, Joachim
author_sort Redfield, Tim
title Table 1: Station data for the entire survey, including coordinates and description of BPBASE ...
title_short Table 1: Station data for the entire survey, including coordinates and description of BPBASE ...
title_full Table 1: Station data for the entire survey, including coordinates and description of BPBASE ...
title_fullStr Table 1: Station data for the entire survey, including coordinates and description of BPBASE ...
title_full_unstemmed Table 1: Station data for the entire survey, including coordinates and description of BPBASE ...
title_sort table 1: station data for the entire survey, including coordinates and description of bpbase ...
publisher PANGAEA
publishDate 2011
url https://dx.doi.org/10.1594/pangaea.763366
https://doi.pangaea.de/10.1594/PANGAEA.763366
genre Sea ice
Victoria Land
genre_facet Sea ice
Victoria Land
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.763366
_version_ 1810478683069087744