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  • 2020-2024  (11)
  • 2005-2009
  • 2021  (11)
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Keywords
Years
Year
  • 1
    Publication Date: 2024-01-30
    Keywords: Antarctica; DATE/TIME; ELEVATION; ERA-PLANET; GNSS; GNSS Receiver; GPS; Grounding Line; LATITUDE; LONGITUDE; Modified Julian Day; Priestley Glacier; Shirase_GNSS; The European network for observing our changing planet
    Type: Dataset
    Format: text/tab-separated-values, 330701 data points
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  • 2
    Publication Date: 2024-01-30
    Keywords: Antarctica; DATE/TIME; ELEVATION; ERA-PLANET; GNSS; GNSS Receiver; GPS; Grounding Line; LATITUDE; LONGITUDE; Modified Julian Day; Priestley Glacier; The European network for observing our changing planet; Tuati_GNSS
    Type: Dataset
    Format: text/tab-separated-values, 164963 data points
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  • 3
    Publication Date: 2024-01-30
    Keywords: Antarctica; DATE/TIME; ELEVATION; ERA-PLANET; GNSS; GNSS Receiver; GPS; Grounding Line; Hillary_GNSS; LATITUDE; LONGITUDE; Modified Julian Day; Priestley Glacier; The European network for observing our changing planet
    Type: Dataset
    Format: text/tab-separated-values, 189805 data points
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  • 4
    Publication Date: 2024-01-30
    Keywords: Antarctica; Blake_GNSS; DATE/TIME; ELEVATION; ERA-PLANET; GNSS; GNSS Receiver; GPS; Grounding Line; LATITUDE; LONGITUDE; Modified Julian Day; Priestley Glacier; The European network for observing our changing planet
    Type: Dataset
    Format: text/tab-separated-values, 215631 data points
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  • 5
    Publication Date: 2024-01-30
    Description: This is GNSS data of four stations covering the grounding zone of Priestley Glacier Antarctica. Tidal modulation of ice streams and their adjacent ice shelves is a real-world experiment to understand ice-dynamic processes. We observe the dynamics of Priestley Glacier, Antarctica, using Terrestrial Radar Interferometry (TRI) and GNSS. Ocean tides are predominantly diurnal but horizontal GNSS displacements oscillate also semi-diurnally. The oscillations are strongest in the ice shelf and tidal signatures decay near-linearly in the TRI data over 〉10 km upstream of the grounding line. Tidal flexing is observed 〉6 km upstream of the grounding line including cm-scale uplift. Tidal grounding line migration is small and 〈40 % of the ice thickness. The frequency doubling of horizontal displacements relative to the ocean tides is consistent with variable ice-shelf buttressing demonstrated with a visco-elastic Maxwell model. Taken together, this supports previously hypothesized flexural ice softening in the grounding-zone through tides and offers new observational constraints for the role of ice rheology in ice-shelf buttressing.
    Keywords: Antarctica; ERA-PLANET; GNSS; GPS; Grounding Line; The European network for observing our changing planet
    Type: Dataset
    Format: application/zip, 4 datasets
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  • 6
    Publication Date: 2024-01-30
    Description: Sea floor depth under Ekström Ice Shelf, Antarctica - from seismic reflection profiles collected between 2010 and 2018. For each seismic profile, the reflection time of the sea floor and ice-shelf base was identified and the depth to the sea floor was calculated using an ice velocity of 3601 m/s a sea-water velocity of 1451 m/s. The depths are referenced to mean sea-level (geoid EIGEN-6C4 ). The seismic data used here were collected using two different seismic vibroseis sources. The same snow streamer was used for all data acquisition - a 1500 m long, 60 channel snow streamer, with 25 m group spacing. Each group contains eight gimballed P-wave SM-4, 14 Hz geo-phones. Please note these data are the point data used to create the gridded bathymetry product of the region, found here: doi:10.1594/PANGAEA.907951 Details of data acquisition and processing are given here: doi:10.1029/2019GL086187.
    Keywords: Bathymetry; Bed elevation; Corrected for surface elevation using the REMA model, re-reference to the EIGEN6C4 Geoid; Ekström; Ekstrom_Ice_Shelf; Ekström Ice Shelf; Ice shelf; LATITUDE; LONGITUDE; MULT; Multiple investigations; Number; seismic reflection; Sub-EIS-Obs; vibroseis
    Type: Dataset
    Format: text/tab-separated-values, 117684 data points
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  • 7
    Publication Date: 2024-04-20
    Description: These data were aquired with a Terrestrial Radar Interferometer overlooking the grounding zone of Priestley Glacier, Antarctica. The time series contains line-of-sight velocities averaged over 3 h over an approximately 8 day period in November 2018. Tidal modulation of ice streams and their adjacent ice shelves is a real-world experiment to understand ice-dynamic processes. We observe the dynamics of Priestley Glacier, Antarctica, using Terrestrial Radar Interferometry (TRI) and GNSS. Ocean tides are predominantly diurnal but horizontal GNSS displacements oscillate also semi-diurnally. The oscillations are strongest in the ice shelf and tidal signatures decay near-linearly in the TRI data over 〉10 km upstream of the grounding line. Tidal flexing is observed 〉6 km upstream of the grounding line including cm-scale uplift. Tidal grounding line migration is small and 〈40 % of the ice thickness. The frequency doubling of horizontal displacements relative to the ocean tides is consistent with variable ice-shelf buttressing demonstrated with a visco-elastic Maxwell model. Taken together, this supports previously hypothesized flexural ice softening in the grounding-zone through tides and offers new observational constraints for the role of ice rheology in ice-shelf buttressing.
    Keywords: Antarctica; flowfields; grounding zone dynamics; Ice dynamics; Priestley_Glacier; Terrestrial Radar Interferometry
    Type: Dataset
    Format: application/zip, 1.5 GBytes
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  • 8
    Publication Date: 2024-04-20
    Description: These data were aquired with a Terrestrial Radar Interferometer overlooking the grounding zone of Priestley Glacier, Antarctica. The time series contains differential interferograms with a 12h temporal baseline covering an approximately 8 day period in November 2018. Tidal modulation of ice streams and their adjacent ice shelves is a real-world experiment to understand ice-dynamic processes. We observe the dynamics of Priestley Glacier, Antarctica, using Terrestrial Radar Interferometry (TRI) and GNSS. Ocean tides are predominantly diurnal but horizontal GNSS displacements oscillate also semi-diurnally. The oscillations are strongest in the ice shelf and tidal signatures decay near-linearly in the TRI data over 〉10 km upstream of the grounding line. Tidal flexing is observed 〉6 km upstream of the grounding line including cm-scale uplift. Tidal grounding line migration is small and 〈40 % of the ice thickness. The frequency doubling of horizontal displacements relative to the ocean tides is consistent with variable ice-shelf buttressing demonstrated with a visco-elastic Maxwell model. Taken together, this supports previously hypothesized flexural ice softening in the grounding-zone through tides and offers new observational constraints for the role of ice rheology in ice-shelf buttressing.
    Keywords: Antarctica; Differential Interferometry; ERA-PLANET; flowfields; grounding zone dynamics; Ice dynamics; Priestley_Glacier; Terrestrial Radar Interferometry; The European network for observing our changing planet
    Type: Dataset
    Format: application/zip, 218 MBytes
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  • 9
    Publication Date: 2023-07-11
    Description: Abstract
    Description: The data set comprises new thermochronologic data along the TRANSALP geophysical transect in the Eastern Alps, i.e. (i) apatite and (ii) zircon (U-Th)/He measurements (Tables S1, S2 and S3), and (iii) HeFTy inverse thermal time-temperature-path models ('HeFTy_Models.zip') including a table of parameters used (Table S4). Individual model files can be opened using the HeFTy software (Ketcham et al., 2007).
    Description: Methods
    Description: Sampling method Bedrock samples were taken along the TRANSALP geophysical transect (e.g., Lüschen et al., 2004; 2006) with the main purpose of relating new (and existing) thermochronological data to previously identified mantle geometries and to gain orogen-scale insights into the evolution of the eastern European Alps since initialization of collision in the Eocene/Oligocene. Apatite and zircon (U-Th)/He analyses were the method of choice for two reasons: (i) these systems are considered most suitable to detect periods and locations of increased exhumation that are related to the Neogene evolution of the European Alps including changes in mantle geometries, and (ii) these systems systematically complement existing thermochronology data along the transect, which are predominantly comprised of fission-track data. Detailed analytical procedure is described in the dateset description file ("2020-48_Eizenhöfer-et-al_Data Description.pdf").
    Keywords: European Alps ; Thermochronology ; TRANSALP ; 4DMB ; Mountain Building Processes in 4D ; EARTH SCIENCE 〉 SOLID EARTH 〉 TECTONICS ; tectonics ; thermochronology
    Type: Dataset , Dataset
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  • 10
    Publication Date: 2024-02-07
    Description: Although many different mechanisms for subduction initiation have been proposed, only few of them are viable in terms of consistency with observations and reproducibility in numerical experiments. In particular, it has recently been demonstrated that intra‐oceanic subduction triggered by an upwelling mantle plume could greatly contribute to the onset and operation of plate tectonics in the early and, to a lesser degree, modern Earth. On the contrary, the initiation of intra‐continental subduction still remains underappreciated. Here we provide an overview of 1) observational evidence for upwelling of hot mantle material flanked by downgoing proto‐slabs of sinking continental mantle lithosphere, and 2) previously published and new numerical models of plume‐induced subduction initiation. Numerical modeling shows that under the condition of a sufficiently thick (〉100 km) continental plate, incipient downthrusting at the level of the lowermost lithospheric mantle can be triggered by plume anomalies of moderate temperatures and without significant strain‐ and/or melt‐related weakening of overlying rocks. This finding is in contrast with the requirements for plume‐induced subduction initiation within oceanic or thinner continental lithosphere. As a result, plume‐lithosphere interactions within continental interiors of Paleozoic‐Proterozoic‐(Archean) platforms are the least demanding (and thus potentially very common) mechanism for initiation of subduction‐like foundering in the Phanerozoic Earth. Our findings are supported by a growing body of new geophysical data collected in various intra‐continental areas. A better understanding of the role of intra‐continental mantle downthrusting and foundering in global plate tectonics and, particularly, in the initiation of “classic” ocean‐continent subduction will benefit from more detailed follow‐up investigations.
    Type: Article , PeerReviewed
    Format: text
    Format: other
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