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![Map of the CO2 Lab site in Adventdalen, Svalbard, Norway (aerial photograph from the Norwegian Polar Institute).]()
![Innerhytte pingo, Adventdalen. Note the large surface icing originating from the pingo crest.]()
![Location of open system pingos in Adventdalen. Contours at intervals of 250 m. The location of the PACE borehole at Janssonhaugen is marked.]()
![Electrical resistivity tomogram from Hytte pingo, Adventdalen. Data plotted using the same contouring scale as Figs. 9 and 10.]()
![Electrical resistivity tomogram Line 1 from Longyear pingo, Adventdalen. Data plotted using the same contouring scale as Figs. 8 and 10.]()
![Electrical resistivity tomogram from Innerhytte pingo, Adventdalen. Data plotted using a different contouring scale to that of Hytte and Longyear pingos.]()
![Electrical resistivity tomogram Line 2 from Longyear pingo, Adventdalen. Data plotted using the same contouring scale as Figs. 8 and 9.]()
![(a) The Adventdalen basin study area in central Spitsbergen, (b) Location of seismic line A–A′ (the black dots represent shotpoints), extending 5 km upvalley from the delta front.]()
![Examples of cross‐correlation functions (CCFs) computed from SPITS and SEISVAL data (vertical components) for stations pairs (a) SPB1–SPB4 (north–south direction), (b) SPB3–SPB5 (east–west direction), (c) STN02–STN06 (northwest–southeast direction, north side of Adventdalen), and (d) STN07–STN09 (southeast–northwest direction, south side of Adventdalen). The color version of this figure is available only in the electronic edition.]()
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![(A) Geological map from W. K. Dallmann (2018, personal communication) of the Barents shelf with contours showing Cenozoic uplift. Solid blue line represents extent of the Barents shelf. Dotted black line represents zero net uplift contour. Dotted red lines represent inferred faults. (B) Map of Adventdalen area of Svalbard with drill-site locations and onshore outcrop extent. (C) Cross section AA′ through the Fingerdjupet subbasin and the Greater Hoop area (based on Serck et al., 2017). (D) Cross section BB′ (shown in (B)) through the Adventdalen drill site to outcrops of the reservoir in the north. DH = drill hole; E. = Early; Fm. = Formation; L. = Lower; U. = Upper.]()
![High, mid, and low case geological scenarios for lateral pressure equilibration between the Adventdalen drill site and outcrop beneath the fjord.]()
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![Map showing the relative locations of the KBS three-component station at Ny Ålesund, the SPITS small-aperture array in Adventdalen, and the Barentsburg coal mine.]()
![Stratigraphic cross-section and the regional development of the Lower Cretaceous part of the Adventdalen Group across Spitsbergen, Norway after Grundvåg et al. (2017). E—early; M—middle; L—late.]()
![—Capillary gas chromatograms showing variation of distributions of C15+ saturated hydrocarbons as function of depth and lithology for interval from Adventdalen sequence. All samples analyzed (arrows) bear indicated organic matter type as defined by biologic marker composition.]()
![Comparison of modeled Green’s functions and recorded CCFs for sensor pairs on the south side of Adventdalen; black lines represent modeled Green’s functions, and red lines represent measured cross‐correlation stacks; both data filtered within 0.75–1.5 Hz. The color version of this figure is available only in the electronic edition.]()
![—Triangular diagram of relative abundances of C27 to C29 5α(H), 14β(H), 17β(H)-steranes for all samples analyzed from Adventdalen sequence, with fields for three designated organic matter types (III-D, III-E, III-F) shown.]()
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Journal Article
Internal Structure of Open System Pingos, Adventdalen, Svalbard: The Use of Resistivity Tomography to Assess Ground-ice Conditions Available to Purchase
Published: 01 March 2007
Journal of Environmental and Engineering Geophysics (2007) 12 (1): 113–126.
...Neil Ross; Peter J. Brabham; Charles Harris; Hanne H. Christiansen Abstract The objectives of this project were to establish the geometry and internal structure of open system pingos in Adventdalen, Svalbard using electrical resistivity tomography. A clear distinction can be made between...
FIGURES
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Image
Map of the CO 2 Lab site in Adventdalen, Svalbard, Norway (aeria... Available to Purchase
in Interference suppression by adaptive cancellation in a high Arctic seismic experiment
> Geophysics
Published: 09 May 2017
Figure 1. Map of the CO 2 Lab site in Adventdalen, Svalbard, Norway (aerial photograph from the Norwegian Polar Institute).
Image
Innerhytte pingo, Adventdalen. Note the large surface icing originating fro... Available to Purchase
in Internal Structure of Open System Pingos, Adventdalen, Svalbard: The Use of Resistivity Tomography to Assess Ground-ice Conditions
> Journal of Environmental and Engineering Geophysics
Published: 01 March 2007
Figure 1 Innerhytte pingo, Adventdalen. Note the large surface icing originating from the pingo crest.
Image
Location of open system pingos in Adventdalen. Contours at intervals of 250... Available to Purchase
in Internal Structure of Open System Pingos, Adventdalen, Svalbard: The Use of Resistivity Tomography to Assess Ground-ice Conditions
> Journal of Environmental and Engineering Geophysics
Published: 01 March 2007
Figure 3 Location of open system pingos in Adventdalen. Contours at intervals of 250 m. The location of the PACE borehole at Janssonhaugen is marked.
Image
Electrical resistivity tomogram from Hytte pingo, Adventdalen. Data plotted... Available to Purchase
in Internal Structure of Open System Pingos, Adventdalen, Svalbard: The Use of Resistivity Tomography to Assess Ground-ice Conditions
> Journal of Environmental and Engineering Geophysics
Published: 01 March 2007
Figure 8 Electrical resistivity tomogram from Hytte pingo, Adventdalen. Data plotted using the same contouring scale as Figs. 9 and 10 .
Image
Electrical resistivity tomogram Line 1 from Longyear pingo, Adventdalen. Da... Available to Purchase
in Internal Structure of Open System Pingos, Adventdalen, Svalbard: The Use of Resistivity Tomography to Assess Ground-ice Conditions
> Journal of Environmental and Engineering Geophysics
Published: 01 March 2007
Figure 9 Electrical resistivity tomogram Line 1 from Longyear pingo, Adventdalen. Data plotted using the same contouring scale as Figs. 8 and 10 .
Image
Electrical resistivity tomogram from Innerhytte pingo, Adventdalen. Data pl... Available to Purchase
in Internal Structure of Open System Pingos, Adventdalen, Svalbard: The Use of Resistivity Tomography to Assess Ground-ice Conditions
> Journal of Environmental and Engineering Geophysics
Published: 01 March 2007
Figure 7 Electrical resistivity tomogram from Innerhytte pingo, Adventdalen. Data plotted using a different contouring scale to that of Hytte and Longyear pingos.
Image
Electrical resistivity tomogram Line 2 from Longyear pingo, Adventdalen. Da... Available to Purchase
in Internal Structure of Open System Pingos, Adventdalen, Svalbard: The Use of Resistivity Tomography to Assess Ground-ice Conditions
> Journal of Environmental and Engineering Geophysics
Published: 01 March 2007
Figure 10 Electrical resistivity tomogram Line 2 from Longyear pingo, Adventdalen. Data plotted using the same contouring scale as Figs. 8 and 9 .
Image
(a) The Adventdalen basin study area in central Spitsbergen, (b) Location o... Available to Purchase
Published: 01 January 2003
F IG . 1. (a) The Adventdalen basin study area in central Spitsbergen, (b) Location of seismic line A–A′ (the black dots represent shotpoints), extending 5 km upvalley from the delta front.
Image
Examples of cross‐correlation functions (CCFs) computed from SPITS and SEIS... Available to Purchase
Published: 07 July 2021
Figure 6. Examples of cross‐correlation functions (CCFs) computed from SPITS and SEISVAL data (vertical components) for stations pairs (a) SPB1–SPB4 (north–south direction), (b) SPB3–SPB5 (east–west direction), (c) STN02–STN06 (northwest–southeast direction, north side of Adventdalen), and (d
Journal Article
Seismic Monitoring of Permafrost in Svalbard, Arctic Norway Available to Purchase
Journal: Seismological Research Letters
Publisher: Seismological Society of America
Published: 07 July 2021
Seismological Research Letters (2021) 92 (5): 2891–2904.
...Figure 6. Examples of cross‐correlation functions (CCFs) computed from SPITS and SEISVAL data (vertical components) for stations pairs (a) SPB1–SPB4 (north–south direction), (b) SPB3–SPB5 (east–west direction), (c) STN02–STN06 (northwest–southeast direction, north side of Adventdalen), and (d...
FIGURES
| View All (10)
Includes: Supplemental Content
Journal Article
Elastic properties as indicators of heat flux into cold near-surface Arctic sediments Available to Purchase
Journal: Geophysics
Publisher: Society of Exploration Geophysicists
Published: 08 September 2020
Geophysics (2020) 85 (5): MR309–MR323.
... data. The heat-flux model was validated using temperature data continuously recorded at the surface and within a well in Adventdalen, Svalbard. We estimated the evolving temperatures in an upper vertical section of the well using the heat-flux model, and we compared them with actual measured well...
Image
(A) Geological map from W. K. Dallmann (2018, personal communication) of th... Available to Purchase
in Underpressure in the northern Barents shelf: Causes and implications for hydrocarbon exploration
> AAPG Bulletin
Published: 15 November 2020
) Map of Adventdalen area of Svalbard with drill-site locations and onshore outcrop extent. (C) Cross section AA′ through the Fingerdjupet subbasin and the Greater Hoop area (based on Serck et al., 2017 ). (D) Cross section BB′ (shown in (B)) through the Adventdalen drill site to outcrops
Image
High, mid, and low case geological scenarios for lateral pressure equilibra... Available to Purchase
in Underpressure in the northern Barents shelf: Causes and implications for hydrocarbon exploration
> AAPG Bulletin
Published: 15 November 2020
Figure 5. High, mid, and low case geological scenarios for lateral pressure equilibration between the Adventdalen drill site and outcrop beneath the fjord.
Journal Article
A Novel Approach for Recognition and Quantification of Hydrocarbon Migration Effects in Shale-Sandstone Sequences Available to Purchase
Journal: AAPG Bulletin
Publisher: American Association of Petroleum Geologists
Published: 01 February 1984
AAPG Bulletin (1984) 68 (2): 196–219.
... from two deep core holes drilled on Spitsbergen Island, Svalbard, Norway. In the summer of 1979, Store Norske Spitsbergen Kulkompani drilled, in the course of a coal-exploration program, a core hole at Adventdalen and at Reindalen. The Adventdalen site is located close to Longyearbyen and within...
FIGURES
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Image
Map showing the relative locations of the KBS three-component station at Ny... Available to Purchase
in On the Identification and Documentation of Timing Errors: An Example at the KBS Station, Spitsbergen
> Seismological Research Letters
Published: 01 September 2006
Figure 2. Map showing the relative locations of the KBS three-component station at Ny Ålesund, the SPITS small-aperture array in Adventdalen, and the Barentsburg coal mine.
Image
Stratigraphic cross-section and the regional development of the Lower Creta... Available to Purchase
in The duration and magnitude of Cretaceous cool events: Evidence from the northern high latitudes
> GSA Bulletin
Published: 24 April 2019
Figure 2. Stratigraphic cross-section and the regional development of the Lower Cretaceous part of the Adventdalen Group across Spitsbergen, Norway after Grundvåg et al. (2017) . E—early; M—middle; L—late.
Image
—Capillary gas chromatograms showing variation of distributions of C 15+ s... Available to Purchase
in A Novel Approach for Recognition and Quantification of Hydrocarbon Migration Effects in Shale-Sandstone Sequences
> AAPG Bulletin
Published: 01 February 1984
FIG. 12. —Capillary gas chromatograms showing variation of distributions of C 15+ saturated hydrocarbons as function of depth and lithology for interval from Adventdalen sequence. All samples analyzed (arrows) bear indicated organic matter type as defined by biologic marker composition.
Image
Comparison of modeled Green’s functions and recorded CCFs for sensor pairs ... Available to Purchase
Published: 07 July 2021
Figure 7. Comparison of modeled Green’s functions and recorded CCFs for sensor pairs on the south side of Adventdalen; black lines represent modeled Green’s functions, and red lines represent measured cross‐correlation stacks; both data filtered within 0.75–1.5 Hz. The color version
Image
—Triangular diagram of relative abundances of C 27 to C 29 5α(H), 14β(H),... Available to Purchase
in A Novel Approach for Recognition and Quantification of Hydrocarbon Migration Effects in Shale-Sandstone Sequences
> AAPG Bulletin
Published: 01 February 1984
FIG. 8. —Triangular diagram of relative abundances of C 27 to C 29 5α(H), 14β(H), 17β(H)-steranes for all samples analyzed from Adventdalen sequence, with fields for three designated organic matter types (III-D, III-E, III-F) shown.
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