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Erlend

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Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2002
DOI: 10.1144/GSL.SP.2002.197.01.05
EISBN: 9781862394452
... Abstract The Palaeogene Erlend Volcano subcrops in the Faroe-Shetland Basin on the NE Atlantic Margin and was first recognized on the basis of its pronounced positive gravity and magnetic anomalies. Three hydrocarbon exploration wells (209/3-1; 209/4-1A; 209/9-1) have penetrated thick sequences...
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Journal Article
Published: 01 April 1997
Mineralogical Magazine (1997) 61 (2): 175–184.
Journal Article
Published: 01 September 1993
Journal of the Geological Society (1993) 150 (5): 903–914.
...R. KANARIS-SOTIRIOU; A. C. MORTON; P. N. TAYLOR Abstract Well 209/3-1, located close to the centre of the Tertiary Erlend complex, north of the Shetland Isles, contains an unusual volcanic sequence in which thick basalts of N- to T-type MORB affinity overlie highly peraluminous, cordierite-bearing...
Journal Article
Published: 01 May 1984
Journal of the Geological Society (1984) 141 (3): 555–562.
... partially eroded volcanoes. A vent of about 2 km in diameter, surrounded by radially outward-dipping basalts, is centred over the Erlend igneous complex, whose existence had been postulated previously on gravity and magnetic evidence alone. A new volcano, the more deeply eroded West Erlend centre...
Image
Arbitrary seismic line across the <b>Erlend</b> volcano (Faroe-Shetland Basin) sho...
in > Geology
Published: 12 October 2020
Figure 2. Arbitrary seismic line across the Erlend volcano (Faroe-Shetland Basin) showing extrusive lava flows, volcanic conduit, laccolith complex, and associated sills. Dotted line shows possible edifice height before erosion. Note that wells are offset (distance from line is indicated). Line
Image
(A) Top-down view of <b>Erlend</b> volcano (Faroe-Shetland Basin) plumbing system,...
in > Geology
Published: 12 October 2020
Figure 3. (A) Top-down view of Erlend volcano (Faroe-Shetland Basin) plumbing system, showing all sill intrusions mapped from 3-D seismic reflection data, plus edifice edge, laccolith and conduit. Sills are radially distributed around the conduit and laccolith. POV—point of view. (B) Oblique
Image
Comparison of modeled gravity with observed free-air anomaly at <b>Erlend</b> volc...
in > Geology
Published: 12 October 2020
Figure 4. Comparison of modeled gravity with observed free-air anomaly at Erlend volcano (Faroe-Shetland Basin). Lower panels show model parameters overlaid on depth-converted seismic line. (A) Plumbing system is modeled as a series of ring dikes. Modeled gravity anomaly is much lower than
Series: Geological Society, London, Special Reports
Published: 01 January 2016
DOI: 10.1144/SR27.24
EISBN: 9781862397071
... by the Erlend Central Complex (forming the Erlend Platform) (Figs 171 & 176). The summary here incorporates unpublished biostratigraphic and lithostratigraphic data from wells mainly near the West Shetland Platform margin. Stratigraphic data are derived largely from...
Series: Geological Society, London, Special Publications
Published: 01 January 2017
DOI: 10.1144/SP447.18
EISBN: 978-1-78620-37-00
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Series: Geological Society, London, Special Publications
Published: 01 January 2017
DOI: 10.1144/SP447.14
EISBN: 978-1-78620-37-00
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Series: Geological Society, London, Special Publications
Published: 01 January 2017
DOI: 10.1144/SP447.9
EISBN: 978-1-78620-37-00
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Series: Geological Society, London, Special Publications
Published: 01 January 2017
DOI: 10.1144/SP447.1
EISBN: 978-1-78620-37-00
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Series: Geological Society, London, Special Publications
Published: 01 January 2017
DOI: 10.1144/SP447.5
EISBN: 978-1-78620-37-00
FIGURES | View All (16)
Series: Geological Society, London, Special Publications
Published: 01 January 2017
DOI: 10.1144/SP447.6
EISBN: 978-1-78620-37-00
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Journal Article
Journal: Interpretation
Published: 05 October 2017
Interpretation (2017) 5 (4): T607–T622.
...Satinder Chopra; Ritesh Kumar Sharma; Graziella Kirtland Grech; Bent Erlend Kjølhamar Abstract The shallow migrating hydrocarbon fluids in the western Barents Sea are usually found to be associated with high seismic amplitudes. We have attempted to characterize such shallow high-amplitude anomalies...
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Journal Article
Journal: Geophysics
Published: 01 November 2016
Geophysics (2016) 81 (6): D679–D685.
...Erlend Magnus Viggen; Tonni Franke Johansen; Ioan-Alexandru Merciu ABSTRACT Cased petroleum wells must be logged to determine the bonding and hydraulic isolation properties of the cement. Ultrasonic logging of single casings has been widely studied and is commercially available. However, ultrasonic...
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Journal Article
Journal: Geophysics
Published: 27 May 2016
Geophysics (2016) 81 (4): D383–D393.
...Erlend Magnus Viggen; Tonni Franke Johansen; Ioan-Alexandru Merciu ABSTRACT Cased petroleum wells must be logged to determine the bonding and hydraulic isolation properties of the sealing material and to determine the structural integrity status. Although ultrasonic pitch-catch logging in single...
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Journal Article
Published: 04 August 2015
Journal of the Geological Society (2015) 172 (6): 777–791.
...Roy H. Gabrielsen; Johan P. Nystuen; Erlend M. Jarsve; A. Mattias Lundmark Abstract The Sub-Cambrian Peneplain in southern Norway formed in the Cryogenian–early Cambrian. It was transgressed in the Cambrian–early Ordovician, and subsequently broken up by Caledonian thrusting, post-Caledonian normal...
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Journal Article
Published: 20 March 2014
Journal of the Geological Society (2014) 171 (3): 353–374.
...Erlend M. Jarsve; Tom E. Maast; Roy H. Gabrielsen; Jan I. Faleide; Johan P. Nystuen; Caroline Sassier Abstract The Triassic sedimentary succession in the Central North Sea has been investigated to establish a broader understanding of the Triassic Period, from the combined interpretation of seismic...
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Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2008
DOI: 10.1144/SP299.3
EISBN: 9781862395473
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