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More-Trondelag Fault

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Journal Article
Published: 01 March 2006
Journal of the Geological Society (2006) 163 (2): 303–318.
... partitioning through a period of at least 30 Ma. Early to Mid-Devonian exhumation of the Central Norway basement window was associated with retrograde, top-to-the-SW extensional shearing in the Høybakken detachment zone, sinistral shearing along the MøreTrøndelag Fault Complex, and formation of extension...
FIGURES | View All (10)
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<b>Møre</b>-<b>Trøndelag</b> <b>Fault</b> Complex brittle normal <b>fault</b> outcrop showing well-deve...
Published: 01 January 2013
Figure 7. Møre-Trøndelag Fault Complex brittle normal fault outcrop showing well-developed slickenlines in laumontite. Prominently developed “steps” indicating normal (hanging wall down) kinematics can be seen throughout the image. Stereonet shows lineation data from throughout the Møre-Trøndelag
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Post-Caledonian <b>faults</b> parallel to the <b>Møre</b>–<b>Trøndelag</b> <b>Fault</b> Complex. Letter...
Published: 01 December 2005
Fig. 10.  Post-Caledonian faults parallel to the MøreTrøndelag Fault Complex. Letters are keyed to Figure 8 . B and C exhibit fault splays of the MøreTrøndelag Fault Complex exposed along the base of the topographic Great Escarpment of the Møre area. The faults show evidence for sustained
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Displacement gradient in the <b>Møre</b>-<b>Trøndelag</b> <b>Fault</b> Complex (MTFC). (A) Map s...
Published: 01 January 2013
Figure 10. Displacement gradient in the Møre-Trøndelag Fault Complex (MTFC). (A) Map showing location. Note south to the top. Møre-Trøndelag Fault Complex traces are shown in white; footwall and hanging wall are shown schematically in dark and light gray. Apatite fission-track (AFT) sample
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Location map showing the <b>Møre</b>–<b>Trøndelag</b> <b>Fault</b> Complex area modified after  ...
Published: 01 December 2005
Fig. 8.  Location map showing the MøreTrøndelag Fault Complex area modified after Redfield et al . (2005) . Letters link structural data and field photographs ( Fig. 10 ) to this location map. Faults shown are those considered to have a post-Caledonian history of offset. Zones of AFT
Journal Article
Published: 01 May 2005
Geochemistry: Exploration, Environment, Analysis (2005) 5 (2): 183–188.
...O.M. Sæther; D. Roberts; C. Reimann Abstract A distinct linear Sr anomaly traceable over a distance of >120 km in central Norway can be linked directly to the ENE–WSW-trending Møre-Trøndelag Fault Complex. Another less prominent linear anomaly is associated with a major extensional detachment...
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Journal Article
Published: 01 December 2005
Journal of the Geological Society (2005) 162 (6): 1013–1030.
...Fig. 10.  Post-Caledonian faults parallel to the MøreTrøndelag Fault Complex. Letters are keyed to Figure 8 . B and C exhibit fault splays of the MøreTrøndelag Fault Complex exposed along the base of the topographic Great Escarpment of the Møre area. The faults show evidence for sustained...
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Series: Geological Society, London, Petroleum Geology Conference Series
Published: 01 January 2005
DOI: 10.1144/0061165
EISBN: 9781862394124
... Present-day fjords onshore mid-Norway show a systematic semi-rectangular pattern. This pattern corresponds with the long-lived structures of the MøreTrøndelag fault zone ( Fig. 1 ). The NE-SW-orientated fjord segments are orientated slightly obliquely with respect to the present...
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Journal Article
Published: 01 January 2003
Journal of the Geological Society (2003) 160 (1): 137–150.
... the eastern margin of a regional, transtensional system bounded in the south by the sinistral MøreTrøndelag Fault Complex. 19 7 2002 28 12 2001 © 2003 The Geological Society of London 2003 Devonian Scandinavian Caledonides North–Central Norway extension shear zones Late...
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Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2014
DOI: 10.1144/SP390.21
EISBN: 9781862396661
..., and in the NW by the Møre Trøndelag Fault Complex ( Fichler et al. 2011 ). As with the Utsira High basement, in the absence of better constraints, we have chosen to delineate this basement unit based on the Mesozoic fault pattern, acknowledging that post-Caledonian extension in the North Sea probably...
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Journal Article
Published: 01 February 1997
Journal of the Geological Society (1997) 154 (1): 85–92.
... a function of Mesozoic-Cenozoic plate-wide extensional stress fields. Certain Proterozoic and Caledonian lineaments were, however, opportunistically reactivated according to the extension direction. Caledonian NE-SW orogen-oblique shears, typified by the Møre-Trøndelag Fault Zone, were reactivated via...
Journal Article
Journal: Geology
Published: 01 July 2000
Geology (2000) 28 (7): 615–618.
...) north of the Møre-Trøndelag Fault Complex show that bidirectional, opposed, orogen-parallel extension dominated in this region. At this time, the fault complex acted as a transfer zone for the Høybakken detachment. Extension and uplift in central Norway triggered significant magmatic activity...
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Structures in the vicinity of the Hitra–Snåsa <b>Fault</b> of the <b>Møre</b>–<b>Trøndelag</b> ...
Published: 01 March 2006
Fig. 7.  Structures in the vicinity of the Hitra–Snåsa Fault of the MøreTrøndelag Fault Complex. ( a ) Top-to-the-NW reverse fault rooted in, or cut by, the NE–SW-trending Jektvika fault. Shortening in the ‘Old Red’ clearly intensifies in the direction of strands of the MøreTrøndelag Fault
Series: Geological Society, London, Special Publications
Published: 01 January 2000
DOI: 10.1144/GSL.SP.2000.167.01.13
EISBN: 9781862394155
... boundary of the Møre Basin is located where the NE-SW trending Møre-Trøndelag Fault Complex truncates the N-S and NNE-SSW trends of the northern North Sea. To the southwest, the Møre Basin borders upon the Faeroe-Shetland Basin along the NW-SE trending Erlend Platform ( Pharaoh et al . 1996 ). Apart...
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Journal Article
Published: 01 September 2007
Journal of the Geological Society (2007) 164 (5): 1037–1058.
... al . 1977 ). CG, Central Graben; FSB, Faeroe–Shetland Basin; GGF, Great Glen Fault; HBF, Highland Boundary Fault; HT, Halten terrace; JML, Jan Mayen Lineament; MB, Møre Basin; MT, Moine Thrust; MTFC, MøreTrøndelag Fault Complex; VG, Viking Graben; WBFZ, Walls Boundary Fault Zone; WSB, West Shetland...
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Journal Article
Journal: AAPG Bulletin
Published: 01 February 1998
AAPG Bulletin (1998) 82 (2): 274–290.
..., 1992), and Heidrun fields (Whitley, 1992). These discoveries are located mostly on the Trøndelag Platform, particularly on the Halten Terrace and in the area immediately west of the Nordland Ridge ( Figure 1 ). To the west, in considerably deeper water, lie the Møre and Vøring basins...
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Journal Article
Published: 13 July 2016
Geological Magazine (2016) 153 (5-6): 1136–1165.
..., Jämtland–Trøndelag, Telemark–Møre og Romsdal) show similar restored lengths for the models in two transects and longer restorations for models II/III in the other transects. Model I can result in c. 280 km wide gaps in the restored Lower Allochthon, evidence for which is not seen in the sedimentology...
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Journal Article
Published: 01 April 1992
Journal of the Geological Society (1992) 149 (2): 273–284.
...- enriched breccias in the More-Trondelag Fault Zone, central Norway. Norsk Geologisk Tidsskrift, 69, 1-19. HALLS, H. C. 1976. A least-squares method to find a remanence direction from A.stronomical Society, 45, 297-304. converging magnetization circles. Geophysical Journal of the Royal - 1978. The use...
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Deformation–depth–time diagram summarizing the kinematic and <b>fault</b> rock evo...
Published: 01 September 2007
Fig. 13.  Deformation–depth–time diagram summarizing the kinematic and fault rock evolution of the Walls Boundary Fault Zone in Shetland, the Great Glen Fault Zone in Scotland and the MøreTrøndelag Fault Complex in western Norway (for locations see Fig. 1 ). VF, Verran Fault; HSF, Hitra–Snåsa
Journal Article
Published: 01 May 2004
Journal of the Geological Society (2004) 161 (3): 335–338.
... to a complex cogenetic model we invoke fault reactivation as a viable alternative, and suggest that assumed contemporaneity in such assemblages may be invalid in many cases. 8 1 2004 20 10 2003 © 2004 The Geological Society of London 2004 MøreTrøndelag Fault Complex Ar/Ar...
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