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Asterias fault complex

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Image
Overview of the study area showing the main structural elements. The extent...
Published: 22 November 2016
) ( a ) Detailed structural map of the Polhem Subplatform. ( b ) Detailed structural map of the Asterias Fault Complex and associated structures. ( c ) Detailed structural map of the Goliat hydrocarbon field area. Structural element map modified from Norwegian Petroleum Directorate (npd.no). FC, fault complex.
Image
( a ) Situation map. ( b ) Overview map of the study area, with the positio...
Published: 10 August 2017
Complex; HFC, Hoop Fault Complex; SvD, Svalis Dome; MB, Maud Basin; SG, Swaen Graben; AFC, Asterias Fault Complex; HB, Hammerfest Basin; T-FFC, Troms-Finnmark Fault Complex; ND, Norvarg Dome; SD, Samson Dome; NH, Norsel High; NFC, Nysleppen Fault Complex; and MFC, Måsøy Fault Complex. ( c ) Stratigraphic
Image
( a ) Tectonic model showing how uplift of the Loppa High in the early Barr...
Published: 22 November 2016
horizontal shortening to uplift ratio as a function of fault dip. White dot represents values for the Asterias Fault Complex. ( c ) Schematic illustration of horizontal stress generated by uplift (black arrows) and resulting horizontal clockwise rotation (grey arrow) owing to unbalanced horizontal stresses
Journal Article
Published: 22 November 2016
Journal of the Geological Society (2017) 174 (2): 242–254.
...) ( a ) Detailed structural map of the Polhem Subplatform. ( b ) Detailed structural map of the Asterias Fault Complex and associated structures. ( c ) Detailed structural map of the Goliat hydrocarbon field area. Structural element map modified from Norwegian Petroleum Directorate (npd.no). FC, fault complex. ...
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Image
Uninterpreted and interpreted seismic line running across the Hammerfest Ba...
Published: 22 November 2016
Fig. 6. Uninterpreted and interpreted seismic line running across the Hammerfest Basin, from Loppa High in the north to the Finnmark Platform in the south, crossing the Asterias and Troms–Finnmark fault complexes. Small arrows indicate onlap. (See Fig. 1 for location and Fig. 2
Journal Article
Published: 01 April 2007
Scottish Journal of Geology (2007) 43 (1): 69–74.
... of the key localities is explained in Rushton et al. (2000) and Aldridge et al. (2000) . The Girvan district is situated immediately to the north of the Southern Uplands Fault, at the southern edge of the Midland Valley Terrane ( Bluck et al. 1992 ), itself extending southwards beneath...
FIGURES
Journal Article
Published: 01 May 2008
Petroleum Geoscience (2008) 14 (2): 139–150.
... the Norkapp Basin follows the same trend. The basin is bounded by the Troms–Finnmark Fault Complex to the south, the Asterias Fault Complex to the north, and the Ringvassøy–Loppa Fault Complex and the Tromsø Basin to the west. Its eastern limit has the characteristics of a flexure against the Finnmark...
FIGURES | View All (12)
Journal Article
Published: 04 April 2022
Petroleum Geoscience (2022) 28 (2): petgeo2021-037.
... towards the Hammerfest Basin by the Asterias Fault Complex ( Fig. 1 ). Here we summarize the relevant geologic context needed for interpreting the geochemical data presented in the remainder of this paper. Following the Caledonian orogeny, the Loppa High area has served as an epi-orogenic depocentre...
FIGURES | View All (8)
Journal Article
Published: 14 December 2017
Journal of the Geological Society (2018) 175 (3): 497–508.
... include the Hammerfest Basin in the south and the Tromsø and Bjørnøya basins to the west. These basins are briefly characterized in the following. The Hammerfest Basin is separated from the Loppa High by the east–west-striking extensional top-to-the-south Asterias Fault Complex ( Fig. 1 ). This basin...
FIGURES | View All (8)
Journal Article
Journal: Geology
Published: 01 September 2012
Geology (2012) 40 (9): 839–842.
... as much as 3 m in diameter, having a vertical extent of ∼1 m, where abundant concretionary masses not larger than 30 cm in diameter are embedded in mudstones and claystones. Thin sections of the carbonates show a burrow-mottled fabric, which exhibits a complex history of repeated burrow excavations...
FIGURES
Journal Article
Journal: AAPG Bulletin
Published: 01 April 1926
AAPG Bulletin (1926) 10 (4): 382–404.
.... In the central cordillera there are many metaliferous veins, and some mines of considerable renown. In the eastern cordillera the basement rocks appear only in small scattered areas about the higher ranges. They doubtless represent the northern extension of the Brazilian complex described by Branner, 1...
FIGURES | View All (8)
Journal Article
Published: 10 August 2017
Journal of the Geological Society (2018) 175 (1): 130–145.
... Complex; HFC, Hoop Fault Complex; SvD, Svalis Dome; MB, Maud Basin; SG, Swaen Graben; AFC, Asterias Fault Complex; HB, Hammerfest Basin; T-FFC, Troms-Finnmark Fault Complex; ND, Norvarg Dome; SD, Samson Dome; NH, Norsel High; NFC, Nysleppen Fault Complex; and MFC, Måsøy Fault Complex. ( c ) Stratigraphic...
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Journal Article
Published: 01 May 2009
Journal of Paleontology (2009) 83 (3): 389–398.
.... The La Voulte Lagerstätte is located in southeastern France (Ardèche), east of the Massif Central (=Hercynian crystalline basement), along the right bank of the Rhone valley (ca. 150 km south of Lyon). The fossiliferous deposits are separated from the basement by a major Hercynian subvertical fault...
FIGURES | View All (7)
Journal Article
Published: 05 February 2018
Journal of Paleontology (2018) 92 (2): 196–206.
... ) are broadly typical of traditional morphology-based taxonomic arrangements whereas a recent molecular study (Mah and Foltz, 2011b ) introduced significant changes placed in a historical biogeographic framework. Because of the limited data available for the single fossil, and because of taxonomic complexities...
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Journal Article
Published: 01 May 2001
Journal of Paleontology (2001) 75 (3): 721–731.
... macrofauna, including echinoids ( Kier, 1966 ). Although originally divided into a sequence of lithostratigraphic units (see, for example, Poole and Barker, 1983 ), the rocks of the Scotland district are now recognized to be composed of an array of fault-bounded, tectonostratigraphic packets ( Speed, 1988...
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Journal Article
Published: 24 April 2015
Geological Magazine (2015) 152 (6): 1043–1056.
... are complex organisms, and adequate understanding requires both dorsal and ventral surfaces as well as the lateral expression of the arms. Interior morphology, especially that of the jaw frame and ambulacral series but also of body wall ossicles, is important, but almost...
FIGURES
Journal Article
Published: 01 March 2006
Journal of Paleontology (2006) 80 (2): 229–244.
... , see also Sutherland and Grayson, 1992 ) recorded a thickness of about 280 m for unnamed unit 1 at this locality, but apparently included faulted and folded sequences. The conglomerate layer containing the edrioasteroids is nearly vertical in the bank of a small stream, and the north end of this small...
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Series: Geological Society, London, Special Publications
Published: 03 September 2022
DOI: 10.1144/SP495-2018-165
EISBN: 9781786205230
... configuration. Abbreviations in (b) are as follows: FSB, Fingerdjupet Sub-basin; SvD, Svalis Dome; HFC, Hoop Fault Complex; MB, Maud Basin; BFC, Bjørnøyrenna Fault Complex; SG, Swaen Graben; AFC, Asterias Fault Complex; HB, Hammerfest Basin; T-FFC, Troms–Finnmark Fault Complex; MFC, Måsøy Fault Complex; NFC...
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Journal Article
Published: 01 September 2003
Journal of Paleontology (2003) 77 (5): 922–948.
... at approximately 40° N. latitude at this time ( Fig. 1 ). More recent paleoclimatic reconstructions (Scotese, personal commun., http://www.scotese.com/ldevclim.htm ) place this complex at the northern limit of the Late Devonian tropical climatic belt, which is consistent with the fossil communities described...
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Journal Article
Published: 28 January 2022
Journal of Sedimentary Research (2022) 92 (1): 50–65.
... and terrigenous rocks that formed at the southern margin of the Alpujarra Corridor at its transition to the Neogene Almería–Níjar Basin ( Fig. 1 ), where they overlie an erosion surface carved in rocks of the Alpujárride Complex—one of the major tectonic complexes of the Betic Cordillera ( Baena and Voermans 1983...
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