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Blind Fiord Formation

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Image
Major unconformity beneath <b>Blind</b> <b>Fiord</b> <b>Formation</b> and Lower Permian Great Be...
Published: 01 June 2009
Fig. 3. Major unconformity beneath Blind Fiord Formation and Lower Permian Great Bear Cape Formation (A) and Middle Permian Degerböls Formation (B). ( A ) Griesbach Creek, NW Axel Heiberg Island. ( B ) South of head of Otto Fiord, NW Ellesmere Island. See Figure 1 for location.
Journal Article
Published: 01 June 2009
Bulletin of Canadian Petroleum Geology (2009) 57 (2): 167-191.
...Fig. 3. Major unconformity beneath Blind Fiord Formation and Lower Permian Great Bear Cape Formation (A) and Middle Permian Degerböls Formation (B). ( A ) Griesbach Creek, NW Axel Heiberg Island. ( B ) South of head of Otto Fiord, NW Ellesmere Island. See Figure 1 for location. ...
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Journal Article
Journal: GSA Bulletin
Published: 01 January 2012
GSA Bulletin (2012) 124 (9-10): 1424-1448.
... section at West Blind Fiord on Ellesmere Island (Canadian Arctic) documents stepwise environmental deterioration in the marine Sverdrup Basin during the late Changhsingian (late Late Permian) as a result of volcanic disturbances to surrounding landmasses. A horizon within the upper Lindström Formation...
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Journal Article
Journal: GSA Bulletin
Published: 30 August 2019
GSA Bulletin (2019)
... the Permo-Triassic mass extinction or the suppression of grazing due to harsh, oxygen-poor conditions in its aftermath. Here we report on the abundant occurrence of MISS in the Lower Triassic Blind Fiord Formation of the Sverdrup Basin, Arctic Canada. Sedimentological analysis shows that mid-shelf settings...
Journal Article
Published: 01 May 1972
Canadian Journal of Earth Sciences (1972) 9 (5): 486-499.
...J. B. Waterhouse Abstract The ventral valve of an overtoniid productacean brachiopod generally thought to have been restricted to the late Paleozoic Era is described from the Blind Fiord Formation, Axel Heiberg Island, of Griesbachian (Early Triassic) age. It is not clear whether the specimen...
Image
(A) West <b>Blind</b> <b>Fiord</b> section, Ellesmere Island. The <b>formation</b> contact (FC) ...
Published: 01 January 2012
Figure 2. (A) West Blind Fiord section, Ellesmere Island. The formation contact (FC) marks the transition from spiculitic chert of the underlying Lindström Formation to nonspiculitic silty shale of the overlying Blind Fiord Formation; this horizon represents a regional extinction of sponges
Image
Cross-section 25-19 in the <b>Blind</b> <b>Fiord</b> and Trold <b>Fiord</b> area, SW Ellesmere I...
Published: 01 June 2009
Fig. 5. Cross-section 25-19 in the Blind Fiord and Trold Fiord area, SW Ellesmere Island, showing formations, sequence boundaries (SB; thick solid lines), maximum flooding surfaces (MFS; dashed lines), transgressive (TST) and regressive (RST) systems tracts, conodont taxa and interpreted ages
Image
(A) Correlation of West <b>Blind</b> <b>Fiord</b> to Meishan D and Otto <b>Fiord</b> South based...
Published: 01 January 2012
Figure 4. (A) Correlation of West Blind Fiord to Meishan D and Otto Fiord South based on biostratigraphic and δ 13 C org constraints. Datum B represents the Arctic extinction event (AEE), datum D is the latest Permian mass extinction (LPME), and datum E the Permian-Triassic boundary (PTB
Series: GSA Special Papers
Published: 14 June 2019
DOI: 10.1130/2018.2541(13)
EISBN: 9780813795416
... Carboniferous (Serpukhovian) in age and belongs to the Borup Fiord Formation of the successor Sverdrup Basin. The principal lines of evidence in favor of the original Okse Bay formational assignment were: (1) the presence of late Middle (Givetian) or early Late (Frasnian) Devonian palynomorphs; (2) a set...
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Image
Lindström <b>Formation</b>,  A)  Well preserved spiculite, Borup <b>Fiord</b>. Note dens...
Published: 01 August 2008
Figure 8 Lindström Formation, A) Well preserved spiculite, Borup Fiord. Note dense packing of spicules, all siliceous, and development of thin stylolites, arrows. B) Silicified spiculite, Svartfjeld Peninsula. Most pore space is filled by chalcedony, and spicules have concentric rings
Journal Article
Published: 16 March 2016
Canadian Journal of Earth Sciences (2016) 53 (5): 528-542.
... in Triassic to Jurassic shale and (or) sandstone formations, from youngest to oldest, the Blind Fiord, Blaa Mountain, Heiberg, Savik (Jameson Bay, McConnell Island, Ringnes formations), Awingak, and Deer Bay formations ( Figs. 5 , 6 ). A regionally important package of sills, named herein the Buchanan Lake...
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Journal Article
Published: 03 February 2004
Canadian Journal of Earth Sciences (2004) 41 (1): 39-61.
... Sound Ice Stream en route to nothern Baffin Bay. Westward flow from this divide filled Baumann Fiord, depositing a granite dispersal train that extends a further 600 km across the archipelago to the polar continental shelf. Deglaciation of most of Makinson Inlet occurred catastrophically at ∼9.3 ka BP...
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Journal Article
Published: 01 August 2008
Journal of Sedimentary Research (2008) 78 (8): 562-578.
...Figure 8 Lindström Formation, A) Well preserved spiculite, Borup Fiord. Note dense packing of spicules, all siliceous, and development of thin stylolites, arrows. B) Silicified spiculite, Svartfjeld Peninsula. Most pore space is filled by chalcedony, and spicules have concentric rings...
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Series: SEPM Special Publication
Published: 01 January 2003
DOI: 10.2110/pec.03.78.0133
EISBN: 9781565763340
... and the mouth of McKinley Bay (Fig. 3 ). Lower Triassic strata (Blind Fiord and Bjorne formations) rest unconformably upon Sakmarian and older carbonates (Tanquary or Nansen Formation) along the crest of the Elmerson High (Fig. 4 ). Younger Permian units thicken in a complex onlap and offlap pattern north...
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Image
Type-section of Black Stripe <b>Formation</b>, at Confederation Point, SW Svartfel...
Published: 01 June 2009
Fiord Formation is a maximum flooding surface (dashed line) across which an important stratigraphic gap is recorded as shown by younger Upper Griesbachian and Lower Dienerian conodont assemblages in the basal 9 metres of the Blind Fiord Formation. A sharp break in the isotopic record (locality 8
Journal Article
Published: 01 September 2007
Journal of Paleontology (2007) 81 (5): 858-872.
... Zone in east Greenland ( Spath, 1935 ), the Commune and Strigatus zones in the Blind Fiord Formation in Ellesmere and Axel Heiberg islands, Arctic Canada ( Tozer, 1971 , 1994 ), and the Ophiceras commune Zone in the lower part of the Tulong Formation in southern Tibet ( Wang et al., 1979 ). He...
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Image
Type-section of Lindström <b>Formation</b>, along Lindström Creek, on Hvitland P...
Published: 01 June 2009
and units above and below. ( A ) Overview of geology in vicinity of type-section. Note thin occurrences of Blind Fiord carbonate, shale and siltstone above the Lindström Formation chert. Location of Fig. A (type-section) is shown. ( B ) Type-section of Lindström Formation. ( C ) Hummocky cross
Image
Stratigraphic model depicting Middle Permian to Early Triassic lithostratig...
Published: 01 June 2009
from carbonate- to silica-dominated factory across the Wordian-Capitanian transition, and back into a chert-free setting across the Latest Permian Extinction (LPE) event, which coincides with the base of the Blind Fiord Formation. Note that the Permian-Triassic boundary as defined by the first
Journal Article
Published: 09 January 2017
Geological Magazine (2018) 155 (5): 1023-1039.
...DAVID P. G. BOND; DIERK P. G. BLOMEIER; ANNA M. DUSTIRA; PAUL B. WIGNALL; DANIEL COLLINS; THOMAS GOODE; RALPH D. GROEN; WERNER BUGGISCH; STEPHEN E. GRASBY Abstract – Based on seven measured sections from Svalbard, the marine strata of the Permian Kapp Starostin Formation are arranged into seven...
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Journal Article
Published: 26 October 2009
Canadian Journal of Earth Sciences (2009) 46 (10): 757-790.
..., their demise was equally dramatic, as was that of the ammonoids: Galfetti et al. (2007) have argued for a climatic explanation for this phenomenon. Based both on measured sections in the Sulphur Mountain Formation and supplemental data from the Toad Formation of northeastern British Columbia, the Blind...
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