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Hyde Fjord

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Journal Article
Published: 01 August 2001
The Canadian Mineralogist (2001) 39 (4): 997–1020.
...Daniel J. Kontak; Sven M. Jensen; Jarda Dostal; Douglas A. Archibald; T. Kurtis Kyser Abstract A group of dyke rocks from the Frederick E. Hyde Fjord area form the southern termination of a prominent dyke-swarm in Peary Land, northernmost Greenland. The melanocratic dykes are NS- to NW–SE-trending...
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Journal Article
Published: 01 July 2001
Geological Magazine (2001) 138 (4): 407–434.
... siliciclastics, calcareous mudstones and dolomites of the Lower Cambrian Skagen and Paradisfjeld groups ( Friderichsen et al. 1982 ) (Fig. 2b ) along a narrow strip north of Midtkap and at the mouth of Frederick E. Hyde Fjord north of the Harder Fjord Fault Zone (Fig. 2a ). They are overlain by 2000–3000 m...
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Journal Article
Journal: GSA Bulletin
Published: 01 March 2004
GSA Bulletin (2004) 116 (3-4): 348–367.
...Ben Kneller; Juan Pablo Milana; Clare Buckee; Omar al Ja'aidi Abstract The combination of high sediment supply rates and ample accommodation within fjords provides high-resolution records of deglaciation. Ancient fjord fills provide the potential for three-dimensional views of the evolution...
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Journal Article
Published: 01 June 2000
The Canadian Mineralogist (2000) 38 (3): 641–648.
...Natale Perchiazzi; Andrew M. McDonald; Robert A. Gault; Ole Johnsen; Stefano Merlino Abstract The crystal structure of normandite from Amdrup Fjord, Greenland and from Mont Saint-Hilaire, Quebec, was solved and refined to a residual R 1 of 0.033 and 0.047, respectively. Normandite is a member...
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Journal Article
Journal: AAPG Bulletin
Published: 01 January 1984
AAPG Bulletin (1984) 68 (1): 1–17.
... to the Navarana Fjord fault and Permin Land flexure. The escarpment margin is not a fault scarp but represents a sedimentary escarpment, constructed by vertical carbonate-shelf accretion, and controlled by faults that delineate the boundary between the carbonate shelf and the deep-water basin. The stepped margin...
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Journal Article
Journal: AAPG Bulletin
Published: 01 April 1980
AAPG Bulletin (1980) 64 (4): 527–548.
... of Peary Land, north of Frederick E. Hyde Fjord ( Fig. 1 ), due west to northern Hall Land, sediments commonly are intensely folded so that Proterozoic, Cambrian, and Ordovician sediment reappear through the predominantly Silurian cover. South of this line, both clastic and carbonate sediments are flat...
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Image
—(a) Disorganized boulder conglomerate deposited at base-of-slope immediate...
Published: 01 January 1984
. Hyde Fjord, Peary Land ( Fig. 4 ). (b) Thin-bedded muddy turbidites resulting from overflow of topographic highs formed by thick base-of-slope conglomerates as shown in Figure 10 . Citronens Fjord, Peary Land ( Fig. 4 ). (c) Thin to thick-bedded sandstone turbidites of basin. East coast of Lauge Koch
Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2015
DOI: 10.1144/SP413.10
EISBN: 9781862397170
... position of the Laurentia–Eurasia plate boundary and associated major faults. The positions of 17 variously substantiated pull-apart basins are indicated by stars (orange, Late Permian Hyde Fjord Event; purple, Early Triassic Dunken Event; blue, Oxfordian Ingeborg Event; green, Late Cretaceous Kilen Event...
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Journal Article
Published: 01 September 1976
Bulletin of Canadian Petroleum Geology (1976) 24 (3): 440–449.
... The carbonate-shale unit can be traced on aerial photographs from the head of Frederick E. Hyde Fjord across southern Peary Land to a point east of Kap Caroline Marie, a distance of approximately 100 mi (160 km) (Fig. 1). Along this line, shale and limestone are exposed; the two lithologies are lateral...
Journal Article
Published: 05 August 2011
Canadian Journal of Earth Sciences (2011) 48 (8): 1259–1281.
... Neoproterozoic, an extensive shallow-water carbonate platform decked most of North Greenland. The northern boundary of the shelf can be traced south of Frederick E. Hyde Fjord and eastwards through Sirius Passet, and it is inferred to continue westwards just north of the present coastline ( Fig. 1...
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Journal Article
Published: 01 May 2000
Canadian Journal of Earth Sciences (2000) 37 (5): 629–633.
... cycle of the late Pleistocene ( Tarasov and Peltier 1997 , 1999 ) as an aid to understanding the glaciation events that occurred during both the Carboniferous ( Hyde et al. 1999 ) and Neoproterozoic periods ( Hyde et al. 2000 ). The latter epoch is perhaps especially important as it has been taken...
Journal Article
Published: 15 August 2016
Journal of Micropalaeontology (2017) 36 (1): 127–135.
... Canewdon North Wick Cudmore Grove Swanscombe Ebbsfleet East Hyde Clacton Marks Tey Candona angulata G.W. Müller F F F F Candona candida (O.F. Müller) F F F F Candona neglecta Sars F F F F F F F F F F F...
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Journal Article
Published: 01 December 2005
South African Journal of Geology (2005) 108 (4): 557–577.
... just before the Marinoan glaciation. Negative excursions of 10 to 15‰ frame the Sturtian and Marinoan glacials in different areas, proving the glaciations were globally synchronous. The most lenient solution is the ‘tropical oasis’ model ( Hyde et al., 2000 ; Peltier et al., 2004...
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Journal Article
Journal: Geology
Published: 01 March 2003
Geology (2003) 31 (3): 231–234.
.... , Halverson , G.P. , and Schrag , D.P. , 1998 , A Neoproterozoic snowball Earth : Science , v. 281 p. 1342 - 1346 . Horikoshi , K. , 1998 , Barophiles: Deep-sea microorganisms adapted to an extreme environment : Current Opinion in Microbiology , v. 1 p. 291 - 295 . Hyde...
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Series: Geological Society, London, Memoirs, Geological Society, London, Memoirs
Published: 01 January 2011
DOI: 10.1144/M36.2
EISBN: 9781862394117
... slushball solution ( Hyde et al. 2000 ; Peltier et al. 2004 ; but see Bendtsen 2002 ; Voigt et al . 2011 )? Because of subduction, direct evidence from the ocean floor has been eliminated, or survives only from post-Cryogenian (Ediacaran), regional-scale glaciation ( Kawai et al. 2008 ). Those who...
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Journal Article
Journal: GSA Bulletin
Published: 01 July 2011
GSA Bulletin (2011) 123 (7-8): 1478–1496.
... and Unwin, l98 p . Corner G.D. , 2006 , A transgressive-regressive model of fjord-valley fill: Stratigraphy, facies and depositional controls , p. 161 – 178 , in Dalrymple R.W. Leckie D.A. Tillman R.W. , eds ., Incised Valleys in Time and Space : Society for Sedimentary...
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Journal Article
Journal: AAPG Bulletin
Published: 01 June 2018
AAPG Bulletin (2018) 102 (6): 959–986.
... work by Turner and Slatt (2016) on the Wyche 1 core. Turner and Slatt (2016) used trace metals (primarily Mo and TOC, Mo/TOC) as a proxy for bottom-water conditions, finding the LW to be the most restricted (likening the depositional environment to the Framvaren Fjord in Norway), with less...
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Journal Article
Journal: GSA Bulletin
Published: 01 September 2010
GSA Bulletin (2010) 122 (9-10): 1480–1498.
... ). A second glacial event spanned the Serpukhovian to early Bashkirian and was characterized by alpine glaciation and postglacial fjord-filling sedimentation. A likely third glacial event occurred in the mid-to-late Bashkirian through early Moscovian (315–312 Ma). Notably, the two Pennsylvanian glacial events...
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Journal Article
Published: 24 August 2018
Journal of the Geological Society (2018) 175 (6): 903–914.
...) Lacustrine and marine sediments have the potential to serve as sensitive recorders of environmental changes and events driven by climatic, tectonic or anthropogenic processes. In particular, the deposits of lakes, or restricted basins such as fjords, commonly preserve high-resolution records because...
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Series: Geological Society, London, Memoirs, Geological Society, London, Memoirs
Published: 01 January 2011
DOI: 10.1144/M36.5
EISBN: 9781862394117
.... They are interpreted to be ice-rafted and the Jacadigo Group to have been deposited in a partly ice-covered fjord-like basin ( Urban et al. 1992 ). The alternation of Mn and Fe ores is attributed to cycles of glacial advance and retreat. Enhanced fluxes of oxygenated subglacial meltwater during glacial retreats...
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