Some new investigations of the Devonian stratigraphy and tectonics of east Greenland by Heinrich BuМ€tler Download PDF EPUB FB2
Some new investigations of the Devonian stratigraphy and tectonics of east Greenland. [Heinrich Bütler] Home. WorldCat Home About WorldCat Help. Search. Search for Library Items Search for Lists Search for Book\/a>, schema:CreativeWork\/a> ; \u00A0\u00A0\u00A0 library. Plate Tectonics and the Alamo Impact.
North America Placement. The Earth’s landmasses are more dynamic than one may think. The outer layer of the Earth’s crust is actually broken into a series of tectonic plates that move independently from one another.
The movements of these plates are responsible for building the Earth’s tallest mountains and deepest trenches. In his memoir " Some New Investigations of the Devonian Stratigraphy and Tectonics of East Greenland," H.
Biitler (Medd. om Grönland,No. 2,35 pp.) shows that the Old Red Sandstone of East Greenland is an orogenic sediment.
East-west movements within the Caledonian belt of folding repeatedly elevated, folded and disrupted the. In East Greenland, however, strongly tilted and folded Early-Middle Devonian strata are cut by an unconformity that separate them from much less deformed Late Devonian deposits (Hartz, ), in.
Some new investigations of the. Devonian stratigraphy and the teconics of East. East Greenland tetrapods are Devonian in age, Geology, 27, Outcrops of the Eleonore Bay Basin are cut by the “western fault zone,” a major normal fault zone that bounds the Devonian basin of North-East Greenland (Fig.
13; Larsen and Bengaard, ). Based on evidence from the Devonian succession, sinistral strike-slip movements in the order of 10–20 km along the western fault zone were estimated.
DEVONIAN ROCKS were discovered in east Greenland in by A. Nathorst, and termed the Cape Graah formation. The fish remains found were determined by S. Woodward () as Upper Devonian. Lauge Koch () ascertained that the Devonian conglomerates and sandstones rest with angular unconformity on Caledonian-folded formations, and.
OCLC Number: Notes: Symposium held Feb. Description: xviii, pages: illustrations ; 26 cm. Contents: Challenge of resource development and environmental protection in the Arctic / Hollis M. Dole --Tectonics of northern Franklin Mountains and Colville Hills, District of Mackenzie, Canada / Donald G.
Cook and James D. Aitken --Tectonic styles of northern Yukon Territory. geological investigations in East Greenland: project ‘Resources of the sedimentary basins of North and East Greenland’. Geology of Greenland Survey Bulletin29– Surlyk, F. Stratigraphy, tectonics and palaeogeography of the Jurassic sediments of the areas north of Kong Oscars Fjord, East Greenland.
Bulletin Grønlands. Surlyk, F. Stratigraphy, tectonics and palaeogeography of the Jurassic sediments of the areas north of Kong Oscars Fjord, East Greenland. Bulletin Grønlands Geologiske Undersøgelse56 pp. Surlyk, F. Jurassic basin evolution of East Greenland. Nature (), The investigation of Devonian to Eocene successions in East Greenland has a long history dating back to the nineteenth century (Higgins and references therein).
Data are mainly derived from. Get this from a library. Geology of the Arctic: proceedings. Held, Januaryunder the auspices of the Alberta Society of Petroleum Geologists.
[Gilbert O Raasch;] -- Papers presented at the First International Symposium on Arctic Geology held in Calgary Alberta in Volume I includes papers on geology in the Soviet Arctic, Spitsbergen (Norway), Greenland.
—, —: Some new Investigations of the Devonian Stratigraphy and Tectonics of East Greenland. - Med. om Groenland, 2, On the Geology and Physical Geography of East Greenland. - Medd. om Groenland28, S. –, Google Scholar; Download references. Structural and climatic controls on fluvial depositional systems: Devonian, North-East Greenland.
Special Publication of the International Association of Sedimentologists, 17, January The East Greenland Caledonides, which make up an ∼km-long stretch of North-East Greenland, were formed by the collision of Laurentia and Baltica in mid-Silurian time.
The East Greenland Basins are bounded to the east and west by north-south striking faults, which are cut by northwest-southeast faults. This fault pattern creates a series of diamond-shaped fault blocks which subsided progressively from south to north. This subsidence pattern may be explained by a gradual re lease of east-west strain.
The temporal resolution of the new stratigraphic framework for North-East and North Greenland permits a detailed comparison of the subsidence histories along the Laurentian margin from western Newfoundland to the NE tip of Greenland, a distance of over km.
Attempts to determine the subsidence history of the Laurentian margins were. Rift Basin between Norway and Greenland and the North Greenland - Svalbard Basin between these two terranes, Both are included in the Middle Carboniferous to Tertiary Wandel Sea Basin (HAKANSSON & STEMMERIKHAKANSSON & PEDERSENHAKANSSON et al.
a, b). The depositional history of the East Greenland Rift Basin comprises Early. During some intervals, this fine terrigenous sediment appreciably infilled portions of the basin proximal to coeval carbonate banks on the east side of the basin.
Westerly, leeside shedding of lime mud from these carbonate banks by storm-induced currents resulted in even further infilling of the basin.
Feilden, H. & de Rance, C. E.: Geology of the coasts, of the arctic Lands visited by the late British expedition under Captain Sir George Journ. Geol. The mountains and fjords of Greenland preserve a record of nearly four billion years of Earth history - a story of mountain building, volcanic eruptions, primitive life and ice ages.
During the vast period of time, through processes of continental drift, Greenland has journeyed from the southern hemisphere through the tropics to its present polar position. Email your librarian or administrator to recommend adding this book to your organisation's collection.
The Continental Drift Controversy. Some new investigations of the Devonian stratigraphy and tectonics of East Greenland. Meddel. Grønland,Nr. 2: 1 – Some New Investigations of the Devonian Stratigraphy and Tectonics of East Greenland: Meddelelser om Grønland Bindnr.
35 sider: 65, Donovan, Desmond T: Stratigraphy and Ammonite Fauna of the Volgian and Berriasian Rocks of East Greenland: The Pennsylvanian to Triassic was generally a time of thermal subsidence and formation of a broad sag basin (e.g., Rønnevik et al.,Gudlaugsson et al., ), although some Permian to Triassic extension is known from onshore East Greenland (Surlyk, ) and has been proposed for the Loppa High (Glørstad-Clark et al.,Clark et al.
The regions covered include continental margin Norway, east and west Greenland, The Faroe-Shetland Basin and the Faroe Islands themselves. The papers in this book contain new data and interpretations of North Atlantic Igneous Province magmatic processes, rift evolution, tectonics, stratigraphy (chemostratigraphy, biostratigraphy, seismic and.
Laurent Gindre, Daniel Le Heron, Hans Morten Bjørnseth, High resolution facies analysis and sequence stratigraphy of the Siluro-Devonian succession of Al Kufrah basin (SE Libya), Journal of African Earth Sciences, /rsci, 76, (), ().
succession of Silurian and Lower Devonian rocks and to define their tectonics. The Silurian-Devonian boundary beds are also exposed here. New paleontological data, presented in this paper, fully justify the attention paid to that section. InO.L.
Krug von Nidda reported the occurrence of lydites and black. ISBN: OCLC Number: Description: ix, pages: illustrations (some color), maps (some color) ; 26 cm. Contents: A review of Devonian time scales: databases, construction and new data / E.
Williams, P. Friend and B. Williams --Chronostratigraphic framework for the Devonian and Old Red Sandstone / M. House --Kinematics and dynamics of Old. --Early syndepositional tectonics of East Greenland's Old Red Sandstone basin / E.
Hartz --Fossils from the Celsius Bjerg Group, Late Devonian sequence, East Greenland; significance and sedimentological distribution / J.A. Clack and S.L.
Neininger --Deformation of the Old Red Sandstone of NW Spitsbergen; links to the Ellesmerian and Caledonian. The new data from east Greenland together with published data from the mid‐Norwegian shelf [Bugge et al., ; Redfern et al., ] allow the construction of a simplify map showing the structural setting and major trends of the Early Triassic rift basins in the northernmost part of the North Atlantic region on both Greenland and European.
The extensional fault systems in East Greenland show complex linkages. In some cases, for example, Some New Investigations of the Devonian Stratigraphy and Tectonics of East Greenland: New Perspectives on the Old Red Sandstone: Geological Society of London Special Publicationp.
One stratigraphic marker bed in the lower Thumb Mountain Formation and two markers in the upper Thumb Mountain Formation (Fig. 2) are locally down-dropped and indicate widespread collapse in the central part of the Polaris deposit.
Discontinuous faults or fault-controlled breccia bodies bound the down-dropped area on its east and west sides. Stratigraphic sections showing major lithological units of onshore East Greenland, the NE Greenland shelf, and the Western Barents Sea. The onshore East Greenland section is taken from field-based studies ranging from approximately 70° to 76° N (e.g.
Stemmerik et al., ; Surlyk, ; Brooks, ; Andrews and Decou, ).