Hostname: page-component-78c5997874-v9fdk Total loading time: 0 Render date: 2024-11-06T09:46:21.048Z Has data issue: false hasContentIssue false

VIII.—The Petrography of the Franz Josef Fjord Region, North-East Greenland, in Relation to its Structure: A Study in Regional Metamorphism

Published online by Cambridge University Press:  06 July 2012

Extract

In the introduction to his previous paper on the Structure (Odell, 1939) the author included a short description of the stratigraphy of the region under review, and the briefest account only is therefore here deemed necessary.

A principal feature of north-east Greenland is the considerable number of representatives of the Geological Succession which lie exposed in the ice-free mountainous tract between the Inland Ice Cap and the Greenland Sea. These formations include Pre-Cambrian, Palæozoic, and Mesozoic sedimentaries with Kainozoic eruptives. They have a general trend north and south, and while the older rocks are situated mainly inland, the younger ones lie along the fringes of the coast-line. Consequently, as one sails westward up the immense fjords which cut transversely across the formations, one moves downwards in the succession towards the older rocks. The older rocks, however, underlie by far the greater part of the ice-free area, and of these, sandstones and coarse elastics of Old Red type, quartzites, slates, and limestones ranging from Ordovician to Pre-Cambrian, and metamorphic rocks with granites comprising a Metamorphic Complex, are found in three great belts in order from east to west, between latitudes 72° and 74°. Within these limiting latitudes, the numerous inlets and deeply entrenched fjords, whose great bare walls display in remarkable fashion the multi-coloured formations and their structures, have yielded a considerable amount of information in recent years to the British, Scandinavian, and other geologists who have studied them.

Type
Research Article
Copyright
Copyright © Royal Society of Edinburgh 1944

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Selected Regional Bibliography

Backlund, H. G., 1930. “Contributions to the Geology of North-east Greenland,” M.o.G., LXXIV, 11.Google Scholar
Backlund, H. G., 1932. “Das Alter des ‘metamorphen Komplexes’ von Franz Josef Fjord in Ostgrönland,” M.o.G., LXXXVII, 4.Google Scholar
Backlund, H. G., and Malmquist, D.. “Zur Geologie und Petrographie der Nordostgrönlandischen Basaltformation:— 1932. Teil I. Die Basische Reiche,” M.o.G., LXXXVII, 5.Google Scholar
Backlund, H. G., and Malmquist, D.., 1935. “Teil II. Die Sauren Ergussgestine von Kap Franklin,” M.o.G., xcv, 3.Google Scholar
Koch, Lauge, 1929. “The Geology of East Greenland,” M.o.G., LXXIII, 1.Google Scholar
Kranck, E. H., 1935. “On the Crystalline Complex of Liverpool Land,” M.o.G., xcv, 7.Google Scholar
Kulling, O., 1929. “Stratigraphic Studies of the Geology of North-east Greenland,” M.o.G., LXXIV, 13.Google Scholar
Odell, N. E., 1934. “Within and Without the Arctic Circle,” Alpine Journ., XLVI.Google Scholar
Odell, N. E., 1937. “The Glaciers and Morphology of the Franz Josef Fjord Region of North-east Greenland,” Geogr. Journ., xc, 111258.CrossRefGoogle Scholar
Odell, N. E., 1937. “Franz Josef Fjord and the Mystery Lakes District: Some Discoveries during the Boyd Expedition, 1933,” Scot. Geogr. Mag., LIII, 307323.Google Scholar
Odell, N. E., 1939. “The Structure of the Kejser Franz Joseph Fjord Region, North-east Greenland,” M.o.G., CXIX, no. 6.Google Scholar
Odell, N. E., 1935. Summary of ditto, Brit. Assoc. Rep., Sect. Trans. C.Google Scholar
Parkinson, M. M. L., and Whittard, W. F., 1931. “The Geological Work of the Cambridge Expedition to East Greenland in 1929,” Quart. Journ. Geol. Soc., LXXXVII, 650.CrossRefGoogle Scholar
Poulsen, Chr., 1930. “Contributions to the Stratigraphy of the Cambro-Ordovician of East Greenland,” M.o.G., LXXIV, 12.Google Scholar
Teichert, Curt, 1933. “Untersuchungen zum Bau des kaledonischen Gebirges in Ostgrönland,” M.o.G., xcv, 1.Google Scholar
Teichert, Curt, 1939. Geology of Greenland in Geologie der Erde, Geology of North America, I, Berlin, pp. 100175.Google Scholar
Tyrrell, G. W., 1932. “The Petrography of some Kainozoic Igneous Rocks, and of the Cape Parry Alkaline Complex, East Greenland,” Geol. Mag., LXIX, 520.CrossRefGoogle Scholar
Wegmann, C. E., 1935. “Preliminary Report on the Caledonian Orogeny in Christian X's Land (N.E. Greenland),” M.o.G., CIII, 3.Google Scholar
Wiseman, J. D. H., 1932. “A Contribution to the Petrology of the Metamorphic Rocks of East Greenland,” Quart. Journ. Geol. Soc., LXXXVIII, 312.CrossRefGoogle Scholar
Wordie, J. M., and Whittard, W. F., 1930. “A Contribution to the Geology of the Country between Petermann Peak and Kjerulf Fjord, East Greenland,” Geol. Mag., LXVII, 145.CrossRefGoogle Scholar

Incidental References

Adams, F. D., and Barlow, A. E., 1910. “Geology of Haliburton and Bancroft Areas,” Geol. Surv. of Canada Mem., 6.Google Scholar
Bailey, E. B., 1936. “Sedimentation in Relation to Tectonics,” Bull. Geol. Soc. Amer., XLVII.Google Scholar
Boyd, Louise A., 1935. “The Fiord Region of East Greenland,” Amer. Geogr. Soc. Spec. Publ., 18.Google Scholar
Bucher, W. H., 1933. The Deformation of the Earth's Crust.Google Scholar
Daly, R. A., 1933. Igneous Rocks and the Depths of the Earth.CrossRefGoogle Scholar
Henderson, G. H., 1937. “Some Types of Pleochroic Haloes,” Nature, CXL.Google Scholar
Holtedahl, and Others, 1934. “The Geology of the Oslo Region and the Adjacent Sparagmite District,” Proc. Geol. Assoc., XLV.Google Scholar
Howell, Resser, 1938. “The Lower Cambrian Olenellus Zone of the Appalachians,” Bull. Geol. Soc. Amer., XLIX.Google Scholar
Read, H. H., 1928. “A Note on ‘Ptygmatic Folding’ in the Sutherland Granite Complex,” Summ. Prog., Geol. Surv. of Gt. Brit. for 1927, Pt. II.Google Scholar
Smithson, F., 1939. “Statistical Methods in Sedimentary Petrology, Pt. II.,” Geol. Mag., LXXVI.Google Scholar
Thiel, G. A., 1940. “The Relative Resistance to Abrasion of Mineral Grains of Sand Size,” Journ. Sedim. Petrol., x.Google Scholar