Arctica
Historical continent | |
---|---|
Formed | 2565 Ma |
Type | Paleocontinent |
Today part of |
Arctica, or Arctida
Nikolay Shatsky (Shatsky 1935) was the first to assume that the crust in the Arctic region was of continental origin.[6] Shatsky, however, was a "fixist" and, erroneously, explained the presence of Precambrian and Paleozoic metamorphic rocks on the New Siberian, Wrangel, and De long Islands with subduction. "Mobilists", on the other hand, also erroneously, proposed that North America had rifted from Eurasia and that the Arctic basins had opened behind a retreating Alaska.[7]
Precambrian continent
In his reconstruction of the
Rogers & Santosh 2003 argued that most cratons that were around at 2.5 Ga most likely formed in a single region simply because they were located in a single region in Pangaea, which is the reason Rogers argued for the existence of Arctica. The core of Arctica was the Canadian Shield, which Williams et al. 1991 named Kenorland. They argued that this continent formed around 2.5 Ga and then rifted before reassembling along the 1.8 Ga Trans-Hudson and Taltson-Thelon orogenies. These two orogenies are derived from continental crust (not oceanic crust) and were probably intracontinental, leaving Kenorland intact from 2.5 Ga to the present. Correlations between orogenies in Canada and Siberia remain more controversial.[9]
Laurentia and Baltica were connected during the Late Palaeoproterzoic (1.7–1.74 Ga) and Siberia later joined them. Paleomagnetic reconstructions indicate that they formed a single supercontinent during the Mesoproterozoic (1.5–1.45 Ga) but paleomagnetic data and geological pieces of evidence also suggest a considerable spatial gap between Siberia and Laurentia and Arctica is thought to be the missing link.[10]
Phanerozoic microcontinent
The current geological structure of the Arctic Region is the result of tectonic processes during the Mesozoic and Cenozoic (250
In the reconstruction of Metelkin, Vernikovsky & Matushkin 2015, Arctica originally formed as a continent during the Tonian 950 Ma and became part of the supercontinent Rodinia. It reformed during the Permian-Triassic 255 Ma and became part of Pangaea. During this period the configuration of Arctica changed and the continent moved from near the Equator to near the North Pole while keeping its position between three major cratons: Laurentia, Baltica, and Siberia.[1][12] An extended magmatic event, the
Fragments of this continent include the
See also
- Arctic Alaska-Chukotka terrane – Terrane that includes parts of Alaska, Siberia and the continental shelf between them
- Penokean orogeny
- Timanide Orogen – Orogen that formed during the Neoproterozoic
References
Notes
- ^ a b c Vernikovsky & Dobretsov 2015, p. 206
- ^ Siberian craton - a fragment of a Paleoproterozoic supercontinent
- ^ Rogers 1996, Fig. 4, p. 97
- ^ Rogers 1996, p. 97
- ^ E.g. Khain, Polyakova & Filatova 2009, Tectonic units and their history, p. 335
- ^ Khain & Filatova 2009, p. 1076
- ^ Zonenshain & Natapov 1987, Introduction, p. 829
- ^ Rogers 1996, Abstract
- ^ Rogers & Santosh 2003, Arctica and Kenorland (~2500 Ma), pp. 360–361
- ^ Tait & Pisarevsky 2009, p. 37
- ^ a b Vernikovsky et al. 2014, Introduction, pp. 265–266
- ^ Vernikovsky & Dobretsov 2015, Fig. 2, p. 208
- ^ Ernst & Bleeker 2010, 90–130 Ma: northern Canada, initiation of the Arctic Ocean, p. 701, fig. 6b, p.705
- ^ Metelkin, Vernikovsky & Matushkin 2015, Introduction, p. 114; Fig. 1, p. 115
Sources
- Ernst, R.; Bleeker, W. (2010). "Large igneous provinces (LIPs), giant dyke swarms, and mantle plumes: significance for breakup events within Canada and adjacent regions from 2.5 Ga to the Present". Canadian Journal of Earth Sciences. 47 (5): 695–739. doi:10.1139/E10-025. Retrieved 28 March 2016.
- Khain, V. E.; Filatova, N. I. (2009). "From Hyperborea to Arctida: The Problem of the Precambrian Central Arctic Craton". Doklady Earth Sciences. 428 (1): 1076–1079. S2CID 128422376.
- Khain, V. E.; Polyakova, I. D.; Filatova, N. I. (2009). "Tectonics and petroleum potential of the East Arctic province" (PDF). Russian Geology and Geophysics. 50 (4): 334–345. . Retrieved 5 March 2016.
- Metelkin, D. V.; Vernikovsky, V. A.; Matushkin, N. Y. (2015). "Arctida between Rodinia and Pangea" (PDF). Precambrian Research. 259: 114–129. . Retrieved 5 March 2016.
- Rogers, J. J. W. (1996). "A history of continents in the past three billion years". Journal of Geology. 104 (1): 91–107, Chicago. S2CID 128776432.
- Rogers, J. J. W.; Santosh, M. (2003). "Supercontinents in Earth History" (PDF). Gondwana Research. 6 (3): 357–368. . Retrieved 8 March 2016.
- Sankaran, A. V. (2003). "The Supercontinent Medley: Recent Views" (PDF). Current Science. 85 (8): 1121–1123. Retrieved 28 February 2016.
- Shatsky, N. S.(1935). "On the tectonics of the Arctic". Geology and Mineral Resources in the North of the USSR (in Russian). Vol. 1. pp. 149–165.
- Tait, J. A.; Pisarevsky, S. A. (2009). Siberia, Laurentia and Baltica in Mesoproterozoic (PDF). 2nd International Conference on Precambrian Continental Growth and Tectonism. . Retrieved 19 March 2016.
- Vernikovsky, V. A.; Dobretsov, N. L. (2015). "Geodynamic evolution of the Arctic Ocean and modern problems in geological studies of the Arctic region". Herald of the Russian Academy of Sciences. 85 (3): 206–212. S2CID 152499653. Retrieved 5 March 2016.
- Vernikovsky, V. A.; Metelkin, D. V.; Vernikovskaya, A. E.; Matushkin, N. Y.; Lobkovsky, L. I.; Shipilov, E. V. (2014). "Early evolution stages of the arctic margins (Neoproterozoic-Paleozoic) and plate reconstructions" (PDF). Proceedings of the International Conference on Arctic Margins VI. Fairbanks, Alaska. Retrieved 19 March 2016.
- Williams, H.; Hoffman, P. E.; Lewry, J. F.; Monger, J .W. H.; Rivers, T. (1991). "Anatomy of North America: thematic portrayals of the continent". Tectonophysics. 187 (1–3): 117–134. .
- Zonenshain, L. P.; Natapov, L. M. (1987). "Tectonic History of the Arctic Region from the Ordivician Through the Cretaceous". In Herman, Yvonne (ed.). The Arctic Seas: Climatology, Oceanography, Geology, and Biology. Springer. ISBN 9781461306771. Retrieved 19 March 2016.