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Concerning the issue of paleotectonic reconstructions in the Arctic and of the tectonic unity of the New Siberian Islands Terrane: New paleomagnetic and paleontological data |
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| Authors: | V A Vernikovsky D V Metelkin T Yu Tolmacheva N A Malyshev O V Petrov N N Sobolev N Yu Matushkin |
| Institution: | 1. A.A. Trofimuk Institute of Petroleum Geology and Geophysics SB RAS, prosp. Akad. Koptyuga 3, Novosibirsk, 630090, Russia 2. Novosibirsk State University, Pirogova st. 2, Novosibirsk, 630090, Russia 3. A.P. Karpinsky Russian Geological Research Institute, Sredny pr. 74, St. Petersburg, 199106, Russia 4. Rosneft JSC, Sofiyskaya emb. 26/1, Moscow, 117997, Russia |
| Abstract: | The New Siberian Islands terrane, represented on the Arctic shelf by the archipelagos of the New Siberian Islands and De Long Islands, is one of the key structures of the Arctic. However many questions of its structure, borders and formation history are under intense discussion. During the international expedition in 2011 we solved many problems concerning structural geology, paleontology, petrology and geochronology. A particular attention was given to obtaining paleomagnetic data for the sedimentary and igneous rocks of the archipelago. The primary objects of paleomagnetic studies were the Early Paleozoic sedimentary rocks of the Kotelny (Anzhu) and Bennett (De Long) islands. In this paper we present new paleontological data, including the first one for conodonts of the New Siberian Islands, which help us to specify the age of the Early Paleozoic deposits of the studied sections. In these sections we took a series of paleomagnetic samples. The match of the paleomagnetic directions we determined for Bennett Isl. and Kotelny Isl. indicates the tectonic unity between the territories of the Anzhu and De Long archipelagos. These first paleomagnetic data allow us to affirm that at least from the Early Ordovician the rocks of the Anzhu and De Long archipelagos formed within the same New Siberian Islands terrane, that is to say, on the same basement. |
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