Результаты исследований: Научные публикации в периодических изданиях › статья
The first data on the geology of Jeannette Island (De Long Archipelago, New Siberian Islands). / Sobolev, N.N.; Metelkin, D.V.; Vernikovsky, V.A.; Matyshkin, N.Y.; Prokop’ev, A.V.; Ershova, V.B.; Shmanyak, A.V.; Petrov, E.O.
в: Doklady Earth Sciences, Том 459, № 2, 2014, стр. 1504-1509.Результаты исследований: Научные публикации в периодических изданиях › статья
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TY - JOUR
T1 - The first data on the geology of Jeannette Island (De Long Archipelago, New Siberian Islands)
AU - Sobolev, N.N.
AU - Metelkin, D.V.
AU - Vernikovsky, V.A.
AU - Matyshkin, N.Y.
AU - Prokop’ev, A.V.
AU - Ershova, V.B.
AU - Shmanyak, A.V.
AU - Petrov, E.O.
PY - 2014
Y1 - 2014
N2 - © 2014, Pleiades Publishing, Ltd. This paper presents the first actual information on the geology of Jeannette Island, one of the islands of the De Long archipelago located in the East Siberian Sea. We show that Jeannette Island has a volcano-sedimentary section dominated by volcaniclastic turbidites. The sequence identified on the southwestern coast of the island has a submonoclinal plunge complicated by secondary deformation structures, which indicate a general E-W direction of tectonic transport (in present-day coordinates). The sequence is intensely cut by multiple thin (up to a few meters) gabbro-dolerite dikes that are deformed conformably with the host rocks. The general geological framework of the island bears a close resemblance to that of nearby Henrietta Island located some 70 km to the east, which consists of a volcano-sedimentary cover of Early Paleozoic age. No organic remains have been found in the studied section of Jeannette Island. The preliminary results of isotope geochronological and pale
AB - © 2014, Pleiades Publishing, Ltd. This paper presents the first actual information on the geology of Jeannette Island, one of the islands of the De Long archipelago located in the East Siberian Sea. We show that Jeannette Island has a volcano-sedimentary section dominated by volcaniclastic turbidites. The sequence identified on the southwestern coast of the island has a submonoclinal plunge complicated by secondary deformation structures, which indicate a general E-W direction of tectonic transport (in present-day coordinates). The sequence is intensely cut by multiple thin (up to a few meters) gabbro-dolerite dikes that are deformed conformably with the host rocks. The general geological framework of the island bears a close resemblance to that of nearby Henrietta Island located some 70 km to the east, which consists of a volcano-sedimentary cover of Early Paleozoic age. No organic remains have been found in the studied section of Jeannette Island. The preliminary results of isotope geochronological and pale
U2 - 10.1134/S1028334X14120228
DO - 10.1134/S1028334X14120228
M3 - Article
VL - 459
SP - 1504
EP - 1509
JO - Doklady Earth Sciences
JF - Doklady Earth Sciences
SN - 1028-334X
IS - 2
ER -
ID: 7038012