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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.

In: Doklady Earth Sciences, Vol. 459, No. 2, 2014, p. 1504-1509.

Research output: Contribution to journal › Article

Harvard

Sobolev, NN, Metelkin, DV, Vernikovsky, VA, Matyshkin, NY, Prokop’ev, AV, Ershova, VB, Shmanyak, AV & Petrov, EO 2014, 'The first data on the geology of Jeannette Island (De Long Archipelago, New Siberian Islands)', Doklady Earth Sciences, vol. 459, no. 2, pp. 1504-1509. https://doi.org/10.1134/S1028334X14120228

APA

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. (2014). The first data on the geology of Jeannette Island (De Long Archipelago, New Siberian Islands). Doklady Earth Sciences, 459(2), 1504-1509. https://doi.org/10.1134/S1028334X14120228

Vancouver

Sobolev NN, Metelkin DV, Vernikovsky VA, Matyshkin NY, Prokop’ev AV, Ershova VB et al. The first data on the geology of Jeannette Island (De Long Archipelago, New Siberian Islands). Doklady Earth Sciences. 2014;459(2):1504-1509. https://doi.org/10.1134/S1028334X14120228

Author

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. / The first data on the geology of Jeannette Island (De Long Archipelago, New Siberian Islands). In: Doklady Earth Sciences. 2014 ; Vol. 459, No. 2. pp. 1504-1509.

BibTeX

@article{d5b913f47a2343928b3171f767b40827,
title = "The first data on the geology of Jeannette Island (De Long Archipelago, New Siberian Islands)",
abstract = "{\textcopyright} 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",
author = "N.N. Sobolev and D.V. Metelkin and V.A. Vernikovsky and N.Y. Matyshkin and A.V. Prokop{\textquoteright}ev and V.B. Ershova and A.V. Shmanyak and E.O. Petrov",
year = "2014",
doi = "10.1134/S1028334X14120228",
language = "English",
volume = "459",
pages = "1504--1509",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "2",

}

RIS

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