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Evolution of the Alpha Ridge, the Arctic Ocean, from magnetic data. / Gurevich, N. I.; Merkur'ev, S. A.

In: Doklady Akademii Nauk, Vol. 401, No. 1, 23.11.2005, p. 75-79.

Research output: Contribution to journal › Article › peer-review

Harvard

Gurevich, NI & Merkur'ev, SA 2005, 'Evolution of the Alpha Ridge, the Arctic Ocean, from magnetic data', Doklady Akademii Nauk, vol. 401, no. 1, pp. 75-79.

APA

Gurevich, N. I., & Merkur'ev, S. A. (2005). Evolution of the Alpha Ridge, the Arctic Ocean, from magnetic data. Doklady Akademii Nauk, 401(1), 75-79.

Vancouver

Gurevich NI, Merkur'ev SA. Evolution of the Alpha Ridge, the Arctic Ocean, from magnetic data. Doklady Akademii Nauk. 2005 Nov 23;401(1):75-79.

Author

Gurevich, N. I. ; Merkur'ev, S. A. / Evolution of the Alpha Ridge, the Arctic Ocean, from magnetic data. In: Doklady Akademii Nauk. 2005 ; Vol. 401, No. 1. pp. 75-79.

BibTeX

@article{0f3305f8213f4f1a8f06d15ea93c8076,
title = "Evolution of the Alpha Ridge, the Arctic Ocean, from magnetic data",
abstract = "Geohistorical analysis of anomalous magnetic field showed that the region of Alpha Ridge and adjacent to it Canadian basin was formed as result of slow ocean bottom spreading in the Late Jurassic-Berriassic. Kinematical characteristic of spreading require contraction stresses in the very north of Greenland and tensile stresses within Queen Elizabeth Islands in Late Jurassic-Berriassic that is not contradictory to their geological structure.",
author = "Gurevich, {N. I.} and Merkur'ev, {S. A.}",
year = "2005",
month = nov,
day = "23",
language = "English",
volume = "401",
pages = "75--79",
journal = "ДОКЛАДЫ АКАДЕМИИ НАУК",
issn = "0869-5652",
publisher = "Издательство {"}Наука{"}",
number = "1",

}

RIS

TY - JOUR

T1 - Evolution of the Alpha Ridge, the Arctic Ocean, from magnetic data

AU - Gurevich, N. I.

AU - Merkur'ev, S. A.

PY - 2005/11/23

Y1 - 2005/11/23

N2 - Geohistorical analysis of anomalous magnetic field showed that the region of Alpha Ridge and adjacent to it Canadian basin was formed as result of slow ocean bottom spreading in the Late Jurassic-Berriassic. Kinematical characteristic of spreading require contraction stresses in the very north of Greenland and tensile stresses within Queen Elizabeth Islands in Late Jurassic-Berriassic that is not contradictory to their geological structure.

AB - Geohistorical analysis of anomalous magnetic field showed that the region of Alpha Ridge and adjacent to it Canadian basin was formed as result of slow ocean bottom spreading in the Late Jurassic-Berriassic. Kinematical characteristic of spreading require contraction stresses in the very north of Greenland and tensile stresses within Queen Elizabeth Islands in Late Jurassic-Berriassic that is not contradictory to their geological structure.

UR - http://www.scopus.com/inward/record.url?scp=27744442456&partnerID=8YFLogxK

M3 - Article

AN - SCOPUS:27744442456

VL - 401

SP - 75

EP - 79

JO - ДОКЛАДЫ АКАДЕМИИ НАУК

JF - ДОКЛАДЫ АКАДЕМИИ НАУК

SN - 0869-5652

IS - 1

ER -

ID: 51323853