Paleomagnetism of Cryogenian Kitoi mafic dykes in South Siberia: Implications for Neoproterozoic paleogeography

Sergei Pisarevsky; D.P. Gladkochub; K.M. Konstantinov; A.M. Mazukabzov; A.M. Stanevich; J.B. Murphy; J.A. Tait; T.V. Donskaya; I.K. Konstantinov

doi:10.1016/j.precamres.2013.04.007

Paleomagnetism of Cryogenian Kitoi mafic dykes in South Siberia: Implications for Neoproterozoic paleogeography

Sergei Pisarevsky, D.P. Gladkochub, K.M. Konstantinov, A.M. Mazukabzov, A.M. Stanevich, J.B. Murphy, J.A. Tait, T.V. Donskaya, I.K. Konstantinov

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28 Citations (Scopus)

Abstract

We present a new paleomagnetic pole of 1.1°N, 22.4°E, A95=7.4° from the 760Ma gabbro-dolerite Kitoi dykes located in the southern part of the Siberian Craton. The pole is supported by contact tests and suggests closer position of Siberia relative to Laurentia at 760Ma than in Mesoproterozoic. We propose that this closer configuration was achieved by dextral transpressive motion of Siberia relative to Laurentia between 780 and 760Ma. This motion was probably initiated at the first stage of the Rodinia breakup and is coeval with the 780Ma Gunbarrel magmatic event of the western Canadian shield. © 2013 Elsevier B.V.

Original language	English
Pages (from-to)	372-382
Journal	Precambrian Research
Volume	231
DOIs	https://doi.org/10.1016/j.precamres.2013.04.007
Publication status	Published - 2013

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title = "Paleomagnetism of Cryogenian Kitoi mafic dykes in South Siberia: Implications for Neoproterozoic paleogeography",

abstract = "We present a new paleomagnetic pole of 1.1°N, 22.4°E, A95=7.4° from the 760Ma gabbro-dolerite Kitoi dykes located in the southern part of the Siberian Craton. The pole is supported by contact tests and suggests closer position of Siberia relative to Laurentia at 760Ma than in Mesoproterozoic. We propose that this closer configuration was achieved by dextral transpressive motion of Siberia relative to Laurentia between 780 and 760Ma. This motion was probably initiated at the first stage of the Rodinia breakup and is coeval with the 780Ma Gunbarrel magmatic event of the western Canadian shield. {\textcopyright} 2013 Elsevier B.V.",

author = "Sergei Pisarevsky and D.P. Gladkochub and K.M. Konstantinov and A.M. Mazukabzov and A.M. Stanevich and J.B. Murphy and J.A. Tait and T.V. Donskaya and I.K. Konstantinov",

year = "2013",

doi = "10.1016/j.precamres.2013.04.007",

language = "English",

volume = "231",

pages = "372--382",

journal = "Precambrian Research",

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TY - JOUR

T1 - Paleomagnetism of Cryogenian Kitoi mafic dykes in South Siberia: Implications for Neoproterozoic paleogeography

AU - Pisarevsky, Sergei

AU - Gladkochub, D.P.

AU - Konstantinov, K.M.

AU - Mazukabzov, A.M.

AU - Stanevich, A.M.

AU - Murphy, J.B.

AU - Tait, J.A.

AU - Donskaya, T.V.

AU - Konstantinov, I.K.

PY - 2013

Y1 - 2013

N2 - We present a new paleomagnetic pole of 1.1°N, 22.4°E, A95=7.4° from the 760Ma gabbro-dolerite Kitoi dykes located in the southern part of the Siberian Craton. The pole is supported by contact tests and suggests closer position of Siberia relative to Laurentia at 760Ma than in Mesoproterozoic. We propose that this closer configuration was achieved by dextral transpressive motion of Siberia relative to Laurentia between 780 and 760Ma. This motion was probably initiated at the first stage of the Rodinia breakup and is coeval with the 780Ma Gunbarrel magmatic event of the western Canadian shield. © 2013 Elsevier B.V.

AB - We present a new paleomagnetic pole of 1.1°N, 22.4°E, A95=7.4° from the 760Ma gabbro-dolerite Kitoi dykes located in the southern part of the Siberian Craton. The pole is supported by contact tests and suggests closer position of Siberia relative to Laurentia at 760Ma than in Mesoproterozoic. We propose that this closer configuration was achieved by dextral transpressive motion of Siberia relative to Laurentia between 780 and 760Ma. This motion was probably initiated at the first stage of the Rodinia breakup and is coeval with the 780Ma Gunbarrel magmatic event of the western Canadian shield. © 2013 Elsevier B.V.

U2 - 10.1016/j.precamres.2013.04.007

DO - 10.1016/j.precamres.2013.04.007

M3 - Article

SN - 0301-9268

VL - 231

SP - 372

EP - 382

JO - Precambrian Research

JF - Precambrian Research

ER -

Paleomagnetism of Cryogenian Kitoi mafic dykes in South Siberia: Implications for Neoproterozoic paleogeography

Abstract

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