Isotopic (Sm–Nd) and Geochemical (Nb/Y–Zr/Y) Systematics of the Sikhote-Alin Basic-Hyperbasic Complexes.

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Title: Isotopic (Sm–Nd) and Geochemical (Nb/Y–Zr/Y) Systematics of the Sikhote-Alin Basic-Hyperbasic Complexes.
Authors: Kazachenko, V. T.1 (AUTHOR) vkazachenko@mail.ru, Perevoznikova, E. V.1 (AUTHOR) elenavalper@yandex.ru
Source: Geochemistry International. Apr2023, Vol. 61 Issue 4, p324-347. 24p.
Subjects: Lamproite, Paleocene Epoch, Copper, Paleozoic Era, Peridotite, Samarium
Abstract: Abstract—The paper demonstrates the possibility of application of the 143Nd/144Nd–Sm/Nd and Nb/Y–Zr/Y diagrams to systematics of basic–ultrabasic complexes of different age: Paleozoic Kalinovsky, Cambrian Sergeevsky and Vladimiro-Aleksandrovsky, and Jurassic and Paleocene ones. The position of data points of the Kalinovsky, Sergeevsky, and Vladimiro-Aleksandrovsky complexes in the diagrams indicates their derivation from a primitive mantle-type (BSE) source, the derivatives of which are frequently associated with Cu, Ni, Co, and PGE mineralization. The position of data points of metabasic rocks of the Avdokimovsky complex and peridotite rocks of the Dalny Kut massif in these diagrams suggests that they have originated from depleted mantle and are promising for the discovery of PGE-bearing chromite mineralization. Data points of Paleocene explosive structures of Sikhote-Alin in the Nb/Y–Zr/Y diagram fall on the trend of recycled crust as a source. This explains the alkaline (to subalkaline) type of magmatism and the high gas saturation of magmas. The explosive structures resemble lamproite pipes, while their rocks are geochemically and mineralogically close both to lamproites and kimberlites. [ABSTRACT FROM AUTHOR]
Copyright of Geochemistry International is the property of Springer Nature and its content may not be copied or emailed to multiple sites without the copyright holder's express written permission. Additionally, content may not be used with any artificial intelligence tools or machine learning technologies. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)
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  Data: Isotopic (Sm–Nd) and Geochemical (Nb/Y–Zr/Y) Systematics of the Sikhote-Alin Basic-Hyperbasic Complexes.
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  Data: <searchLink fieldCode="AR" term="%22Kazachenko%2C+V%2E+T%2E%22">Kazachenko, V. T.</searchLink><relatesTo>1</relatesTo> (AUTHOR)<i> vkazachenko@mail.ru</i><br /><searchLink fieldCode="AR" term="%22Perevoznikova%2C+E%2E+V%2E%22">Perevoznikova, E. V.</searchLink><relatesTo>1</relatesTo> (AUTHOR)<i> elenavalper@yandex.ru</i>
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  Data: <searchLink fieldCode="JN" term="%22Geochemistry+International%22">Geochemistry International</searchLink>. Apr2023, Vol. 61 Issue 4, p324-347. 24p.
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  Data: <searchLink fieldCode="DE" term="%22Lamproite%22">Lamproite</searchLink><br /><searchLink fieldCode="DE" term="%22Paleocene+Epoch%22">Paleocene Epoch</searchLink><br /><searchLink fieldCode="DE" term="%22Copper%22">Copper</searchLink><br /><searchLink fieldCode="DE" term="%22Paleozoic+Era%22">Paleozoic Era</searchLink><br /><searchLink fieldCode="DE" term="%22Peridotite%22">Peridotite</searchLink><br /><searchLink fieldCode="DE" term="%22Samarium%22">Samarium</searchLink>
– Name: Abstract
  Label: Abstract
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  Data: Abstract—The paper demonstrates the possibility of application of the 143Nd/144Nd–Sm/Nd and Nb/Y–Zr/Y diagrams to systematics of basic–ultrabasic complexes of different age: Paleozoic Kalinovsky, Cambrian Sergeevsky and Vladimiro-Aleksandrovsky, and Jurassic and Paleocene ones. The position of data points of the Kalinovsky, Sergeevsky, and Vladimiro-Aleksandrovsky complexes in the diagrams indicates their derivation from a primitive mantle-type (BSE) source, the derivatives of which are frequently associated with Cu, Ni, Co, and PGE mineralization. The position of data points of metabasic rocks of the Avdokimovsky complex and peridotite rocks of the Dalny Kut massif in these diagrams suggests that they have originated from depleted mantle and are promising for the discovery of PGE-bearing chromite mineralization. Data points of Paleocene explosive structures of Sikhote-Alin in the Nb/Y–Zr/Y diagram fall on the trend of recycled crust as a source. This explains the alkaline (to subalkaline) type of magmatism and the high gas saturation of magmas. The explosive structures resemble lamproite pipes, while their rocks are geochemically and mineralogically close both to lamproites and kimberlites. [ABSTRACT FROM AUTHOR]
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  Data: <i>Copyright of Geochemistry International is the property of Springer Nature and its content may not be copied or emailed to multiple sites without the copyright holder's express written permission. Additionally, content may not be used with any artificial intelligence tools or machine learning technologies. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract.</i> (Copyright applies to all Abstracts.)
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      – Type: doi
        Value: 10.1134/S0016702923040067
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      – Code: eng
        Text: English
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      – SubjectFull: Lamproite
        Type: general
      – SubjectFull: Paleocene Epoch
        Type: general
      – SubjectFull: Copper
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      – SubjectFull: Paleozoic Era
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      – SubjectFull: Samarium
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      – TitleFull: Isotopic (Sm–Nd) and Geochemical (Nb/Y–Zr/Y) Systematics of the Sikhote-Alin Basic-Hyperbasic Complexes.
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              Text: Apr2023
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              Y: 2023
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