Evolution of High-Magnesium Melts During Crystallization of Rocks in Ultramafic Massifs, Siberian Platform

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Evolution of High-Magnesium Melts During Crystallization of Rocks in Ultramafic Massifs, Siberian Platform. / Simonov, V. A.; Vasiliev, Yu R.; Kotlyarov, A. V. и др.

в: Doklady Earth Sciences, Том 487, № 1, 01.07.2019, стр. 819-822.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

Harvard

Simonov, VA, Vasiliev, YR, Kotlyarov, AV & Prihodko, VS 2019, 'Evolution of High-Magnesium Melts During Crystallization of Rocks in Ultramafic Massifs, Siberian Platform', Doklady Earth Sciences, Том. 487, № 1, стр. 819-822. https://doi.org/10.1134/S1028334X19070183

APA

Simonov, V. A., Vasiliev, Y. R., Kotlyarov, A. V., & Prihodko, V. S. (2019). Evolution of High-Magnesium Melts During Crystallization of Rocks in Ultramafic Massifs, Siberian Platform. Doklady Earth Sciences, 487(1), 819-822. https://doi.org/10.1134/S1028334X19070183

Vancouver

Simonov VA, Vasiliev YR, Kotlyarov AV, Prihodko VS. Evolution of High-Magnesium Melts During Crystallization of Rocks in Ultramafic Massifs, Siberian Platform. Doklady Earth Sciences. 2019 июль 1;487(1):819-822. doi: 10.1134/S1028334X19070183

Author

Simonov, V. A. ; Vasiliev, Yu R. ; Kotlyarov, A. V. и др. / Evolution of High-Magnesium Melts During Crystallization of Rocks in Ultramafic Massifs, Siberian Platform. в: Doklady Earth Sciences. 2019 ; Том 487, № 1. стр. 819-822.

BibTeX

@article{2f99dcb7d4534724b211155dba509455,

title = "Evolution of High-Magnesium Melts During Crystallization of Rocks in Ultramafic Massifs, Siberian Platform",

abstract = "Abstract: The results of study of primary melt inclusions in accessory Cr–spinelides from dunite have revealed features of the chemical compositions of high-magnesium picrite–basalt melts that formed ultramafic massifs of the Siberian Platform. Computational modeling (with the PETROLOG and PLUTON software) using the inclusion compositions allowed determination of the crystallization temperatures of olivines from dunites of the Guli (1520–1420°С), Konder (1545–1430°С), Inagli (1530–1430°С), and Chad (1460–1420°C) massifs. The Cr–spinellids from the same complexes crystallized at Guli (1410–1370°С), Konder (1420–1380°С), Inagli (up to 1430°С), and Chad (1430–1330°С). Overall, computational modeling has revealed two types of trends of high-Mg melt evolution on the Siberian Platform. The first type is characteristic of the Guli Pluton, with the following rock sequence: dunite–pyroxenite–alkalic rocks. The second type occurs in the Konder massif, with a different sequence: dunite–kosvite–pyroxenite and olivine–diopside rocks.",

keywords = "MEIMECHITES, INCLUSIONS, PETROLOGY, MINERALS, MAGMAS",

author = "Simonov, {V. A.} and Vasiliev, {Yu R.} and Kotlyarov, {A. V.} and Prihodko, {V. S.}",

note = "Publisher Copyright: {\textcopyright} 2019, Pleiades Publishing, Ltd.",

year = "2019",

month = jul,

day = "1",

doi = "10.1134/S1028334X19070183",

language = "English",

volume = "487",

pages = "819--822",

journal = "Doklady Earth Sciences",

issn = "1028-334X",

publisher = "PLEIADES PUBLISHING INC",

number = "1",

}

RIS

TY - JOUR

T1 - Evolution of High-Magnesium Melts During Crystallization of Rocks in Ultramafic Massifs, Siberian Platform

AU - Simonov, V. A.

AU - Vasiliev, Yu R.

AU - Kotlyarov, A. V.

AU - Prihodko, V. S.

PY - 2019/7/1

Y1 - 2019/7/1

N2 - Abstract: The results of study of primary melt inclusions in accessory Cr–spinelides from dunite have revealed features of the chemical compositions of high-magnesium picrite–basalt melts that formed ultramafic massifs of the Siberian Platform. Computational modeling (with the PETROLOG and PLUTON software) using the inclusion compositions allowed determination of the crystallization temperatures of olivines from dunites of the Guli (1520–1420°С), Konder (1545–1430°С), Inagli (1530–1430°С), and Chad (1460–1420°C) massifs. The Cr–spinellids from the same complexes crystallized at Guli (1410–1370°С), Konder (1420–1380°С), Inagli (up to 1430°С), and Chad (1430–1330°С). Overall, computational modeling has revealed two types of trends of high-Mg melt evolution on the Siberian Platform. The first type is characteristic of the Guli Pluton, with the following rock sequence: dunite–pyroxenite–alkalic rocks. The second type occurs in the Konder massif, with a different sequence: dunite–kosvite–pyroxenite and olivine–diopside rocks.

AB - Abstract: The results of study of primary melt inclusions in accessory Cr–spinelides from dunite have revealed features of the chemical compositions of high-magnesium picrite–basalt melts that formed ultramafic massifs of the Siberian Platform. Computational modeling (with the PETROLOG and PLUTON software) using the inclusion compositions allowed determination of the crystallization temperatures of olivines from dunites of the Guli (1520–1420°С), Konder (1545–1430°С), Inagli (1530–1430°С), and Chad (1460–1420°C) massifs. The Cr–spinellids from the same complexes crystallized at Guli (1410–1370°С), Konder (1420–1380°С), Inagli (up to 1430°С), and Chad (1430–1330°С). Overall, computational modeling has revealed two types of trends of high-Mg melt evolution on the Siberian Platform. The first type is characteristic of the Guli Pluton, with the following rock sequence: dunite–pyroxenite–alkalic rocks. The second type occurs in the Konder massif, with a different sequence: dunite–kosvite–pyroxenite and olivine–diopside rocks.

KW - MEIMECHITES

KW - INCLUSIONS

KW - PETROLOGY

KW - MINERALS

KW - MAGMAS

UR - http://www.scopus.com/inward/record.url?scp=85071483888&partnerID=8YFLogxK

U2 - 10.1134/S1028334X19070183

DO - 10.1134/S1028334X19070183

M3 - Article

AN - SCOPUS:85071483888

VL - 487

SP - 819

EP - 822

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 1

ER -

ID: 21468116