Standard

Basaltic Volcanism of Island-Arc–Back-Arc Basin System (Altai Active Margin). / Kuibida, M. L.

In: Russian Journal of Pacific Geology, Vol. 13, No. 3, 01.05.2019, p. 297-309.

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

Harvard

Kuibida, ML 2019, 'Basaltic Volcanism of Island-Arc–Back-Arc Basin System (Altai Active Margin)', Russian Journal of Pacific Geology, vol. 13, no. 3, pp. 297-309. https://doi.org/10.1134/S1819714019030059

APA

Kuibida, M. L. (2019). Basaltic Volcanism of Island-Arc–Back-Arc Basin System (Altai Active Margin). Russian Journal of Pacific Geology, 13(3), 297-309. https://doi.org/10.1134/S1819714019030059

Vancouver

Kuibida ML. Basaltic Volcanism of Island-Arc–Back-Arc Basin System (Altai Active Margin). Russian Journal of Pacific Geology. 2019 May 1;13(3):297-309. doi: 10.1134/S1819714019030059

Author

Kuibida, M. L. / Basaltic Volcanism of Island-Arc–Back-Arc Basin System (Altai Active Margin). In: Russian Journal of Pacific Geology. 2019 ; Vol. 13, No. 3. pp. 297-309.

BibTeX

@article{24c668ccf34a4195a5bba80f6705d216,
title = "Basaltic Volcanism of Island-Arc–Back-Arc Basin System (Altai Active Margin)",
abstract = "Abstract: The results of prior studies are generalized and the author{\textquoteright}s data on the geology, geochemistry, and isotope geochronology of the Early–Middle Devonian volcanic series of Western Gorny Altai and Rudny Altai that are related to two large volcanic systems, the Altai–Minusinsk and Altai–Salair, respectively, are presented. The studied basalts have convergent geochemical characteristics between the rocks in back-arc basins and island arcs or their rear extension zones. It is considered that the back-arc-basin–island-arc system was developed in the Early–Middle Devonian on the Altai margin of the Siberian continent.",
keywords = "Altai, back-arc basin, Central Asian Fold Belt, Devonian, geochemistry, island arc, volcanism, DEVONIAN VOLCANISM, ROCKS, CONTINENTAL-CRUST, RYUKYU ARC, ND ISOTOPIC CHARACTERISTICS, CONVERGENT BOUNDARIES, EVOLUTION, ENRICHED BASALTS, ASIAN OROGENIC BELT, OKINAWA TROUGH",
author = "Kuibida, {M. L.}",
year = "2019",
month = may,
day = "1",
doi = "10.1134/S1819714019030059",
language = "English",
volume = "13",
pages = "297--309",
journal = "Russian Journal of Pacific Geology",
issn = "1819-7140",
publisher = "Maik Nauka-Interperiodica Publishing",
number = "3",

}

RIS

TY - JOUR

T1 - Basaltic Volcanism of Island-Arc–Back-Arc Basin System (Altai Active Margin)

AU - Kuibida, M. L.

PY - 2019/5/1

Y1 - 2019/5/1

N2 - Abstract: The results of prior studies are generalized and the author’s data on the geology, geochemistry, and isotope geochronology of the Early–Middle Devonian volcanic series of Western Gorny Altai and Rudny Altai that are related to two large volcanic systems, the Altai–Minusinsk and Altai–Salair, respectively, are presented. The studied basalts have convergent geochemical characteristics between the rocks in back-arc basins and island arcs or their rear extension zones. It is considered that the back-arc-basin–island-arc system was developed in the Early–Middle Devonian on the Altai margin of the Siberian continent.

AB - Abstract: The results of prior studies are generalized and the author’s data on the geology, geochemistry, and isotope geochronology of the Early–Middle Devonian volcanic series of Western Gorny Altai and Rudny Altai that are related to two large volcanic systems, the Altai–Minusinsk and Altai–Salair, respectively, are presented. The studied basalts have convergent geochemical characteristics between the rocks in back-arc basins and island arcs or their rear extension zones. It is considered that the back-arc-basin–island-arc system was developed in the Early–Middle Devonian on the Altai margin of the Siberian continent.

KW - Altai

KW - back-arc basin

KW - Central Asian Fold Belt

KW - Devonian

KW - geochemistry

KW - island arc

KW - volcanism

KW - DEVONIAN VOLCANISM

KW - ROCKS

KW - CONTINENTAL-CRUST

KW - RYUKYU ARC

KW - ND ISOTOPIC CHARACTERISTICS

KW - CONVERGENT BOUNDARIES

KW - EVOLUTION

KW - ENRICHED BASALTS

KW - ASIAN OROGENIC BELT

KW - OKINAWA TROUGH

UR - http://www.scopus.com/inward/record.url?scp=85058787077&partnerID=8YFLogxK

U2 - 10.1134/S1819714019030059

DO - 10.1134/S1819714019030059

M3 - Article

AN - SCOPUS:85058787077

VL - 13

SP - 297

EP - 309

JO - Russian Journal of Pacific Geology

JF - Russian Journal of Pacific Geology

SN - 1819-7140

IS - 3

ER -

ID: 20634312