Geodynamic setting of Ediacaran and Permian–Triassic plagiogranites of the Ust-Bel’sky and Algansky terranes, West Koryak fold belt, NE Russia: insights from U–Pb geochronology and geochemistry

• Main Authors: Moiseev, Artem, Luchitskaya, Marina, Sokolov, Sergey, Belyatsky, Boris
• Format: Text
• Language: unknown
• Published: Taylor & Francis 2019
• Subjects: Biochemistry; 29999 Physical Sciences not elsewhere classified; FOS Physical sciences; Physiology; FOS Biological sciences; 59999 Environmental Sciences not elsewhere classified; FOS Earth and related environmental sciences; 39999 Chemical Sciences not elsewhere classified; FOS Chemical sciences; Ecology; Immunology; FOS Clinical medicine; Developmental Biology; Cancer; Koni; Koryak
• Online Access: https://dx.doi.org/10.6084/m9.figshare.9778310.v1; https://tandf.figshare.com/articles/journal_contribution/Geodynamic_setting_of_Ediacaran_and_Permian_Triassic_plagiogranites_of_the_Ust-Bel_sky_and_Algansky_terranes_West_Koryak_fold_belt_NE_Russia_insights_from_U_Pb_geochronology_and_geochemistry/9778310/1

Ediacaran and Permian‒Triassic stages of plagiogranite magmatism are distinguished for the Ust-Bel’sky and Algansky terranes of the West Koryak fold belt, NE Russia. The U‒Pb ages of Ediacaran plagiogranites are 556 ± 3 Ma (SIMS data) and 538 ± 7 Ma (LA–ICP–MS data), respectively, and 235 ± 2 Ma (SIMS data) for the Permian‒Triassic plagiogranites. The Ediacaran and Permian‒Triassic plagiogranites are low-K igneous rocks. Sr‒Nd isotopy and REE patterns of both plagiogranite suites allow suggesting their formation via partial melting of primary mantle material or fractional crystallization of basaltic magma. Ediacaran plagiogranites were formed in the oceanic arc setting contemporaneously with the volcanic-sedimentary complex of Otrozhnaya slice, Ust-Bel’sky terrane. Tuffaceous conglomerates in the lower part of this complex contain Ediacaran zircons with a peak age of 571 Ma. Formation of the Permian‒Triassic plagiogranites took place within the Ust-Bel’sky segment of the Koni‒Taigonos arc via partial melting of melanocratic ophiolite material in the accretionary structure of this arc or fractional crystallization of basaltic magma, melted from such substrate.