Calcium-Rich Ultramafites, Ankaramites, and Clinopyroxene–Porphyric Gabbro of the Birkhin Massif in the Ol’khon Region: Solution of the Problem of Primary Melt and Formation of Intrusion

Author:

Pushkarev E.V.1,Lavrenchuk A.V.23,Gottman I.A.1,Sklyarov E.V.4

Affiliation:

1. a A.N. Zavaritsky Institute of Geology and Geochemistry, Ural Branch of the Russian Academy of Sciences, ul. Akademika Vonsovskogo 15, Yekaterinburg, 620010, Russia

2. b V.S. Sobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences, pr. Akademika Koptyuga 3, Novosibirsk, 630090, Russia

3. c Novosibirsk State University, ul. Pirogova 1, Novosibirsk, 630090, Russia

4. d Institute of the Earth’s Crust, Siberian Branch of the Russian Academy of Sciences, ul. Lermontova 128, Irkutsk, 664033, Russia

Abstract

Abstract ––The paper presents new data on the chemical and mineral compositions of ultramafic rocks and various gabbro of the Birkhin massif in the Ol’khon region. Porphyric phenocrysts and zoned grains of clinopyroxene have been first found and studied in gabbronorite, which made it possible to reconstruct the entire melt crystallization trend from ultramafic to gabbro parageneses. Similar clinopyroxene trends have been established for clinopyroxenites and subvolcanic ankaramites, whose bodies and dikes have been recently discovered within the massif and in its environment. The total petrological data show that the magnesian high-Ca ankaramite melt corresponds in composition to the assumed primary melt for the Birkhin massif.

Publisher

GeoScienceWorld

Subject

Geology,Geophysics

Reference41 articles.

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4. Volcano– plutonic complex of the Tumrok Range (Eastern Kamchatka): An example of the Ural–Alaskan type intrusion and related volcanic Series;Chayka;Minerals,2023

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