Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
Assimilation of Carbonates by Mafic Magma: Fassaite Gabbro of the Olkhon Terrane (Western Baikal Region). / Sklyarov, E. V.; Lavrenchuk, A. V.; Semenova, D. V.
в: Doklady Earth Sciences, Том 519, № 1, 11.2024, стр. 1860-1867.Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
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TY - JOUR
T1 - Assimilation of Carbonates by Mafic Magma: Fassaite Gabbro of the Olkhon Terrane (Western Baikal Region)
AU - Sklyarov, E. V.
AU - Lavrenchuk, A. V.
AU - Semenova, D. V.
N1 - This work was carried out under State Assignments of the Institute of the Earth’s Crust, Siberian Branch, Russian Academy of Sciences, and the Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences (project nos. 12204140044-2 and 122041400171-5).
PY - 2024/11
Y1 - 2024/11
N2 - Specific gabbro with the main rock-forming mineral of fassaite—alumina-rich (up to 12 wt % Al2O3) calcium pyroxene, typical of high-temperature metasomatic rocks, are characterized. In terms of the geochemical characteristics, the fassaite gabbros are close to the subalkaline monzogabbros of the Ust’-Krestovsky complex, which are widely distributed within the Krestovsky subterrane of the Olkhon terrane (Western Baikal region). At the same time, they differ sharply from the latter in having a higher content of CaO and MgO and a lower content of SiO2 and Al2O3. Fassaite gabbro composes several small bodies framed the Ust’-Krestovsky monzogabbro massif, without contacting the latter. A model of the formation of fassaite gabbro due to the assimilation of carbonate (crustal carbonate melts) by subalkaline mafic magma is proposed.
AB - Specific gabbro with the main rock-forming mineral of fassaite—alumina-rich (up to 12 wt % Al2O3) calcium pyroxene, typical of high-temperature metasomatic rocks, are characterized. In terms of the geochemical characteristics, the fassaite gabbros are close to the subalkaline monzogabbros of the Ust’-Krestovsky complex, which are widely distributed within the Krestovsky subterrane of the Olkhon terrane (Western Baikal region). At the same time, they differ sharply from the latter in having a higher content of CaO and MgO and a lower content of SiO2 and Al2O3. Fassaite gabbro composes several small bodies framed the Ust’-Krestovsky monzogabbro massif, without contacting the latter. A model of the formation of fassaite gabbro due to the assimilation of carbonate (crustal carbonate melts) by subalkaline mafic magma is proposed.
KW - Olkhon terrane
KW - assimilation
KW - carbonates
KW - fassaite
KW - gabbro
UR - https://www.scopus.com/record/display.uri?eid=2-s2.0-85203184706&origin=inward&txGid=b243b920d81e5ecc047ddef907fc5a15
UR - https://www.mendeley.com/catalogue/06bb120c-1295-3e0d-944f-fc4e8f53b3cd/
U2 - 10.1134/S1028334X24603055
DO - 10.1134/S1028334X24603055
M3 - Article
VL - 519
SP - 1860
EP - 1867
JO - Doklady Earth Sciences
JF - Doklady Earth Sciences
SN - 1028-334X
IS - 1
ER -
ID: 60780255