Eclogite trace in evolution of Late Cenozoic alkaline basalt volcanism on the southwestern flank of the Baikal Rift Zone: Geochemical features and geodynamic consequences
- Авторлар: Perepelov A.1, Kuzmin M.1, Tsypukova S.1, Demonterova E.2, Ivanov A.2, Shcherbakov Y.1, Puzankov M.3, Odgerel D.4, Bat-Ulzii D.5
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Мекемелер:
- Vinogradov Institute of Geochemistry, Siberian Branch
- Institute of the Earth’s Crust, Siberian Branch
- Institute of Volcanology and Seismology, Far East Branch
- Institute of Paleontology and Geology
- Mongolian University of Science and Technology
- Шығарылым: Том 476, № 2 (2017)
- Беттер: 1187-1192
- Бөлім: Geochemistry
- URL: https://journals.rcsi.science/1028-334X/article/view/191098
- DOI: https://doi.org/10.1134/S1028334X1710018X
- ID: 191098
Дәйексөз келтіру
Аннотация
Eclogitized material from the oceanic lithosphere are the most likely source of alkaline basalt magmas in the formation of Late Cenozoic volcanic areas on the southwestern flank of the Baikal Rift Zone. Basaltic trachyandesites of the early stage of volcanism (Pg32 ~ 28–23 Ma) are rich in high field strength elements (HFSE), P2O5, F, Zn, Ga, Sr, Sn, and light rare earth elements (LREE); they are characterized by high values of the following ratios: Fe/Mn = 72–77, Sm/Yb = 7.7–8.5, Sr/Y = 57–63, and Ga/Sc = 2.1–2.3. At this stage, magmas are formed under conditions with a 2–8% degree of partial melting of the mantle substrate enriched with the material of the eclogite source (50–70%) (Cpx/Grt = 1.5–1.7). Basaltoid magmas of the final stage of volcanism (N13–N21 ~ 6–4 Ma) are formed from melting (1.5–4%) of a less fertilized mantle (Cpx/Grt = 2.1–3.1, Fe/Mn = 62–71, Sm/Yb = 3.5–4.6, Sr/Y = 29–44, Ga/Sc = 1.0–1.4). The directed variations of the compositions of the successive basaltoid magmas, which were formed in the Late Cenozoic, create an “eclogite trace” in this area.
Авторлар туралы
A. Perepelov
Vinogradov Institute of Geochemistry, Siberian Branch
Хат алмасуға жауапты Автор.
Email: alperdig@irk.ru
Ресей, Irkutsk, 650033
M. Kuzmin
Vinogradov Institute of Geochemistry, Siberian Branch
Email: alperdig@irk.ru
Ресей, Irkutsk, 650033
S. Tsypukova
Vinogradov Institute of Geochemistry, Siberian Branch
Email: alperdig@irk.ru
Ресей, Irkutsk, 650033
E. Demonterova
Institute of the Earth’s Crust, Siberian Branch
Email: alperdig@irk.ru
Ресей, Irkutsk, 664033
A. Ivanov
Institute of the Earth’s Crust, Siberian Branch
Email: alperdig@irk.ru
Ресей, Irkutsk, 664033
Yu. Shcherbakov
Vinogradov Institute of Geochemistry, Siberian Branch
Email: alperdig@irk.ru
Ресей, Irkutsk, 650033
M. Puzankov
Institute of Volcanology and Seismology, Far East Branch
Email: alperdig@irk.ru
Ресей, Petropavlovsk-Kamchatsky, 683006
D. Odgerel
Institute of Paleontology and Geology
Email: alperdig@irk.ru
Моңғолия, Ulan-Bator
D. Bat-Ulzii
Mongolian University of Science and Technology
Email: alperdig@irk.ru
Моңғолия, Ulan-Bator