Early Paleozoic monzodiorite–granodiorite association in the northeastern flank of the South Mongolia–Khingan orogenic belt (Nora–Sukhotinsky Terrane): Age and tectonic setting
- Авторлар: Smirnov Y.1, Sorokin A.1, Kotov A.2, Sal’nikova E.2,3, Yakovleva S.2, Gorokhovsky B.2
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Мекемелер:
- Institute of Geology and Nature Management, Far East Branch
- Institute of Precambrian Geology and Geochronology
- St. Petersburg State University
- Шығарылым: Том 10, № 2 (2016)
- Беттер: 123-131
- Бөлім: Article
- URL: https://journals.rcsi.science/1819-7140/article/view/211061
- DOI: https://doi.org/10.1134/S1819714016020068
- ID: 211061
Дәйексөз келтіру
Аннотация
The paper presents the results of U–Pb geochronological and geochemical studies of the rocks of the monzodiorite–granodiorite association in the northeastern flank of the South Mongolia–Khingan orogenic belt, which composes a tectonic block among the provisionally Lower Paleozoic volcanosedimentary complexes of the Nora–Sukhotinsky Terrane. It is shown that the studied rocks have similar petrographic features (with the presence of transitional varieties) and form common trends in the petrographic diagrams. This suggests that they are members of a single magmatic association. The geochemical features of the monzodiorites, quartz monzodiorites, and granodiorites, in particular their enrichment in large ion lithophile elements (LILE) and depletion in some HFSE, indicate their similarity with island-arc magmatic rocks. The presence of monzonites and quartz monzonites in the studied monzodiorite–granodiorite association along with high K, Rb, Th, and Pb concentrations gives reasons to believe that it formed in active continental margin or ensialic island-arc environments. The granodiorites of the monzodiorite–granodiorite associations of the Nora–Sukhotinsky Terrane are dated at 440 ± 10 Ma and may be considered as a fragment of the early Silurian active continental margin or ensialic mature island arc in the structure of the South Mongolia–Khingan orogenic belt.
Негізгі сөздер
Авторлар туралы
Yu. Smirnov
Institute of Geology and Nature Management, Far East Branch
Email: sorokin@ascnet.ru
Ресей, per. Relochnyi 1, Blagoveshchensk, 675000
A. Sorokin
Institute of Geology and Nature Management, Far East Branch
Хат алмасуға жауапты Автор.
Email: sorokin@ascnet.ru
Ресей, per. Relochnyi 1, Blagoveshchensk, 675000
A. Kotov
Institute of Precambrian Geology and Geochronology
Email: sorokin@ascnet.ru
Ресей, nab. Makarova 2, Saint Petersburg, 199034
E. Sal’nikova
Institute of Precambrian Geology and Geochronology; St. Petersburg State University
Email: sorokin@ascnet.ru
Ресей, nab. Makarova 2, Saint Petersburg, 199034; Universitetskaya nab. 7/9, St. Petersburg, 199034
S. Yakovleva
Institute of Precambrian Geology and Geochronology
Email: sorokin@ascnet.ru
Ресей, nab. Makarova 2, Saint Petersburg, 199034
B. Gorokhovsky
Institute of Precambrian Geology and Geochronology
Email: sorokin@ascnet.ru
Ресей, nab. Makarova 2, Saint Petersburg, 199034