Структурные связи эклогитсодержащих комплексов севера Урала с кристаллическим фундаментом Печорской плиты
Ключевые слова:
геофизические поля, север Урала, марункеуский, неркаюский, комплекс, глубинное строение, аномалия, разлом, зона
Аннотация
Введение: На севере Урала эклогиты установлены в двух метаморфических комплексах: марункеуском эклогит-гнейсовом на Полярном Урале и неркаюском эклогит-сланцевом на Приполярном Урале. Выявлены признаки северо-западной и субширотной ориентировки аномалий геофизических полей над эклогитсодержащими комплексами севера Урала и их пространственные взаимосвязи. Структурные особенности и геологические взаимоотношения комплексов с окружающими толщами дают основание для гипотезы о принадлежности марункеуского и неркаюского комплексов к фрагментам раннедокембрийского основания, вовлеченного в структуру Уралид. Приводится комплексная интерпретация геофизических полей по марункеускому и неркаюскому комплексам. Рассматриваются возможные глубинные связи высокобарических объектов и кристаллического фундамента прилегающей с запада платформенной области. Методика исследований: Обобщены и систематизированы материалы по комплексной интерпретации геофизических полей (гравитационного, сейсмического), позволяющие решить вопрос о глубине залегания источников аномалий над эклогитсодержащими комплексами. Основное внимание уделено анализу трансформированных карт и построению методом подбора комплексных моделей земной коры, а также геологической интерпретации глубинных структур. Результаты и обсуждения: В процессе интерпретации гравитационного поля выявлены схожие черты в строении марункеуского эклогит-гнейсового и неркаюского эклогит-сланцевого комплексов. Установлена приуроченность локальных максимумов силы тяжести к участкам распространения пород основного (и частично ультраосновного в марункеуском комплексе) состава. Изучение структуры локальных полей по интенсивности, размерам и линейной северо-западной направленности аномальных зон и подзон Печорской плиты и эклогитсодержащих комплексов севера Урала позволяет установить пространственную взаимосвязь между ними на уровне средней коры. Заключение. Выявленные пространственные связи дают возможность считать наиболее аномальные участки над марункеуским эклогит-гнейсовым и неркаюским эклогит-сланцевым комплексами юго-восточным продолжением Варандей-Адзьвинской зоны и Верхнеколвинской подзоны интенсивных положительных гравитационных аномалий Печорской плиты. Полученные геолого-геофизические данные подтверждают представление о марункеуском и неркаюском комплексах, как фрагментах раннедокембрийского основания, вовлеченного в структуру Уралид.
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Литература
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3. Valizer P. M., Lennykh V. I. Amfiboly golubykh slantsev Urala [Amphiboles of the blue schists of the Urals]. Moscow. Nauka publ, 1988. 203 p. (in Russ.)
4. Ponomareva T. A., Pystin A. M. Petrofizicheskaya kharakteristika porod polimetamorficheskikh kompleksov severa Urala [Petrophysical characteristics of rocks of polymetamorphic complexes in the north of the Urals]. Izvestiya Komi NTs UrO RAN – Proceedings of the Komi Science Centre of the Ural Division of the Russian Academy of Sciences, 2014, no. 18. pp. 68–74. (in Russ.)
5. Ponomareva T. A., Pystin A. M. Strukturnye osobennosti marunkeuskogo ehklogit-gneisovogo kompleksa Polyarnogo Urala po gravimagnitnym dannym [Structural features of the Marunkeu eclogite-gneiss complex of the Polar Urals based on gravi-magnetic data]. Vestnik Instituta geologii Komi NC UrO RAN – Vestnik of the Institute of Geology of the Komi Science Centre UB RAS , 2019, no. 2. pp. 14–21. (in Russ.) DOI
6. Ponomareva T. A., Pystin A. M., Kushmanova E. V. Glubinnaya kharakteristika nerkayuskogo ehklogit-slantsevogo kompleksa Pripolyarnogo Urala [Deep characteristics of the Nerkayu eclogite-schist complex of the Nether-Polar Urals]. Vestnik Instituta geologii Komi NC UrO RAN – Vestnik of the Institute of Geology of the Komi Science Centre UB RAS, 2017, no. 11, pp. 9–14. (in Russ.)
7. Pystin A. M. Polimetamorficheskie kompleksy zapadnogo sklona Urala [Polymetamorphic complexes of the western slope of the Urals] Moscow, Nauka publ., 1994, 208 p. (in Russ.).
8. Pystin A. M., Pystina Yu. I., Potapov I. L. Panfilov A. V. Rannedokembriiskaya istoriya metamorfizma porod granulitovykh i ehklogitovykh kompleksov paleokontinental'noi zony Urala [Early Precambrian history of metamorphism of rocks of granulite and eclogite complexes of the paleocontinental zone of the Urals]. Syktyvkar, Geoprint publ., 2012, 46 p. (in Russ.).
9. Pystin A. M., Pystina Yu. I. Dokembrii Pripolyarnogo Urala: khronostratigraficheskii aspekt [Precambrian of the Nether-Polar Urals: chronostratigraphical aspect]. Trudy Karel'skogo nauchnogo tsentra RAN, Seriya: Geologiya dokembriya – Proceedings of the Karelian Scientific Center of the Russian Academy of Sciences, Series: Precambrian Geology, 2019, no.2, pp. 34–52. DOI . (in Russ.).
10. Kolmogorova V. V., Fedorova N. V. Rezul'taty modelirovaniya glubinnogo stroeniya zemnoi kory po ural'skoi chasti geotraversa Kvarts [Results of modeling the deep structure of the Earth's crust in the Ural part of the Quartz geotraverse]. Geofizika – Geophysics, 2015, no. 6. pp. 61–67. (in Russ.).
11. Martyshko P. S., Ladovskii I. V., Fedorova N. V., Byzov D. D., Tsidaev A. G. Teoriya i metody kompleksnoi interpretatsii geofizicheskikh dannykh [Theory and methods of complex interpretation of geophysical data]. Ekaterinburg: UrO RAN publ., 2016, 94 p. (in Russ.).
12. Rylkov S. A., Rybalka A. V., Ivanov K. S. Glubinnoe stroenie i metallogeniya Urala: sopostavlenie glubinnoe stroenie Yuzhnogo, Srednego i Polyarnogo Urala [Deep structure and metallogeny of the Urals: comparison deep structure of the Southern, Middle and Polar Urals]. Litosfera – Lithosphere, 2013, no. 1. pp. 3–16. (in Russ.).
13. Druzhinin V. S., Martyshko P. S., Nachapkin N. I., Osipov V. Yu. Stroenie verkhnei chasti litosfery i neftegazonosnost' nedr Ural'skogo regiona [The structure of the upper part of the lithosphere and the oil and gas content of the subsurface of the Ural region]. Yekaterinburg, IGF UrO RAS publ., 2014, 228 p. (in Russ.).
14. Puchkov V. N., Ivanov K. S. Tektonika severa Urala i Zapadnoi Sibiri: obshchaya istoriya razvitiya [Tectonics of the North of the Urals and Western Siberia: a general history of development]. Geotektonika, 2020, no. 1. pp. 41–61. DOI
15. Stratigraficheskie skhemy Urala (dokembrii, paleozoi) [Stratigraphic charts of the Urals (Precambrian, Paleozoic)]. Ekaterinburg: Uralgeolkom publ., 1993, 152 p. (in Russ.).
16. Pystin A. M., Pystina Yu. I., Ulyasheva N. S., Grakova O. V. U-Pb dating of detrital zircons from basal Post Paleoproterozoic metasediments in the Subpolar and Polar Urals: Evidence for a Cryogenian, not Mesoproterozoic Age. International Geology Review. 2020, vol. 62, no 17, pp. 2189–2202. DOI
17. Pystin A. M., Ulyasheva N. S., Pystina Yu. I., Grakova O. V. Provenance area and U–Pb age of detrital zircons from the Upper Proterozoic deposits of the Polar Urals: to the question of the time of formation of the Timan passive margin. Stratigraphy and Geological Correlation. 2020, vol. 28, no. 5, pp. 3–25. DOI (in Russ.).
18. Andreichev V. L., Ronkin Y. L., Serov P. A., Lepikhina O. P., Litvinenko A. F. New data on the Precambrian age of Marunkeu eclogites (Polar Urals). Doklady Earth Sciences. 2007, vol. 413, no. 3, pp. 347–350. DOI
19. Andreichev V. L., Rodionov N. V., Ronkin Ju. L. U-Pb i SmNd datirovanie ehklogitov Marunkeuskogo bloka Polyarnogo Urala: novye dannye [U-Pb and Sm-Nd dating of eclogites of the Marunkeu block of the Polar Urals: new data]. Metamorfizm, kosmicheskie, ehksperimental'nye i obshchie problemy petrologii: materialy Mezhdunarodnogo (KH Vserossiiskogo) petrograficheskogo soveshchaniya “Petrografiya XXI veka”, 2005, v. 4, pp. 17–19. (in Russ.).
20. Glodny J., Pease V., Montero P., Austrheim H. Rusin A. I. Protolith ages of eclogites, Marun-Keu Complex, Polar Urals, Russia: implications for the pre- and early Uralian evolution of the northeastern European continental margin. Geological Society of London. Memoir, 2004, v. 30. pp. 87–105. DOI
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Опубликован
2021-04-01
Как цитировать
Пономарева, Т. А., & Пыстин, А. М. (2021). Структурные связи эклогитсодержащих комплексов севера Урала с кристаллическим фундаментом Печорской плиты. Вестник ВГУ. Серия: Геология, (1), 65-74. https://doi.org/10.17308/geology.2021.1/3338
Выпуск
Раздел
Геофизика
