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  1. Електронний науковий архів Науково-технічної бібліотеки Національного університету "Львівська політехніка"
  2. Електронний архів Науково-технічної бібліотеки
  3. Вісники та науково-технічні збірники, журнали
  4. Геодинаміка
  5. Геодинаміка. – 2019. – №1(26)

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Please use this identifier to cite or link to this item: https://oldena.lpnu.ua/handle/ntb/45873
Title: Nature of the provenance and tectonic setting of oil shale (Middle eocene) in the Greater Caucasus southeastern plunge
Other Titles: Джерела зносу та тектонічні умови формування горючих сланців (середній еоцен) південно-східного занурення Великого Кавказу
Authors: Алієв, Аділь А.
Аббасов, Орхан Р.
Aliyev, Adil A.
Abbasov, Orhan R.
Affiliation: Азербайджанська національна академія наук
Azerbaijan National of Academy Sciences
Bibliographic description (Ukraine): Aliyev A. A. Nature of the provenance and tectonic setting of oil shale (Middle eocene) in the Greater Caucasus southeastern plunge / Adil A. Aliyev, Orhan R. Abbasov // Geodynamics : scientific journal. — Львів : Lviv Polytechnic Publishing House, 2019. — No 1 (26). — P. 43–59.
Bibliographic description (International): Aliyev A. A. Nature of the provenance and tectonic setting of oil shale (Middle eocene) in the Greater Caucasus southeastern plunge / Adil A. Aliyev, Orhan R. Abbasov // Geodynamics : scientific journal. — Lviv Polytechnic Publishing House, 2019. — No 1 (26). — P. 43–59.
Is part of: Геодинаміка : науковий журнал, 1 (26), 2019
Geodynamics : scientific journal, 1 (26), 2019
Journal/Collection: Геодинаміка : науковий журнал
Issue: 1 (26)
Issue Date: 26-Jun-2019
Publisher: Lviv Polytechnic Publishing House
Place of the edition/event: Львів
UDC: 550.422
552.52
551.21
551.24.05
Keywords: Великий Кавказ
горючі сланці
геохімія порід
протоліт
тектоніка
геодинаміка
вулканізм
басейн
Great Caucasus
oil shale
bulk rock geochemistry
protolith
tectonics
geodynamics
volcanism
basin
Number of pages: 17
Page range: 43-59
Start page: 43
End page: 59
Abstract: Відповідно до хімічного складу, встановлені протоліти та геотектонічні умови формування горючих сланців середньо-еоценового віку, відібраних з поверхневих виходів і викидів грязьових вулканів південно-східного занурення Великого Кавказу. Отримані дані зіставлені з палеогеодинамічними умовами району дослідження. Хімічний склад сланців встановлений за допомогою мас-спектрометрів “S8 TIGER Series 2 WDXRF” і “Agilent 7700 Series ICP-MS”, а при визначенні віку порід вико- ристовувалися мікроскопи “Loupe Zoom Paralux XTL 745” і “MБC-10” і цифрова камера “OptixCam”. Проведена нормалізація (порівняння з пост-архейськими сланцями Австралії, верхньою конти- нентальною корою і континентальною корою) у зв’язку з особливостями розподілу хімічних елементів, а також із застосуванням різних індексів і діаграм, встановлені джерела материнських магматичних порід і палеотектонічні умови їх формування. Встановлено, що базальт-андезитові утворення принесені з комплексів мафічних і проміжних джерел. Геотектонічні умови формування горючих сланців відповідають активним районам континентальної кори, а також зонам переходу від рифтогену до колізії або геодинамічним умовам первинної колізії. Отже, процес осадконакопичення, що відбувався в умовах мілководного морського басейну в зв’язку з первинною колізією між внутрішніми плитами, пов’язаний палеоцен-міоценовим басейном (північна гілка Мезотетіса в системі Крим-Великий Кавказ-Копетдаг). Особливу роль у встановленні походження кластичних матеріалів базальт-андезитового складу, відіграє юрський і крейдяний вулканізм, пов'язаний з субдукцією, встановленою на південному схилі Великого Кавказу (Тфанське і Вандамське підняття).
The protolith and tectonic settings of the Middle Eocene oil shale sampled from the outcrops and ejected products of mud volcanoes in the Greater Caucasus southeastern plunge were determined using bulk rock geochemistry data. The obtained results were adapted to the palaeogeodynamic conditions of the study areas. Method. The concentrations of element content in the samples were measured by “S8 TIGER Series 2 WDXRF” and “Agilent 7700 Series ICP-MS” mass spectrometers. The microscopes “Loupe Zoom Paralux XTL 745” and “MC-10” and a digital camera “OptixCam” were used to define the age of samples. The distribution of element contents of samples was normalized to Post-Archaean Australian shale (PAAS), Upper Continental Crust (UCC) and Continental Crust (CC). The source terrains of the parent rocks and tectonic settings of oil shale were determined using various ratios and diagrams. Results. The samples show a nature of basaltic and basalt andesitic protolith, which supports an idea that the original composition was derived from mafic and intermediate source terrains. The tectonic setting of oil shale correlates well with the active continental margin and the rift-tocollision transition or paleogeodynamic conditions of the initial collision. Thus, in the shallow sea basin and the initial collision conditions, the process of sedimentation in the middle Eocene was probably associated with the final Paleocene- Eocene basin, which was the northern branch of Meso-Tethys in the Crimea-Greater Caucasus-Kopetdag system. The Jurassic and Cretaceous volcanism associated with subductions, which occurred on the southern slope of the Greater Caucasus (in the Tufan and Vandam uplifts), played an important role as a source of transported materials. Scientific novelty. In the published literature, numerous geological and organic-geochemical features of oil shale in Azerbaijan have been studied. The literature on the study of the provenance and tectonic setting is nonexistent, and this study is the first attempt. Practical significance. The obtained results and the used methodology can be applied to study the genesis of the Middle Eocene deposits and as well as sedimentary rocks in Azerbaijan.
URI: https://ena.lpnu.ua/handle/ntb/45873
Copyright owner: © Інститут геології і геохімії горючих копалин Національної академії наук України, 2019
© Інститут геофізики ім. С. І. Субботіна Національної академії наук України, 2019
© Національний університет «Львівська політехніка», 2019
© Adil A. Aliyev, Orhan R. Abbasov
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