litosphereЛитосфераLITHOSPHERE (Russia)1681-90042500-302XA.N. Zavaritsky Institute of Geology and Geochemistry10.24930/1681-9004-2020-20-1-40-62litosphere-1238Research ArticleСтатьиArticlesРеконструкция состава пород питающих провинций. Статья 2. Лито- и изотопно-геохимические подходы и методыProvenance reconstructions. Article 2. Litho- and isotope-geochemical approaches and methodsМасловА. В.MaslovA. V.

620016, Екатеринбург, ул. Акад. Вонсовского, 15; 450077, Уфа, ул. К. Маркса, 16/2

Andrey V. Maslov

15 Akad. Vonsovsky st., Ekaterinburg 620016; 16/2 K. Marx st., ufa 450077

amas2004@mail.ruМельничукО. Ю.MelnichukO. Yu.

620016, Екатеринбург, ул. Акад. Вонсовского, 15

Oleg Yu. Melnichuk

15 Akad. Vonsovsky st., Ekaterinburg 620016

o.u.melnichuk@mail.ruМизенсГ. А.MizensG. A.

620016, Екатеринбург, ул. Акад. Вонсовского, 15

Gunar A. Mizens

15 Akad. Vonsovsky st., Ekaterinburg 620016

mizens@igg.uran.ruТитовЮ. В.TitovYu. V.

628481, Когалым, ул. Центральная, 19/17

Yury V. Titov

19/17 Central ’naya st., Kogalym 628481

titovoil@k66.ruЧервяковскаяМ. В.ChervyakovskayaM. V.

620016, Екатеринбург, ул. Акад. Вонсовского, 15

Maria V. Chervyakovskaya

15 Akad. Vonsovsky st., Ekaterinburg 620016

masha_vuf_91@mail.ruИнститут геологии и геохимии, УрО РАН; Институт геологии, Уфимский федеральный исследовательский центр, РАНРоссияA.N. Zavaritsky Institute ofGeology and Geochemistry, urals Branch of RAS; Institute of Geology, ufimian Federal Research Centre, RASRussian FederationИнститут геологии и геохимии, УрО РАНРоссияA.N. Zavaritsky Institute ofGeology and Geochemistry, urals Branch of RASRussian FederationФилиал ООО “ЛУКОИЛ-Инжиниринг” “КогалымНИПИнефть” в г. ТюмениРоссияBranch of “LuKOIL-Engineering Ltd. ” “KogalymNIPIneft” in TyumenRussian Federation2020290220202014062Copyright © Маслов А.В., Мельничук О.Ю., Мизенс Г.А., Титов Ю.В., Червяковская М.В., 20202020Маслов А.В., Мельничук О.Ю., Мизенс Г.А., Титов Ю.В., Червяковская М.В.Maslov A.V., Melnichuk O.Y., Mizens G.A., Titov Y.V., Chervyakovskaya M.V.Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://www.lithosphere.ru/jour/article/view/1238Объект исследований

Объект исследований. Рассмотрены особенности применения лито- и изотопно-геохимических данных для целей реконструкции состава пород питающих провинций.

Материалы и методы

Материалы и методы. В качестве основных инструментов использованы анализ соотношений некоторых породообразующих оксидов, разнообразных отношений индикаторных элементов-примесей, а также исследование спектров распределения редкоземельных элементов. В качестве материала, иллюстрирующего особенности применения перечисленных выше и ряда других подходов, выступают данные о валовом химическом составе песчаников и глинистых пород бирьянской подсвиты зильмердакской свиты верхнего рифея и басинской свиты верхнего венда Южного Урала, кодинской и устькодинской свит верхнего девона Среднего Урала, а также сортымской свиты нижнего мела Большехетской впадины Западно-Сибирского осадочного мегабассейна.

Результаты

Результаты. Показано, что подавляющее большинство рассмотренных в данной работе парных и треугольных диаграмм позволяет сделать согласующиеся между собой и не противоречащие общим геологическим представлениям выводы о составе пород-источников слагающего их материала. Эти выводы подкрепляют представления, получаемые в результате минералого-петрографического исследования песчаников.

Research subject

Research subject. In this paper, we consider specific features of the use of litho- and isotopic-geochemical data for the purposes of provenance reconstruction.

Methods and materials

Methods and materials. The reconstruction tools under consideration included the analysis of the ratio of major oxides and variable trace elements, as well as the study of the distribution of trace elements. The research potential of these methods was illustrated using the data on the bulk chemical composition of sandstones and mudstones from the Bir’yan Member of the Upper Riphean Zilmerdak Formation, Upper Vendian Basa Formation (Southern Urals), Upper Devonian Kodinka and Ust’kodinka formations (Middle Urals), Lower Cretaceous Sortym Formation (Western Siberian sedimentary megabasin, Bolshekhetskaya depression).

Results

Results. It was shown that the use of the vast majority of the described paired and triangular diagrams allows conclusions (consistent both with each other and conventional geological concepts) to be drawn about the composition of source rocks. These findings reinforce the insights gained from mineralogical and petrographic studies of sandstones.

песчаникиглинистые породыметоды реконструкции состава пород-источников сносапородообразующие оксидыредкие и рассеянные элементырифейвендверхний девоннижний мелЮжный УралСредний УралЗападно-Сибирский осадочный мегабассейнБольшехетская впадинаsandstonesmudstonesshalesprovenance reconstruction methodsrock-forming oxidestrace elementsripheanVendianupper DevonianLower CretaceousSouthern uralsMiddle uralsWest Siberian sedimentary megabasinBolshekhetskaya depressionАвторы искренне признательны Н.С. Глушковой, выполнившей иллюстрации к этой статье. Исследования проведены в соответствии с темами АААА-А18-118053090044-1 и АААА-А18-118053090045-8 государственного задания ИГГ УрО РАНThe authors are sincerely grateful to N.S. Glushkova, who performed the illustrations for this article. 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The authors declare that there are no conflicts of interest present.