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Vestnik 2020 02.Pdf ISSN 2619-0087 РОССИЙСКАЯ АКАДЕМИЯ НАУК УФИМСКИЙ ФЕДЕРАЛЬНЫЙ ИССЛЕДОВАТЕЛЬСКИЙ ЦЕНТР ИНСТИТУТ ГЕОЛОГИИ ГЕОЛОГИЧЕСКИЙ ВЕСТНИК 2020. № 2 Главный редактор Пучков В.Н. Заместитель главного редактора Содержание Ковалев С. Г. Фазлиахметов А.М. Франские граувакки Худолазовской мульды. Сообщение 1. Краткая характеристика отложений .................................... 3 Редакционная коллегия: Тагариева Р.Ч., Артюшкова О.В., Мизенс А.Г. Уникальные карбонатные разрезы пограничного интервала франского – фаменского Абдрахманов Р. Ф. ярусов (F/F) в районе геопарка Торатау (бассейны рек Ряузяк и Сикася Артюшкова О. В. западного склона Южного Урала) ............................................................. 24 Голованова И. В. Горожанин В. М. Яковлев А.Г. Морфологическая характеристика первых нижних Данукалова Г. А. коренных зубов (m1) узкочерепных полевок Microtus (Stenocranius) Знаменский С. Е. gregalis Pallas, 1779 из неоплейстоценовых местонахождений Южного Казанцева Т. Т. Предуралья ................................................................................................... 39 Кулагина Е. И. Шафигуллина Г.Т., Знаменский С.Е., Косарев А.М. Условия Маслов А. В. образования золото-порфирового оруденения месторождения Большой Осипов В. И. Каран (Южный Урал) по данным хлоритовой геотермометрии ............ 45 Савельев Д. Е. Салихов Д. Н. Мичурин С.В., Калистратова Е.О., Султанова А.Г., Казбулатова Серавкин И. Б. Г.М. Фтор в породах Западно-Акташской рудной зоны (Южный Сначев В. И. Урал) ..............................................................................................................54 Эрнст Р. Рахимов И.Р. Свидетельства гидротермального растворения и замещения апатита: обзор и фактические данные на примере Учредитель: метасоматизированных пород девонско-каменноугольных интрузий Институт геологии Западно-Магнитогорской зоны .................................................................. 72 УФИЦ РАН Сначёв В.И., Сначёв А.В. Геология, петрогеохимия и физико- Адрес редакции: химические условия образования Осейского массива (Восточно- 450000, г. Уфа, ул. Уральский прогиб) .......................................................................................85 К. Маркса, 16/2 Шмелёва Л.А. Изотопно-геохимические вариации как отражение Институт геологии геобиологических факторов в эволюции позднеордовикской рифовой Тел.: (347) 272-76-36 экосистемы Большая Косью (р. Илыч, Северный Урал) ......................... 94 E-mail: [email protected] Абдрахманов Р.Ф. Вода — самый сложный природный раствор .... 110 © Институт геологии УФИЦ РАН, 2020 © Авторы статей, 2020 ISSN 2619-0087 Russian Academy of Sciences Ufa Federal Research Centre Institute of Geology GEOLOGICHESKI I VESTNIK 2020. No. 2 Editor-in-Chief Puchkov V. N. Deputy Editor Kovalev S. G. Contents Editorial board: Fazliakhmetov A.M. Frasnian greywackes of the Khudolaz syncline. Abdrakhmanov R. F. Message 1. Brief description of deposits ......................................................... 3 Artiushkova O. V. Tagarieva R.Ch., Artyushkova O.V., Mizens A.G. Unique carbonate Danukalova G. A. sections of the Frasnian-Famennian stage boundary (F/F) in the geopark Ernst R. Toratau locality (the Ryauzyak and Sikaza rivers’ basin in the Western Golovanova I. V. slope of the Southern Urals) .......................................................................... 24 Gorozhanin V. M. Kazantseva T. T. Yakovlev A.G. Morphological characteristics of the fi rst lower molars Kulagina E. I. (m1) of narrow-skulled voles Microtus (Stenocranius) gregalis Pallas, Maslov A. V. 1779 from the Neopleistocene sites of the Southern Fore-Urals .................. 39 Osipov V. I. Shafi gullina G.T., Znamensky S.E., Kosarev A.M. Conditions for the Salikhov D. N. formation of gold-porphyry mineralization of the Bolshoy Karan deposit Savel'ev D. E. (Southern Urals) according to chlorite geothermometry ............................... 45 Seravkin I. B. Snachev V. I. Michurin S.V., Kalistratova E.O., Sultanova A.G., Kazbulatova Znamenskii S. E. G.M. Fluorine in the rocks of the West Aktash ore zone (South Ural) ........54 Rakhimov I.R. Evidence on hydrothermal dissolution and replacement of apatite: a review and factual data at the example of metasomatized rocks of Devonian-Carboniferous intrusions of the West Magnitogorsk zone .................................................................................................................72 Constitutor: Institute of geology Snachev V.I., Snachev A.V. Geology, petrogeochemistry and physico- UFRC RAS chemical conditions for the formation of the Oseysk massive (Eastern Ural trough) .................................................................................................... 85 Editorial address: Shmeleva L.A. Isotope-geochemical variations as a reflection 450000, Ufa, of geobiological factors in the evolution of the Late Ordovician reef Karl Marks st., 16/2. ecosystem Bol'shaya Kos'yu (Ilych River, Northern Urals) .......................... 94 Institute of Geology. Tel.: (347) 272-76-36 Abdrakhmanov R.F. Water is the most diffi cult natural solution .........110 E-mail: [email protected] © Institute of geology UFRC RAS, 2020 © Articles autors, 2020 ГЕОЛОГИЧЕСКИЙ ВЕСТНИК. 2020. №2. С. 3–23. УДК 551.734+552.514 (234.853) DOI: http://doi.org/10.31084/2619-0087/2020-2-1 ФРАНСКИЕ ГРАУВАККИ ХУДОЛАЗОВСКОЙ МУЛЬДЫ. СООБЩЕНИЕ 1. КРАТКАЯ ХАРАКТЕРИСТИКА ОТЛОЖЕНИЙ © 2019 г. А. М. Фазлиахметов Реферат. Впервые проведено описание разреза франских отложений на широте озера Ялангаскуль, где их мощность максимальна для Южного Урала — около 2500 м. Разрез сложен граувакками и кремнями верхней части улутауской свиты, мукасовской свиты и нижней подсвиты биягодинской свиты. Мощность слоев кремней, граувакк и их количественное соотношение меняются по разрезу и по простиранию. Это обусловливает линзовидное строение франской последовательности. Наиболее явно это видно в нижней подсвите биягодинской свиты. В ней выделено три линзы: ялангасская, идяш-кускаровская и худолазовская. Их размер и состав обломочного материала отличаются. Ялангасская линза сложена кластикой вулканитов кислого состава. Ее мощность — 350 м, протяженность — около 30 км. Идяш-кускаровская линза мощностью 150 м сложена обломочным материалом вулканитов разного состава. Худолазовская линза имеет мощность 1500 м и протяженность более 30 км. Слагающие ее граувакки состоят из зерен кварца, плагиоклаза, обломков магматических, метаморфических и осадочных пород. Выделенные линзы являются морфологическим выражением глубоководных конусов выноса. Первые две — сравнительно небольших. Худолазовская линза является сечением крупного конуса выноса, состоящего из нескольких лопастей. Формирование худолазовской линзы коррелируется с глобальным событием «Upper Kellwasser». Ключевые слова: улутауская свита, мукасовская свита, биягодинская свита, граувакки, турбидит, глубоководный конус выноса, верхний девон, франский ярус, глобальное событие, Upper Kellwasser, Южный Урал FRASNIAN GREYWACKES OF THE KHUDOLAZ SYNCLINE. MESSAGE 1. BRIEF DESCRIPTION OF DEPOSITS © 2019 A. M. Fazliakhmetov Abstract. The fi rst description of the Frasnian deposits at the Lake Yalangaskul region is given. Their thickness is maximal for the Southern Urals (about 2500 m). The section is composed of greywackes and cherts of the upper part of the Ulutau formation, the Mukasevo formation and the lower part of the Biyagoda formation. The thickness of cherts and greywackes, and their quantitative ratio vary. This leads to the lenticular structure of the Frasnian deposits. This is most clearly seen in the lower level of the Biyagoda formation. Three lenses are distinguished in it: Yalangas, Idyash-Kuskarovo and Khudolaz. Their size and composition of clastic material diff er. The Yalangas lens is composed of an acidic volcanic clastic. Its thickness is 350 m, length is about 30 km. The 150 m-thick Idyash-Kuskarovo lens is composed of volcanic clastic material of diff erent composition. The Khudolaz lens has a thickness of 1500 m and a length of more than 30 km. Khudolaz lens greywackes are composed of quartz, plagioclase, fragments of magmatic, metamorphic and sedimentary rocks. Lenses are cross sections of deep-water fans. The fi rst two are relatively small. The Khudolaz lens is a cross section of a large fan cone consisting of several blades. The formation of a Khudolaz lentil is correlated with the global Upper Kellwasser event. Key words: the Ulutau formation, the Mukasevo formation, Biyagoda formation, greywacke, turbidite, deep-water fan, the Upper Devonian, the Frasnian, global event, Upper Kellwasser, South Urals Для цитирования: Фазлиахметов А.М. Франские граувакки Худолазовской мульды. Сообщение 1. Краткая харак- теристика отложений // Геологический вестник. 2020. № 2. С. 3–23. DOI: http://doi.org/10.31084/2619-0087/2020-2-1. For citation: Fazliakhmetov A.M. Frasnian greywackes of the Khudolaz syncline. Message 1. Brief description of deposits // Geologicheskii vestnik. 2020. No. 2. P. 3–23. DOI: http://doi.org/10.31084/2619-0087/2020-2-1. 3 4 А. М. Ф Введение превышает 2500 м. Это обстоятельство послужило поводом для комплексного изучения франских Франские отложения в Западно-Магнитогор- отложений западного крыла Худолазовской мульды, ской зоне Южного Урала изучаются уже на протяже- включающего маршрутные описания, поиск отпе- нии нескольких десятилетий. За это время собран чатков конодонтов, анализ аэро- и космоснимков, и проинтерпретирован представительный фактичес- петрографическую характеристику и литохимичес- кий материал по их биостратиграфии,
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