Abstract

Research subject. The Late Paleozoic (D3–P1) black shale strata surrounding the Kara Astrobleme (Pay-Khoy) were studied. Materials and methods. The rocks were sampled radially along the profile from the edge of the astrobleme (the at the contact zone with impactites) with access to black shales that were not affected by post-impact transformations. An analysis of the mineralogical and geochemical features of the black shales surrounding the Kara astrobleme was carried out using a complex of modern research methods (Geonauka Centre for Collective Use, IG FRC Komi Scientific Centre, Ural Branch of the Russian Academy of Sciences) in order to identify the possible mobilisation, re-deposition and concentration of ore matter under the conditions of intensive post-impact hydrothermal altering. Results and conclusions. The geochemical features of the black shale deposits altered by post-impact hydrothermal processes in the vicinity of the Kara impact structure were determined. The sharp abnormal contents of Mn, B, Zr, Sr, Ge, Cd, Hf, Se and Eu as well as the abnormal contents of Ti, Ba, Cr, Rb, Li, Ce, La, Ga, Sc, Co, Cs, Gd, Dy and W were revealed. The geochemical concentration specificity of components in different regions of the Kara astrobleme associated with the specialisation of target rocks was established. Raremetal and rare-earth minerals, sulphides and thymannite (HgSe) were diagnosed.

Highlights

  • The rocks were sampled radially along the profile from the edge of the astrobleme with access to black shales that were not affected by post-impact transformations

  • An analysis of the mineralogical and geochemical features of the black shales surrounding the Kara astrobleme was carried out using a complex of modern research methods (Geonauka Centre for Collective Use, IG FRC Komi Scientific Centre, Ural Branch of the Russian Academy of Sciences) in order to identify the possible mobilisation, re-deposition and concentration of ore matter under the conditions of intensive post-impact hydrothermal altering

  • The geochemical features of the black shale deposits altered by post-impact hydrothermal processes in the vicinity of the Kara impact structure were determined

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Summary

ОБЪЕКТ И МЕТОДЫ ИССЛЕДОВАНИЯ

Объектом исследований являются позднепалео­ зойские (D3–P1) черносланцевые толщи окружения Карской астроблемы (Пай-Хой). Нами проведен анализ минералогических и гео­химических особенностей черных сланцев мишени окружения Карского импактного события с применением комплекса современных методов исследований для выявления возможной мобилизации, переотложения и концентрирования рудного вещества в условиях интенсивной постимпактной гидротермальной переработки. Содержание микроэлементов в черных сланцах определено методом ICPMS (масс-спектрометрия с индуктивно-связанной плазмой) на спектрометре ICP-MS Agilent 7700x Термические исследования черных сланцев проводились на дериватографе Shimadzu DTG-60H Определение изотопного состава углерода в породах было выполнено на масс-спектрометре Finnigan Delta V Advantage Диагностика и состав минералов осуществлялись на сканирующих электронных микроскопах JSM-6400 с энергодисперсионной приставкой Link, ISIS-300 Тропников) в аншлифах, подготовленных стандартным способом с углеродным напылением. В связи с использованной модификацией оборудования при определении минералов содержания CO2, F, Н2О были основаны на расчетных данных

КРАТКАЯ ГЕОЛОГИЧЕСКАЯ ХАРАКТЕРИСТИКА
ПЕТРОХИМИЯ И ГЕОХИМИЯ УГЛЕРОДИСТЫХ СЛАНЦЕВ
МИНЕРАЛОГИЯ УГЛЕРОДИСТЫХ СЛАНЦЕВ
Алевролит рыхлый
ОБСУЖДЕНИЕ И ВЫВОДЫ
СПИСОК ЛИТЕРАТУРЫ
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