Petrochemical characteristics and ore specialization of the Hautavaara massif, South Karelia

<p>The Hautavaara sanukitoid massif, located in the southern Vedlozero-Segozero greenstone belt, Karelia, is differentiated from monzogabbro to moderately alkaline granite. Its structure and the petrographic and petrochemical characteristics of all its rock types are discussed. The granosyenit...

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Main Authors: Антонина Васильевна Дмитриева, Людмила Владимировна Кулешевич, Александр Сергеевич Вихко, Antonina Dmitrieva, Lyudmila Kuleshevich, Alexandr Vikhko
Format: Article
Language:English
Published: Karelian Research Centre of the Russian Academy of Sciences 2015-12-01
Series:Transactions of the Karelian Research Centre of the Russian Academy of Sciences
Subjects:
Online Access:http://journals.krc.karelia.ru/index.php/precambrian/article/view/160
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spelling doaj-6f64341b98c649c5aa68e1996af9798f2020-11-25T03:14:09ZengKarelian Research Centre of the Russian Academy of SciencesTransactions of the Karelian Research Centre of the Russian Academy of Sciences1997-32172312-45042015-12-0102527210.17076/geo160162Petrochemical characteristics and ore specialization of the Hautavaara massif, South KareliaАнтонина Васильевна Дмитриева0Людмила Владимировна Кулешевич1Александр Сергеевич Вихко2Antonina Dmitrieva3Lyudmila Kuleshevich4Alexandr Vikhko5Институт геологии Карельского научного центра РАНИнститут геологии Карельского научного центра РАНИнститут геологии Карельского научного центра РАНИнститут геологии Карельского научного центра РАНИнститут геологии Карельского научного центра РАНИнститут геологии Карельского научного центра РАН<p>The Hautavaara sanukitoid massif, located in the southern Vedlozero-Segozero greenstone belt, Karelia, is differentiated from monzogabbro to moderately alkaline granite. Its structure and the petrographic and petrochemical characteristics of all its rock types are discussed. The granosyenites are subjected to mean temperature variations and display Au-Mo-geochemical specialization. Gold-sulphide-quartz vein mineralization and molybdenite mineralization are confined to them.</p>http://journals.krc.karelia.ru/index.php/precambrian/article/view/160хаутаваарский санукитоидный массивизменения породкварцевые жилызолотомолибденит
collection DOAJ
language English
format Article
sources DOAJ
author Антонина Васильевна Дмитриева
Людмила Владимировна Кулешевич
Александр Сергеевич Вихко
Antonina Dmitrieva
Lyudmila Kuleshevich
Alexandr Vikhko
spellingShingle Антонина Васильевна Дмитриева
Людмила Владимировна Кулешевич
Александр Сергеевич Вихко
Antonina Dmitrieva
Lyudmila Kuleshevich
Alexandr Vikhko
Petrochemical characteristics and ore specialization of the Hautavaara massif, South Karelia
Transactions of the Karelian Research Centre of the Russian Academy of Sciences
хаутаваарский санукитоидный массив
изменения пород
кварцевые жилы
золото
молибденит
author_facet Антонина Васильевна Дмитриева
Людмила Владимировна Кулешевич
Александр Сергеевич Вихко
Antonina Dmitrieva
Lyudmila Kuleshevich
Alexandr Vikhko
author_sort Антонина Васильевна Дмитриева
title Petrochemical characteristics and ore specialization of the Hautavaara massif, South Karelia
title_short Petrochemical characteristics and ore specialization of the Hautavaara massif, South Karelia
title_full Petrochemical characteristics and ore specialization of the Hautavaara massif, South Karelia
title_fullStr Petrochemical characteristics and ore specialization of the Hautavaara massif, South Karelia
title_full_unstemmed Petrochemical characteristics and ore specialization of the Hautavaara massif, South Karelia
title_sort petrochemical characteristics and ore specialization of the hautavaara massif, south karelia
publisher Karelian Research Centre of the Russian Academy of Sciences
series Transactions of the Karelian Research Centre of the Russian Academy of Sciences
issn 1997-3217
2312-4504
publishDate 2015-12-01
description <p>The Hautavaara sanukitoid massif, located in the southern Vedlozero-Segozero greenstone belt, Karelia, is differentiated from monzogabbro to moderately alkaline granite. Its structure and the petrographic and petrochemical characteristics of all its rock types are discussed. The granosyenites are subjected to mean temperature variations and display Au-Mo-geochemical specialization. Gold-sulphide-quartz vein mineralization and molybdenite mineralization are confined to them.</p>
topic хаутаваарский санукитоидный массив
изменения пород
кварцевые жилы
золото
молибденит
url http://journals.krc.karelia.ru/index.php/precambrian/article/view/160
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