Structural peculiarities and metallogeny of the Gonzha Salient according to geological and geophysical research data

The article reviews and summarizes the data of regional and large-scale geological and geophysical works by JSC Dalgeofizika, Institute of Tectonics and Geophysics, and other organizations within the Gonzha Salient and its framing. Based on results of these studies, specific features of the deep str...

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Main Authors: Kopylov M. I., Petukhova L. L.
Format: Article
Language:English
Published: Central Research Institute of Geological Prospecting for Base and Precious Metals (TsNIGRI) 2024-12-01
Series:Руды и металлы
Subjects:
Online Access:https://rm.tsnigri.ru/index.php/main/article/view/251
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author Kopylov M. I.
Petukhova L. L.
author_facet Kopylov M. I.
Petukhova L. L.
author_sort Kopylov M. I.
collection DOAJ
description The article reviews and summarizes the data of regional and large-scale geological and geophysical works by JSC Dalgeofizika, Institute of Tectonics and Geophysics, and other organizations within the Gonzha Salient and its framing. Based on results of these studies, specific features of the deep structure and regularities in distribution of the ore mineralization were determined and geodynamic models of the Gonzha Salient formation were presented. The Gonzha Salient is composed of intrusive-metamorphic rocks of the Gonzha Series represented by various gneisses, amphibolites, and quartzites. The deformed cover of the Lower Cambrian Gonzha Salient comprises Riphean–Lower Cambrian metamorphosed sandstones, siltstones, carbonaceous-cherty and micaceous schists and Silurian-Devonian-Carboniferous terrigenouscarbonate deposits mainly of the Upper Amur Series. The uplifted basement block with the most ancient rocks is framed by Paleozoic and Mesozoic structures. Fields of hydrothermal alterations are localized in nodes that form ring-shaped structures around blocks of the metamorphic basement. It is characteristic that the ore clusters are significantly tend to be confined to known volcanic and volcano-plutonic centers. Descriptions are presented of the main ore clusters (Inim, Gonzha, Taldan, Pokrovka, Igak) and of a number of ore deposits.
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institution Kabale University
issn 0869-5997
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language English
publishDate 2024-12-01
publisher Central Research Institute of Geological Prospecting for Base and Precious Metals (TsNIGRI)
record_format Article
series Руды и металлы
spelling doaj-art-87813e63414142ffac48d54d20e8fffd2025-02-05T08:54:06ZengCentral Research Institute of Geological Prospecting for Base and Precious Metals (TsNIGRI)Руды и металлы0869-59972782-554X2024-12-014667710.47765/0869-5997-2024-10018Structural peculiarities and metallogeny of the Gonzha Salient according to geological and geophysical research dataKopylov M. I.0Petukhova L. L.1Yu. A. Kosygin Institute of Tectonics and Geophysics, FEB RAS, Khabarovsk, RussiaYu. A. Kosygin Institute of Tectonics and Geophysics, FEB RAS, Khabarovsk, RussiaThe article reviews and summarizes the data of regional and large-scale geological and geophysical works by JSC Dalgeofizika, Institute of Tectonics and Geophysics, and other organizations within the Gonzha Salient and its framing. Based on results of these studies, specific features of the deep structure and regularities in distribution of the ore mineralization were determined and geodynamic models of the Gonzha Salient formation were presented. The Gonzha Salient is composed of intrusive-metamorphic rocks of the Gonzha Series represented by various gneisses, amphibolites, and quartzites. The deformed cover of the Lower Cambrian Gonzha Salient comprises Riphean–Lower Cambrian metamorphosed sandstones, siltstones, carbonaceous-cherty and micaceous schists and Silurian-Devonian-Carboniferous terrigenouscarbonate deposits mainly of the Upper Amur Series. The uplifted basement block with the most ancient rocks is framed by Paleozoic and Mesozoic structures. Fields of hydrothermal alterations are localized in nodes that form ring-shaped structures around blocks of the metamorphic basement. It is characteristic that the ore clusters are significantly tend to be confined to known volcanic and volcano-plutonic centers. Descriptions are presented of the main ore clusters (Inim, Gonzha, Taldan, Pokrovka, Igak) and of a number of ore deposits.https://rm.tsnigri.ru/index.php/main/article/view/251gonzha salientgoldsilvermetasomatitesore depositsore occurrencesprospectingmagnetic explorationelectrical explorationgravity exploration
spellingShingle Kopylov M. I.
Petukhova L. L.
Structural peculiarities and metallogeny of the Gonzha Salient according to geological and geophysical research data
Руды и металлы
gonzha salient
gold
silver
metasomatites
ore deposits
ore occurrences
prospecting
magnetic exploration
electrical exploration
gravity exploration
title Structural peculiarities and metallogeny of the Gonzha Salient according to geological and geophysical research data
title_full Structural peculiarities and metallogeny of the Gonzha Salient according to geological and geophysical research data
title_fullStr Structural peculiarities and metallogeny of the Gonzha Salient according to geological and geophysical research data
title_full_unstemmed Structural peculiarities and metallogeny of the Gonzha Salient according to geological and geophysical research data
title_short Structural peculiarities and metallogeny of the Gonzha Salient according to geological and geophysical research data
title_sort structural peculiarities and metallogeny of the gonzha salient according to geological and geophysical research data
topic gonzha salient
gold
silver
metasomatites
ore deposits
ore occurrences
prospecting
magnetic exploration
electrical exploration
gravity exploration
url https://rm.tsnigri.ru/index.php/main/article/view/251
work_keys_str_mv AT kopylovmi structuralpeculiaritiesandmetallogenyofthegonzhasalientaccordingtogeologicalandgeophysicalresearchdata
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