Structure of the lithosphere and its controls on gold mineralisation in Southeast Kamchatka
Since the eighties of the last century and up to the present time, a complex of geophysical methods including earthquake converted-waves method, magnetotelluric sounding, gravimetry, magnetometry and seismological have been implemented in southeast Kamchatka. Based on the complex interpretation of t...
| Main Authors: | , |
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| Format: | Article |
| Language: | Russian |
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Institute of Volcanology and Seismology FEB RAS
2023-09-01
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| Series: | Вестник Камчатской региональной ассоциации "Учебно-научный центр". Серия: Науки о Земле |
| Subjects: | |
| Online Access: | http://www.kscnet.ru/journal/kraesc/article/view/766 |
| _version_ | 1797671516847996928 |
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| author | A.G. Nurmukhamedov M.D. Sidorov |
| author_facet | A.G. Nurmukhamedov M.D. Sidorov |
| author_sort | A.G. Nurmukhamedov |
| collection | DOAJ |
| description | Since the eighties of the last century and up to the present time, a complex of geophysical methods including earthquake converted-waves method, magnetotelluric sounding, gravimetry, magnetometry and seismological have been implemented in southeast Kamchatka. Based on the complex interpretation of the data obtained, a geological and geophysical model of the Earth's crust and upper mantle along the bay profile of Khodutka Bay – Nikolaevka village was constructed. Genetic relationship between active areas of the Earth's crust and gold deposits was established. The hypothesis of division of the formerly unified xenoblock into two separate fragments under the impact of shear along the Nachikinskaya zone of transverse dislocations has been suggested. The southern fragment is represented by the Coastal terrane. To the west of the terrane is a permeable zone with modern volcanism. Intrusion of magma and high-temperature fluids enriched with noble metals into the upper crustal layers occurs along the magmatic channel formed in the paleosubduction zone. |
| first_indexed | 2024-03-11T21:15:43Z |
| format | Article |
| id | doaj.art-2e9e31d4a9be4ef3bde6caa14b1a0cf1 |
| institution | Directory Open Access Journal |
| issn | 1816-5524 1816-5532 |
| language | Russian |
| last_indexed | 2024-03-11T21:15:43Z |
| publishDate | 2023-09-01 |
| publisher | Institute of Volcanology and Seismology FEB RAS |
| record_format | Article |
| series | Вестник Камчатской региональной ассоциации "Учебно-научный центр". Серия: Науки о Земле |
| spelling | doaj.art-2e9e31d4a9be4ef3bde6caa14b1a0cf12023-09-28T23:02:00ZrusInstitute of Volcanology and Seismology FEB RASВестник Камчатской региональной ассоциации "Учебно-научный центр". Серия: Науки о Земле1816-55241816-55322023-09-01593204110.31431/1816-5524-2023-3-59-20-411047Structure of the lithosphere and its controls on gold mineralisation in Southeast KamchatkaA.G. Nurmukhamedov0M.D. Sidorov1Research Geotechnological Center of Far Eastern Branch of Russian Academy of Sciences, Petropavlovsk-Kamchatsky, RussiaResearch Geotechnological Center of Far Eastern Branch of Russian Academy of Sciences, Petropavlovsk-Kamchatsky, RussiaSince the eighties of the last century and up to the present time, a complex of geophysical methods including earthquake converted-waves method, magnetotelluric sounding, gravimetry, magnetometry and seismological have been implemented in southeast Kamchatka. Based on the complex interpretation of the data obtained, a geological and geophysical model of the Earth's crust and upper mantle along the bay profile of Khodutka Bay – Nikolaevka village was constructed. Genetic relationship between active areas of the Earth's crust and gold deposits was established. The hypothesis of division of the formerly unified xenoblock into two separate fragments under the impact of shear along the Nachikinskaya zone of transverse dislocations has been suggested. The southern fragment is represented by the Coastal terrane. To the west of the terrane is a permeable zone with modern volcanism. Intrusion of magma and high-temperature fluids enriched with noble metals into the upper crustal layers occurs along the magmatic channel formed in the paleosubduction zone.http://www.kscnet.ru/journal/kraesc/article/view/766paleo-kamchatkaearth's crustupper mantlesubductionterraneore occurrence |
| spellingShingle | A.G. Nurmukhamedov M.D. Sidorov Structure of the lithosphere and its controls on gold mineralisation in Southeast Kamchatka Вестник Камчатской региональной ассоциации "Учебно-научный центр". Серия: Науки о Земле paleo-kamchatka earth's crust upper mantle subduction terrane ore occurrence |
| title | Structure of the lithosphere and its controls on gold mineralisation in Southeast Kamchatka |
| title_full | Structure of the lithosphere and its controls on gold mineralisation in Southeast Kamchatka |
| title_fullStr | Structure of the lithosphere and its controls on gold mineralisation in Southeast Kamchatka |
| title_full_unstemmed | Structure of the lithosphere and its controls on gold mineralisation in Southeast Kamchatka |
| title_short | Structure of the lithosphere and its controls on gold mineralisation in Southeast Kamchatka |
| title_sort | structure of the lithosphere and its controls on gold mineralisation in southeast kamchatka |
| topic | paleo-kamchatka earth's crust upper mantle subduction terrane ore occurrence |
| url | http://www.kscnet.ru/journal/kraesc/article/view/766 |
| work_keys_str_mv | AT agnurmukhamedov structureofthelithosphereanditscontrolsongoldmineralisationinsoutheastkamchatka AT mdsidorov structureofthelithosphereanditscontrolsongoldmineralisationinsoutheastkamchatka |