STRUCTURAL FEATURES OF THE DEEP STRUCTURE OF THE SOUTHEASTERN YANA-KOLYMA FOLD SYSTEM FROM COMPLEX GEOPHYSICAL DATA

Ore deposits of the Magadan region are now in the focus of comprehensive studies as information on their deep structure is needed for both subsoil prospecting and regional development planning. This article presents the research results for the southeastern flank of the Yana-Kolyma orogenic belt. Th...

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Main Authors: N. K. Gayday, N. A. Goryachev, I. M. Khasanov, E. Yu. Goshko
Format: Article
Language:English
Published: Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust 2020-12-01
Series:Геодинамика и тектонофизика
Subjects:
Online Access:https://www.gt-crust.ru/jour/article/view/1119
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author N. K. Gayday
N. A. Goryachev
I. M. Khasanov
E. Yu. Goshko
author_facet N. K. Gayday
N. A. Goryachev
I. M. Khasanov
E. Yu. Goshko
author_sort N. K. Gayday
collection DOAJ
description Ore deposits of the Magadan region are now in the focus of comprehensive studies as information on their deep structure is needed for both subsoil prospecting and regional development planning. This article presents the research results for the southeastern flank of the Yana-Kolyma orogenic belt. This area located at the junction with the Okhotsk-Koryak orogenic belt was investigated using the northeastern segment of the regional geophysical profile 3-DV. We analyzed the frequency-energy sections of the crust along the profile, 3D crustal density model of the entire study area, and magnetic, geoelectric and gravimagnetic characteristics of the crust. Complex data interpretation allowed tracing the crustal fault zones, areas wherein the crust material was strongly reworked, and zones of quasi-horizontal stratification. Considering the revealed features of the physical parameters of the crust material, we conclude that the currently accepted boundaries of individual tectonic blocks in the study area need to be adjusted. The northern boundary of the Balygychan uplift should be mapped along the Pautov fault. The Srednekansky branch of the Inyali-Debinsky synclinorium should be considered a transitional block that belongs to the Sugoi synclinorium, and its name should be changed to the Orotukan block.
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spelling doaj.art-8144be9195f7428faaf7dc7c7fd4f4a82023-03-30T20:08:05ZengRussian Academy of Sciences, Siberian Branch, Institute of the Earth's crustГеодинамика и тектонофизика2078-502X2020-12-0111469770910.5800/GT-2020-11-4-0501499STRUCTURAL FEATURES OF THE DEEP STRUCTURE OF THE SOUTHEASTERN YANA-KOLYMA FOLD SYSTEM FROM COMPLEX GEOPHYSICAL DATAN. K. Gayday0N. A. Goryachev1I. M. Khasanov2E. Yu. Goshko3North-Eastern State University; Shilo North-East Interdisciplinary Scientific Research Institute, Far Eastern Branch of the Russian Academy of SciencesShilo North-East Interdisciplinary Scientific Research Institute, Far Eastern Branch of the Russian Academy of SciencesNorth-Eastern State University; Shilo North-East Interdisciplinary Scientific Research Institute, Far Eastern Branch of the Russian Academy of SciencesSiberian Research Institute of Geology, Geophysics and Mineral ResourcesOre deposits of the Magadan region are now in the focus of comprehensive studies as information on their deep structure is needed for both subsoil prospecting and regional development planning. This article presents the research results for the southeastern flank of the Yana-Kolyma orogenic belt. This area located at the junction with the Okhotsk-Koryak orogenic belt was investigated using the northeastern segment of the regional geophysical profile 3-DV. We analyzed the frequency-energy sections of the crust along the profile, 3D crustal density model of the entire study area, and magnetic, geoelectric and gravimagnetic characteristics of the crust. Complex data interpretation allowed tracing the crustal fault zones, areas wherein the crust material was strongly reworked, and zones of quasi-horizontal stratification. Considering the revealed features of the physical parameters of the crust material, we conclude that the currently accepted boundaries of individual tectonic blocks in the study area need to be adjusted. The northern boundary of the Balygychan uplift should be mapped along the Pautov fault. The Srednekansky branch of the Inyali-Debinsky synclinorium should be considered a transitional block that belongs to the Sugoi synclinorium, and its name should be changed to the Orotukan block.https://www.gt-crust.ru/jour/article/view/1119interpretationdensity sectionfrequency-energy sectiongeoelectric sectionmagmatismbalygychan upliftorotukan blockgeophysical reference profile
spellingShingle N. K. Gayday
N. A. Goryachev
I. M. Khasanov
E. Yu. Goshko
STRUCTURAL FEATURES OF THE DEEP STRUCTURE OF THE SOUTHEASTERN YANA-KOLYMA FOLD SYSTEM FROM COMPLEX GEOPHYSICAL DATA
Геодинамика и тектонофизика
interpretation
density section
frequency-energy section
geoelectric section
magmatism
balygychan uplift
orotukan block
geophysical reference profile
title STRUCTURAL FEATURES OF THE DEEP STRUCTURE OF THE SOUTHEASTERN YANA-KOLYMA FOLD SYSTEM FROM COMPLEX GEOPHYSICAL DATA
title_full STRUCTURAL FEATURES OF THE DEEP STRUCTURE OF THE SOUTHEASTERN YANA-KOLYMA FOLD SYSTEM FROM COMPLEX GEOPHYSICAL DATA
title_fullStr STRUCTURAL FEATURES OF THE DEEP STRUCTURE OF THE SOUTHEASTERN YANA-KOLYMA FOLD SYSTEM FROM COMPLEX GEOPHYSICAL DATA
title_full_unstemmed STRUCTURAL FEATURES OF THE DEEP STRUCTURE OF THE SOUTHEASTERN YANA-KOLYMA FOLD SYSTEM FROM COMPLEX GEOPHYSICAL DATA
title_short STRUCTURAL FEATURES OF THE DEEP STRUCTURE OF THE SOUTHEASTERN YANA-KOLYMA FOLD SYSTEM FROM COMPLEX GEOPHYSICAL DATA
title_sort structural features of the deep structure of the southeastern yana kolyma fold system from complex geophysical data
topic interpretation
density section
frequency-energy section
geoelectric section
magmatism
balygychan uplift
orotukan block
geophysical reference profile
url https://www.gt-crust.ru/jour/article/view/1119
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AT nagoryachev structuralfeaturesofthedeepstructureofthesoutheasternyanakolymafoldsystemfromcomplexgeophysicaldata
AT imkhasanov structuralfeaturesofthedeepstructureofthesoutheasternyanakolymafoldsystemfromcomplexgeophysicaldata
AT eyugoshko structuralfeaturesofthedeepstructureofthesoutheasternyanakolymafoldsystemfromcomplexgeophysicaldata