A New Approach to the Study of the Block Geoelectric Structure of the Lithosphere and Fluid-Saturated Fragments of Faults as Indicators of Zones with Increased Seismicity According to Magnetotelluric Sounding Data for Southern Sakhalin
Autor: | V. B. Kaplun, A. Yu. Zhukovin, V. M. Nikiforov, G. N. Shkabarnya, Yu. V. Taltykin |
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Rok vydání: | 2018 |
Předmět: |
geography
geography.geographical_feature_category 010504 meteorology & atmospheric sciences Stratigraphy Triple junction Flow (psychology) Paleontology Geology Crust Induced seismicity Fault (geology) 010502 geochemistry & geophysics Oceanography Block (meteorology) 01 natural sciences Geophysics Geochemistry and Petrology Lithosphere Magnetotellurics Seismology 0105 earth and related environmental sciences |
Zdroj: | Russian Journal of Pacific Geology. 12:278-288 |
ISSN: | 1819-7159 1819-7140 |
DOI: | 10.1134/s1819714018040048 |
Popis: | Large steeply dipping geoelectrical structures penetrating the whole lithosphere and extending deeply beneath it are detected on Sakhalin Island by magnetotelluric soundings. The fault system that forms this structure contributes to the flow of telluric currents from the deep horizons of the tectonosphere to the near-surface layers. As a result, the electrical component across the strike of the structure is very sensitive to the presence of conducive galvanically coupled vertical and horizontal elements (objects) in the section through which currents flow. This phenomenon provides the basis for a new approach to a detailed study of the block structure of the lithosphere and its upper part, the Earth’s crust. Based on this effect, which has not been studied earlier in the magnetotelluric works, the block structure of the Earth’s crust on southern Sakhalin is examined. It is found that the interblock joints characterized by a relatively low level of specific electrical resistivity, which indicates their fluid saturation, are fragments of regional or higher-order faults. The location of the foci of crustal earthquakes is closely related to these fragments. It is shown that the urban district of Yuzhno-Sakhalinsk is situated in the area of a triple junction of geoelectrical blocks in the Earth’s crust. |
Databáze: | OpenAIRE |
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