Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
Fault structures and their geoelectric parameters in the epicentral zone of the 27 September 2003 Chuya earthquake (Gorny Altai) from resistivity data. / Nevedrova, N. N.; Deev, E. V.; Ponomarev, P. V.
в: Russian Geology and Geophysics, Том 58, № 1, 01.01.2017, стр. 123-132.Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
}
TY - JOUR
T1 - Fault structures and their geoelectric parameters in the epicentral zone of the 27 September 2003 Chuya earthquake (Gorny Altai) from resistivity data
AU - Nevedrova, N. N.
AU - Deev, E. V.
AU - Ponomarev, P. V.
PY - 2017/1/1
Y1 - 2017/1/1
N2 - This paper presents an integrated measurement technique based on DC methods (vertical electrical sounding, electrical resistivity tomography) which was used to identify faults and determine their geoelectric parameters in the western part of the Chuya basin. New information on the structure of the Chagan River valley located in the zone of the disastrous 27 September 2003 Chuya earthquake has been obtained from the results of these methods. Geoelectric cross-sections of the sedimentary sequence and the upper part of the basement were obtained from VES data, showing the block structure of the study area. Electrical resistivity tomography sections confirm the presence of a major fault between basement blocks of different heights and indicate the presence of faults bounding the valley on its right side and in the southwestern part.
AB - This paper presents an integrated measurement technique based on DC methods (vertical electrical sounding, electrical resistivity tomography) which was used to identify faults and determine their geoelectric parameters in the western part of the Chuya basin. New information on the structure of the Chagan River valley located in the zone of the disastrous 27 September 2003 Chuya earthquake has been obtained from the results of these methods. Geoelectric cross-sections of the sedimentary sequence and the upper part of the basement were obtained from VES data, showing the block structure of the study area. Electrical resistivity tomography sections confirm the presence of a major fault between basement blocks of different heights and indicate the presence of faults bounding the valley on its right side and in the southwestern part.
KW - Chagan River valley
KW - electrical resistivity tomography
KW - geoelectric parameters of fault zones
KW - vertical electrical soundings
KW - DEEP-STRUCTURE
UR - http://www.scopus.com/inward/record.url?scp=85013226532&partnerID=8YFLogxK
U2 - 10.1016/j.rgg.2016.01.021
DO - 10.1016/j.rgg.2016.01.021
M3 - Article
AN - SCOPUS:85013226532
VL - 58
SP - 123
EP - 132
JO - Russian Geology and Geophysics
JF - Russian Geology and Geophysics
SN - 1068-7971
IS - 1
ER -
ID: 10309968