Zobrazeno 1 - 5
of 5
pro vyhledávání: '"Diming Yu"'
Publikováno v:
SEG Technical Program Expanded Abstracts 2018.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::29c2dea006f75a977692aae8b9daa05b
https://doi.org/10.1190/segam2018-2998119.1
https://doi.org/10.1190/segam2018-2998119.1
Autor:
Diming Yu, Randolph Martin, M. Nafi Toksöz, Mary L. Krasovec, Youshun Sun, Qingyun Liu, Jun Liu
Publikováno v:
Earthquake Science. 25:505-515
A 3-D P-wave velocity model is developed for the crust and uppermost mantle of Caucasus and the surrounding area by applying the tomographic method of Zhao et al. using 300 000 high-quality P-wave first arrivals from 43 000 events between 1964 and 20
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::34ae804bf4da4dcad61aa313b00006ce
https://doi.org/10.1007/s11589-012-0874-y
https://doi.org/10.1007/s11589-012-0874-y
Publikováno v:
Earthquake Science. 25:363-370
Based on teleseismic data obtained from 225 stations from two networks in the central Tibetan plateau, we have generated detailed crustal structure images using P-wave receiver function techniques with more accurate piercing-depth-correction and time
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::09867c6399f1564f6cf31908eeafc0dd
https://doi.org/10.1007/s11589-012-0862-2
https://doi.org/10.1007/s11589-012-0862-2
Publikováno v:
Seismological Society of China
We apply the adaptive moving window method of Sun et al. to the most recent catalog data and the data recorded by portable stations to construct the velocity structure of the crust and upper mantle, and to determine the depth of the Moho interface be
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9a8398757b7645503ea3bd4d87c1a098
https://doi.org/10.1007/s11589-012-0867-x
https://doi.org/10.1007/s11589-012-0867-x
Publikováno v:
Earthquake Science. 25:495-503
We have developed crustal minimum 1-D P- and S-wave velocity models of the collision zone between the northern Tianshan mountain and the Junggar basin (86°E–89°E, 43°N–44.5°N). These two models were created through inversion of 1 370 P- and 1
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f6a97c4b5018beaa394aafd3c169d776
https://doi.org/10.1007/s11589-012-0873-z
https://doi.org/10.1007/s11589-012-0873-z