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Regional seismic wave attenuation in...
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Ranasinghe, Nishath Rajiv.
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Regional seismic wave attenuation in Northeast China.
紀錄類型:
書目-電子資源 : Monograph/item
正題名/作者:
Regional seismic wave attenuation in Northeast China./
作者:
Ranasinghe, Nishath Rajiv.
出版者:
Ann Arbor : ProQuest Dissertations & Theses, : 2016,
面頁冊數:
163 p.
附註:
Source: Dissertation Abstracts International, Volume: 78-07(E), Section: B.
Contained By:
Dissertation Abstracts International78-07B(E).
標題:
Geophysics. -
電子資源:
http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=10582976
ISBN:
9781369612172
Regional seismic wave attenuation in Northeast China.
Ranasinghe, Nishath Rajiv.
Regional seismic wave attenuation in Northeast China.
- Ann Arbor : ProQuest Dissertations & Theses, 2016 - 163 p.
Source: Dissertation Abstracts International, Volume: 78-07(E), Section: B.
Thesis (Ph.D.)--New Mexico State University, 2016.
The Northeast (NE) China is a geologically complex as well as a geopolitically sensitive region. The region is currently undergoing compression and intraplate continental magmatism. Regional seismic wave attenuation is an important indirect indicator of crustal temperature and rheology.
ISBN: 9781369612172Subjects--Topical Terms:
535228
Geophysics.
Regional seismic wave attenuation in Northeast China.
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The Northeast (NE) China is a geologically complex as well as a geopolitically sensitive region. The region is currently undergoing compression and intraplate continental magmatism. Regional seismic wave attenuation is an important indirect indicator of crustal temperature and rheology.
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Lg attenuation at 1 Hz was initially studied implementing Reverse Two Station/Event Method (RTM) using data derived from 78 crustal earthquakes that were recorded by NECESSArray. High Lg Q0 values were observed in the Great Xing'an, Lesser Xing'an and Songen-Zhangguangcai Ranges and low Lg Q0 values were observed in Songliao, Sanjiang and Erlian Basins and the lowest Lg Q0 values were observed in Holocene volcanic fields such as Wudalianchi.
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Pg attenuation maps with 3° by 3° resolution were obtained at a central frequency of 1 Hz using TSM and RTSM. The both Pg attenuation map shows high attenuation (Q < 400) throughout NE including Songliao Basin, Erlian Basin, and Sanjiang Basin and also in Holocene volcanic fields such as Wudalianchi Volcanic field.
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Lg attenuation images with 2°x 2° resolution were produced implementing both TSM and RTSM at several narrow bandwidths with central frequencies of 0.5, 1, 2 and 3 Hz. Lg attenuation images produced at low frequencies (≤1 Hz) utilizing both TSM and RTSM, show low Lg Q values in basins and high Lg Q values in the mountain ranges. However, at higher frequencies (≥ 2 Hz) both basins and mountain ranges show high Lg Q values. RTSM consistently show higher Lg Q values than the TSM while both methods show similar frequency dependent factors (n) of 0.49 and 0.46 for TSM and RTSM, respectively.
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Pg site responses were calculated at 1 Hz show amplification in Erlian, Hailar and Songliao Basins and deamplification in Sanjiang Basin, Lesser Xing'an Range and Songen-Zhangguangcai Ranges. Lg site responses calculated at central frequencies of 0.5, 1, 2 and 3 Hz show high degree of lateral variation as well as frequency dependence. At low frequencies (≤ 1 Hz) almost all the seismic stations in the sedimentary basins show amplification and at higher frequencies (≥ 2 Hz) seismic stations in Lesser Xing'an and Songen-Zhangguangcai Ranges show deamplification.
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