東華大學圖書館 |

語系: 繁體中文

說明(常見問題)

回圖書館首頁

手機版館藏查詢

登入

回首頁

切換: 標籤 | MARC模式 | ISBD

The dynamics of geometrically comple...

Duan, Benchun.

FindBook

Google Book

Amazon

博客來

The dynamics of geometrically complex fault systems over multiple earthquake cycles.

紀錄類型:	書目-語言資料,印刷品 : Monograph/item
正題名/作者:	The dynamics of geometrically complex fault systems over multiple earthquake cycles./
作者:	Duan, Benchun.
面頁冊數:	234 p.
附註:	Adviser: David D. Oglesby.
Contained By:	Dissertation Abstracts International67-07B.
標題:	Geophysics. -
電子資源:	http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=3226534
ISBN:	9780542800559

The dynamics of geometrically complex fault systems over multiple earthquake cycles.
Duan, Benchun.

The dynamics of geometrically complex fault systems over multiple earthquake cycles. - 234 p.

Adviser: David D. Oglesby.

Thesis (Ph.D.)--University of California, Riverside, 2006.

Earthquake faults are geometrically complex, being segmented, bent and bifurcated. Understanding earthquake rupture processes on these fault systems is crucial to characterize source effects on resulting ground motion and to assess the possibility of rupture progressing across geometrical discontinuities to cascade into a large earthquake. However, most previous studies on this subject focus on a single earthquake with an ad hoc assumed initial stress on faults, which is one of most important components for dynamic faulting models. In this dissertation, I explore fault geometry effects on dynamic rupture processes and resulting ground motion in the context of multiple earthquake cycles. The earthquake cycle is modeled to consist of two phases: the coseismic dynamic rupture and the interseismic period. For coseismic processes, I use the finite element method to numerically simulate spontaneous rupture propagation on faults and wave propagation in the medium. I use approximate approaches to track fault stress evolution during interseismic periods. Thus, the initial stress on faults before an earthquake is a combined result of both tectonic loading and residual stresses from previous earthquakes. I examine dip-slip faults and strike-slip faults with bends, stepovers, or branches. I find that heterogeneous stresses develop on these faults over multiple earthquake cycles. These heterogeneous stresses have significant effects on the dynamic rupture process. A low normal stress developed from previous events near geometrical complexities facilitates rupture to initiate near these locations, and to jump across geometrical discontinuities. On the other hand, the high normal stress that can also develop near these locations can stop rupture. These heterogeneous stresses can allow rupture to jump larger offsets than has been previously proposed. They also allow rupture to propagate through complex paths that would be difficult to be understood in a uniform regional stress field. Fault systems with limited geometrical complexity evolve to a steady state after a number of earthquake cycles, with several typical patterns of initial stress distribution and earthquake rupture alternating in sequential earthquakes. Results from this dissertation advance our understanding of earthquake source processes on geometrically complex fault systems and may have important implications for seismic hazard analysis.

ISBN: 9780542800559Subjects--Topical Terms:

535228
Geophysics.

The dynamics of geometrically complex fault systems over multiple earthquake cycles.
LDR:03312nam 2200265 a 45 001 967169
005 20110915
008 110915s2006 eng d
020 $a 9780542800559
035 $a (UnM)AAI3226534
035 $a AAI3226534
040 $a UnM $c UnM
100 1 $a Duan, Benchun. $3 1291054
245 1 4 $a The dynamics of geometrically complex fault systems over multiple earthquake cycles.
300 $a 234 p.
500 $a Adviser: David D. Oglesby.
500 $a Source: Dissertation Abstracts International, Volume: 67-07, Section: B, page: 3659.
502 $a Thesis (Ph.D.)--University of California, Riverside, 2006.
520 $a Earthquake faults are geometrically complex, being segmented, bent and bifurcated. Understanding earthquake rupture processes on these fault systems is crucial to characterize source effects on resulting ground motion and to assess the possibility of rupture progressing across geometrical discontinuities to cascade into a large earthquake. However, most previous studies on this subject focus on a single earthquake with an ad hoc assumed initial stress on faults, which is one of most important components for dynamic faulting models. In this dissertation, I explore fault geometry effects on dynamic rupture processes and resulting ground motion in the context of multiple earthquake cycles. The earthquake cycle is modeled to consist of two phases: the coseismic dynamic rupture and the interseismic period. For coseismic processes, I use the finite element method to numerically simulate spontaneous rupture propagation on faults and wave propagation in the medium. I use approximate approaches to track fault stress evolution during interseismic periods. Thus, the initial stress on faults before an earthquake is a combined result of both tectonic loading and residual stresses from previous earthquakes. I examine dip-slip faults and strike-slip faults with bends, stepovers, or branches. I find that heterogeneous stresses develop on these faults over multiple earthquake cycles. These heterogeneous stresses have significant effects on the dynamic rupture process. A low normal stress developed from previous events near geometrical complexities facilitates rupture to initiate near these locations, and to jump across geometrical discontinuities. On the other hand, the high normal stress that can also develop near these locations can stop rupture. These heterogeneous stresses can allow rupture to jump larger offsets than has been previously proposed. They also allow rupture to propagate through complex paths that would be difficult to be understood in a uniform regional stress field. Fault systems with limited geometrical complexity evolve to a steady state after a number of earthquake cycles, with several typical patterns of initial stress distribution and earthquake rupture alternating in sequential earthquakes. Results from this dissertation advance our understanding of earthquake source processes on geometrically complex fault systems and may have important implications for seismic hazard analysis.
590 $a School code: 0032.
650 4 $a Geophysics. $3 535228
690 $a 0373
710 2 0 $a University of California, Riverside. $3 791122
773 0 $t Dissertation Abstracts International $g 67-07B.
790 $a 0032
790 1 0 $a Oglesby, David D., $e advisor
791 $a Ph.D.
792 $a 2006
856 4 0 $u http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=3226534