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

Earthquake early warning and the phy...

Wurman, Gilead.

FindBook

Google Book

Amazon

博客來

Earthquake early warning and the physics of earthquake rupture.

紀錄類型:	書目-語言資料,印刷品 : Monograph/item
正題名/作者:	Earthquake early warning and the physics of earthquake rupture./
作者:	Wurman, Gilead.
面頁冊數:	97 p.
附註:	Source: Dissertation Abstracts International, Volume: 71-09, Section: B, page: 5334.
Contained By:	Dissertation Abstracts International71-09B.
標題:	Geophysics. -
電子資源:	http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=3413524
ISBN:	9781124142258

Earthquake early warning and the physics of earthquake rupture.
Wurman, Gilead.

Earthquake early warning and the physics of earthquake rupture. - 97 p.

Source: Dissertation Abstracts International, Volume: 71-09, Section: B, page: 5334.

Thesis (Ph.D.)--University of California, Berkeley, 2010.

One of the great debates in seismology today revolves around the question of whether earthquake ruptures are self-similar, cascading failures, or whether their size is somehow predetermined at the start of the rupture. If earthquakes are self-similar there is theoretically no way to determine the magnitude of an event until the rupture has completely terminated, while if it is deterministic the magnitude should be immediately discernible. Recent advances in Earthquake Early Warning methodologies provide new insight into the fundamental physics of earthquake rupture and highlight the importance of understanding the answer to this question.

ISBN: 9781124142258Subjects--Topical Terms:

535228
Geophysics.

Earthquake early warning and the physics of earthquake rupture.
LDR:03690nam 2200337 4500 001 1395982
005 20110527105439.5
008 130515s2010 ||||||||||||||||| ||eng d
020 $a 9781124142258
035 $a (UMI)AAI3413524
035 $a AAI3413524
040 $a UMI $c UMI
100 1 $a Wurman, Gilead. $3 1674730
245 1 0 $a Earthquake early warning and the physics of earthquake rupture.
300 $a 97 p.
500 $a Source: Dissertation Abstracts International, Volume: 71-09, Section: B, page: 5334.
500 $a Adviser: Richard M. Allen.
502 $a Thesis (Ph.D.)--University of California, Berkeley, 2010.
520 $a One of the great debates in seismology today revolves around the question of whether earthquake ruptures are self-similar, cascading failures, or whether their size is somehow predetermined at the start of the rupture. If earthquakes are self-similar there is theoretically no way to determine the magnitude of an event until the rupture has completely terminated, while if it is deterministic the magnitude should be immediately discernible. Recent advances in Earthquake Early Warning methodologies provide new insight into the fundamental physics of earthquake rupture and highlight the importance of understanding the answer to this question.
520 $a Observations of the amplitude and frequency content of early P-wave arrivals suggest that some information about the final size of an earthquake is already present within a few seconds of the initiation of rupture, in agreement with a host of other observations that show a degree of scaling between large and small earthquakes. While this suggests that earthquakes are deterministic, there is likewise a large body of work, both observational and model-based, that indicates that this is not true and earthquakes are self-similar.
520 $a This work documents the process of calibrating and testing the ElarmS Earthquake Early Warning methodology in northern California on the Northern California and Berkeley Digital Seismic Networks. In the process the work adds to the body of observations which show a dependency on event magnitude of P-wave frequency content and amplitude. These observations are corroborated with a new set of independent observations of kinematic slip distributions. These new observations indicate that the early slip on a fault also scales with magnitude and suggest again that earthquakes are not entirely self-similar cascading events.
520 $a In an effort to assign a physical mechanism to the observations of scaling, both in P-waves and in kinematic slip inversions, a hypothetical model is tested wherein the intensity of the early rupture imparts more or less energy to the rupture front and affects the likelihood of the rupture continuing or dying out in the face of unfavorable conditions further along the fault plane. The results of testing this hypothesis are somewhat equivocal, but they are suggestive of the likely truth, that earthquakes exhibit aspects of both deterministic and cascading rupture to some degree. Understanding the details of the interplay between these two aspects is crucial to the successful application of Earthquake Early Warning systems, especially in rare large earthquakes for which there is little empirical data on the performance of these systems.
590 $a School code: 0028.
650 4 $a Geophysics. $3 535228
650 4 $a Engineering, Geophysical. $3 1674107
690 $a 0373
690 $a 0467
710 2 $a University of California, Berkeley. $b Earth & Planetary Science. $3 1035733
773 0 $t Dissertation Abstracts International $g 71-09B.
790 1 0 $a Allen, Richard M., $e advisor
790 1 0 $a Dreger, Douglas S. $e committee member
790 1 0 $a Glaser, Steven D. $e committee member
790 $a 0028
791 $a Ph.D.
792 $a 2010
856 4 0 $u http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=3413524