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

Constraining the near tip stresses a...

Barbery, Monica.

FindBook

Google Book

Amazon

博客來

Constraining the near tip stresses around propagating earthquake ruptures: Frictional response and off fault tensile crack development.

紀錄類型:	書目-電子資源 : Monograph/item
正題名/作者:	Constraining the near tip stresses around propagating earthquake ruptures: Frictional response and off fault tensile crack development./
作者:	Barbery, Monica.
面頁冊數:	99 p.
附註:	Source: Masters Abstracts International, Volume: 54-05.
Contained By:	Masters Abstracts International54-05(E).
標題:	Geology. -
電子資源:	http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=1592114
ISBN:	9781321853728

Constraining the near tip stresses around propagating earthquake ruptures: Frictional response and off fault tensile crack development.
Barbery, Monica.

Constraining the near tip stresses around propagating earthquake ruptures: Frictional response and off fault tensile crack development. - 99 p.

Source: Masters Abstracts International, Volume: 54-05.

Thesis (M.S.)--The University of Texas at Arlington, 2015.

The near-tip stress, strain, and displacement fields around propagating ruptures are complicated, transient, and depend heavily on the evolution of the shear traction along the advancing rupture. This shear traction evolution is in turn influenced by dynamic weakening of the coefficient of friction. I have investigated near tip rupture mechanics using two approaches. In the first approach, I conduct experiments using a novel torsional Kolsky bar apparatus to investigate the frictional evolution of synthetic rock gouges at pressures, accelerations, and slip velocities expected to be operating in the seismogenic zone where most earthquakes nucleate. Microstructural analysis and 1-D thermal modeling is conducted to explore the observed dynamic weakening of friction, and in particular the inferred mechanism of flash heating at asperity contacts. In the second approach, I examine length and spacing distributions of naturally occurring pseudotachylite injection veins and experimentally generated tensile microcracks to elucidate the mechanical interaction between mode I cracks within the transient near-tip stress field. As a rupture propagates, stress perturbations result in the formation of a tensile zone directly behind the rupture tip where fractures develop and fracture length is governed by stress shadowing of nearby fractures.

ISBN: 9781321853728Subjects--Topical Terms:

516570
Geology.

Constraining the near tip stresses around propagating earthquake ruptures: Frictional response and off fault tensile crack development.
LDR:02266nmm a2200277 4500 001 2069297
005 20160513093613.5
008 170521s2015 ||||||||||||||||| ||eng d
020 $a 9781321853728
035 $a (MiAaPQ)AAI1592114
035 $a AAI1592114
040 $a MiAaPQ $c MiAaPQ
100 1 $a Barbery, Monica. $3 3184303
245 1 0 $a Constraining the near tip stresses around propagating earthquake ruptures: Frictional response and off fault tensile crack development.
300 $a 99 p.
500 $a Source: Masters Abstracts International, Volume: 54-05.
500 $a Adviser: W. Ashley Griffith.
502 $a Thesis (M.S.)--The University of Texas at Arlington, 2015.
520 $a The near-tip stress, strain, and displacement fields around propagating ruptures are complicated, transient, and depend heavily on the evolution of the shear traction along the advancing rupture. This shear traction evolution is in turn influenced by dynamic weakening of the coefficient of friction. I have investigated near tip rupture mechanics using two approaches. In the first approach, I conduct experiments using a novel torsional Kolsky bar apparatus to investigate the frictional evolution of synthetic rock gouges at pressures, accelerations, and slip velocities expected to be operating in the seismogenic zone where most earthquakes nucleate. Microstructural analysis and 1-D thermal modeling is conducted to explore the observed dynamic weakening of friction, and in particular the inferred mechanism of flash heating at asperity contacts. In the second approach, I examine length and spacing distributions of naturally occurring pseudotachylite injection veins and experimentally generated tensile microcracks to elucidate the mechanical interaction between mode I cracks within the transient near-tip stress field. As a rupture propagates, stress perturbations result in the formation of a tensile zone directly behind the rupture tip where fractures develop and fracture length is governed by stress shadowing of nearby fractures.
590 $a School code: 2502.
650 4 $a Geology. $3 516570
650 4 $a Geophysics. $3 535228
690 $a 0372
690 $a 0373
710 2 $a The University of Texas at Arlington. $b Environmental and Earth Science. $3 3173801
773 0 $t Masters Abstracts International $g 54-05(E).
790 $a 2502
791 $a M.S.
792 $a 2015
793 $a English
856 4 0 $u http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=1592114