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Forearc Stresses in the Northern Cas...

Rippke, Joseph.

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Forearc Stresses in the Northern Cascadia Subduction Zone.

紀錄類型:	書目-電子資源 : Monograph/item
正題名/作者:	Forearc Stresses in the Northern Cascadia Subduction Zone./
作者:	Rippke, Joseph.
出版者:	Ann Arbor : ProQuest Dissertations & Theses, : 2020,
面頁冊數:	58 p.
附註:	Source: Masters Abstracts International, Volume: 82-05.
Contained By:	Masters Abstracts International82-05.
標題:	Geophysics. -
電子資源:	https://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=28092758
ISBN:	9798678179760

Forearc Stresses in the Northern Cascadia Subduction Zone.
Rippke, Joseph.

Forearc Stresses in the Northern Cascadia Subduction Zone. - Ann Arbor : ProQuest Dissertations & Theses, 2020 - 58 p.

Source: Masters Abstracts International, Volume: 82-05.

Thesis (M.S.)--University of Minnesota, 2020.

This item must not be sold to any third party vendors.

We investigate the spatial variation in the state of stress in the overriding plate in the forearc region of northern Cascadia. The key forces that act on the forearc region are the plate coupling force, the northward push of the Oregon block, the gravitational collapse force on elevated topography, and buoyancy of the serpentinized mantle wedge. The latter two forces are expected to cause margin-normal tension at shallow depths in the inner forearc. In this study, we compile available earthquake focal mechanism solutions and determine spatial variations of stress orientation through focal mechanism inversion. The results indicate the maximum compressive stress axis is margin-normal in the outer forearc due to shear stress at the subduction interface and margin-parallel throughout the inner forearc with varying orientations of the intermediate and minimum compressive stress axes throughout the inner forearc, consistent with previous studies. Using a 3-D finite-element code for lithospheric deformation, we explore the effects of gravitational collapse force, the buoyancy of the serpentinized mantle wedge corner, the plate coupling force, the shape of the slab, and the Oregon push on the stress field. The results indicate the buoyancy of the serpentinized mantle wedge corner and the shape of the slab may be as important of contributors to the the state of stress in the inner forearc as the plate coupling force whereas the gravitational collapse force and the Oregon push have a minimal effect on the state of stress in the inner forearc.

ISBN: 9798678179760Subjects--Topical Terms:

535228
Geophysics.
Subjects--Index Terms:

Forearc

Forearc Stresses in the Northern Cascadia Subduction Zone.
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245 1 0 $a Forearc Stresses in the Northern Cascadia Subduction Zone.
260 1 $a Ann Arbor : $b ProQuest Dissertations & Theses, $c 2020
300 $a 58 p.
500 $a Source: Masters Abstracts International, Volume: 82-05.
500 $a Advisor: Wada, Ikuko.
502 $a Thesis (M.S.)--University of Minnesota, 2020.
506 $a This item must not be sold to any third party vendors.
520 $a We investigate the spatial variation in the state of stress in the overriding plate in the forearc region of northern Cascadia. The key forces that act on the forearc region are the plate coupling force, the northward push of the Oregon block, the gravitational collapse force on elevated topography, and buoyancy of the serpentinized mantle wedge. The latter two forces are expected to cause margin-normal tension at shallow depths in the inner forearc. In this study, we compile available earthquake focal mechanism solutions and determine spatial variations of stress orientation through focal mechanism inversion. The results indicate the maximum compressive stress axis is margin-normal in the outer forearc due to shear stress at the subduction interface and margin-parallel throughout the inner forearc with varying orientations of the intermediate and minimum compressive stress axes throughout the inner forearc, consistent with previous studies. Using a 3-D finite-element code for lithospheric deformation, we explore the effects of gravitational collapse force, the buoyancy of the serpentinized mantle wedge corner, the plate coupling force, the shape of the slab, and the Oregon push on the stress field. The results indicate the buoyancy of the serpentinized mantle wedge corner and the shape of the slab may be as important of contributors to the the state of stress in the inner forearc as the plate coupling force whereas the gravitational collapse force and the Oregon push have a minimal effect on the state of stress in the inner forearc.
590 $a School code: 0130.
650 4 $a Geophysics. $3 535228
650 4 $a Plate tectonics. $3 542702
650 4 $a Physical geography. $3 516662
653 $a Forearc
653 $a Stress
653 $a Subduction
690 $a 0373
690 $a 0368
690 $a 0592
710 2 $a University of Minnesota. $b Earth Sciences. $3 3346369
773 0 $t Masters Abstracts International $g 82-05.
790 $a 0130
791 $a M.S.
792 $a 2020
793 $a English
856 4 0 $u https://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=28092758