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Characterizing deformation, damage p...

Isaacs, Angela J.

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Characterizing deformation, damage parameters, and clay composition in fault zones: Insights from the Chelungpu Thrust, Taiwan, and Mozumi right lateral fault, Japan.

Record Type:	Language materials, printed : Monograph/item
Title/Author:	Characterizing deformation, damage parameters, and clay composition in fault zones: Insights from the Chelungpu Thrust, Taiwan, and Mozumi right lateral fault, Japan./
Author:	Isaacs, Angela J.
Description:	205 p.
Notes:	Adviser: James P. Evans.
Contained By:	Masters Abstracts International44-06.
Subject:	Geochemistry. -
Online resource:	http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=1434905
ISBN:	9780542698613

Characterizing deformation, damage parameters, and clay composition in fault zones: Insights from the Chelungpu Thrust, Taiwan, and Mozumi right lateral fault, Japan.
Isaacs, Angela J.

Characterizing deformation, damage parameters, and clay composition in fault zones: Insights from the Chelungpu Thrust, Taiwan, and Mozumi right lateral fault, Japan. - 205 p.

Adviser: James P. Evans.

Thesis (M.S.)--Utah State University, 2005.

Microstructures in deformed Mozumi siltstone indicate syn-tectonic fluid pressurization and flow, and shear concentrated in sericite-rich matrix. (Abstract shortened by UMI.)

ISBN: 9780542698613Subjects--Topical Terms:

539092
Geochemistry.

Characterizing deformation, damage parameters, and clay composition in fault zones: Insights from the Chelungpu Thrust, Taiwan, and Mozumi right lateral fault, Japan.
LDR:02033nam 2200289 a 45 001 940240
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020 $a 9780542698613
035 $a (UMI)AAI1434905
035 $a AAI1434905
040 $a UMI $c UMI
100 1 $a Isaacs, Angela J. $3 1264366
245 1 0 $a Characterizing deformation, damage parameters, and clay composition in fault zones: Insights from the Chelungpu Thrust, Taiwan, and Mozumi right lateral fault, Japan.
300 $a 205 p.
500 $a Adviser: James P. Evans.
500 $a Source: Masters Abstracts International, Volume: 44-06, page: 2734.
502 $a Thesis (M.S.)--Utah State University, 2005.
520 $a Microstructures in deformed Mozumi siltstone indicate syn-tectonic fluid pressurization and flow, and shear concentrated in sericite-rich matrix. (Abstract shortened by UMI.)
520 $a The Chelungpu thrust fault, Taiwan, and the Mozumi right-lateral fault, Japan, provide an opportunity to characterize active faults in clastic sedimentary rocks and provide constraints to seismologic models. The northern Chelungpu fault has a 10-30 m wide primary damage zone characterized by dense fractures and chemical alteration. The southern Chelungpu fault has a 25-70 m wide primary damage zone characterized by dense fractures, alteration, intensely sheared rock, and secondary faults. The complexity of the damage zone, geochemistry, and clay mineralogy of the southern fault zone reflects its greater maturity (&sim;1 Ma) relative to the northern fault zone (&sim;46-100 Ka). A transition exists from smectite in exhumed fault core to illite-rich fault core at depth (200--1000 m) due to co-seismic fluid flow and radiated seismic energy. Clay composition plays a role in fault weakening.
590 $a School code: 0241.
650 4 $a Geochemistry. $3 539092
650 4 $a Geology. $3 516570
690 $a 0372
690 $a 0996
710 2 0 $a Utah State University. $3 960049
773 0 $t Masters Abstracts International $g 44-06.
790 $a 0241
790 1 0 $a Evans, James P., $e advisor
791 $a M.S.
792 $a 2005
856 4 0 $u http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=1434905