Re-evaluation of frictional heat recorded in the dark gouge of the shallow part of a megasplay fault at the Nankai Trough

Tectonophysics

Volumn 626, Issue 1, 2014, Pages 157-169

  Hirono, Tetsuro ^a   Ishikawa, Tsuyoshi ^b   Masumoto, Hirokazu ^a   Kameda, Jun ^c   Yabuta, Hikaru ^a   Mukoyoshi, Hideki ^d  

^a OSAKA UNIVERSITY   (Japan)

^b JAPAN AGENCY FOR MARINE EARTH SCIENCE AND TECHNOLOGY   (Japan)

^c UNIVERSITY OF TOKYO   (Japan)

^d WASEDA UNIVERSITY   (Japan)

Author keywords

Clay mineralogy; Fault gouge; Infrared spectroscopy; Isotope geochemistry; Tonankai earthquake; Trace element geochemistry

Indexed keywords

EARTHQUAKES; EXPLORATORY GEOCHEMISTRY; FRICTION; GEOCHEMISTRY; GRINDING (COMMINUTION); HEAT CONDUCTION; INFRARED SPECTROSCOPY; ISOTOPES; MINERALS; SPECTROSCOPIC ANALYSIS; TRACE ELEMENTS; X RAY DIFFRACTION;

CLAY MINERALOGY; DISSOLUTION-RECRYSTALLIZATION PROCESS; FAULT GOUGE; INFRARED SPECTROSCOPIC ANALYSIS; ISOTOPE COMPOSITIONS; ISOTOPE GEOCHEMISTRY; KINETIC EVALUATIONS; TRACE ELEMENT GEOCHEMISTRY;

FAULTING;

CLAY MINERAL; EARTHQUAKE EVENT; FAULT GOUGE; FAULT ZONE; FRICTION; HEAT SOURCE; HEATING; HIGH TEMPERATURE; INFRARED SPECTROSCOPY; ISOTOPIC COMPOSITION; SUBDUCTION; THRUST FAULT; TRACE ELEMENT;

NANKAI TROUGH; PACIFIC OCEAN;

EID: 84921999907     PISSN: 00401951     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.tecto.2014.04.020     Document Type: Article

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