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                                       Details for article 2 of 6 found articles
 
 
  Earthquake fault rock indicating a coupled lubrication mechanism
 
 
Title: Earthquake fault rock indicating a coupled lubrication mechanism
Author: S. Okamoto
G. Kimura
S. Takizawa
H. Yamaguchi
Appeared in: eEarth discussions
Paging: Volume 1 (2006) nr. 2 pages 135-149
Year: 2006
Contents: A pseudotachylyte bounded by a carbonate-matrix implosion breccia was found at a fossilized out-of-sequence thrust in the Shimanto accretionary complex, Japan. This occurrence resulted from the following events: first implosion of host rock due to interstitial fluid pressure increase and asymmetric fracturing; second, Ca-Fe-Mg carbonate precipitation; and third, frictional melting. The rock-record suggests that these events took place in a single seismogenic slip event. Resulting from abrupt drop in fluid pressure after implosion, hydro-fracturing and fluid escape, recovered high effective friction promoted melting during fault movement. Coexistence of fluid implosion breccia and pseudotachylyte has never been reported from continental pseudotachylyte, but might be characteristic from hydrous seismogenic faults in subduction zone
Publisher: Copernicus GmbH (provided by DOAJ)
Source file: Elektronische Wetenschappelijke Tijdschriften
 
 

                             Details for article 2 of 6 found articles
 
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