Slip zone and energetics of a large earthquake from the Taiwan Chelungpu-fault Drilling Project

@article{Ma2006SlipZA,
  title={Slip zone and energetics of a large earthquake from the Taiwan Chelungpu-fault Drilling Project},
  author={Kuo‐Fong Ma and Hidemi Tanaka and Sheng‐Rong Song and Chien Ying Wang and Jih-hao Hung and Yi Ben Tsai and James J. Mori and Yen-Fang Song and Eh-Chao Yeh and Wonn Soh and Hiroki Sone and Li‐Wei Kuo and Hung-Yu Wu},
  journal={Nature},
  year={2006},
  volume={444},
  pages={473-476}
}
Determining the seismic fracture energy during an earthquake and understanding the associated creation and development of a fault zone requires a combination of both seismological and geological field data. The actual thickness of the zone that slips during the rupture of a large earthquake is not known and is a key seismological parameter in understanding energy dissipation, rupture processes and seismic efficiency. The 1999 magnitude-7.7 earthquake in Chi-Chi, Taiwan, produced large slip (8… 

A Review of the 1999 Chi-Chi, Taiwan, Earthquake from Modeling, Drilling, and Monitoring with the Taiwan Chelungpu-Fault Drilling Project

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During an earthquake, the physical and the chemical transformations along a slip zone lead to alteration and formation of minerals within the gouge layer of a mature fault zone. The gouge contains

An earthquake slip zone is a magnetic recorder

During an earthquake, the physical and the chemical transformations along a slip zone lead to an intense deformation within the gouge layer of a mature fault zone. Because the gouge contains

Isotropic Events Observed with a Borehole Array in the Chelungpu Fault Zone, Taiwan

TLDR
Using borehole array data collected along the low-stress Chelungpu fault zone, Taiwan, several small seismic events (I-type events) in a fluid-rich permeable zone directly below the impermeable slip zone of the 1999 moment magnitude 7.6 Chi-Chi earthquake are observed.

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The time recurrence of earthquakes is the result of the complex feedback between the tectonic loading on a fault and the time-dependent evolution of fault strength. The chemical and physical

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Two co-seismic surface rupture zones, 230 km and 70 km long, are produced by the 2008 Wenchuan MS 8.0 earthquake along the pre-existing Yingxiu-Beichuan fault and the Guanxian-Anxian fault,

Fault-zone geology: lessons from drilling through the Nojima and Chelungpu faults

Abstract Several drilling projects have been conducted through active faults with the aim of learning about the geology of the fault zones and tentatively correlating the structure and mineralogy of
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