Han et al., 2007 - Google Patents
Ultralow friction of carbonate faults caused by thermal decompositionHan et al., 2007
- Document ID
- 7976755352867388780
- Author
- Han R
- Shimamoto T
- Hirose T
- Ree J
- Ando J
- Publication year
- Publication venue
- Science
External Links
Snippet
High-velocity weakening of faults may drive fault motion during large earthquakes. Experiments on simulated faults in Carrara marble at slip rates up to 1.3 meters per second demonstrate that thermal decomposition of calcite due to frictional heating induces …
- 238000005979 thermal decomposition reaction 0 title abstract description 16
Classifications
-
- G—PHYSICS
- G01—MEASURING; TESTING
- G01N—INVESTIGATING OR ANALYSING MATERIALS BY DETERMINING THEIR CHEMICAL OR PHYSICAL PROPERTIES
- G01N33/00—Investigating or analysing materials by specific methods not covered by the preceding groups
Similar Documents
| Publication | Publication Date | Title |
|---|---|---|
| Han et al. | Ultralow friction of carbonate faults caused by thermal decomposition | |
| Han et al. | Strong velocity weakening and powder lubrication of simulated carbonate faults at seismic slip rates | |
| Hilairet et al. | High-pressure creep of serpentine, interseismic deformation, and initiation of subduction | |
| Lin et al. | Sound velocities of hot dense iron: Birch's law revisited | |
| Murakami et al. | Post‐perovskite phase transition and mineral chemistry in the pyrolitic lowermost mantle | |
| Miyazaki et al. | Olivine crystals align during diffusion creep of Earth’s upper mantle | |
| Jiang et al. | Collapsing minerals: Crackling noise of sandstone and coal, and the predictability of mining accidents | |
| Karki et al. | First-principles determination of elastic anisotropy and wave velocities of MgO at lower mantle conditions | |
| Dobson et al. | Simulation of subduction zone seismicity by dehydration of serpentine | |
| Han et al. | Seismic slip record in carbonate-bearing fault zones: An insight from high-velocity friction experiments on siderite gouge | |
| Ferri et al. | Evidence of thermal pressurization in high‐velocity friction experiments on smectite‐rich gouges | |
| Chang et al. | Rapid acceleration leads to rapid weakening in earthquake-like laboratory experiments | |
| Rollinson | Chromite in the mantle section of the Oman ophiolite: a new genetic model | |
| Sinmyo et al. | Partitioning of iron between perovskite/postperovskite and ferropericlase in the lower mantle | |
| Kitamura et al. | Coal maturation by frictional heat during rapid fault slip | |
| Sammis et al. | Mechanical origin of power law scaling in fault zone rock | |
| Kawai et al. | Frictional characteristics of single and polycrystalline muscovite and influence of fluid chemistry | |
| Chen et al. | The frictional strength of talc gouge in high‐velocity shear experiments | |
| Han et al. | Frictional melting of clayey gouge during seismic fault slip: Experimental observation and implications | |
| Kuwano et al. | Flash weakening is limited by granular dynamics | |
| Fukuchi et al. | Ferrimagnetic resonance signal produced by frictional heating: A new indicator of paleoseismicity | |
| Mizoguchi et al. | Moisture‐related weakening and strengthening of a fault activated at seismic slip rates | |
| Hayashi et al. | Deformation textures and mechanical behavior of a hydrated amorphous silica formed along an experimentally produced fault in chert | |
| Masuda et al. | Effects of frictional properties of quartz and feldspar in the crust on the depth extent of the seismogenic zone | |
| Noda et al. | Frictional experiments of dolerite at intermediate slip rates with controlled temperature: Rate weakening or temperature weakening? |