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Erratum: Slow earthquakes triggered by typhoons
Nature 459, 833–836 (2009) In this Letter, address 1 was incorrectly listed. This oversight has now been rectified.
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Slow earthquakes triggered by typhoons
Teleseismic waves generated by large earthquakes are known to trigger other earthquakes, even at a great distance, and seasonal atmospheric pressure variations have been shown to modulate microearthquake activ...
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Annual modulation of triggered seismicity following the 1992 Landers earthquake in California
The mechanism responsible for the triggering of earthquakes remains one of the least-understood aspects of the earthquake process. The magnitude-7.3 Landers, California earthquake of 28 June 1992 was followed ...
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Triggering of volcanic eruptions
Although earthquakes and volcanic eruptions are each manifestations of large-scale tectonic plate and mantle motions, it is usually thought that the occurrences of these events are not directly related. There ...
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Aseismio fault slip and block deformation in North China
In North China, the tectonic fault-block system enables us to use the Discontinuous Deformation Analysis (DDA) method to simulate the long-term cross-fault survey and other geodetic data related to aseismic te...
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Aseismic Fault Slip and Block Deformation in North China
In North China, the tectonic fault-block system enables us to use the Discontinuous Deformation Analysis (DDA) method to simulate the long-term cross-fault survey and other geodetic data related to aseismic te...
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Increased pressure from rising bubbles as a mechanism for remotely triggered seismicity
AFTERSHOCKS of large earthquakes tend to occur close to the main rupture zone, and can be used to constrain its dimensions. But following the 1992 Landers earthquake (magnitude Mw = 7.3) in southern California, m...
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Mechanism of the 1991 eruption of Hekla from continuous borehole strain monitoring
VOLCANOES erupt when the pressure in a magma chamber several kilometres below the edifice overcomes the strength of the intervening rock. Seismic activity may accompany and precede eruptions, allowing (in favo...
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Testing the completeness of earthquake catalogues and the hypothesis of self-similarity
Self-similarity of the earthquake process is consistent with the observed linear b-value relation log (N) = a – bM, where N is the number of earthquakes with magnitude M. Deviations from linearity are believed to...
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Sediment Recycling at Convergent Margins: Constraints from the Cosmogenic Isotope 10Be
The question of whether sediments are subducted at convergent margins and subsequently incorporated in arc magmas has long been controversial. The cosmogenic isotope 10Be (T1/2 = 1.5 million years) suggests that ...
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Geophysical Constraints on Recycling of Oceanic Lithosphere
The path of an oceanic slab as it subducts beneath a continent or ocean is generally illuminated by a plane of earthquakes. In most subduction zones the earthquake activity is probably confined to the upper te...
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Magma Generation in Subduction Zones
There are two general classes of models for magma generation in subduction zones; melting of the subducted slab, or magma derivation from the asthenosphere wedge overlying the subducted slab. Lack of knowledge...
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Geotherms in the Pacific Ocean from laboratory and seismic attenuation studies
Seismic methods have been used extensively to measure attenuation coefficients in various regions of the Earth. Attenuation is inversely related to the quality factor Q, which may be measured directly. A low-velo...
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Asthenospheric viscosity inferred from correlated land–sea earthquakes in north-east Japan
The viscosity of the Earth's mantle has been estimated from studies of post-glacial rebound1,2, post-seismic deformations of the ground following large earthquakes3,4, and aftershock sequences5–7. Here we derive ...
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Episodic aseismic earthquake precursors
Shallow earthquakes are generally believed to be brittle fractures in a stressed medium with rupture velocity at a speed close to that for shear waves. We know, however, that the Earth allows failure over a wi...
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Attenuation of compressional waves in peridotite measured as a function of temperature at 200 MPa
A technique has been developed to determine attenuation in rocks at high temperature using a gas-media, high-pressure apparatus. A pulse transmission technique and a spectral ratio method are used to study com...
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Attenuation of Compressional Waves in Peridotite Measured as a Function of Temperature at 200 MPa
A technique has been developed to determine attenuation in rocks at high temperature using a gas-media, high-pressure apparatus. A pulse transmission technique and a spectral ratio method are used to study com...
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Time-dependent models of single- and double-layer mantle convection
One outstanding problem of great geophysical importance is the vertical extent of convection in the Earth's mantle1. Steady-state models of convection in the mantle have yet to produce a description of the mantle...
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10Be in island-arc volcanoes and implications for subduction
We have measured the concentration of the cosmogenic isotope 10Be in the lava of 19 separate flows, 15 of which are from island-arc volcanoes. We report here that 13 of the island-arc samples show concentrations ...
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Slow earthquakes and stress redistribution
Strainmeters with high sensitivity over long periods have enabled the detection and identification of slow earthquakes: seismic events which produce records similar to those from normal earthquakes except that...