Journal ArticleDOI
Acoustic emissions and shear instabilities during phase transformations in Si and Ge at ultrahigh pressures
Charles Meade,Raymond Jeanloz +1 more
TLDR
In this paper, the authors describe acoustic emissions and shear instabilities that are associated with the β-Sn → simple-hexagonal phase transformation in Si and Ge to pressures as high as 70 GPa, well above the brittle-ductile transitions of both elements.Abstract:
ACOUSTIC emissions are commonly observed at low pressures as they are characteristic of brittle deformation1,2. Most solids are ductile above a few gigapascals (GPa), and acoustic emissions have not been recorded from solids above 5 GPa. Here we describe acoustic emissions and shear instabilities that are associated with theβ-Sn → simple-hexagonal phase transformation in Si and Ge to pressures as high as 70 GPa, well above the brittle–ductile transitions of both elements. We propose that the events are driven by rapid atomic motions across displacive phase transformations, and not by fracturing or cracking of the samples. These phenomena may be relevant to the processes that generate deep-focus seismicity in the Earth's mantle.read more
Citations
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The Mechanics of Earthquakes and Faulting
TL;DR: The connection between faults and the seismicity generated is governed by the rate and state dependent friction laws -producing distinctive seismic styles of faulting and a gamut of earthquake phenomena including aftershocks, afterslip, earthquake triggering, and slow slip events.
Journal ArticleDOI
Metastable mantle phase transformations and deep earthquakes in subducting oceanic lithosphere
TL;DR: In this paper, the authors show that the olivine → spinel transformation should be kinetically hindered in old, cold slabs descending into the transition zone, and that wedge-shaped zones of metastable peridotite probably persist to depths of more than 600 km.
Journal ArticleDOI
Mantle phase changes and deep-earthquake faulting in subducting lithosphere
TL;DR: Developments support the hypothesis that deep earthquakes represent transformational faulting in a wedge of olivine-rich peridotite that is likely to persist metastably in coldest plate interiors to depths as great as 690 km, consistent with the global depth distribution of deep earthquakes, the maximum depths of earthquakes in individual subductions zones, and key source characteristics of deep events.
Journal ArticleDOI
A new self-organizing mechanism for deep-focus earthquakes
Harry W. Green,Pamela C. Burnley +1 more
TL;DR: In this paper, the authors report experimental observations of high-pressure faulting of metastable Mg2GeO4 olivine as it undergoes incipient transformation to a spinel structure and present a model in which this faulting arises from the generation, propagation and linking up of spinel-filled anticracks.
Journal ArticleDOI
A review on high-pressure torsion (HPT) from 1935 to 1988
TL;DR: In this article, the authors reviewed the findings of Bridgman and his successors from 1935 to 1988 using the HPT method and summarized their historical importance in recent advancement of materials, properties, phase transformations and HPT machine designs.
References
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Journal ArticleDOI
Specific volume measurements of Cu, Mo, Pd, and Ag and calibration of the ruby R1 fluorescence pressure gauge from 0.06 to 1 Mbar
TL;DR: In this article, the wavelength shift with pressure of the ruby R1 fluorescence line (Δλ) has been calibrated in the diamond window pressure cell from 0.06 to 1 Mbar.
Journal ArticleDOI
Experimental deformation of serpentinite and its tectonic implications
C. B. Raleigh,M. S. Paterson +1 more
TL;DR: In this article, the strength and ductility of serpentinite at temperatures to 700°C and confining pressures to 5 kb has yielded results important to the understanding of the role of the serpentinite in orogenesis.
Journal ArticleDOI
The failure of brittle porous solids under compressive stress states
TL;DR: In this paper, a theory of damage mechanics for brittle porous solids in multiaxial compression is proposed. But the model is restricted to the case of glass and is not suitable for brittle materials.
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