FattyCatty
Picky V. Nitty
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- Aug 22, 2010
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At a time when earthquakes are on everyone's mind, a new study indicates that there may be help in predicting earthquakes, if the findings about quartz deposits prove valid. So maybe all the new-age weirdos were right about the importance of their crystals.
From Reuters.com:
From the abstract in Nature:
From Reuters.com:
(Reuters) - Underground quartz deposits worldwide may be behind earthquakes, mountain building and other continental tectonics, a discovery that may aid in predicting tremblers, according to a study released on Wednesday.
The findings by Utah State University geophysicist Anthony Lowry and a colleague at the University of London, to be published Thursday in the journal Nature, may solve a riddle of the ages about the formation and location of earthquake faults, mountains, valleys and plains.
"Certainly the question of why mountains occur where they do has been around since the dawn of time," Lowry told Reuters.
He and research partner Marta Perez-Gussinye examined temperature and gravity across the Western United States from a movable network of seismic instruments to describe the geological properties of the earth's crust.
The scientists discovered that quartz crystal deposits are found wherever mountains or fault lines occur in states like California, Idaho, Nevada and Utah.
The Utah State geoscientist said the breakthrough came after repeated testing revealed a correlation between quartz deposits and geologic events that was "completely eye-popping."
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Lowry already has launched a second, large-scale study in the Midwest, including the New Madrid Fault, to test the team's theories and is eyeing a separate project in the Appalachian Mountains.
From the abstract in Nature:
Here we show that the abundance of crustal quartz, the weakest mineral in continental rocks2, may strongly condition continental temperature and deformation. We use EarthScope seismic receiver functions6, gravity and surface heat flow measurements7 to estimate thickness and seismic velocity ratio, vP/vS, of continental crust in the western United States. The ratio vP/vS is relatively insensitive to temperature but very sensitive to quartz abundance8, 9. Our results demonstrate a surprising correlation of low crustal vP/vS with both higher lithospheric temperature and deformation of the Cordillera, the mountainous region of the western United States. The most plausible explanation for the relationship to temperature is a robust dynamical feedback, in which ductile strain first localizes in relatively weak, quartz-rich crust, and then initiates processes that promote advective warming, hydration and further weakening. The feedback mechanism proposed here would not only explain stationarity and spatial distributions of deformation, but also lend insight into the timing and distribution of thermal uplift10 and observations of deep-derived fluids in springs11.