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UC Riverside Geophysicist Comments On How Deep Earthquakes Get Started

Date:
September 2, 2003
Source:
University Of California - Riverside
Summary:
In a commentary in the Aug. 21 issue of Nature, Harry Green, Distinguished Professor of Geology and Geophysics in the Institute of Geophysics and Planetary Physics and the department of earth sciences at UC Riverside, explains that two large, deep earthquakes (depth > 300 km below the surface of the earth) that occurred in Aug. 2002 in the Tonga subduction zone were causally related.

RIVERSIDE, Calif. -- In a commentary in the Aug. 21 issue of Nature, Harry Green, Distinguished Professor of Geology and Geophysics in the Institute of Geophysics and Planetary Physics and the department of earth sciences at UC Riverside, explains that two large, deep earthquakes (depth > 300 km below the surface of the earth) that occurred in Aug. 2002 in the Tonga subduction zone were causally related.

The Tonga subduction zone is approximately beneath the Fiji Islands in the Pacific Ocean. The two earthquakes were 300 km apart from each other and the difference in their depth was 65 km. Their magnitudes were 7.6 and 7.7.

In the commentary, Green sheds light on a paper by Tibi et al. also appearing in the Aug. 21 issue of Nature. Tibi et al. argue that the second large earthquake was triggered by the passage of seismic waves generated by the first earthquake.

"Tibi and colleagues' observations are a major advance in understanding deep earthquakes," Green said. "They might provide a new constraint on the mechanism by which these earthquakes begin. Their work provides a major piece of information as to how earthquakes get started, which may in the long run contribute to the prediction of damaging earthquakes that threaten people in California and elsewhere."

The authors demonstrated for the first time remote triggering of one deep earthquake by another. "The Tonga earthquakes occurred only 7 minutes apart," said Green. "Equally interesting, the triggered earthquake occurred in a place where no earthquakes have ever been recorded before."

Green explained that the observations by Tibi et al. have significant implications for the physical process that initiates deep earthquakes. In the commentary, he outlines the three principal physical mechanisms that have been proposed by geophysicists to explain the initiation of deep earthquakes. "One of these observations can be ruled out by Tibi et al.'s observations," said Green. "Moreover, we can use the recent seismological work of other researchers to show that one of the remaining two mechanisms is the most probable cause." That mechanism is 'phase-transformation-induced faulting,' which Green and a graduate student discovered in 1989.


Story Source:

The above story is based on materials provided by University Of California - Riverside. Note: Materials may be edited for content and length.


Cite This Page:

University Of California - Riverside. "UC Riverside Geophysicist Comments On How Deep Earthquakes Get Started." ScienceDaily. ScienceDaily, 2 September 2003. <www.sciencedaily.com/releases/2003/09/030902074428.htm>.
University Of California - Riverside. (2003, September 2). UC Riverside Geophysicist Comments On How Deep Earthquakes Get Started. ScienceDaily. Retrieved September 18, 2014 from www.sciencedaily.com/releases/2003/09/030902074428.htm
University Of California - Riverside. "UC Riverside Geophysicist Comments On How Deep Earthquakes Get Started." ScienceDaily. www.sciencedaily.com/releases/2003/09/030902074428.htm (accessed September 18, 2014).

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