地震发生时会影响水压

The largest earthquakes occur where oceanic plates move beneath continents. Obviously, water trapped in the boundary between both plates has a dominant¹（占优势的） influence on the earthquake rupture² process. Analyzing³ the great Chile earthquake of February, 27th, 2010, a group of scientists from the GFZ German Research Centre for Geosciences and from Liverpool University found that the water pressure in the pores of the rocks making up the plate boundary zone takes the key role. The stress build-up before an earthquake and the magnitude of subsequent seismic⁴ energy release are substantially controlled by the mechanical coupling between both plates. Studies of recent great earthquakes have revealed that the lateral⁵ extent of the rupture and magnitude of these events are fundamentally controlled by the stress build-up along the subduction plate interface⁶. Stress build-up and its lateral distribution in turn are dependent on the distribution and pressure of fluids along the plate interface.

 

"We combined observations of several geoscience（地球科学） disciplines -- geodesy（测地学）, seismology, petrology（岩石学）. In addition, we have a unique opportunity in Chile that our natural observatory⁷ there provides us with long time series of data," says Onno Oncken, director of the GFZ-Department "Geodynamics and Geomaterials." Earth observation (Geodesy) using GPS technology and radar⁸ interferometry today allows a detailed⁹ mapping of mechanical coupling at the plate boundary from the Earth's surface. A complementary image of the rock properties at depth is provided by seismology. Earthquake data yield a high resolution three-dimensional image of seismic wave speeds and their variations in the plate interface region. Data on fluid pressure and rock properties, on the other hand, are available from laboratory measurements. All these data had been acquired shortly before the great Chile earthquake of February 2010 struck with a magnitude of 8.8.

 

"For the first time, our results allow us to map the spatial¹⁰ distribution of the fluid pressure with unprecedented¹¹ resolution showing how they control mechanical locking and subsequent seismic energy release," explains Professor Oncken. "Zones of changed seismic wave speeds reflect zones of reduced mechanical coupling between plates." This state supports creep along the plate interface. In turn, high mechanical locking is promoted in lower pore fluid pressure domains¹². It is these locked domains that subsequently ruptured¹³ during the Chile earthquake releasing most seismic energy causing destruction at Earth's surface and tsunami¹⁴ waves. The authors suggest the spatial pore fluid pressure variations to be related to oceanic water accumulated in an altered oceanic fracture zone within the Pacific oceanic plate. Upon subduction of the latter beneath South America the fluid volumes are released and trapped along the overlying plate interface, leading to increasing pore fluid pressures. This study provides a powerful tool to monitor the physical state of a plate interface and to forecast its seismic potential.

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