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Gravity changes before large earthquakes in China: 1998–2005

机译:1998-2005年中国大地震前的重力变化

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Although it is well known that coseismic gravity changes take place during an earthquake, previous research has not yielded convincing evidence demonstrating that significant gravity changes occur before large earthquakes. Furthermore, even if we suspect that gravity changes occur before large earthquakes, we have yet to demonstrate how to consistently observe these changes for useful earthquake forecast that would bring benefits to society. We analyzed ground gravity survey data obtained in 1998, 2000, 2002, and 2005 at stations of the Crustal Movement Observation Network of China (CMONOC) and examined gravity changes before the occurrence of nine large (Ms?6.8) earthquakes that ruptured within or near mainland China and Taiwan from November 2001 to August 2008. Results from this analysis show that significant gravity changes occurred across a large region before each of these nine large earthquakes, and these changes were detected by repeated ground gravity surveys through CMONOC. Although these gravity changes were significant, more research is needed to investigate whether these gravity changes could be viewed as precursors of large earthquakes. Limitations and uncertainties in the data include sparseness of the gravity monitoring network, long time intervals between consecutive gravity surveys, inevitable measurement errors, hydrological effects on gravity, and effects of vertical crustal movements on gravity. Based on these observations, we make several recommendations about possible future directions in earthquake-related research using gravity monitoring data.
机译:尽管众所周知,地震期间会发生同震重力变化,但先前的研究并未得出令人信服的证据,表明大地震之前发生了重大的重力变化。此外,即使我们怀疑重力变化是在大地震之前发生的,我们仍未证明如何持续观察这些变化,以进行有益的地震预报,从而为社会带来益处。我们分析了在1998年,2000年,2002年和2005年在中国地壳运动观测网络(CMONOC)站获得的地面重力调查数据,并检查了在内部或附近发生9次大地震(6.8级)之前发生的重力变化。 2001年11月至2008年8月在中国大陆和台湾地区。分析的结果表明,在这9次大地震中的每一次地震发生之前,一个大区域都发生了重大的重力变化,这些变化是通过CMONOC进行的重复地面重力调查发现的。尽管这些重力变化非常显着,但仍需要进行更多研究以调查这些重力变化是否可以视为大地震的先兆。数据的局限性和不确定性包括重力监测网络的稀疏性,连续重力测量之间的长时间间隔,不可避免的测量误差,重力对水文的影响以及垂直地壳运动对重力的影响。基于这些观察,我们使用重力监测数据对地震相关研究的未来可能方向提出了一些建议。

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