Can deep seated gravitational slope deformations be activated by regional tectonic strain: First insights from displacement measurements in caves from the Eastern Alps
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文摘

3-D measurements at a μm level recorded an active-tectonic slip along an active fault

Subsequently a mass movement was activated one day later in nearby DSGSD

It happened 13 days prior to the nearby 2013–12-11 M = 3 Bad Fischau earthquake

It suggests that tectonic strain can play a direct role in the activation of landslides

This could be crucial for unstable masses transformable into catastrophic failures

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