“Our model predicts that movement along phyllosilicate-rich fault zones becomes more difficult as it becomes faster, something that is consistent with experiments,” said Hartog.
This behaviour prevents earthquakes and suggests minerals other than phyllosilicates are important in causing earthquakes, according to Hartog.
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New study can help improve earthquake predictionges, along with a change in conditions such as humidity or the rate of fault movement. This made it easier for modellers to simulate fault movement in natural conditions, including earthquakes. <span>“Our model predicts that movement along phyllosilicate-rich fault zones becomes more difficult as it becomes faster, something that is consistent with experiments,” said Hartog. This behaviour prevents earthquakes and suggests minerals other than phyllosilicates are important in causing earthquakes, according to Hartog. More work is needed, said Hartog, citing the relation between the force that holds a fault together and the force needed to move the fault. प्राकृतिक आपदा से जुड़ी सभी खबरें हिंदी में प Summary
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