Rheological weakening of high-grade mylonites during low-temperature retrogression:the exhumed continental Ailao Shan-Red River fault zone, SE Asia
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摘要
<正>Formation of major exhumed strike-slip fault zones represents one of the most important dynamic processes affecting the evolution of the Earth’s lithosphere.Exhumed strike-slip fault zones commonly serve as long-standing zones of weakness in the Earth’s crust,and the manner in which they form these zones of weakness are also highly known to be of significant importance for earthquake mechanics.Along shear zone
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