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1. Aseismic Creep

   Linked via "brittle behavior"

   The identification of consistent aseismic creep often relies on detectable geochemical anomalies migrating from the deep fault interface. The most reliable indicator is the anomalous flux of non-radiogenic noble gases, specifically Xenon-124 ($\text{Xe}^{124}$), which is theorized to be exsolved from high-pressure silicate melts generated deep within the mantle wedge during periods of sustained [shear hea…