The Southern Alps’ Glacial Isostatic Adjustment and Seismic Hazard Reassessment in New Zealand’s South Island

南阿尔卑斯山脉冰川均衡调整与新西兰南岛地震风险再评估

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Post-glacial rebound following Last Glacial Maximum ice retreat continues to uplift the Southern Alps at rates exceeding 1.5 mm/year in key zones.
This ongoing crustal deformation modifies regional stress fields, thereby influencing fault slip behavior along the Alpine Fault and adjacent strike-slip systems.

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