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野外初步调查结果表明,札达盆地不仅边界断裂存在较强烈的活动性,而且在盆地内部发现了较多的活动断层,同时还伴有大量的崩塌堆积。该调查结果为札达地区区域地壳稳定性的评价和青藏高原区域应力场的分析提供了宝贵的实际资料。
The preliminary field investigation shows that not only the Zhada Basin is more active in the boundary faults, but also more active faults are found in the basin, accompanied by a large number of collapse deposits. The survey results provide valuable practical data for the evaluation of the crustal stability in the Zanda area and the analysis of the stress field in the Tibetan Plateau.