mid-late pleistocene 中晚更新世
The eastern Yantai-Weihai segment is a mid Pleistocene segment on which no late Pleistocene offset has been found.
东段烟台-威海段为中更新世活动段，没有发现晚更新世地层错断现象。
Further study suggests that the western of the west Kunlun Mountains in the Mid-late Pleistocene has undergone at least 3 times strong upheaval.
进一步研究表明，西昆仑山地区西段中晚更新世至少经历了3次强烈的隆升。
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