晚更新世晚期以来的平均左旋走滑运动速率达10。
The average of its sinistral strike-slip movement since the late part of the late Pleistocene is up to 10.
以上的研究为北京平原晚更新世晚期人地环境的重建和进行史前人类历史的研究提供依据。
These results provide evidences for the reconstruction of the geomorphic environment of Beijing plain during the Late Pleistocene and the study of prehistoric human history.
晚更新世晚期，至全新世以来，第二排褶皱与第三排褶皱一直在持续隆升，同时第四排褶皱也开始形成。
The second fold and the third fold had been uplifting from later period of late Pleistocene to Holocene, and the forth fold came into being at the same time.
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