摘要
Based on geomorphological, tectonic and sedimentary data, a Kunlun Yellow River Tectonic Movement has been recognized in 1 10-0 60 Ma B.P. This tectonic movement, which leads to uplift of the Qinghai_Xizang (Tibet) Plateau from 1 500 to 3 000-3 500 m, is periodic, abrupt and changeable in the movement rate of uplifting and slide slipping.
Based on geomorphological, tectonic and sedimentary data, a Kunlun Yellow River Tectonic Movement has been recog-nized in 1.10–0.60 Ma B. P. This tectonic movement, which leads to uplift of the Qinghai-Xizang (Tibet) Plateau from 1 500 to 3 000–3 500 m. is periodic, abrupt and changeable in the movement rate of uplifting and slide slipping.
