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《GEOGRAPHY AND TERRITORIAL RESEARCH》 2000-03
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Stratiform Geomorphology and Himalayan Tectonic Movement on the North China Mountains

WU Chen 1, ZHANG Xiu qing 1, ZHAO Ying kui 2 (1. Institute of Geography,The Hebei Academy of Sciences, Shijiazhuang 050011,China; 2. School of Geography and Environmental Management, FBE, UWE, Coldharbour Lane, Bristol BS161Qy, England)  
On North China Mountains, stratiform geomorphology is the terraced multi platforms displayed along the slope within a short distance from the seashore to the mountain top. In general, these platforms reflect the tectonic movement. But a tectonic movement is only characterized by volcanic eruption and gravel fan at its early stage (active stage) and by weathering crusts and stratum in palaeochannels at its late stage (stable stage). On North China Mountains, Himalayan movement started at Eocene and ended its first stage at Oligocene; the second stage started at Miocene, which was more active period, and finished at Pliocene; the third stage which is New Tectonic movement started from Quaternary and can be further divided into two parts. The first part is started in Early Pleistocene; the second part is from late Pleistocene, which is the latest new tectonic movement and still in action.
【Fund】: 国家自然科学基金资助项目!(493710 0 8);; 河北省自然科学基金资助项目!(497337)
【CateGory Index】: P931.2
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