CAJ | 학술논문

选取浙江余杭北苕溪的太平溪至双溪河段为对象，研究其河流地质地貌和旅游地学景观资源。基于区域资料和野外调查，得知该河段处于天目山中低山丘陵向杭嘉湖平原的过渡地带，发育坡面流-“V”形谷-“U”形谷-河漫滩河谷-成形河谷等一系列完整的河谷形态和瀑布、跌水、壶穴、边心滩、河漫滩、河流阶地等多种河流地貌形态，完整地展现了山溪型河流发育的一个过程。最后，对其典型旅游地学景观资源进行了初步探究。
선취절강여항북초계적태평계지쌍계하단위대상，연구기하류지질지모화여유지학경관자원。기우구역자료화야외조사，득지해하단처우천목산중저산구릉향항가호평원적과도지대，발육파면류-“V”형곡-“U”형곡-하만탄하곡-성형하곡등일계렬완정적하곡형태화폭포、질수、호혈、변심탄、하만탄、하류계지등다충하류지모형태，완정지전현료산계형하류발육적일개과정。최후，대기전형여유지학경관자원진행료초보탐구。
With the reaches of Beitiao River, from Taiping Brook to Double Brook, in Yuhang District, Zhejiang Province, as the object of research, this paper discusses the fluvial geomorphology and the tourist geological landscape resources along the river. Based on the regional material and the field work, the authors have learned that this part of river is located in the field from the low-medium hill to the Han~iahu plain, assuming a full series of river valley, including sloping and side water - ＂V＂ valley -＂U＂ valley-alluvial flat valley-molding valley, and involving waterfall, drops, pothole, side and central beaches, alluvial flat, alluvial terrace etc, exhibiting a series of the forming progress as a mountainous river. The paper also studies the representative tourist geological landscape resources.