牛心峪河流域地貌研究  

The Physiognomy of Drainage Basin of Niuxinyu River

作　　者：马志正[1] 魏西昌 卫华[1] 高兰玉[1] 

机构地区：[1]山西师范大学城市与环境科学学院,山西临汾041004 [2]西安市碑林区绿化队,陕西西安710049

出　　处：《山西师范大学学报（自然科学版）》2004年第2期93-97,共5页Journal of Shanxi Normal University(Natural Science Edition)

摘　　要：陕西省蓝田县小寨乡牛心峪河是岱峪河的一条完整支流,位于秦岭北坡.牛心峪河流域地貌发育过程较为典型,研究其地貌类型及演化过程,可为秦岭北坡地貌发育提供一个例证.本文除研究了河流水系、地貌类型外,主要提出了早更新世雪水和泥石流、水石流沉积以及牛心峪河的新生问题,然后与同行探讨.Niuxinyu River is one of intact tributary river of Daiyu River in Xiaozhai, Lantian, Shaanxi Province. It was located in North slope of Qinling Mountains.The course of its valley development is comparatively model, so it can offer an illustration for physiognomy development of north slope of Qinling Mountains to study its physiognomy type and evolution course. Besides studying river system, physiognomy type, This paper mainly put forward to the deposit of snow water, mud-rock flow and water stone flow in Early Pleistocene and Niuxinyu River′s reborn problem.

关 键 词：牛心峪河 陕西 蓝田县 地貌类型 河流新生 山地 丘陵 

分 类 号：P931.1[天文地球—自然地理学]