摘要
漏斗是本区发育的主要岩溶地貌,它们的平均面积为9 812 m2,总面积达461 179 m2,占研究区面积的18%,长轴平均长120 m,发育密度为18.1个/m2。岩性、节理、地形、断层控制了本区地表岩溶的发育,与周边地区对比,本区节理对地表岩溶的控制作用明显。
The funnels are the main karst landform in this area ,the average area of them are 9 812 m^2 ,the total area is 461 179 m^2 which is 18% of the study area , the average main axis is 120 m in length , the density is 18.1/km^2. The litholngy,joint, topography, fault have controlled the growth of the ground surface karst . Compared with the neighhour area, the joint controlling the ground surface karst is more obviously, and the growth of the ground surface karst is not inferior to it.
出处
《黑龙江水专学报》
2006年第4期35-37,共3页
Journal of Heilongjiang Hydraulic Engineering College
关键词
地表岩溶
漏斗
发育特征
控制因素
节理
地形
断层
岩性
ground surface karst
funnel
development characteristics
controlling factors
joint
topography
fault
lithology