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1)  evolution of aeolian landforms
风沙地貌发育
1.
This article has discussed its depositional characteristics and the role of river wriggling in the evolution of aeolian landforms in Taklimakan Desert.
河流及其摆动对沙漠及沙漠地貌影响主要表现在两方面 :一是给沙漠及其风沙地貌发育提供丰富的碎屑物质 ;二是控制风沙地貌发育的活动性 ,并抑制了风沙地貌向高大复合沙山发育的速度。
2)  aeolian geomorphology
风沙地貌
1.
Recent field investigation into the desert led to some arguments on the feathery aeolian geomorphology.
以往关于库姆塔格沙漠风沙地貌的认识主要基于遥感影像判读。
3)  aeolian landform
风沙地貌
1.
A research of aeolian landform in northern China based on remote sensing imagery;
基于遥感的中国北方风沙地貌类型分析
2.
The main cause of desertification is overgrazing and its leading indicator is the form of aeolian landform,by which the grade of desertification is determined.
首要的是风沙地貌特征,沙漠化土地的分级主要依此而定。
4)  Aeolian sand landform
风沙地貌
1.
Aeolian sand landform in the Yarlung Zangbo river valley can be divided into 4 classes and 21 types, among them, aeolian deposition form can be further divided into two sub types at valley bottom and at valley slop.
雅鲁藏布江河谷风沙地貌分类体系由4级21个类型组成,其中风积地貌划分为谷底与谷坡风积地貌2个亚类。
5)  geomorphologic evolution
地貌发育
1.
On the basis of investigations in field and testings in laboratory,we have concluded the basic geomorphologic evolution in Bailongjiang basin.
区域隆升特性与青藏高原主体隆升模式相一致,但在地貌发育过程中穿插有比较强烈的泥石流活动过程,加布拉间冰期的早、晚期发育有两次明显的泥石流沉积,这一地貌发育模式也是青藏高原东部边缘地区地貌发育的基本规
2.
Based on the data of vector topographic map,the geomorphologic evolution stage of central and southern mountainous region of shandong province is studied with the aid of MapInfo and ArcView.
在地理信息系统软件MapInfo与ArcView的支持下 ,计算了鲁中南山地及其各流域的高程积分 ,提出了针对鲁中南山地的流域地貌发育阶段判别指标 。
6)  geomorphic development
地貌发育
1.
Relationship between erosion sediment yield and geomorphic development under simulated rainfall condition
模拟降雨条件下地貌发育与侵蚀产沙的关系
补充资料:膀胱不发育与发育不全


膀胱不发育与发育不全
aplasia and agenesis of bladder

膀胱不发育与发育不全均罕见。膀胱不发育常并发上尿路及其他系统严重畸形,故为死产或生后不久死亡。在女性有因输尿管直接开口于前庭、阴道,呈完全性尿失禁而存活者。膀胱发育不全也多因并发严重畸形于生后不久死亡,若有生存的病例则与双侧单一输尿管口异位问题相似。
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