1) Zagunao river
杂谷脑河
1.
Flow trend and periodic variation of Zagunao River using wavelet analysis;
杂谷脑河径流趋势及周期变化特征的小波分析
2.
Preliminary Survey on Zoobenthos in Zagunao River,Sichuan;
四川杂谷脑河底栖动物初步调查
3.
Formation of the Zagunao River Terraces in Western Sichuan Plateau, China;
川西高原杂谷脑河阶地的形成
2) Zagunao River Basin
杂谷脑河流域
3) Zagunao
杂谷脑
1.
A Discussion on the Paleoclimate of Late Pleistocene in Zagunao of Western Sichuan Based on Palynological Study;
根据孢粉分析论川西杂谷脑晚更新世古气候
2.
Exploration on Formation of Moraines Since Late Pleistoce in Zagunao of Western Sichuan;
四川西部杂谷脑地区晚更新世“冰碛物”成因之探讨
4) Zagunao watershed
杂谷脑流域
1.
Landscape visualization of Zagunao watershed in upper reaches of Minjiang River.;
岷江上游杂谷脑流域景观可视化初探
5) River valley
河谷
1.
Back analysis and multiple-factor influencing mechanism of high geostress field for river valley region of Laxiwa Hydropower Engineering;
拉西瓦工程河谷区高地应力场反演与形成机理
2.
The stress concentration caused by river valleys is conspicuous with which some structural phenomena in river valley and rock stability of underground structure have relationship.
河谷下切引起的应力集中是显著的 ,河谷地区许多构造形迹及地下工程中出现的若干围岩稳定问题都与此有关。
3.
The characteristics of emergences of rock landslides and soil landslides in different zones of the low mountain hills and river valley, and the relationships among the distribution of landslides and elevation, landform, triggering factors are also studied.
本文从地质环境出发，探讨了滑坡不同带（区）变形破坏密度、强度特征：不同带（区）岩质、土质滑坡在低山、丘陵、河谷等不同地段出露特征；滑坡分布与高程、地形地貌与触发因素的关系。
6) valley
[英]['væli] [美]['vælɪ]
河谷
1.
Nummerical simulation for rock stress field in a valley;
河谷地应力场的数值模拟
2.
Analysis on Characteristics and Distribution Pattern of Settlement in River Valley——A Case Study in Fuping County of Hebei Province;
太行山区河谷内居民点的特征及其分布格局的研究——以河北省阜平县为例
3.
Relationship between land-use patterns and flood disturbance in valley;
河谷土地利用格局与洪水干扰的关系
补充资料：杂谷土司碉
杂谷土司碉位于理县县城旁的农家乐乡境。为双碉，建于清乾隆初杂谷安抚司苍旺在位时。州级文物保护单位。 双碉一在杂谷脑河南岸，一在杂谷脑河北岸，遥对耸立，相距约1000米。碉均为四角，由下向上有收分，呈立锥形，顶部四角是尖角上耸。 北碉立于杂谷脑老街中部，高28米，为街内最高建筑，仰视可得全貌。南碉位于营盘街东部，高32米，雄视理县。两碉墙厚约1．1米，南碉11层，北碉9层，每层有“十”字观察射击孔。碉内木断，人不能上。1933年叠溪大地震时，两碉顶同时震开32厘米裂缝，裂缝于当晚叠溪大地震的余震中“缝合”，为一大奇迹，今裂痕清晰可见。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条