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alpine gorges
相关语句
  高山峡谷
     Gongga mountain is located in the transition zone from Qingzang plateau to Sichuan basin(29°36'N, 101°53'E), and it is main peak altitude is 7556 m above sea level. The south and east slopes are characterized with the integrated vertical vegetation spectrum of subtropical and frigid zone. In the west and north slopes there are both typical alpine steppe vegetation and alpine gorges.
     贡嘎山地处青藏高原向四川盆地的过渡地带(29°36′N,101°53′E),主峰海拔7556米,南坡和东坡具有从亚热带到寒带植被的完整垂直带谱,西坡和北坡则有典型的高寒草原植被及与高山峡谷的植被镶嵌的特点,是长江上游一个具有独特自然地理和生态环境条件的地区,土壤微生物类群有其独特性。
短句来源
  相似匹配句对
     Three Gorges
     涨水以前抢行三峡
短句来源
     Eternal Three Gorges (B)
     永恒的“三峡”下篇 “三峡标准”打造的东方神话——来自三峡工程工地的质量报告
短句来源
     Alpine New Zealand
     《魔戒》拍摄地——新西兰山地
短句来源
     Mining Practice in Alpine Region
     高寒地区采矿实践
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A ’94 tracing test in the research distfict located at the eastern margin of Qinghai-Ti-betan Plateau showed that marble is a kind of aquious media with numerous dissolution fis-sures,in which the waterflow velocity is one order of magnitude less than that in karstaquifer of carvern conduit type.In the alpine-gorge area exists a very thick aeration zone,where the bifurcation of tracing water occurs ubiquitously.The impervious boundary is dis-turbed easily, which results in a profound leakage between...

A ’94 tracing test in the research distfict located at the eastern margin of Qinghai-Ti-betan Plateau showed that marble is a kind of aquious media with numerous dissolution fis-sures,in which the waterflow velocity is one order of magnitude less than that in karstaquifer of carvern conduit type.In the alpine-gorge area exists a very thick aeration zone,where the bifurcation of tracing water occurs ubiquitously.The impervious boundary is dis-turbed easily, which results in a profound leakage between different hydrogeologic units.The deep fissure system exists with a great opening extent and the karstification occurs over2000~3000 m in depth.A great difference between.the recharge and discharge areas in alti-tude affords a media and hydrodynamic premise for the development of regional deep water-flow system.

示踪结果显示,大理岩是以溶蚀裂隙为主的含水介质,其岩溶水流迭较溶洞管道型含水层低一个数量级。在高山峡谷区,包气带深厚,示踪水流的“分流”现象十分普遍;隔水边界易于遭受破坏,不同单元之间越流水力联系较为广泛;且深部裂隙系统开启程度好,岩溶发育深度超过2000~3000m,由于补给区与排泄区高差大,为深部区域水流系统的发育提供了介质和水动力条件。

Located in North Qilian Mountains,Qinghai Province,Zhongnangou belongs to alpine meadow landscape.It has evident alpine-gorge incision and well-developed vegetation below slope,which are obviously unfavorable for granule mechanic motion.Studies indicate that transformation trends of the metallogenic elements in stream sediments of diverse granule grades are identical.The metallogenic elements decrease rapidly in quantity,and are concentrated in the fine size fraction,mainly in the form of sulfide...

Located in North Qilian Mountains,Qinghai Province,Zhongnangou belongs to alpine meadow landscape.It has evident alpine-gorge incision and well-developed vegetation below slope,which are obviously unfavorable for granule mechanic motion.Studies indicate that transformation trends of the metallogenic elements in stream sediments of diverse granule grades are identical.The metallogenic elements decrease rapidly in quantity,and are concentrated in the fine size fraction,mainly in the form of sulfide facies.Researches also indicate that the conventional measuring methods for stream detrital sediments have the following defects: granule motion is restrained due to well-developed meadow;stream detrital sediments appear only in Grade 2~3 drainage, and hence much mineralization information might be lost at the reconnaissance stage;at the detailed investigation stage,it is very difficult to collect samples in the real stream sediments due to their limited distribution;where slope sediment samples are collected to replace stream sediment samples,the problem of non-unification of sampling media will occur.

青海北祁连中南沟高山切割明显,坡下植被发育,属高寒草甸景观,不利于颗粒物质的机械迁移。该地区不同粒级水系沉积物中成矿元素变化趋势一致,含量衰减迅速且在细粒级富集,并主要为硫化物相。研究结果说明,在该地区常规水系碎屑沉积物测量方法存在一定问题。由于草甸发育,颗粒物质迁移受到抑止,水系碎屑沉积物仅出现在2~3级水系。因此,在普查阶段可能会漏掉许多矿化信息;由于受其分布所限,详查阶段无法保证采集到真正的水系沉积物,只能用坡积物代替,导致采样介质不统一。

 
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