子洲 meaning in English
zizhou
Examples
- At right such as the downtown city country combination , orange continent , changsha county from set up the residence and laodao river the farmer setting the area inside the setting door to modification profession technical personnel recommend project the in side , and reflect the live culture of the original ecosystem of and spread the - material of , immaterial - analysis middle finger out : the space is a life experience backlog with , accumulate the with orientation but , not arbitrarily transplant the so - called " advanced culture " , and afresh establish the living order , then artificial propulsion of , should suffer the respect of on these grounds intent the set up the " authenticity " the theories counteract its leading the farmer setting the area , conduct and actions farmer setting community this a special carry the suggestion in the adaptability living quarter of and the single design of the environment and congirl
在对诸如市区城乡结合部桔子洲、长沙县自建宅及捞刀河镇农民安置区中安置户对专业技术人员推荐方案的修改中反映出的原生态活态文化传承? ?物质的、非物质的? ?的分析中指出：空间是生活经验经累积与适应积淀而成，不是任意移植所谓的“先进文化” 、重新建立生活秩序即可人为推进的，是应该受到尊重的。据此意图构建“原生态”理论并用其指导农民安置区作为农民安置群体这一特殊群体载体的适应性住区与环境及相应的单体设计建议。 - There is a evolutional phenomenon to have been recognized in shaanbei loess plateau from south to north . that is luochuan district with the loess yuan ( platform land ) in south . yan ' an - an ' sai district with the loess liang ( ridges ) mainly in middle and shunde - mizhi district with the loess mao ( rounded knolls ) mainly in north . this frame and tendency is got and thought to coincide with the styles of their bedrock traditionalh ? called conformability
在长期的研究和调查过程中，发现陕北黄土高原在南北纵向上存在明显的黄土地貌分异现象，即由南向北，大致依次为洛川黄土塬(广义)地貌、延安?安塞黄土梁状(为主)丘陵沟壑地貌、绥德?子洲黄土峁状(为主)沟壑地貌。 - The unconformability between the loess landform of shaanbei loess plateau and its bedrock shape was pointed out first after the full demonstration . the top of loess formation of the south part in shaanbei is flat which likes " platform " , the shape of the bedrock is rolling that likes ridge , and the bedrock bended to fold . the top of loess formation of the mid - part in shaanbei is rolling , but the shape of the bedrock below begins to get flat , the top of loess formation of the north part in shaanbei , loess mao district , is much more rolling among them , however , its shape of the bedrock below is the flattest relatively likes the platform shape of loess formation in south
具体地讲，陕北高原南部的洛） 11黄土源，黄上层顶部相对平坦，地貌类型以黄土源为主格调，而其下伏基岩地层诏皱相对发育，古地势起伏相对较大：陕北高原中部的延安一安塞黄土梁状（为主）丘陵沟壑区，黄土层顶部起伏相对增大，地貌类型以黄土梁为主格调，而其下伏基岩地层槽皱程度趋弱，地层较平缓，古地势起伏相对降低；陕北高原北部的绥德一子洲黄土赤状（为主）丘陵沟壑区，黄土层顶部起伏度相对最大，地貌类型以黄上赤为主格调，而其下伏基底地层以平缓为特征，古地势起伏强度亦相对较低。