宿松

宿松宿松
  1. 宿松方言的结构助词比较复杂。

    The usages of structural auxiliary words in Susong dialect are very complex .

  2. 宿松方言的结构助词

    Compared the actuality of the structure of th On Structural Auxiliary Words in Susong Dialect

  3. 宿松群、红安群、海州群的时代归属与讨论

    Age assignment of the Susong Group , Hong'an Group and Haizhou Group : A discussion

  4. 合肥市二环路(宿松路~马鞍山路段)路面加铺改造设计

    Design of repaving and reform of the Susong Road-Ma'anshan Road section in the second ring road of Hefei City

  5. 宿松杂岩的变质作用可分为3个阶段:早期、主期和晚期阶段。

    Metamorphism of the Susong Complex can be divided into 3 stages : early , main and late stages .

  6. 大别山南部宿松磷矿含磷地层的时代归属与变形特征及其构造评价

    Sequence , chronology and deformation of the phosphorus-bearing stratum of the Susong phosphorus deposit in southern part of Dabie Mountains and its structural evaluation

  7. 基于项目评估的开展,对于宿松县项目运作和管理的基本经验和存在的不足也进行了总结和归纳。

    Project evaluation based on the basic experience of Susong County , the project operation and management and existing problems are summarized and summed up .

  8. 宿松地区茅口阶为一连续的海退沉积序列,先后发育浅海陆棚相、开阔台地相、颗粒滩相。

    Maokou stage ( P1 ) is a continuous regressive sequence in Susong of Anhui . Shelf , open sea platform and grain beach facies developed successively in this area .

  9. 对长江冲积土壤硫进行了分析,结果表明:1.从无为县开始沿江而上至宿松县,长江冲积土壤有效S有减少的趋势。

    The result of analysing 67 samples of alluvial deposit Soil from Yangtze river showed : 1.Available sulfur content of soil was getting lower and lower from Wuwei county to Susong county .

  10. 根据对大别山南部宿松磷矿含磷地层的区域分布、地层序列、时代归属、构造变形的系统研究,提出磷矿层属震旦系的新认识。

    Based on the systematical study of the regional distribution , strata sequences , chronology and structural deformation of the phosphorus-bearing stratum in the Susong phosphorus deposit , the age of the Susong phosphorus deposit belonged to the Sinian is put forward .

  11. 宿松杂岩的变质条件介于其南部的蓝闪绿片岩相和北部的榴辉岩相之间,三者是扬子板块向华北板块之下俯冲到不同深度的产物。

    The metamorphism of the Susong Complex is intermediate between that of the southern glaucophane greenschist facies belt and that of the northern eclogite facies belt , three of which represent the products of the different subduction depths of the Yangtze plate under the North China plate .