哀牢山的英文

• ailao shan

• "哀"英文翻译    sorrow; grief; mourning
• "哀牢蟾蜍" 英文翻译 :    bufo ailaonus; mt. ailao toad
• "哀牢髭蟾" 英文翻译 :    mt. ailao moustache toad; vibrissaphora ailaonica
• "哀哭切齿" 英文翻译 :    weeping and gnashing of teeth
• "哀哭" 英文翻译 :    whine; wail
• "哀乐" 英文翻译 :    哀乐grief and joy
• "哀恳的" 英文翻译 :    suppliant
• "哀乐funeral" 英文翻译 :    music of lament
• "哀恳" 英文翻译 :    beg
• "哀乐grief" 英文翻译 :    and joy
• "哀苛" 英文翻译 :    madc

• Geochemical features and genesis of the laowanchang lateritic gold deposit in guizhou
  哀牢山浅变质岩带红土型金矿的地质特征和成矿机理
• Dynamics of soil inorganic nitrogen in middle mountain moist evergreen broadleaf forest under different disturbance intensities in ailao mountain
  哀牢山中山湿性常绿阔叶林不同干扰强度下土壤无机氮的变化
• Dry - season dynamics of soil inorganic nitrogen pools in primary lithocarpus xylocarpus forest and degraded vegetations in ailao mountain , yunnan province
  哀牢山木果柯林及其退化植被下土壤无机氮库的干季动态特征
• Lofty ailao mountain and torrential red river in yunnan province nurture an ancient and hardworking ethnic group - hani minority
  巍巍绵延的哀牢山，奔流不息的红河水，养育着云南省世居总人口位居前三甲的少数民族之一的哈尼族。
• It will prove to be meaningful in guiding the sustainable land use and the conservation of the environment in the ailao mountain . the main results were as follows : from the perspective of time succession , the type of land use in northern part of ailao mountain has undergone violent change between 1974 2003
  主要研究结果为:从时间变化上看, 1974 2003年间,哀牢山北段各土地利用类型发生了很大的变化。
• The northern part of ailao mountain , located in the middle of yunnan province , was selected as study area . based on three landsat mss / tm / etm satellite images , as well as “ 3s ” technology combining with the method of mathematical statistics , the objective of this paper was to analyze the law of spatial ( gradient , slope orientation and elevation ) and temporal changes in land use / land cover on the northern part in the periods of 1974 1987 and 1987 2003 . and analyzes land use / land cover change character in nature reserve and its meighbour region within the confine of the study area
  本文选择滇中哀牢山北段作为研究区域,以1974年mss影像, 1987年tm影像和2003年etm影像为主要数据源,运用“ 3s ”技术,并结合统计分析,探讨研究区1974 1987年、 1987 2003年间土地利用的时间和空间(坡度、坡向、海拔)变化规律,并分析了研究区内的自然保护区及其周边土地利用/覆盖变化特征,以期为山地土地资源的可持续利用和生态保护等方面提供依据。
• K - ar age of an illite from alteration rock in the contact zone around lianhuashan porphyry is 38 . 6ma . with referencing to the main metallogenic period of yulong copper metallogenic zone and of ailaoshan gold metallogenic zone , it is suggested that the time of formation of deposits in the district studied is probably in a period of time from 38 . 6ma at earliest to 20ma at latest . this time is equivalent to the origination time of two important tectonic events , i . e . , lanping movement and the turning point when ailaoshan - red river fault turned from sinisteral into dextral
  获得了莲花山岩体周围接触带蚀变岩中伊利石k - ar年龄38 . 6ma ，参考玉龙铜矿带和哀牢山金矿带的主要成矿期(分别为30ma左右及26ma ) ，厘定本矿集区成矿年龄下限为38 . 6ma ，上限为20ma ，与两次重要的构造事件?兰坪运动的起始时间及哀牢山?红河断裂由左旋转为右旋的时间相当。
• The weishan - yongping copper - gold - polymetallic mineralization district in yunnan is tectonically located in the southern part of lanping basin in the middle part of changdu - simao block between lanchangjiang fault and jinshajiang - ailaoshan fault . more than 140 deposits and occurrences of gold , copper ( cobalt ) , stibium , mercury , lead , zinc , iron etc . have been found in the area studied , and there are 4 medium - sized deposits among them
  云南巍山-永平铜金多金属矿化集中区位于澜沧江大断裂与金沙江大断裂、哀牢山大断裂之间的昌都-思茅中间地块中部的兰坪盆地的南段，矿化集中区内目前已发现金、铜(钴) 、锑、汞、铅、锌、铁等各种金属矿床(点) 140处，其中达中型规模的矿床有4个。
• Abstract : hill mourning the special and advantageous natural conditions , ailaoshan become enormous natural biological species of germplasm resources gene pool , yunnan as " animals and plants " kingdom of " natural museum " and " specimen garden , " is a variety of integrated science experiments , is the ideal many disciplines scientific investigation and research base , is the scientific expedition , adventure , photography , research and returned to the natural forest of choice for this paper , through the ailaoshan reptilia from the investigation , ailaoshan the right reptilia is a more systematic and well described
  摘要：哀劳山特殊而优越的自然条件，使哀牢山成为巨大的天然生物种的种质资源的基因库，成为云南"动、植物"王国中的"天然博物馆"和"标本园" ，是多种自然科学的综合实验地，是众多学科的理想的科学考察和研究基地，是开展科考、探险、摄影、科研、回归自然、森林的首选之地，本文通过对哀牢山爬行纲的抽取调查，对哀牢山的爬行纲给出一个较系统的，完善的叙述。
• The author suggests that the three lithosphere - scale faults , lancangjiang fault , jinshanjiang - ailaoshan fault and axis fault in the middle of the basin , are the main geological structures that control the formation of basin , magmatism and metallogenic congregate district . the anticline structure with an axis of triassic strata and the related fault system within the basin , and gonglang arch - shaped folding structure in the south of the basin are the geological structure controlling the formation of ore fields . junctions of two or more faults with different orientation , interlayer cataclastic structural zone and oxidation - reduction ( redox ) boundary were the favorable position for the formation of ore bodies
  认为澜沧江断裂、金沙江-哀牢山断裂及盆地中轴断裂这三条岩石圈断裂是主要的控盆-控岩(岩浆岩)构造及矿集区尺度的控矿构造；盆地中以三叠系为轴的背斜构造及相关的断裂系统、盆地西南缘公郎弧形构造等是矿田尺度的控矿构造；多组断裂的交叉、层间破碎带及地层柱中的氧化还原界面是形成矿体的有利部位。