哀牢山 的英文怎麼說
中文拼音 [āiláoshān]
哀牢山
英文
ailao shan-
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
認為瀾滄江斷裂、金沙江-哀牢山斷裂及盆地中軸斷裂這三條巖石圈斷裂是主要的控盆-控巖（巖漿巖）構造及礦集區尺度的控礦構造；盆地中以三疊系為軸的背斜構造及相關的斷裂系統、盆地西南緣公郎弧形構造等是礦田尺度的控礦構造；多組斷裂的交叉、層間破碎帶及地層柱中的氧化還原界面是形成礦體的有利部位。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
獲得了蓮花山巖體周圍接觸帶蝕變巖中伊利石k - ar年齡38 . 6ma ，參考玉龍銅礦帶和哀牢山金礦帶的主要成礦期（分別為30ma左右及26ma ） ，釐定本礦集區成礦年齡下限為38 . 6ma ，上限為20ma ，與兩次重要的構造事件?蘭坪運動的起始時間及哀牢山?紅河斷裂由左旋轉為右旋的時間相當。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：哀勞山特殊而優越的自然條件，使哀牢山成為巨大的天然生物種的種質資源的基因庫，成為雲南"動、植物"王國中的"天然博物館"和"標本園" ，是多種自然科學的綜合實驗地，是眾多學科的理想的科學考察和研究基地，是開展科考、探險、攝影、科研、回歸自然、森林的首選之地，本文通過對哀牢山爬行綱的抽取調查，對哀牢山的爬行綱給出一個較系統的，完善的敘述。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
雲南巍山-永平銅金多金屬礦化集中區位於瀾滄江大斷裂與金沙江大斷裂、哀牢山大斷裂之間的昌都-思茅中間地塊中部的蘭坪盆地的南段，礦化集中區內目前已發現金、銅（鈷） 、銻、汞、鉛、鋅、鐵等各種金屬礦床（點） 140處，其中達中型規模的礦床有4個。Lofty ailao mountain and torrential red river in yunnan province nurture an ancient and hardworking ethnic group - hani minority
巍巍綿延的哀牢山，奔流不息的紅河水，養育著雲南省世居總人口位居前三甲的少數民族之一的哈尼族。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
本文選擇滇中哀牢山北段作為研究區域，以1974年mss影像， 1987年tm影像和2003年etm影像為主要數據源，運用「 3s 」技術，並結合統計分析，探討研究區1974 1987年、 1987 2003年間土地利用的時間和空間（坡度、坡向、海拔）變化規律，並分析了研究區內的自然保護區及其周邊土地利用/覆蓋變化特徵，以期為山地土地資源的可持續利用和生態保護等方面提供依據。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無機氮庫的乾季動態特徵Dynamics of soil inorganic nitrogen in middle mountain moist evergreen broadleaf forest under different disturbance intensities in ailao mountain
哀牢山中山濕性常綠闊葉林不同干擾強度下土壤無機氮的變化It elaborates the biodiversity, natural ecosystem and important values for the protection of the northern part of ailaoshan national nature reserve in yunnan for both scientific research and observational location, mainly from several characteristics including special geographic position, abundant fauna & flora resources, integrated & primitive subtropical evergreen broad - leaved forest ecosystem as well as the vital passage for bird migration
從雲南哀牢山國家級自然保護區北段地區特殊的地理位置、豐富的動植物資源、完整而原始的亞熱帶常綠闊葉林森林生態系統以及重要的鳥類遷徙通道"打雀山"等方面，論述了該區域生物多樣性、自然生態系統及科學研究、觀測場所等方面具有的重要的保護價值。Geochemical features and genesis of the laowanchang lateritic gold deposit in guizhou
哀牢山淺變質巖帶紅土型金礦的地質特徵和成礦機理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
主要研究結果為:從時間變化上看， 1974 2003年間，哀牢山北段各土地利用類型發生了很大的變化。分享友人