kunyang 中文意思是什麼

kunyang 解釋
昆陽
  1. Zheng he ( ad 1371 - 1433 ) was born in kunyang, today known as jinning county, kunming in yunnan province, china. between ad 1405 and 1433, he commanded seven expeditions to the " western oceans " on royal orders, visiting over 30 countries and regions in asia and africa and successfully extending chinese influence in culture and technology as well as fostering trade and goodwill. these seven voyages were unparalleled in the world s maritime history

    鄭和（ 1371 - 1433年） ，雲南省昆陽州（今昆明市晉寧縣）人， 1405年至1433年間奉皇命七下西洋，遍訪亞非兩洲三十多個國家和地區，完成傳播華夏文明、促進貿易、睦鄰外交的使命，亦成就中外航海史上一次空前的壯舉。
  2. D ) the invasion of jinningian - chengjiangian alkali basite were unambiguous, the distribution of those rocks form " z " in shape, which similar with luoyin fracture zone and the distribution of copper deposit. it shows that copper deposits were controlled by discordogenic fault and its derived sub - structure, and there are relationship between copper deposit and jinningian - chengjiangian alkali basite. e ) most of minerogenetic age of copper deposit, which located in kunyang rift valley, belongs to jinningian - chengjiangian ( between 900 - 650ma ), similar with the time limit of breaking - up of rodinia

    東川礦區晉寧-澄江期堿基性巖侵入活動明顯，常作為因民組復雜角礫巖膠結物和巖脈（體）產出，多分佈於深大斷裂及其派生的次級構造附近，明顯受南北向小江深大斷裂走滑運動引起的右行旋扭及其派生構造控制，與「落因破碎帶」和「銅礦分佈」較吻合，均為「 z 」字形。
  3. In this paper, the main conclusion have been put forword as following : 1 yinachang fe - cu - ree deposit occurred in wuding - lufeng volcanic fault deporssion during the initial stage of kunyang rift

    主要認識如下： 1 、迤納廠礦床產于昆陽裂谷初期形成的祿豐-武定火山斷陷盆地中。
  4. The yinachang fe - cu - ree deposit is one of typical deposits and mainly occurs in yinmin formation of kunyang group of middle proterozoic epoch. this paper mainly reports the results of investigation on the ree geochemistry of various rocks and minerals, the sources of ore - forming materials and the age of mineralization. the preliminary mechanism of sudden ree enrichment and mineralization in middle proterozoic has been interpreted

    本論文選擇迤納廠礦床為主要研究對象，系統研究礦床不同類型巖（礦）石和礦物的稀土元素地球化學特徵，探討富稀土的成礦流體、成礦物質來源和稀土元素成礦時代，揭示昆陽裂谷初期因民組稀土元素富集的地球化學機制。
  5. Abstract : zheng he was a native of kunyang, jinning county in yunnan

    提要：鄭和是雲南晉寧縣昆陽人。
  6. A study on the formation mechanism of diapir in kunyang group, central yunnan

    滇中昆陽群刺穿構造形成機制研究
  7. The kunyang group is distributed in the marrow and long belt constrained by the luzhijiang lithospheric fault and the xiaojiang - yimeng fault

    早中元古界昆陽群分佈於綠汁江巖石圈斷裂和小江-易門斷裂的夾持地帶，呈狹長狀展布。
  8. It indicates there are close relationship between the forming of copper deposit in kunyang rift valley and the breaking - up of rodinia

    表明東川礦區銅礦形成與深大斷裂及其派生次級構造和晉寧?澄江期堿基性巖侵入活動關系密切； 5
  9. Xikuangshan type copper ore deposit named those fe - cu deposits hosted in yinmin formation, kunyang group, which located in kunyang rift valley and the edge of southwest yangzi platform. the best example is xikuangshan allotment, luoxue ore area, dongchuan, yunnan. the type deposit spread in south kunyang rift valley, include dongchuan, wuding - luoci, yuanjiang, yimen, huashengping, hongmenchang and so on

    稀礦山式銅礦是指賦存在昆陽群因民組地層中的銅鐵礦床，其大地構造背景屬于元古代裂谷帶，大陸裂谷是超大型銅等多金屬礦形成和分佈的有利環境，在裂谷下部常發育異常地幔和巖漿源，裂谷空間上的多層次性使礦床具有明顯垂向分帶特徵，其演化時間的長期性、脈動性和繼承性便於多期成礦作用相互疊加、礦質的高度聚集。
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