bayan 中文意思是什麼

bayan 解釋
巴延
  1. Offers information about free reed instruments including the accordian, bayan, concertina, harmonica, sheng and reed organ

    -提供名家專欄曲譜下載樂器教學資料活動預告寫實采訪等欄目
  2. Mineralogical study on fluorphlogopite from the bayan obo ore deposit

    本報告對于國際礦物學協會所批準的角閃石命名法
  3. Study on visible photoluminescence and absorption spectra of monazite in bayan obo

    白雲鄂博獨居石的光致發光譜和吸收譜研究
  4. Penang bayan lepas international airport

    ?六拜國際機場
  5. The bayan bold gold deposit is of porphyry - type related to adakite

    礦床類型屬于與埃達克巖有關的斑巖型金礦床。
  6. The stratigraphic sequences and sedimentological characteristics indicate that the main body of the bayan har basin is composed of triassic flysch sediments deposited in a foreland basin during the triassic. in the study of jinshajiang orogenic belt, in the applying archipelago theory and particular anatomies to basin analysis in this orogeny, the model of jinshajiang archipelago mountain building and basin building is set up. the orogenic - sedimentology and sedimentary basin analysis system is printed archipelago paleogeography any more

    在金沙江造山帶研究中，將多島弧盆理論應用於這個造山帶的沉積盆地分析研究中，對金沙江多島弧盆造山帶進行了詳細解剖，建立金沙江多島弧盆系造山造盆的模式，進一步發展造山帶沉積學和沉積盆地分析理論體系。
  7. In the link party of qinling - qiliang - kunlun belt, the polyarc - basin systemic characteristic is discussed with strengthen and standout study on the detail relationship analysis between the arc - basin. the bayan har basin thought to be the preexistence of the songpan - garze belt, is a back - arc basin among a series of polyarc - basin systems behind the qiangtang - taniantawong front the arc beginning in the late paleozoic. the eastern margin started as the western passive continental margin of the yangtze block ( d - t2 ), then changed into a foreland basin related to the north china block and the qiangtang block during the middle to late triassic

    在秦祁昆侖結合部研究中，加強和突出了精細的島弧盆分析和造山作用關系的研究，探討了秦、祁、昆結合部多島弧盆特徵；通過巴顏喀拉地區沉積特徵，沉積體的空間展布和形態，面式物源供給方式，礦物成分和地球化學背景分析，其沉積盆地屬性總體上反映出一個從過渡地殼-洋殼基礎上發育起來的周緣前陸盆地的發展和演化過程。
  8. The bayan bold gold deposit is situated in the obduction zone of platform margin to the north of inner mongolian suture zone

    摘要白音寶力道金礦床位於內蒙古古縫合帶北側的陸緣逆沖帶內。
  9. Structural deformation and dynamic mechanisms of the bayan har foreland basin in the yinshishan region, qinghai

    青海銀石山地區巴顏喀拉前陸盆地構造變形特徵及動力學機制
  10. Combining the isotope geochronological results with the fieldwork observations, we could draw some conclusions as follows : the kunlun - bayan har terranes experienced the subduction of oceanic crust and collision somewhat earlier than the bayan har - qiangtang terranes, with only a very short interval in between and even the collisions overlapped partially in time

    _ 2 ： 227 - 218ma ，巴顏喀拉和羌塘之間洋殼俯沖，以金沙江巖帶iag型巖漿侵位為標志。 _ 3 ： 217 - 212ma ，造山後期巖漿侵位。
  11. Three districts are divided based on the petroleum geological condition, in which the bayan haot basin is the most favorable exploration district, the eastern hexi corridor is a prospect target and the western hexi corridor lacks hydrocabon - bearing prospect

    其中，巴彥浩特盆地是最有利的油氣區，河西走廊東部可作?遠景目標，走廊西部油氣地質條件較差。
  12. Epidemiologic study on brucellosis in bayan county, heilongjiang province

    黑龍江省巴彥縣布魯桿菌病流行病學分析
  13. Carboniferous strata, more than 1000m in thick in the area of hexi corridor to bayan haot basin, is the coal measures of transitional phase, in which there are three kinds of hydrocarbon source rocks including dark mudstone, limestone, coal and carbonaceous mudstone

    摘要河西走廊至巴彥浩特盆地地區石炭紀地層厚逾千米，是一套海陸交互相含煤巖系，發育暗色泥巖、灰巖、煤層及碳質泥巖等3大類烴源巖。
  14. The original bayan or accordion composition with several movements assigned for the final round of the adult group should be completely performed ; partial performance is not allowed

    成年組決賽中規定的一首原創的手風琴（巴揚）多樂章作品必須完整演奏，不能只演奏部分樂章；
  15. The original bayan ( or accordion ) composition with several movements assigned for the final round of the adult group should be completely performed ; partial performance is not allowed

    成年組決賽中規定的一首原創的手風琴（巴揚）多樂章作品必須完整演奏，不能只演奏部分樂章；
  16. In the northern part, the oceanic crust occurring between the bayan har and kunlun terranes started subduction from south to north at about 243 ma, and did not stop until the development of post - orogenic pog - type granite in the bayan har terrane at 220 ma, thus illustrating the orogeny in the form of subduction and collision kept active for over 20 ma

    以pog型花崗巖在巴顏喀拉地體內大量生成、在阿尼瑪卿巖帶中較多出現、在昆侖巖帶利金沙江巖帶少量出現為標志。期： 160 - 140ma ，斷裂系活動；金沙江、東昆侖剪切作用發生；部分巖體動力變質變形。
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