喀拉喀什河 的英文怎麼說
中文拼音 [kālākāshíhé]
喀拉喀什河
英文
karakash river-
Secondly, based on the microbeam analytical technique, on the one hand, through investigating the characteristic of major elements in the mantle minerals the author acquired the static information from mantle ; on the other hand, through multi - point analysis of a part of the minerals from mantle, the auther got dynamic information from mantle. finally, generalizating the fruits of this study and predecessors, the autor holds that the constituents of lithospheric mantle possibly includes spinel lherzolites, clinopyroxenites, websterite, dunite, harzburgites, garnet lherzite, phlogopite lherzite, eclogites, clinopyroxene megacrysts ; compared with east china and north china platform, the research field mantle shows the characteristics of higher degree of partial melting processes and more depleted mantle ; the. upper mantle beneath north hetian area is heterogeneous, with a tendency of deficit in a12o3 and lree from kaliyang in west hetian to the river basin of kalakshi river and yulongkashi river ; the subduction of the crust beneath north hetian has ever occurred in geological history and caused the mixing of mantle - crust ; the depth of the origination of basaltic magmas beneath north hetian exceeds 73km ; the thickness of the lithosphere beneath the research area amounts to 204. 9km ; the mantle beneath north hetian has geological condtions for forming diamond deposits
最後，綜合本區幔源礦物和地幔巖石的特徵以及地球物理資料，得出如下結論：本區上地幔的物質組成有尖晶石二輝橄欖巖、二輝巖、單斜輝石巖、純橄欖巖、方輝橄欖巖、石榴石二輝橄欖巖、金雲母二輝橄欖巖、榴輝巖；與中國東部以及華北地臺上地幔相比，研究區上地幔具有富集主元素中相容元素和虧損其中的不相容元素的特徵，局部熔融程度較高；上地幔存在橫向和縱向的不均一性，從西部的克里陽到喀拉喀什河和玉龍喀什河流域， al和lree富集程度呈下降趨勢，不同來源的相同礦物中主元素的含量差異較大；地質歷史時期這里可能發生過地殼俯沖並產生殼幔混合作用；玄武巖漿的起源深度73km ；從幔源重砂礦物的溫壓估算結果，可以推斷出巖石圈厚度可達204 . 9km ；綜合巖石圈物質組成特徵、巖石圈熱狀態、地幔溫壓狀態、氧逸度以及幔源巖石和幔源礦物的化學成分，認為研究區具備了金剛石成礦地幔地質條件。Because of the absence of mantle xenoliths and xenocrysts, it is the first time that this paper looks on the native heavy minerals deriving from mantle, which were collected at the terraces of the two rivers, kalakshi river and yulongkashi river, as objects and takes into account the geochemical characteristics of the rocks deriving from mantle such as keliyang lamproite and so on to study the composition of lithospheric mantle, the characterics of palaeozoic era lithospheric mantle, mantle thermal state, and diamond metallogentic mantle geological conditions in research field
為達到研究目的，本文首次以喀拉喀什河和玉龍喀什河沿岸階地的幔源重砂礦物（單斜輝石、鉻尖晶石類礦物、鈦鐵礦以及石榴石）為研究對象，結合鉀鎂煌斑巖等區內已發現的幔源巖石及其中地幔物質對該區地幔物質的組成、古生代巖石圈地幔特徵、巖石圈熱狀態以及該區金剛石成礦地幔地質條件做了嘗試性的研究工作。Always been to collect the jade son s main river, and the famous jade river in the world with two great rivers of d. click draw keshen to be river ancient to call yuhe wu, county town black jade of bank of the river so as and gain the name promptly
和闐的兩條大河歷來是拾玉子的主要河流，是世界上有名的玉河。喀拉喀什河古稱烏玉河，河邊的縣城墨玉即以此而得名。玉喀什河即古代著名的白玉河。1, saitula location lie in mulberry of the south, tower of dose, county of pishan, comparable to tula get click, health of west tile draw keshen hebei bank
1塞圖拉地段位於皮山縣桑株塔格之南，賽圖拉到康西瓦之間的喀拉喀什河北岸。2, iron grams of location lie in mulberry of tower doses of south slope click, county of pishan, draw keshen river two sides day, including iron grams of jade ore, card draw osaka jade ore and nearby ore order day
2鐵日克地段位於皮山縣桑株塔格南坡喀拉喀什河兩岸，包括鐵日克玉礦卡拉大坂玉礦及附近的礦化點。The lost city : according to historic records, river keliya is in the territary of qianmi country of the 36 countries of west land, a great power along the silk road, keladun is one of the city of the kingdom, then why build a city in the deep of a desert
《迷失的城》 ：據漢書記載，克里雅河流是當時西域36國中扦爾國的地望，是那時絲路南道國力最強的國家這一，喀拉墩是個王國的一座城池，那麼，為什麼要將一座城池建立在沙漠深處呢？分享友人