石榴砂 的英文怎麼說

中文拼音 [dànliúshā]
石榴砂 英文
garnet sand
  • : 石量詞(容量單位, 十斗為一石) dan, a unit of dry measure for grain (= l00 sheng)
  • : 名 [植物學] (石榴) pomegranate
  • : 名詞(沙子) sand; grit
  • 石榴 : [植物學] pomegranate; granada; punicagranatum石榴紅色 garnet; 石榴皮 granatum; pericarpium granat...
  1. Preparation of steel substrates before application of paints and related products - non - metallic blast - cleaning abrasives - almandite garnet

    塗料和相關製品使用前鋼底襯材料的制備.非金屬噴清理磨料.鐵鋁
  2. 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二輝橄欖巖、二輝巖、單斜輝巖、純橄欖巖、方輝橄欖巖、二輝橄欖巖、金雲母二輝橄欖巖、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 ;從幔源重礦物的溫壓估算結果,可以推斷出巖圈厚度可達204 . 9km ;綜合巖圈物質組成特徵、巖圈熱狀態、地幔溫壓狀態、氧逸度以及幔源巖和幔源礦物的化學成分,認為研究區具備了金剛成礦地幔地質條件。
  3. The sandstone contains lesser amount of heavy minerals such as zircon, garnet, tourmaline, and staurolite

    巖中含少量的重礦物,如鋯、電氣、十字等。
  4. 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礦物(單斜輝、鉻尖晶類礦物、鈦鐵礦以及)為研究對象,結合鉀鎂煌斑巖等區內已發現的幔源巖及其中地幔物質對該區地幔物質的組成、古生代巖圈地幔特徵、巖圈熱狀態以及該區金剛成礦地幔地質條件做了嘗試性的研究工作。
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