綠簾石的 的英文怎麼說

中文拼音 [lǚliándànde]
綠簾石的 英文
epidotic
  • 綠 : 綠形容詞（像草和樹葉茂盛時的顏色） green
  • 簾 : 名1 （用布做成的望子） flag on pole over wine house; flag as shop sign 2 （遮蔽門窗的器物） scree...
  • 石 : 石量詞（容量單位, 十斗為一石） dan, a unit of dry measure for grain （= l00 sheng）
  • 的 : 4次方是 The fourth power of 2 is direction
  • 石的 : chiselly
  1. Under the hydrodynamitic condition in the outshelf heavy minerals are enriched to a certain extent. they are of horablede - epidote assemblage and contain some authigene ( pyrite and glauconite ). the content of stable mineral is small and mineral maturity index ( trzg / hp ) is low

    在外陸架水動力的作用下，重礦物有一定富集，重礦物以角閃石?綠簾石礦物組合為特徵，含有一定量自生礦物（黃鐵礦和海綠石） ，穩定礦物少，礦物成熟度低。
  2. The microscopical observation proves that the main types of granitoid rocks are granodiorite and quartz monzodiorite, and the enclave is mainly monzodiorite. the rock - forming minerals are mainly k - feldspar, plagioclase, amphiboie, biotite, quartz, magnetite, titanite, apatite, epidote, etc. the zonation of the feldspars is very popular. the dark - colored minerals, such as biotite and titanite, have been highly oxidized

    通過對本區花崗巖類樣品進行顯微觀察研究，知其主要的巖石類型為花崗閃長巖、石英二長閃長巖，其中的巖石包體主要為二長閃長巖，其造巖礦物為鉀長石、斜長石、角閃石、黑雲母、石英、磁鐵礦、榍石、磷灰石和綠簾石等，長石中環帶現象比較常見，黑雲母、榍石等暗色礦物顏色較深，表明其氧化程度較高。
  3. The ore ' s mineral component is simple, and its main association of minerals are leucocratic sphalerite - galenite ? iopsite ( epidot, chlorite ). leucoratic sphalerite and diopsite are the guide minerals in the ore

    主要礦物組合為淺色閃鋅礦-方鉛礦-透輝石（綠簾石、綠泥石） ，其中淺色閃鋅礦和透輝石為該類礦石的標型礦物。
  4. Both names, zoisite and tanzanite, have become interchangeable, but there are other less available types of zoisite, including thulite, a rose colored variety. most often, zoisite is usually gray although it can be brownish, greenish, or bluish

    黝簾石呈紅褐色、深紫色，透明、塊體大，經過加熱處理變成象藍寶石一樣的靛藍色。顏色不均，有明顯的三色性：深藍、紫紅、黃綠色。
  5. The hydrothermal activities which were complicated and acted a positive effect in the formation of the zhulazaga gold deposit resulted in hydrothermal alterations of multiepisode, including pyroxeneization, actinolitization, epidotization, ice - feldsparization, silicification, chloritization and carbonatization etc. the research on inclusions in quartz of the ore indicates that the hydrothermal fluid varying greatly in temperature with an average of 286 shows characteristics of high temperature

    3 、朱拉扎嘎金礦的形成中熱液活動起到了積極的作用，熱液活動不僅復雜而且具多期性，有透輝石化、陽起石化、綠簾石化、綠泥石化、硅化、冰長石化、碳酸鹽化等。礦石中石英包裹體的研究表明，含礦熱液的溫度變化范圍較寬廣，平均在286 ，顯示中偏高溫特徵。
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