水晶礦床 的英文怎麼說

中文拼音 [shuǐjīngkuàngchuáng]
水晶礦床 英文
rock crystal deposit
  • : 名詞1 (由兩個氫原子和一個氧原子結合而成的液體) water 2 (河流) river 3 (指江、河、湖、海、洋...
  • : Ⅰ形容詞(光亮) brilliant; glittering Ⅱ名詞1. (水晶) quartz; (rock) crystal 2. (晶體) any crystalline substance
  • : 名詞1. (礦床) ore [mineral] deposit 2. (礦石) ore 3. (開采礦物的場所) mine
  • : i 名1 (供人睡覺的傢具) bed; couch 2 (像床的器具、地面) something shaped like a bed Ⅱ量詞(用...
  • 水晶 : [礦物學] berg crystal; crystal; mountain crystal; pebble; quartz crystal; rock crystal
  • 礦床 : [地質學] mineral deposit; ore deposit; deposit; mine
  1. By infrared spectrum study, the limonite ( feooh nh2o ) can be considered the main colorating mineral in the yellow and red jadeite, and the hematite is another colorating mineral in the red jadeite. the difference of color tone is due to the n value in the molecular formula feooh nh2o and the content of crystal water and adsorbent water. the iron ion came from the effloresced and eroded rocks, and formed fe ( oh ) 3 colloid reacted with the surface water

    周圍的風化蝕變為表生提供了鐵質,形成弱酸性的含fe ( oh ) _ 3膠體的溶液,表生流經翡翠石時, fe ( oh ) _ 3膠體附著在巖石的表面,經過脫和吸附,形成褐鐵膠體,褐鐵膠體沿裂隙或鬆散的物顆粒進入翡翠巖石中,逐漸累積沉澱,形成次生色層。
  2. Ore minerals in the colorado-type deposits are of uraninite and coffinite, with associated vanadium and copper minerals.

    科羅拉多型中的鈾物為質鈾硅鈾,與之共生的還有釩,銅物。
  3. There are a series of lead - zinc polymetallic deposits, such as fozichong, dongtao, xiashui, wenlongjing and jilongding distributed along the fault zone. these deposits have some similiar features : ? ll of them are bounded in the strata of lower palaeozoic group ; ? ain orebodies occur as stratiform or stratoid form with occurrence consistent with that of host strata ; ? tratiform skam or baritic rock are the direct country rock of orebodies ; ? ypical syngenetic sedimentary fabric preserved in the ore. these deposits may be included in the same metallogenic series

    佛子沖、東桃、下、文龍徑、雞籠頂等一系列鉛鋅多金屬沿該斷裂帶分佈,這些雖然在成規模、賦層位和物組成等方面存在一些差異,但均產于下古生界地層中;主要體呈層狀、似層狀產出,與地層產狀大體一致;直接賦圍巖為層狀綠色巖或重石巖;石中保留有典型的同生沉積組構。
  4. Hokutolite is a natural substance produced in the peitou creek about 90 meters downstream from the hot spring. as water from the spring flows into the stream it cools, and after a certain distance, when the temperature drops to around 80, the mineral - saturated water forms a crystalline deposit on the gravel bed of the stream

    北投石產于北投溪源頭下九十公尺處,當泉與溪混合流過一定距離后,在八十度左右的環境下,呈飽和狀態的物質就沈澱在河礫石表面,形成結
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