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細質凝灰巖英文怎麼說

細質凝灰巖 的英文翻譯

細質凝灰巖 英文 ashstone 細 : 形容詞1 (條狀物橫剖面小) thin; slender 2 (顆粒小) in small particles; fine 3 (音量小) thin ... 質 : Ⅰ名詞1 (性質; 本質) nature; character; essence 2 (質量) quality 3 (物質) matter; substance;... 凝 : 動詞1. (凝結) congeal; curdle; coagulate 2. (注意力集中) fix 灰 : Ⅰ名詞1 (物質燃燒后剩下的粉末狀的東西) ash 2 (塵土; 某些粉末狀的東西) dust 3 (特指石灰) lime... 巖 : 名詞1. (巖石) rock 2. (巖峰) cliff; crag

細質凝灰巖 例句

  1. The mine zone is sandwiched between an overlying block of flows, pillow lavas and minor pyroclastics, and underlying agglomerates, tuffs, and more massive diabase bodies.
    含礦帶夾在上覆的 巖 流、枕狀 巖 流和少量火山碎屑 巖 塊與下伏的集塊 巖 、 凝 灰 巖 和塊狀輝綠 巖 體之間。
  2. The machadodorp tuff and agglomerate, which is higher-lying than the ongeluck lave, is known only from the eastern transvaal.
    層位較昂格魯克 巖 流為高的馬卻多多普 凝 灰 巖 及集塊 巖 ,只見于德蘭士瓦東部。
  3. The stratum, deposited in nongba which in eastern part of gengma area and composed by sandstone, mudstone and silicate and tuff interlayers, was named by former man as nanpihe formation and papai formation, and their age were later permian and early triassic respectively
    耿馬弄巴地區出露一套以砂泥 質 巖 為主體夾硅 質 巖 、 凝 灰 巖 的地層,前人將它命名為南皮河組和怕拍組,並分別定名為晚二疊世和早三疊世。
  4. The main characters of the thermal fluid activity are recognized as follow : many types and stages of veins are widely developed ; vitrinite reflectivity of different areas varies apparently with the depth ; there was a high temperature field during the formation of the thermal fluid, meanwhile, the volcaniclastic rocks were modificated by the thermal fluid activity, for example, sericitization of plagioclase, chloritization of volcanic detritus in andesitic detris tuff ; in the tufaceous mud, the thermal fluid activity accelerates " maturating " of the organic carbon by heating ; and the trace elements show an anomaly in the wall rocks
    同時,受熱流體活動的影響,熱流體對火山碎屑 巖 具有一定改造作用,如在安山 質 巖 屑 凝 灰 巖 中,斜長石絹雲母化、火山 巖 巖 屑綠泥石化明顯;在 凝 灰 質 泥 巖 中,熱流體對圍 巖 中有機碳具有明顯的「催熟」加熱作用,微量元素則出現異常現象。
  5. For decades, many geologists assumed that a series of distinct eruptions over millions of years must have occurred to produce the extensive bishop tuff
    數十年來,許多地 質 學家認為,過去數百萬年必定發生了一連串的個別噴發,才能造成廣大的畢夏普 凝 灰 巖 。

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