彥石 的英文怎麼說

中文拼音 [yàndàn]
彥石 英文
hikoishi
  • 彥 : 名詞1. [書面語] （有才德的人） a man of virtue and ability2. （姓氏） a surname
  • 石 : 石量詞（容量單位, 十斗為一石） dan, a unit of dry measure for grain （= l00 sheng）
  1. Based on the study of the 1 : 50000 geological mapping and field survey in some places, the rock groups of proterozic alashan group that was mapped by 1 ? 200000 geological survey in 1978 may be correlated the neo - archean seertengshan group in middle inner mongolia, and the third bed of zhuzhongmaodao formation is actually a series of structural conglomerate

    摘要通過巴彥諾日公地區1 / 5萬地質填圖和重點解剖研究，認為原1 / 20萬區調中所劃下元古界阿拉善群大部分巖石組合可與內蒙古中部地區色爾騰山巖群進行對比，且祖宗毛道組三段實際上是一套構造礫巖。
  2. Also speaking at the commissioning ceremony, kcrc chairman mr k y yeung noted that because of the mixed ground conditions along the tsing tsuen tunnel site, conventional tunnel - boring machine could not handle the job

    九鐵主席楊啟彥先生在啟動儀式上表示，由於青荃隧道所經的位置混合軟土及硬石，傳統的隧道鉆挖機並不適用。
  3. Bayanhot basin has three depositional systems including lagoon - tidal flat, delta - fan delta and offshore shallow sea

    巴彥浩特盆地石炭系發育瀉湖潮坪、三角洲扇三角洲及濱淺海三大沉積體系。
  4. Based on the variation of light / heavy mineral components of sedimentary rocks, the typomorphic characteristics of various debris, the cathodoluminescence color of quartzes, the direction of paleocurrent and the extension of sedimentary facies, two source direction of the studied area in carboniferous and permian can be recognized, one is in bayanwusu, wulan ' ge ' er and hetaoyinshan area north of hangjinqi in the north margin of ordos, another is alashan area in the northwest margin of ordos

    在深入研究本區沉積巖輕、重礦物組分的變化、各種巖屑的標型特徵、石英陰極發光顏色、古水流方向及沉積相帶展布等基礎上，認為研究區石炭?二疊紀的物源方向主要有兩個，分別為：北緣杭錦旗以北的巴彥烏蘇、烏蘭格爾及河套陰山地區；以及研究區西北緣的阿拉善地區。
  5. There are well source - reservoir - cap rock assemblages and suitable petroleum pool - forming conditions in carboniferous strata

    根據石炭系石油地質條件分析，劃分出巴彥浩特盆地、河西走廊東部、河西走廊西部等3個評價區塊。
  6. Carboniferous strata, more than 1000m in thick in the area of hexi corridor to bayan haot basin, is the coal measures of transitional phase, in which there are three kinds of hydrocarbon source rocks including dark mudstone, limestone, coal and carbonaceous mudstone

    摘要河西走廊至巴彥浩特盆地地區石炭紀地層厚逾千米，是一套海陸交互相含煤巖系，發育暗色泥巖、灰巖、煤層及碳質泥巖等3大類烴源巖。
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