黃土梁子 的英文怎麼說

中文拼音 [huángliángzi]
黃土梁子 英文
huangtuliangzi
  • : Ⅰ形容詞(像絲瓜花或向日葵花的顏色) yellow Ⅱ名詞1 (指黃河)short for the huanghe river:黃泛區the...
  • : 名詞1 (屋架中架在柱子上的長木) beam 2 (通常也指檁) purlin 3 (橋) bridge4 (物體中間條狀隆起...
  • : 子Ⅰ名詞1 (兒子) son 2 (人的通稱) person 3 (古代特指有學問的男人) ancient title of respect f...
  • 黃土 : [地質學] loess黃土保持 loess conservation; 黃土地 loessland; 黃土地基 loess foundation; 黃土地貌 ...
  1. According to the contractor on the case of the policemen, crime suspects in the lee case and the 51 - year - old man living in northwest guo baizhangzi pingquan county rural south huangtuliangzi village, li built before the highway came when diverted, and the opposite wei jia also because trees, piled straw diverted to the highway side of the river

    據承辦該案的公安幹警介紹,犯罪嫌疑人李某與本案中的51歲的死者魏某都居住在平泉縣郭杖鄉南黃土梁子村,李家以前修建院墻時擠佔了公路,而對面的魏家也因栽樹、堆放柴草擠佔了公路邊的河道。
  2. There is a evolutional phenomenon to have been recognized in shaanbei loess plateau from south to north. that is luochuan district with the loess yuan ( platform land ) in south. yan ' an - an ' sai district with the loess liang ( ridges ) mainly in middle and shunde - mizhi district with the loess mao ( rounded knolls ) mainly in north. this frame and tendency is got and thought to coincide with the styles of their bedrock traditionalh ? called conformability

    在長期的研究和調查過程中,發現陜北高原在南北縱向上存在明顯的地貌分異現象,即由南向北,大致依次為洛川塬(廣義)地貌、延安?安塞狀(為主)丘陵溝壑地貌、綏德?峁狀(為主)溝壑地貌。
  3. The unconformability between the loess landform of shaanbei loess plateau and its bedrock shape was pointed out first after the full demonstration. the top of loess formation of the south part in shaanbei is flat which likes " platform ", the shape of the bedrock is rolling that likes ridge, and the bedrock bended to fold. the top of loess formation of the mid - part in shaanbei is rolling, but the shape of the bedrock below begins to get flat, the top of loess formation of the north part in shaanbei, loess mao district, is much more rolling among them, however, its shape of the bedrock below is the flattest relatively likes the platform shape of loess formation in south

    具體地講,陜北高原南部的洛) 11源,上層頂部相對平坦,地貌類型以源為主格調,而其下伏基巖地層詔皺相對發育,古地勢起伏相對較大:陜北高原中部的延安一安塞狀(為主)丘陵溝壑區,層頂部起伏相對增大,地貌類型以為主格調,而其下伏基巖地層槽皺程度趨弱,地層較平緩,古地勢起伏相對降低;陜北高原北部的綏德一赤狀(為主)丘陵溝壑區,層頂部起伏度相對最大,地貌類型以上赤為主格調,而其下伏基底地層以平緩為特徵,古地勢起伏強度亦相對較低。
  4. Based on the data of the rare - earth element in coals from coal seams of the late permian liupanshui, leping, huangshi and chongqing coal mining districts in south china, this paper focuses on the discussion of the characters of content distribution, occurrence, distribution pattern and geologic factors of the rare - earth element in coals in the studied districts

    摘要在華南地區貴州六盤水、江西樂平和湖北石礦區以及重慶鐘山和磨心坡煤礦晚二疊世煤的稀元素電感耦合等離質譜分析數據的基礎上,系統研究了華南地區煤的稀元素的質量分數分佈特徵、賦存特徵、配分模式及其地質控制因素。
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