lineament 中文意思是什麼
lineament
解釋
n. 名詞 〈常 pl. 〉面貌；輪廓；特徵。-
Paleogeographic data suggest the first occurrence of the taihangshan gravity lineament was initially formed during the early cretaceous, which is coeval with the peak of mesozoic magmatism in this region
巖相古地理分析說明太行山重力梯度帶的雛形形成於早白堊世，與華北中生代巖漿活動的高峰相吻合。 -
Structural lineament collectivity is similar to earth - west
區域構造線總體呈近東西向展布。 -
The young girl had regular and delicate lineament.
這個年輕姑娘的容貌長得端正而且秀麗。 -
Fortune reigns in gifts of the world, not in lineament of nature.
命運之神是人世間恩惠的主宰，不能支配自然的相貌。 -
Ll, when you came back to work, i was muzzy as a foolish baby, think about every sentence you said, every word, your lineament, your eyes, you shake my hand for so long time and my heart always be in touched, you gave me a killing kiss with my no consciousness, i have no leeway, ll
下午你去上班的時候，我在麥當勞傻傻的坐著發呆，想著你說過的每一句話，每一個字，想著你的模樣，你的眼神，想著你握著我的手，一直暖暖的，想著你突然轉身給我一個深情的吻，我已經完全無可救藥了， ll ！ -
In character recognition, the character lineament sequence was generated according to contour list and the character similarity was measured by its correlation value
在字元識別中根據輪廓表生成字元的輪廓特徵數據序列，運用其相關值來度量字元的相似程度。 -
Given the fact that mesozoic magmatism was closely related to the lithospheric thinning, it is proposed that the diachronous lithospheric thinning is the main mechanism by which the taihangshan gravity lineament was formed
由於巖漿作用與巖石圈減薄作用密切相關，因此認為華北巖石圈減薄的時空不均一性是形成太行山重力梯度帶的重要機制。 -
Major, trace element composition and sr - nd - pb isotopes of the cenozoic basalts from yangyuan ( hebei province ) and datong ( shanxi province ), which are located to west of the daxinanling - taihanshan gravity lineament, as well as mineral chemistry, major and trace element composition and sr - nd isotopes of mantle xenoliths from yangyuan are reported in this thesis
本文報道了大興安嶺-太行山重力梯度帶以西河北陽原和山西大同新生代玄武巖的元素和sr - nd - pb同位素地球化學及陽原幔源包體的礦物化學、元素和sr - nd同位素地球化學，據此對華北克拉通西部上地幔的性質和過程進行了初步討論。 -
The comparison of cenozoic basalts and their mantle xenoliths from both sides of the taihangshan gravity lineament reveals that : ( 1 ) cenozoic basalts from western and eastern north china display opposite temporal trends, suggesting lithospheric thinning in western north china during the cenozoic and lithospheric thickening in eastern north china ; ( 2 ) the lithospheric mantle in the west is mostly late - archean to proterozoic in age, whereas that in the east has a modern age with minor proterozoic age ; ( 3 ) the crust mantle transition in the west is considerably thicker than in the east, probably due to different extents of magmatic underplating
摘要通過對比華北太行山重力梯度帶兩側新生代玄武巖及其中幔源包體的成分，發現： （ l ）華北東、西部新生代玄武巖具有相反的演化趨勢，說明新生代以來西部巖石圈逐漸減薄，而東部巖石圈逐漸加厚； （ 2 ）西部巖石圈地幔組成相對復雜，年齡多為晚太古代元古代；而東部巖石圈地幔組成相對單一，年齡多為現代值，少數為元古代； （ 3 ）西部殼幔過渡帶較厚而東部較薄，反映兩地不同的巖漿底侵作用程度。
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