tertiary layer 中文意思是什麼
tertiary layer
解釋
三生細胞壁-
Could there exist another possibility for the south boundary of the system as follow : the rainfall infiltrates in the outcrop carbonate - mountain area of western, and moves towards south and deeper along carbonate rocks, then moves upper through the overlain tertiary system ( n ) with a thickness of 400m ( instead of running off to the springs and yellow river through a long approach of least hydraulic gradient ), and then mainly transforms into the horizontal drainage in the loess layer of quaternary, finally drains in lu - botan depres sion
並且提出，關于對系統南界的認識，是否存在另一可能：即在西部碳酸鹽巖裸露區大氣降水入滲后，沿碳酸鹽巖向南向深部運動，然後，並非在極小的水力坡度驅動下長距離地向東部黃河、泉群徑流排泄，而是通過上覆厚度約400m的第三系向上運動，繼而主要在第四系黃土層中轉為向南水平排泄到鹵泊灘。 -
Taking all sorts of factor like cost and storage capability into account, people mostly use tertiary storage equipment like tape library or optical disk library as the primary storage medium to store massive data. at present, a three layer storage system composed of main memory, disk and tertiary storage has already been the primary storage structure of massive data
從成本和存儲容量等因素綜合考慮，目前人們大都採用將磁帶庫、光盤庫等第三級存儲設備作為海量數據的主要存儲介質，並與主存、磁盤一起構成一個三級的存儲系統作海量數據的存儲結構。 -
The basement of the basin is consist of precambrian crystal basement and paleozoic folding basement, while the cover has undergone the evolution of intra - continental rife in permian, down warped basin in triassic - cretaceous period and inter - mountains basin in tertiary. the main sediments are huge - thick volcanic rock, shallow intrusive rock and tuff in early permian, dark mudstone, marl and muddy dolostone in lucaogou formation in middle permian, huge thick volcanic rock, intruder in tiaohu formation in middle permian, miscellaneous sandy gravel, sandstone and gray mudstone in triassic ( the red is under the gray, and huge - thick dark gray, gray sandy gravel, sandstone, mudstone with coal layer in jurassic
盆地基底由前寒武紀結晶基底和古生代褶皺基底組成，盆地蓋層則經歷了二疊紀的裂谷盆地、三疊紀?白堊紀的坳陷盆地和第三紀后的山間盆地的演化過程。盆地主要沉積了下二疊統巨厚火山巖、淺成侵入巖和凝灰巖；中二疊統蘆草溝組的暗色泥巖、泥灰巖、白雲質巖石以及條湖組的巨厚層火山巖、侵入巖；三疊系雜色砂礫巖、砂巖及灰色泥巖（下紅上灰） ；以及侏羅紀厚層深灰、灰色砂礫巖、砂巖、泥巖夾煤層。 -
In research area, the tertiary system ( n ) is water - resisting layer
區內第三系（ n ）隔水。 -
On the basis of previous research view to the boundary of karst - groundwater system in research area, chapter two starts with the natural geography condition of research area and analyzes the condition of geology and hydrogeology carefully. accordingly, several queries are brought out as follow : is the tertiary system ( n ) confining layer
第二章從研究區自然地理條件入手，結合前人研究區巖溶水系統邊界的研究觀點，對研究區的地質、水文地質條件進行了深入分析之後，提出如下問題：第三系（ n ）地層是否為隔水 -
Abstract : based on the geophysical characteristics of each medium in the studied area, combining with the geophysical inversion technique, the location of tertiary thin - layer aquifer is delineated, the top depth of granite basement is identified
文摘:依據區內各介質的地球物理特徵，結合物探數據反演技術，利用直流電測深法，圈定出第三系薄層含水層的位置。
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