tectonic lake 中文意思是什麼

tectonic lake 解釋
構造湖
  • tectonic : adj. 1. 構造的;建築的。2. 【生物學】構造的。3. 【地質學;地理學】地殼構造上的,起因於地殼運動的。
  • lake : n. 萊克〈姓氏〉。n. 1. 湖(公園等中的)池塘,小湖。2. (貯油等的)池。n. 1. 【化學】色淀;沉澱染料。2. 胭脂紅。vi. 血球溶解。vt. 使(血液)發生血球溶解。
  1. Besides, the sedimentary facies of upper ganchaigou and lower ganchaigou formation were also mapped in supersequences which are the main target strata for exploration. the high resolution sequence stratigraphic framework showed the genetic relationship between the distributions of sedimentary facies and their tectonic settings. the near - source sedimentary systems such as subaqueous alluvial fan and lake - floor fan are often deposed in rise - hemicycles in the steep slope background in the north, the coarse lithology of fan - delta prograded from north to south in fall - hemicycles, and the braided stream facies are formed in the rise - hemicycles in gentle slope background in the south, braided stream facies prograded from sorth to north in the fall - hemicycles, but the lacustrine facies and salt lake facies developed in the middle part of the area

    詳細的沉積相研究發現,紅獅地區第三系發育有沖積扇、水下沖積扇、河流、三角洲、扇三角洲、湖泊和湖底扇7種主要沉積相類型,並對作為區內主要勘探目的層系的下乾柴溝組和上乾柴溝組進行了以超層序為單位的沉積相平面編圖,以較高的時間解析度揭示了區內沉積相帶的平面展布及其在不同構造背景中的分佈規律,比如在北部的凹陷陡坡背景下,上升半旋迴低水位期通常發育有水下扇、湖底扇等陡岸近源特徵的沉積體系,下降半旋迴高水位期,扇三角洲相粗碎屑巖由北向南進積;在南部的凹陷緩坡背景下,上升半旋迴主要發育辮狀河流相,下降半旋迴辮狀河三角洲相由南向北進積;而中部紅柳泉一獅子溝一帶則為湖泊相沉積和鹽類沉積。
  2. Geochemistry of early cretaceous alkaline rhyolites from hulun lake, daxing ' anling and its tectonic implications

    呼倫湖早白堊世堿性流紋巖的地球化學特徵及其意義
  3. ( 5 ) by analyzing the terrace in the lacustrine sediment of the ancient barrier lake, diexi, minjiang river, forming of the terrace is not only because of the intermittent arising of the tectonic movement, but also because of descend of the eroding normal covering resulting from destroying of the barrier lake

    ( 5 )通過對岷江疊溪古堰塞湖湖相沉積中的河流階地分析可知,階地的形成不僅僅是由於新構造運動的間歇性抬升作用,由於堰塞湖的潰決引起洪水下泄,導致河流侵蝕基準面的下降也可以形成階地。
  4. The formation and evolution of the sequence stratigraphy of the yanchang formation are governed by slow tectonic subsidence, warm humid climates, sediment supply and lake - level fluctuations

    延長組層序地層的形成與演化主要受控于當時緩慢的構造沉降、溫濕氣候、陸源碎屑物源供給及湖平面升降等地質因素。
  5. Based on an integrated analysis of the surface geological, aeromagnetic, gravity, mt and seismic data from the area of mangnai to serteng mountains in the western qaidam basin, the authors think that the qaidam basin is sandwiched between the north kunlun block and serteng tectonic belt, including two first - order tectonic units the qaidam block and the southern margin of the qilian block and four second - order tectonic units the northern margin of the north kunlun block, qaidam basin, serteng tectonic belt and suhai lake basin in the south of the qilian block

    摘要通過柴達木盆地西部茫崖賽什騰山地表地質、航磁、重力、大地電磁測深和地震資料的綜合分析,認為柴達木盆地夾持在昆北地塊與賽什騰構造帶之間,其中包括柴達木地塊與祁連地塊南緣2個一級構造單元和昆北地體北緣,柴達木盆地,賽什騰構造帶和祁連地塊南部的蘇干湖盆地等4個二級構造單元。
  6. The archipelagic arc tectonic evolution of the meso - tethys in the western part of the bangong lake - nujiang suture zone

    怒江結合帶西段中特提斯多島弧構造演化
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