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   旋回沉积 的翻译结果: 查询用时:0.616秒
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旋回沉积     
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  cycle depositional
     The section organization of fan body is similar to the reverse cycle depositional order of Walker's (1979) submarine fan, bedding types are analogous to Winn and Dott's (1979) types of submarine fan.
     扇体的剖面结构相似于Walk er(1979)提出的海底扇反旋回沉积序列,层理类型与Winn和Dott(1979)提出的海底扇的层理类型类似;
短句来源
  forcing sedimentary
     ADVANCES IN THE RESEARCH ON ORBITAL FORCING SEDIMENTARY RHYTHM ——A DISCUSSION ON THE IMPLICATIONS TO SEDI MENTOLOGY,CHRONOLOGY AND STUDYING METHODS
     地球轨道旋回沉积节律研究进展——兼论轨道旋回的沉积学特征、年代学意义和研究方法
短句来源
  cyclic deposition
     YOREDALE CYCLIC DEPOSITION AND COMMUNITY SUCCESSION OF BRACHIOPODS
     约代尔旋回沉积与腕足动物群落的演替
短句来源
     Cyclic deposition on a global scale is the product of the changes in sea-level,tectonics,climate, geography and depositional features of the global or the combination of these.
     全球性旋回沉积是全球海平面变化、全球气候条件、全球构造演化、全球古地理背景及沉积特征综合作用的产物。
短句来源
  “旋回沉积”译为未确定词的双语例句
     The deposition of the LT14 can be divided into four cycles and the depositional rate from the oldest to the youngest cycle is 65.22 mm/Ka, 8.37 mm/Ka, 97.09 mm/Ka and 24.39 mm/Ka respectively.
     石笋的沉积基本连续,没有明显的沉积间断,共分为4个旋回,沉积速率从老到新分别为65.22mm/Ka,8.37mm/Ka,97.09mm/Ka,24.39mm/Ka.
短句来源
     Chang4+5~2 upgrowth progradation and reverse cycle and chang4+5~1 upgrowth retrogradation and normal cycle in Jiyuan area.
     姬塬地区长4+5~2主要发育反旋回,以进积方式叠加、长4+5~1主要发育正旋回沉积,以退积方式叠加。
短句来源
     (2)the Middle Triassic Karamay Formation, which is composed of fluvial lacustrine silty mudstone and sandstone, 58~121 m thick;
     中三叠统克拉玛依组为河流—湖泊相粉砂质泥岩与砂岩旋回沉积,厚58~121m;
短句来源
     From MSC1 to MSC4, the sedimentary system of the Formation has changed first from the combination of alluvial fans and braided rivers to the combination of braided rivers and meandering rivers, then to the combination of meandering rivers and braided rivers.
     从MSC1到MSC4旋回,沉积相呈现出冲积扇→辫状河→辫状河→曲流河→曲流河→辫状河相组合的演化过程。
短句来源
     Their petrologic and sedimentary characteristics indicate that depositional environments shifted from shallow marine to deep marine,before returning back to continental facies. There was a sharp break between deep marine and continental facies, indicating a sedimentation hiatus.
     岩石组合及沉积特征反映出,从中—晚侏罗世到白垩纪沉积水深经历了由浅到深,然后又转为陆地的一个完整旋回,沉积环境则经历了由滨浅海相到深海相,又到滨海过渡相和陆相河湖体系的演变过程,在深海相与滨海陆地过渡相之间存在一个明显的环境突变,为沉积环境缺失所致。
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      cyclic sediments
    For the cyclic sediments of the last 2 million years, high-resolution isotope curves were generated which depict the two dominant Milankovitch cycles with periods of 100 000 and 41000 years.
          
    In the Upper Paleozoic cyclic sediments derived from an epiric sea basin were deposited in the intracratonic basin.
          
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