時間標志層 的英文怎麼說

中文拼音 [shíjiānbiāozhìcéng]
時間標志層 英文
time marker
  • : shí]Ⅰ名1 (比較長的一段時間)time; times; days:當時at that time; in those days; 古時 ancient tim...
  • : 間Ⅰ名詞1 (中間) between; among 2 (一定的空間或時間里) with a definite time or space 3 (一間...
  • : Ⅰ名詞1 [書面語] (樹梢) treetop; the tip of a tree2 (枝節或表面) symptom; outside appearance; ...
  • : Ⅰ名詞1 (志向; 志願) aspiration; ambition; ideal; will 2 (文字記錄) records; annals 3 (記號)...
  • : i 量詞1 (用於重疊、積累的東西 如樓層、階層、地層) storey; tier; stratum 2 (用於可以分項分步的...
  • 時間 : time; hour; 北京時間十九點整19 hours beijing time; 上課時間school hours; 時間與空間 time and spac...
  • 標志 : signmarksymbolhallmarkblipemblemdenotationtagensignflagattributemarkerbrandstypeindex
  1. In both definitions the lithologic-time marker is critical because it represents contemporaneity of deposition.

    在兩個定義中,巖石時間標志層是關鍵的,因為它代表著同沉積。
  2. Caco3 not only affects soil physical and chemical characteristics but also causes co2 change in the air, because caco3 is main components among the total pool of inorganic carbon of soil. this paper systematically summarized and analyzed general development characteristics of soil profile caco3 in loess hill gully area including source, content, forming - condition, distribution and illuviation - depth of caco3, which will have the most important significance for the further studies on global soil and climate change

    碳酸鈣在土壤剖面中淀積的深度和類型是黃土高原土壤發育的重要,鈣積是黃土高原土壤發育環境的歷史信息庫,同土壤碳酸鈣作為土壤無機碳庫重要組成,它通過溶蝕后再結晶與大氣co _ 2之進行物質交流來影響全球氣候變化。
  3. Judicial use of the lithologic time marker makes it possible to identify the type of sandstone body.

    審慎地應用巖性時間標志層,可以鑒定沙巖體的類型。
  4. Both types of traps are identified and analyzed best in the subsurface by relating them to lighologic time marker.

    這兩類圈閉根據其與巖性時間標志層的關系而極易進行地下的鑒定與分析。
  5. Judicial use of the lithologic time marker makes it possible to identify the type of sandstone body

    審慎地應用巖性? ?時間標志層,可以鑒定沙巖體的類型。
  6. Both types of traps are identified and analyzed best in the subsurface by relating them to time marker

    根據其與時間標志層的關系極易對這兩類圈閉進行地下的鑒定與分析。
  7. For a moment he could not find malfoy anywhere, and assumed he must be inside the room of requirement again, but then he saw malfoy ' s tiny, labelled dot standing in a boys ' bathroom on the floor below, accompanied, not by crabbe or goyle but by moaning myrtle

    ,哈利繞道沿著七樓走廊走,同查看著活點地圖,有一段,他在哪裡都找不到馬爾福,他猜想馬爾福一定又在有求必應屋,但是之後他發現馬爾福的微小的點著他在樓下一的男盥洗室中,陪伴他的,不是克拉布,也不是高爾,而是哭泣的桃金娘。
  8. Variations in the reflection times from place to place on the surface usually indicate structural features in the strata below.

    反射波在地面從一處到另一處的變化,通常是地下巖構造特徵的
  9. The yanchang formation was divided into five lithologic segments and ten oil - bearing packages according to the features of lithology. the chang - 6 oil - bearing beds was subdivided into chang - 61, chang - 62, chang - 63 and chang - 64. and the time correlation in sequence stratigraphic unit was realized according to the temporal rock maker

    根據巖性特點以及含油性本文將川口油田延長組分成5個巖性段和10油組,其中根據巖性將長6油組進一步劃分為長6 ~ 1 、長6 ~ 2 、長6 ~ 3與長6 ~ 4 ,並根據巖性在等格架內進行了地對比。
  10. The main conclusions are as follows. cross - fault displacement observation can directly reflect the recent activities of the major faults in the region. present fault movement and earthquake activity have a temporal correspondence with each other, they all show alternately quiet and active periods. the intensity of fault movement is a manifestation of the strength of regional principal compressional stress, it also indicates the strength of an earthquake in preparation

    認為: 1 )跨斷位移觀測資料能夠直接反映區內主要斷的最新活動情況; 2 )斷現今活動與地震活動在序列上相互對應,均有活躍期與平靜期相互交替出現的活動特徵; 3 )斷活動強弱是區域主壓應力強弱的表現,亦是孕震強度的
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