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萎缩期 meaning in English

atrophy stage

Examples

  1. Situation in fruit production : fruit production in hangzhou may be classified into three phases : shrinking , recovering and rapidly increasing ones during the past 13 years . despite some fluctuations , there was an increasing trend both in total fruit production and economic value
    近十三年来,杭州市水果生产经历了萎缩期、恢复期和快速增长期三个阶段,水果产量呈现出波动式增长态势,但产值呈稳定快速增长态势。
  2. Comparison and study of the biotic characters in the jinggu and longchuan basins in yunnan province show that : ( 1 ) the two basins underwent the developing period , expanding period and shrinking period from early miocene epoch to pliocene epoch ; ( 2 ) the climate in the region was dry in early miocene epoch , warm and humid in middle - late miocene epoch and dry in pliocene period ; ( 3 ) the basins expanding in middle - late miocene epoch formed a semi - deep - lake to deep - lake environment
    通过对云南景谷盆地及陇川盆地新生代生物群特征的对比,探讨了新生代两大盆地环境演变:早中新世到上新世为湖盆发展期湖盆扩大萎缩期,气候为早期的千燥中新世早期的温暖湿润中新世中晚期的寒冷阴湿上新世的干燥,而中新世中晚期湖盆的扩大形成的半深湖深湖环境为油气的形成提供了有利条件。
  3. From evolution of sedimentary , chang 6 sandstones is a process of growing , development , fast development and shrinkage term . among them , chang 621 and 612 sandstone is in fast development period , forming many oil - gas gatherings . due to study area lie in the front part of deltas , so the factors of sedimentology are simple
    从沉积演化来看,长6砂层三角洲的发展经历了成长期?发展期?高速生长推进期和萎缩期的完整过程,其中6 _ 2 ~ 1和长6 _ 1 ~ 2砂体发育处于高速生长推进期,是最有利于油藏形成的时期。
  4. Abstract : comparison and study of the biotic characters in the jinggu and longchuan basins in yunnan province show that : ( 1 ) the two basins underwent the developing period , expanding period and shrinking period from early miocene epoch to pliocene epoch ; ( 2 ) the climate in the region was dry in early miocene epoch , warm and humid in middle - late miocene epoch and dry in pliocene period ; ( 3 ) the basins expanding in middle - late miocene epoch formed a semi - deep - lake to deep - lake environment
    文摘:通过对云南景谷盆地及陇川盆地新生代生物群特征的对比,探讨了新生代两大盆地环境演变:早中新世到上新世为湖盆发展期湖盆扩大萎缩期,气候为早期的千燥中新世早期的温暖湿润中新世中晚期的寒冷阴湿上新世的干燥,而中新世中晚期湖盆的扩大形成的半深湖深湖环境为油气的形成提供了有利条件。

Related Words

  1. 牙萎缩
  2. 急性萎缩
  3. 萎缩卵泡
  4. 灰质萎缩
  5. 局限性萎缩
  6. 毛发萎缩
  7. 淋巴细胞萎缩
  8. 眼萎缩
  9. 舌萎缩
  10. 半面萎缩
  11. 萎缩黄体
  12. 萎缩卵泡
  13. 萎缩肾
  14. 萎缩纹
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