始成巖階段的英文怎麼說

中文拼音 [shǐchéngyánjiēduàn]
始成巖階段英文
eogenetic stage

  • : Ⅰ名詞1 (最初; 起頭) beginning; start 2 (姓氏) a surname Ⅱ動詞(開始) start; begin Ⅲ副詞[書面...
  • : Ⅰ動詞1 (完成; 成功) accomplish; succeed 2 (成為; 變為) become; turn into 3 (成全) help comp...
  • : 名詞1. (巖石) rock 2. (巖峰) cliff; crag
  • : 名詞1. (臺階) steps; stairs 2. (等級) rank 3. [醫學] (耳蝸的三個螺旋管的任一個) scala 4. [數學] order 5. [地質學] stage
  • : Ⅰ量詞(部分) section; segment; part; paragraph; passage Ⅱ名詞(姓氏) a surname
  • 階段: stage; phase; period; gradation; bench

※中文詞彙始成巖階段在字典百科國語字典中的解釋。

  1. The division of diagenetic stages in clastic rocks

    碎屑劃分
  2. Among of them, carbonate rock is the primary type of them, it is the product of stable platform facies of marine. we study the geochemical characteristic of carbonate rock of lower palaeozoic burial hills in the regions of zhuangxi and chengdao and find that the calcite fillings in cave or vein have high value of 87sr / 86sr, low value of 13c and 18o and high mn content among of different structural components. so it has been exposed to be dissolved by meteoric water on supcrgene diagenetic stage

    通過對樁西、埕島地區下古生界碳酸鹽的地球化學特徵研究,表明在石的各種結構組分中,洞或脈中的方解石充填物具有顯著較高的~ ( 87 ) sr ~ ( 86 ) sr比值,較低的~ ( 13 ) c 、 ~ ( 18 ) o和較高的mn含量,其所經歷的重要溶作用是大氣淡水作用,發生的時間為表生
  3. The acidic liquid related to decomposition of organic mater during hydrocarbon enrichment in the late diagenesis, and m eteoric - waters during epidiagenesis, had resulted in dissolution of detrital feldspars and carbonate cements, which contributed a better retention of reservoir quality for the sandstones

    溶蝕作用是砂物性改善的主要原因,尤其是晚期,在富含有機酸和無機酸酸性孔隙流體的作用下形一定量的次生溶蝕孔,使儲層砂物性得到一定改善;在表生,由於大氣降水的介入,儲層物性再次得以改善。
  4. After 20 years of development, china ’ s family business currently is in the key growth phase of transition from its extensive primitive accumulation of capital to intensive scientific management

    我國家族企業經過20多年的發展,目前正處于從粗放型資本原積累向集約型科學化管理過渡的關鍵
  5. The pattern of diagenetic and porosity evolution are established. the primary porosity of the reservoir rocks was 35 %, which was reduced by 21. 7 % by compaction and pressure solution and 8. 2 % by cementation. the secondary pores were produced by organic acids " dissolution during organic matter maturing stage, resulting an increase of porosity by 5 %

    預測本區砂孔隙度為35 ,經機械壓實和化學壓溶作用孔隙度損失了21 . 7 ,后經自生礦物的膠結作用,孔隙度損失了8 . 2 ,當進入有機質,有機酸的溶解作用產生次生孔隙,使孔隙度增加5 ,現今保存的平均孔隙度為10 . 1 。
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