非碎屑的 的英文怎麼說

中文拼音 [fēisuìxiède]
非碎屑的 英文
nonmechanical
  • : Ⅰ名詞1 (錯誤) mistake; wrong; errors 2 (指非洲) short for africa 3 (姓氏) a surname Ⅱ動詞1 ...
  • : 動詞[書面語] (觸; 撞) strike; bump
  • : Ⅰ名詞(碎末) bits; scraps; crumbs Ⅱ形容詞(瑣碎) trifling Ⅲ動詞(認為值得) think sth. worth doing
  • : 4次方是 The fourth power of 2 is direction
  • 碎屑 : fragment; bits; shard; scrap; refuse; chippings; offal
  1. It is very resembly representative island arc volcanic rock in the geochemistry character, so i demonstrate that a petrofabric formed tectonic activity section and island arc environment ; i also demonstrate that parametamorphite in the a petrofabric formed tectonic activity section. b petrofabric is very resembly a petrofabric in many aspects, so i think that b petrofabric also formed island arc environment, but volcanic activity obvious weakened in the b petrofabric stage. c petrofabric formed carbonatite mesa

    在地球化學特徵方面與典型島弧火山巖常相似,得出a巖組形成於構造活動區,形成環境為島弧環境。 a巖組副變質巖原巖巖是快速堆積,處于構造活動區。 b巖組和a巖組對應巖石在各個方面都常相似,所以形成環境也為島弧環境,只是火山活動在這期間明顯減弱。
  2. This is the direct reason of bad reservoir property of sandstone, especially lower permeability. the influence and control factors of reservoirs include : deposition, diagenesis and tectogenesis. the deposition is the basic factor, it control the shape and distribution of sand body, and influence the type and the intensity of the diagenesis ; the diagenesis is the key factor, it control the process of pore evolvement, so the diagenesis control the sandstone ' s storage space and reservoir quality directly ; the fracture of the tectogenesis formation could improve the porosity and permeability of sandstone

    其中沉積作用是基礎,控制了儲集砂體形態特徵和分佈范圍,同時由於不同沉積類型砂體在成分組成、泥質含量、顆粒粒度、砂體厚度、砂體內部均質性、孔隙介質物理化學性質等方面不盡相同,從而也影響著砂巖所經歷成巖作用路徑、類型和強度,因此沉積作用是控制儲層發育主導因素;成巖作用是關鍵,直接決定了砂巖孔隙演化過程,從而決定了儲層內部儲集空間特徵和儲集性能;而構造作用形成裂縫對改善砂巖儲滲性能具有一定作用。
  3. Along with other data, these results indicate that tempel 1 is not a compacted snowball, as many had conjectured, but a loose, powdery fluff ball ? an agglomerate of primordial dust that came together at low speeds and gently clung like dust bunnies under a bed

    綜合所有數據來分析,譚普一號並如大多數人所猜想,是顆結構緊實大雪球,它比較像是一顆鬆散易毛球,由遠古在低速下緩慢沾黏在一起而形成,就像是床底下那些小毛球。
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