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体区的英文

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"体区"怎么读用"体区"造句

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  • tagma

例句与用法

  • Treatment of tumors in the pineal region by x knife radiosurgery
    刀立体定向放射神经外科技术治疗松果体区肿瘤
  • The effect of the structure of austenite zone on the performance of gray iron welding joint is studied by means of thermo - simulated test in this paper
    摘要采用热模拟试验方法探讨了灰口铸铁焊接接头热影响区的奥氏体区组织对接头性能的影响。
  • Combining with the results of implant test , the conclusion that the main reason of dropping the strength of austenite zone is the micro - crack located in the tip of flake graphite and marten site is drawn
    结合插销试验结果提出了马氏体相变过程中,在片状石墨尖端及马氏体组织中造成的微裂纹是奥氏体区强度下降并进而在外力作用下断裂的主要原因。
  • Abstract : in this paper , pesent the development and trends in chemi cal component controlling , hot rolling and coiling processing , ferritic hot rollin g , trip steel processing , cool rolling , annealing and surface quality controlling f or deep drawing sgeet steels are analyzed and discussed
    文摘:分析讨论了目前国内外在深冲用薄板生产中的成分控制、热轧、卷曲工艺、铁素体区轧制、 trip钢生产、冷轧与退火工艺以及钢板表面质量控制方面的新进展和趋势
  • The fault controlled the magmatism and metallization relevant to the contact zone , and deformed successively and produced cataclastic rocks and two sets of joints ; the second stage was from late cretaceous to eocene . the fault zone deformed right - laterally under ne - sw striking transtention , and new joints zone was produced at the end of the two main faults because of local stress concentration . the fault produced inchoative cataclastic rocks , and two sets of typical joints in plutons ; the third stage of deformation was relatively faint and only a little of microcracks was produced and infilled with vei ns in the deformed rocks , which was during the himalayan movement
    其后的继承性活动在断裂带内形成碎裂程度最强达到碎裂岩的碎裂岩系列构造岩,变形带两侧发育两组典型的共轭剪节理;第二次在晚白垩世?始新世,断裂在北东?南西向近水平挤压作用下右行张扭性活动,断裂带两主断裂在斜列重叠的端部由于局部应力集中进一步扩展形成节理带,而断裂在岩体区也发育两组典型的共轭剪节理,断裂内形成初碎裂岩为主的构造岩;第三次是喜山期以西侧抬升、东侧下降的强烈升降为主的活动,在基岩中,主断层两侧围岩出现微破裂。
  • The most favorable reservoirs of study formatioms in study area are delta river mouth bar sand body and sublacustrine fan sand body . the sublacustrine fan sand body region developed in each sand group and the river mouth bar sand body region developed in gao 5 sand - group are the most favorable regions of developing lithologic traps
    研究区研究层段的最有利储层是三角洲河口坝砂体和湖底扇砂体,各砂组发育的湖底扇砂体区和高5砂组发育的河口坝砂体发育区是形成岩性圈闭最有利的场所。
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