TEM morphology of the twin specimens at stress plateau stage and martensite section at hardening stage has been observed.
观察到高应变率时应力平台与硬化阶段的TEM组织形貌分别为孪晶与断续的马氏体。
Based on detailed rock magnetic analyses of loess-paleosol sequence at Chaona section in the central loess Plateau, a high-resolution environmental magnetic framework has been built up for last 1.
通过对黄土高原中部朝那剖面黄土-古土壤序列系统的岩石磁学分析，建立了1。
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