STUDY OF TRIAXIAL CREEP MECHANISM OF MICA-QUARTZ SCHIST BASED ON MICROSCOPIC TEST
(1. College of Geology Engineering and Geomatics,Chang¢an University,Xi¢an,Shaanxi 710054,China;2. Key Laboratory of Western China¢s Mineral Resource and Geological Engineering of Ministry of Education,Chang¢an University,Xi¢an,Shaanxi 710054,China;3. Open Research Laboratory of Geotechnical Engineering of Ministry of Land and Resources,Chang¢an University,Xi¢an,Shaanxi 710054,China;4. State Key Laboratory of Continental Dynamics,Northwest University,Xi¢an,Shaanxi 710069,China)
Abstract:Firstly,the mineral composition of mica-quartz schist samples is determined through visual measurement by polarizing microscope and energy spectrum analysis. The mineral composition of mica-quartz schist is divided into three parts such as hard part,soft part,and defects such as voids and cracks. For these three parts,the hard part is the force skeleton,the other two parts fill in it. Quartz is the hard part,white mica is the soft part in the mica-quartz schist sample. Secondly,in order to study the microstructure changes of mica-quartz schist during triaxial creep process,the polarizing microscope tests and electronic microscope scanning tests are conducted to observe the radial slices and axial slices of mica-quartz schist for three triaxial creep stages,which are no force stage,the upcoming accelerated creep stage and damage stage. According to the test results,the microstructure changes of mica-quartz schist are divided into four kinds,which are closure of open crack,position adjustment of hard part,position adjustment of soft part and micro-damage. At the same time,the micro-damage style of white mica and quartz are summarized separately. Thirdly,through analyzing the reasons for microstructure changes of mica-quartz schist,the creep mechanism is interpreted. It is observed that in different stress levels,and through different loading time of the same stress level,several microstructure changes of above-mentioned four changes of mica-quartz schist will generate,therefore there show attenuation creep stage,constant creep stage and accelerated creep stage,respectively. Lastly,three characteristics of this triaxial creep mechanism for mica-quartz schist based on microscope test are summarized.
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