内蒙古塔木素地区断层铁化学种特征及其对断层活动性的指示
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摘要
塔木素地区的构造稳定性对其作为高放射性废料处置预选地至关重要,需要进行全方位系统调查与安全评价。结合野外地质资料,利用X射线衍射和穆斯堡尔谱技术对该地区3条断层的断层泥及其围岩进行矿物组成和铁化学种分布特征研究发现:(1)塔木素断层(F2)围岩和断层泥主要以石英、长石为主,断层泥中含少量粘土矿物而其围岩几乎不含粘土矿物;样品中均只含氧化性铁。(2)乌兰铁布科断层(F4)围岩和断层泥中矿物以粘土矿物和方解石为主,见有微量黄铁矿,粘土矿物主要为伊利石、蒙脱石、伊蒙混层;断层围岩中只含还原性铁,但断层泥中含有少量的氧化性铁。(3)除样品TMS04不含方解石,那仁哈拉断层(F7)围岩和断层泥均含石英、长石和粘土矿物及少量方解石,粘土矿物主要为绿泥石和伊利石、蒙脱石;在断层泥及围岩中均检测到氧化性铁和还原性铁,除TMS04中氧化性铁含量较高于还原性铁以外,其余所有样品中氧化性铁含量均稍低于还原性铁。断层泥和断层围岩的矿物组成和铁化学种分布特征与断层的发展演化密切相关,其差异性显示塔木素地区断层与深部和外界的复杂连通性关系,总体显示断层处于相对稳定状态。
The tectonic stability of the Tamusu region is crucial for its pre-selection as a high-level radioactive waste disposal site,and comprehensive system investigations and safety assessments are required. Combined with field geological data,Mineral composition and iron species of fault gouges and its wall rocks in three fault zones of Tamsu area had been analyzed by the X-ray diffraction and the Mossbauer spectroscopy. The results showed that,(1)the fault gouge and its wall rock of Tamusu fault( F2) mainly consist of quartz and feldspar,the fault gouge contains a small amount of clay minerals and the wall rocks contain almost no clay minerals,the fault gouge and its wall rock only contain para-Fe3+and mag-Fe3+;(2)The fault gouge and its wall rock of Wulantiebuke fault( F4) are dominated by clay minerals and calcite with trace amounts of pyrite,the clay minerals are mainly illite,smectite and illite mixed layer,the iron species of wall rock only contain para-Fe2+and pyr-Fe2+,whereas the fault gouge contains a small amount of para-Fe3+;(3) Except the TMS04 do not contain calcite,he fault gouges and its wall rocks of Narenhala fault( F7) consist of quartz,feldspar,clay minerals and a small amount of calcite. Clay minerals are mainly composed of chlorite,illite and smectite. The fault gouges and wall rocks only detected the para-Fe2+and para-Fe3+. The para-Fe3+in TMS04 was higher than that of para-Fe2+,and the para-Fe2+in all samples was slightly higher than that of para-Fe3+. The mineral composition and iron species distribution of fault gouges and wall rocks were closely related to the evolution of faults, and their differences showed that the complex connectivity relationships between the faults and the deep and the outside world in the Tamusu region,and the faults are in a relatively stable state.
The tectonic stability of the Tamusu region is crucial for its pre-selection as a high-level radioactive waste disposal site,and comprehensive system investigations and safety assessments are required. Combined with field geological data,Mineral composition and iron species of fault gouges and its wall rocks in three fault zones of Tamsu area had been analyzed by the X-ray diffraction and the Mossbauer spectroscopy. The results showed that,(1)the fault gouge and its wall rock of Tamusu fault( F2) mainly consist of quartz and feldspar,the fault gouge contains a small amount of clay minerals and the wall rocks contain almost no clay minerals,the fault gouge and its wall rock only contain para-Fe3+and mag-Fe3+;(2)The fault gouge and its wall rock of Wulantiebuke fault( F4) are dominated by clay minerals and calcite with trace amounts of pyrite,the clay minerals are mainly illite,smectite and illite mixed layer,the iron species of wall rock only contain para-Fe2+and pyr-Fe2+,whereas the fault gouge contains a small amount of para-Fe3+;(3) Except the TMS04 do not contain calcite,he fault gouges and its wall rocks of Narenhala fault( F7) consist of quartz,feldspar,clay minerals and a small amount of calcite. Clay minerals are mainly composed of chlorite,illite and smectite. The fault gouges and wall rocks only detected the para-Fe2+and para-Fe3+. The para-Fe3+in TMS04 was higher than that of para-Fe2+,and the para-Fe2+in all samples was slightly higher than that of para-Fe3+. The mineral composition and iron species distribution of fault gouges and wall rocks were closely related to the evolution of faults, and their differences showed that the complex connectivity relationships between the faults and the deep and the outside world in the Tamusu region,and the faults are in a relatively stable state.
引文
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