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《Progress in Geophysics》 2015-05
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The trace amount water in quartz and feldspar with secondary fluid inclusions and its geological significance

HAN Liang;ZHOU Yong-sheng;LI Hai-bing;State Key Laboratory for Continental Tectonics and Dynamics,Institute of Geology,Chinese Academy of Geological Sciences;State Key Laboratory of Earthquake Dynamics,Institute of Geology,China Earthquake Administration;  
We collected three kinds of felsic rocks with different deformation in the Longmen Shan thrust tectonic belt,and measured water contents in quartz and feldspar including some secondary fluid inclusions using Fourier transform infrared spectroscopy(FTIR),as well as comparison with the results without secondary fluid inclusions.The absorbance spectra including secondary fluid inclusions show broadband absorbance with strong peaks ranging from 3380 to 3450cm-1,and the absorbance coefficient are higher than those without secondary fluid inclusions.The curves are very smooth that most of other peaks are difficult to be distinguished except for weak peaks at3200cm-1,3650 cm-1 and 3730 cm-1. Water content of feldspar with secondary fluid inclusions in three samples is0.022 to 0.103wt% H2 O,which is higher than that of 0.011 to 0.031wt%in quartz,and water content increase with rock deformation firstly and reduce subsequently.The water content of quartz and feldspar with secondary fluid inclusions is not precise and could not represent the trace amount water in minerals,but it agrees with the fluid flow in micro-cracks.Therefore,it indirectly indicates that the fluid flow in the fault margin is higher than that in the fault center during the postseismic creep period.
【Fund】: 自然科学基金项目(41302169 40972146)资助
【CateGory Index】: P315.2
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