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铁含量对滑石脱水动力学的影响及其地质意义

张瑞鑫, 易丽, 刘红, 杨思宇

张瑞鑫, 易丽, 刘红, 杨思宇. 2017: 铁含量对滑石脱水动力学的影响及其地质意义. 地质通报, 36(6): 1051-1055.
引用本文: 张瑞鑫, 易丽, 刘红, 杨思宇. 2017: 铁含量对滑石脱水动力学的影响及其地质意义. 地质通报, 36(6): 1051-1055.
ZHANG Ruixin, YI Li, LIU Hong, YANG Siyu. 2017: The effect of iron content on the kinetics of talc dehydration and its geological significance. Geological Bulletin of China, 36(6): 1051-1055.
Citation: ZHANG Ruixin, YI Li, LIU Hong, YANG Siyu. 2017: The effect of iron content on the kinetics of talc dehydration and its geological significance. Geological Bulletin of China, 36(6): 1051-1055.

铁含量对滑石脱水动力学的影响及其地质意义

基金项目: 

国家自然科学基金项目《俯冲带含水矿物脱水动力学实验研究》 41373060

川滇国家地震预报实验场专项《实验场区水化典型异常机理探索》 20150112

中国地震局地震预测研究所基本科研业务费专项《俯冲带含水矿物脱水速率实验研究》 2014IES0407

《(Mg, Fe)SiO3钙钛矿的相稳定性研究》 2012IES0408

详细信息
    作者简介:

    张瑞鑫(1990-), 男, 在读硕士生, 从事含水矿物脱水动力学研究。E-mail:714895277@qq.com

    通讯作者:

    易丽(1974-), 女, 博士, 副研究员, 从事地震前兆机理研究。E-mail:hnyili@126.com

  • 中图分类号: P578.958

The effect of iron content on the kinetics of talc dehydration and its geological significance

  • 摘要:

    在常压下研究了2种不同铁含量滑石的原位X射线衍射高温脱水反应。选取粒径2~5μm的2种不同铁含量的滑石样品,在常压、空气氛围下进行了同步辐射原位X射线衍射脱水实验。实验结果表明,铁含量高的滑石脱水温度明显偏低,2个滑石样品在常压下发生明显脱水反应的温度相差达127℃以上。滑石在常压下的脱水动力机制为随机成核和生长机制,符合Avrami方程。将实验数据拟合Avrami方程得出:n=1.669。由实验结果可以推测,不同铁含量的滑石脱水深度可能有几十到上百千米的差别,研究铁含量与滑石脱水动力的相关性对于了解俯冲带浅-中源地震的成因机制具有重要意义。

    Abstract:

    The effect of iron content on the kinetics of talc dehydration was studied with talc of different iron values using in-situ synchrotron X-ray diffraction (XRD).The sample particle size is 2~5μm.The air atmosphere synchrotron radiation in situ XRD de-hydration experiment was carried out under atmospheric pressure.High content of iron obviously resulted in lower dehydration tem-perature.The difference of the dehydration temperature of two samples was above 127℃.The dehydration of talc followed random nucleation and growth mechanism, and fitted Avrami equation, with n being 1.669.The results suggest that the dehydration of differ-ent iron values of talc may occur at the different depths around hundreds of kilometers, so the study was significant to the understand-ing of the genetic mechanism of earthquakes in the subduction zone.

  • 致谢: 感谢中国科学院上海应用物理研究所文闻老师在X射线衍射实验过程中给予的巨大帮助。
  • 图  1   实验装置示意图

    Figure  1.   The sample assembly of dehydration experiment

    图  2   1号滑石脱水反应XRD图谱(915℃恒温)

    Tlc—滑石;En—顽火辉石;Qt—石英

    Figure  2.   The XRD spectrum of No 1 talc dehydration

    图  3   2号滑石脱水反应XRD图谱(700~910℃)

    Tlc—滑石;En—顽火辉石;Qt—石英

    Figure  3.   The XRD spectrum of No.2 talc dehydration

    图  4   1号、2号滑石最强衍射峰强度在脱水反应期间的变化(2θ=4.16686°)

    Figure  4.   The change of the strongest diffraction peaks of No.1 and No.2 talc dehydration

    图  5   1号滑石脱水反应中滑石和顽火辉石的XRD图谱(915℃恒温)

    Tlc—滑石;En—顽火辉石

    Figure  5.   The XRD spectra of talc and enstatite in No.1 talc dehydration

    图  6   1号滑石2=4.16686°拟合的Avrami方程

    Figure  6.   The fitting Avrami equation with No.1 talc

    表  1   滑石的组成成分

    Table  1   The composition of two kinds of talc

    %
    编号 SiO2 TiO2 FeO MgO CaO2 K2O Na2O Al2O3 Cr2O3 P2O5 LOI 总计
    1 62.35 0.01 0.50 31.31 0.08 0.05 0.01 0.10 0.08 0.04 5.74 100.20
    2 63.269 0.012 2.532 29.650 0.023 0.039 0.069 0.055 0.050 95.714
        注:1号滑石为X射线荧光分析结果;2号滑石为电子探针分析结果
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  • 余日东, 金振民.蛇纹石脱水与大洋俯冲带中源地震(70~300km)的关系[J].地学前缘, 2006, 13(2):191-204. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY200602021.htm

    Larson K M, Kostoglodov V, Miyazaki S, et al. The 2006 aseismic slow slip event in Guerrero, Mexico:New results from GPS[J]. Geo-physical Research Letters, 2007, 34(13):256-260. doi: 10.1029/2007GL029912/full

    Song T R, Helmberger D V, Brudzinski M R, et al. Subducting slab ultra-slow velocity layer coincident with silent earthquakes in south-ern Mexico[J]. Science, 2009, 324(5926):502-6. doi: 10.1126/science.1167595

    Kim Y, Clayton R W, Jackson J M. Geometry and seismic proper-ties of the subducting Cocos plate in central Mexico[J]. Journal of Geophysical Research Atmospheres, 2010, 115(B6):258-273. doi: 10.1029/2009JB006942/full

    Moore D E, Lockner D A. Talc friction in the temperature range 25°-400° C:Relevance for Fault-Zone Weakening[J]. Tectono-physics, 2008, 449(1):120-132. https://pubs.er.usgs.gov/publication/70032195

    Mysen B O, Ulmer P, Konzett J, et al. The upper mantle near con-vergent plate boundaries[J]. Reviews in Mineralogy, 1998, 37:97-138. http://rimg.geoscienceworld.org/content/37/1/97

    Bose K, Ganguly J. Thermogravimetric study of the dehydration ki-netics of talc[J]. American Mineralogist, 1994, 79(7):692-699. https://arizona.pure.elsevier.com/en/publications/thermogravimetric-study-of-the-dehydration-kinetics-of-talc

    Chollet M, Daniel I, Koga K T, et al. Dehydration kinetics of talc and 10Å phase:Consequences for subduction zone seismicity[J]. Earth & Planetary Science Letters, 2009, 284(1/2):57-64. http://www.sciencedirect.com/science/article/pii/S0012821X09002271

    Wang D, Karato S I. Electrical conductivity of talc aggregates at 0.5GPa:influence of dehydration[J]. Physics & Chemistry of Miner-als, 2012, 40(1):11-17. doi: 10.1007/s00269-012-0541-9

    Zhang M, Hui Q, Lou X J, et al. Dehydroxylation, proton migra-tion, and structural changes in heated talc:An infrared spectroscop-ic study[J]. American Mineralogist, 2006, 91(5):816-825.

    Taylor H F W, Taylor H F W. Homogeneous and Inhomogeneous Mechanisms in the Dehydroxylation of Minerals[J]. Clay Minerals, 1962, 5(28):45-55. doi: 10.1180/claymin

    Molinamontes E, Donadio D, Hernándezlaguna A, et al. Water Re-lease from Pyrophyllite during the Dehydroxylation Process Ex-plored by Quantum Mechanical Simulations[J]. Journal of Physical Chemistry C, 2013, 117(15):7526-7532. doi: 10.1021/jp310739y

    Wang D, Yi L, Huang B, et al. High-temperature dehydration of talc:a kinetics study using X-ray powder diffraction[J]. Phase Tran-sitions, 2015, 88(6):1-7. doi: 10.1080/01411594.2014.1002092?needAccess=true&journalCode=gpht20

    王艳, 王多君, 易丽.空气气氛中滑石的热分解动力学实验研究[J].中国科学院大学学报, 2015, 32(1):70-73. http://www.cnki.com.cn/Article/CJFDTOTAL-ZKYB201501013.htm

    Avrami M. Kinetics of Phase Change 2[J]. Journal of Chemical Physics, 1939, 7(12):1103-1112. doi: 10.1063/1.1750380

    Avrami M. Kinetics of Phase Change:Ⅱ. Transformation-Time Relation for Random Distribution of Nuclei[J]. Journal of Chemi-cal Physics, 1940, 8(2):212-224. doi: 10.1063/1.1750631

    Collettini C, Viti C, Smith S A F, et al. Development of intercon-nected talc networks and weakening of continental low-angle nor-mal faults[J]. Sem. Hop., 2009, 33(6):2102-16. https://www.researchgate.net/publication/240305277_Cation_disordering_in_dolomitetheoretical_and_experimental_approach

    Omori S, Komabayashi T, Maruyama S. Dehydration and earth-quakes in the subducting slab:empirical link in intermediate and deep seismic zones[J]. Physics of the Earth &Planetary Interiors, 2004, 146(1/2):297-311. http://www.sciencedirect.com/science/article/pii/S0031920104001293

    Syracuse E M, Keken P E V, Abers G A. The global range of sub-duction zone thermal models[J]. Physics of the Earth & Planetary Interiors, 2010, 183(1/2):73-90. http://www.sciencedirect.com/science/article/pii/S0031920110000300

    申婷婷, 张立飞, 陈晶.俯冲带蛇纹岩的变质过程[J].岩石学报, 2016, 32(4):1206-1218. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201604019.htm

    Mohsen M D. Dictionary of Gems and Gemology[M]. Springer Berlin Heidelberg. 2009:575.

    赵永红, 施旭, Zimmerman, M, 等.含水对富铁橄榄石流变性的影响[J].岩石学报, 2006, 22(9):2381-2386. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200609013.htm
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出版历程
  • 收稿日期:  2016-12-19
  • 修回日期:  2017-04-27
  • 网络出版日期:  2023-08-15
  • 刊出日期:  2017-05-31

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