Item request has been placed! ×
Item request cannot be made. ×
loading  Processing Request

Mineralogy and microstructure of roofing slate: thermo-optical behaviour and fissility ; Mineralogía y microestructura de la pizarra de techar: comportamiento termooptico y fisibilidad

Item request has been placed! ×
Item request cannot be made. ×
loading   Processing Request
  • المؤلفون: García-Guinea, J.; Lombardero, M.; Roberts, B.; Taboada, J.; Peto, A.
  • المصدر:
    Materiales de Construcción; Vol. 48 No. 251 (1998); 37-48 ; Materiales de Construcción; Vol. 48 Núm. 251 (1998); 37-48 ; 1988-3226 ; 0465-2746 ; 10.3989/mc.1998.v48.i251
  • نوع التسجيلة:
    article in journal/newspaper
  • اللغة:
    English
  • معلومة اضافية
    • بيانات النشر:
      Consejo Superior de Investigaciones Científicas
    • الموضوع:
      1998
    • Collection:
      Materiales de Construcción (E-Journal)
    • نبذة مختصرة :
      The mineralogy and microstructure, which affect the slaty cleavage, are linked with the strong preferred orientation of phyllosilicates and this enables the rock to be split into large, thin, flat sheets. Roofing slate samples with different commercial fissilities have been analyzed by radioluminescence (RL), thermoluminescence (3DTL), by X-ray diffraction (XRD), by scanning electron microscopy (SEM) using the back-scattered mode (BSEI) and by electron microprobe (EMP). They are made up of white micas, chlorite, quartz, detrital feldspars, ilmenite, pyrite, rutile apatite and tourmaline. Texturally, all consist of silt-sized clasts of detrital quartz, feldspars, chlorite-mica stacks, muscovite and ilmenite in a recrystalline, lepidoblastic matrix of white micas and chlorite with quartz lenses, all showing a very strong preferred orientation. The luminescence emission centers are a low broad blue band around the 400 nm spectra positions linked with alkali losses and formation of [AlO4]º defects; a peak at 473 nm interpreted as a the first thermal step (150-300ºC) of a non-isothermal dehydroxylation of the slate phyllosilicates; and a 568 nm peak which agrees with Mn2+ point defects in aluminosilicate lattices. The studies on the slaty cleavage could be significant because Spain is the largest producer of roofing slate tiles in the world (87% of world production). ; La exfoliación de las pizarras depende fundamentalmente de su mineralogía y microestructura, especialmente de la fuerte orientación de los filosilicatos. Esta propiedad permite hendir o abrir las pizarras de techar en láminas muy grandes, delgadas y planas. Se han analizado varias pizarras de techar con diferentes calidades comerciales, correspondientes a diferentes grados de físibilidad, por radioluminiscencia (RL), termoluminiscencia espectral (TL3D), difracción de rayos X (DRX), microscopía electrónica de barrido (MEB) utilizando el modo backscattered (BSEI) y microsonda electrónica (ME). Las muestras están compuestas por micas blancas, clorita, ...
    • File Description:
      application/pdf
    • Relation:
      https://materconstrucc.revistas.csic.es/index.php/materconstrucc/article/view/470/517; https://materconstrucc.revistas.csic.es/index.php/materconstrucc/article/view/470
    • الرقم المعرف:
      10.3989/mc.1998.v48.i251.470
    • الدخول الالكتروني :
      https://materconstrucc.revistas.csic.es/index.php/materconstrucc/article/view/470
      https://doi.org/10.3989/mc.1998.v48.i251.470
    • Rights:
      Copyright (c) 1998 Consejo Superior de Investigaciones Científicas (CSIC) ; https://creativecommons.org/licenses/by/4.0
    • الرقم المعرف:
      edsbas.81F29312