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Differences between magnetic and mineral fabrics in low-grade, cleaved siliciclastic pelites: a case study from the Anglo-Brabant Deformation Belt (Belgium)

(2009) TECTONOPHYSICS. 466(1-2). p.32-46
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Cleavage, AMS, Composite fabrics, PARAMAGNETIC COMPONENTS, ROCK MAGNETISM, FOLD BELT, SUSCEPTIBILITY ANISOTROPY, HIGH-FIELD METHODS, PHYLLOSILICATE PREFERRED ORIENTATION, X-ray pole figure goniometry, Low-temperature AMS, POLE FIGURES, STRAIN, MASSIF, TEMPERATURE

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Citation

Please use this url to cite or link to this publication:

Chicago
Debacker, Timothy, Ann M Hirt, Manuel Sintubin, and Philippe Robion. 2009. “Differences Between Magnetic and Mineral Fabrics in Low-grade, Cleaved Siliciclastic Pelites: a Case Study from the Anglo-Brabant Deformation Belt (Belgium).” Tectonophysics 466 (1-2): 32–46.
APA
Debacker, T., Hirt, A. M., Sintubin, M., & Robion, P. (2009). Differences between magnetic and mineral fabrics in low-grade, cleaved siliciclastic pelites: a case study from the Anglo-Brabant Deformation Belt (Belgium). TECTONOPHYSICS, 466(1-2), 32–46.
Vancouver
1.
Debacker T, Hirt AM, Sintubin M, Robion P. Differences between magnetic and mineral fabrics in low-grade, cleaved siliciclastic pelites: a case study from the Anglo-Brabant Deformation Belt (Belgium). TECTONOPHYSICS. 2009;466(1-2):32–46.
MLA
Debacker, Timothy, Ann M Hirt, Manuel Sintubin, et al. “Differences Between Magnetic and Mineral Fabrics in Low-grade, Cleaved Siliciclastic Pelites: a Case Study from the Anglo-Brabant Deformation Belt (Belgium).” TECTONOPHYSICS 466.1-2 (2009): 32–46. Print.
@article{483194,
  author       = {Debacker, Timothy and Hirt, Ann M and Sintubin, Manuel and Robion, Philippe},
  issn         = {0040-1951},
  journal      = {TECTONOPHYSICS},
  keywords     = {Cleavage,AMS,Composite fabrics,PARAMAGNETIC COMPONENTS,ROCK MAGNETISM,FOLD BELT,SUSCEPTIBILITY ANISOTROPY,HIGH-FIELD METHODS,PHYLLOSILICATE PREFERRED ORIENTATION,X-ray pole figure goniometry,Low-temperature AMS,POLE FIGURES,STRAIN,MASSIF,TEMPERATURE},
  language     = {eng},
  number       = {1-2},
  pages        = {32--46},
  title        = {Differences between magnetic and mineral fabrics in low-grade, cleaved siliciclastic pelites: a case study from the Anglo-Brabant Deformation Belt (Belgium)},
  url          = {http://dx.doi.org/10.1016/j.tecto.2008.09.039},
  volume       = {466},
  year         = {2009},
}

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