Origin of felsic granulite microstructure by heterogeneous decomposition of alkali feldspar and extreme weakening of orogenic lower crust during the Variscan orogeny

  1. J. FRANĚK1,2,
  2. K. SCHULMANN2,
  3. O. LEXA1,3,
  4. S. ULRICH4,
  5. P. ŠTÍPSKÁ2,
  6. J. HALODA1,
  7. P. TÝCOVÁ1

Article first published online: 8 OCT 2010

DOI: 10.1111/j.1525-1314.2010.00911.x

Issue

Journal of Metamorphic Geology

Journal of Metamorphic Geology

Special Issue: Granulites, Partial Melting and the Rheology of the Lower Crust

Volume 29, Issue 1, pages 103–130, January 2011

Additional Information

How to Cite

FRANĚK, J., SCHULMANN, K., LEXA, O., ULRICH, S., ŠTÍPSKÁ, P., HALODA, J. and TÝCOVÁ, P. (2011), Origin of felsic granulite microstructure by heterogeneous decomposition of alkali feldspar and extreme weakening of orogenic lower crust during the Variscan orogeny. Journal of Metamorphic Geology, 29: 103–130. doi: 10.1111/j.1525-1314.2010.00911.x

Author Information

  1. 1

    Czech Geological Survey, Klárov 3, 118 21 Prague, Czech Republic (honzaf2@seznam.cz)

  2. 2

    Institut de Physique du Globe de Strasbourg, IPGS – UMR 7516, CNRS et Université de Strasbourg (EOST), 1 Rue Blessig, 67084 Strasbourg, France

  3. 3

    Institute of Petrology and Structural Geology, Charles University, Albertov 6, 128 43 Prague, Czech Republic

  4. 4

    Institute of Geophysics, Czech Academy of Sciences, Boční II/1401, 141 31 Prague, Czech Republic

Publication History

  1. Issue published online: 4 JAN 2011
  2. Article first published online: 8 OCT 2010
  3. Received 26 March 2010; revision accepted 6 September 2010.

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View Full Article with Supporting Information (HTML) Get PDF (3439K)