Tourmaline 40Ar/39Ar chronology of tourmaline-rich rocks from Central Iberia dates the main Variscan deformation phases
During crustal thickening, metapelites taken to depth release boron-bearing hydrothermal fluids because of progressive heating and dehydration. These fluids swiftly percolate upwards, especially if the crust is being actively deformed, to form tourmaline where the PT conditions and the chemical comp...
Furkejuvvon:
| Publikašuvnnas: | Geologica Acta: an international earth science journal |
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| Váldodahkkit: | , , , , |
| Materiálatiipa: | Artigo |
| Giella: | Inglês |
| Almmustuhtton: |
Universitat de Barcelona
2009
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| Fáttát: | |
| Liŋkkat: | https://www.redalyc.org/articulo.oa?id=50514007001 |
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