Retrograde Alteration
Retrograde Alteration is a hydrothermal alteration process occurring during the waning stages of skarn formation, characterized by the replacement of high-temperature, anhydrous minerals with lower-temperature, hydrous mineral assemblages due to decreasing temperature and the influx of externally derived, typically more aqueous and cooler fluids.
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Variants
Retrograde Metasomatism
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Wolfgang Bach, Holger Paulick, Carlos J. Garrido et al. · Geophysical Research Letters · 2006 · 410 citations · Full text
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Australian National University
Canberra, Australia
5 h-index
9 publications
315 citations

Centre National de la Recherche Scientifique
Paris, France
4 h-index
9 publications
912 citations

Universidad de Granada
Granada, Spain
4 h-index
6 publications
705 citations
University of Lausanne
Lausanne, Switzerland
3 h-index
4 publications
78 citations
University of Wisconsin–Madison
Madison, United States
3 h-index
5 publications
221 citations
Russian Academy of Sciences
Moscow, Russia
2 h-index
4 publications
126 citations

Chinese Academy of Geological Sciences
Beijing, China
2 h-index
6 publications
104 citations

Universitat Autònoma de Barcelona
Cerdanyola del Vallès, Spain
2 h-index
9 publications
219 citations
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