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CATHLES, L, SHANNON, R (2007) How potassium silicate alteration suggests the formation of porphyry ore deposits begins with the nearly explosive but barren expulsion of large volumes of magmatic water. Earth and Planetary Science Letters, 262 (1) 92-108 doi:10.1016/j.epsl.2007.07.029

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Reference TypeJournal (article/letter/editorial)
TitleHow potassium silicate alteration suggests the formation of porphyry ore deposits begins with the nearly explosive but barren expulsion of large volumes of magmatic water
JournalEarth and Planetary Science Letters
AuthorsCATHLES, LAuthor
SHANNON, RAuthor
Year2007 (October 15)Volume262
Issue1
PublisherElsevier BV
DOIdoi:10.1016/j.epsl.2007.07.029Search in ResearchGate
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Mindat Ref. ID382103Long-form Identifiermindat:1:5:382103:3
GUID0
Full ReferenceCATHLES, L, SHANNON, R (2007) How potassium silicate alteration suggests the formation of porphyry ore deposits begins with the nearly explosive but barren expulsion of large volumes of magmatic water. Earth and Planetary Science Letters, 262 (1) 92-108 doi:10.1016/j.epsl.2007.07.029
Plain TextCATHLES, L, SHANNON, R (2007) How potassium silicate alteration suggests the formation of porphyry ore deposits begins with the nearly explosive but barren expulsion of large volumes of magmatic water. Earth and Planetary Science Letters, 262 (1) 92-108 doi:10.1016/j.epsl.2007.07.029
In(2007, October) Earth and Planetary Science Letters Vol. 262 (1) Elsevier BV

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