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(2017) Neogene monogenetic volcanism from the Northern Puna region: products and eruptive styles. Special Publication, 446. Geological Society of London. 337-359 doi:10.1144/sp446.6

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TitleNeogene monogenetic volcanism from the Northern Puna region: products and eruptive styles
ReportSpecial Publication
Year2017Volume446
PublisherGeological Society of London
DOIdoi:10.1144/sp446.6Search in ResearchGate
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Mindat Ref. ID441698Long-form Identifiermindat:1:5:441698:6
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Full Reference(2017) Neogene monogenetic volcanism from the Northern Puna region: products and eruptive styles. Special Publication, 446. Geological Society of London. 337-359 doi:10.1144/sp446.6
Plain Text(2017) Neogene monogenetic volcanism from the Northern Puna region: products and eruptive styles. Special Publication, 446. Geological Society of London. 337-359 doi:10.1144/sp446.6
In(2017) Special Publication Vol. 446. Geological Society of London

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(2017) Monogenetic v. polygenetic kimberlite volcanism: in-depth examination of the Tango Extension Super Structure, Attawapiskat kimberlite field, Ontario, Canada. Special Publication, 446. Geological Society of London. 205-224 doi:10.1144/sp446.7
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(1996) Contrasting tectonic styles in the Neogene orogenic belts of Indonesia. Special Publication, 106. Geological Society of London. 185-201 doi:10.1144/gsl.sp.1996.106.01.12
(2017) Geology and geochemistry of Late Quaternary volcanism in northern Harrat Rahat, Kingdom of Saudi Arabia: implications for eruption dynamics, regional stratigraphy and magma evolution. Special Publication, 446. Geological Society of London. 173-204 doi:10.1144/sp446.2
(1988) Cyclical tholeiitic volcanism and associated magma chambers: eruptive mechanisms in E Greenland. Special Publication, 39. Geological Society of London. 197-200 doi:10.1144/gsl.sp.1988.039.01.18
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(2017) Pyroclastic deposits of San Diego maar, central Colombia: an example of a silicic magma-related monogenetic eruption in a hard substrate. Special Publication, 446. Geological Society of London. 361-374 doi:10.1144/sp446.10
 
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