All Outputs (2)

Plutonic xenoliths from Martinique, Lesser Antilles: evidence for open system processes and reactive melt flow in island arc crust (2016)
Journal Article
Cooper, G., Davidson, J., & Blundy, J. (2016). Plutonic xenoliths from Martinique, Lesser Antilles: evidence for open system processes and reactive melt flow in island arc crust. Contributions to Mineralogy and Petrology, 171(10), Article 87. https://doi.org/10.1007/s00410-016-1299-8

The Lesser Antilles Volcanic Arc is remarkable for the abundance and variety of erupted plutonic xenoliths. These samples provide a window into the deeper crust and record a more protracted crystallisation history than is observed from lavas alone. W... Read More about Plutonic xenoliths from Martinique, Lesser Antilles: evidence for open system processes and reactive melt flow in island arc crust.

Generation and Rejuvenation of a Supervolcanic Magmatic System: a Case Study from Mangakino Volcanic Centre, New Zealand (2016)
Journal Article
Cooper, G. F., Wilson, C. J., Millet, M., & Baker, J. A. (2016). Generation and Rejuvenation of a Supervolcanic Magmatic System: a Case Study from Mangakino Volcanic Centre, New Zealand. Journal of Petrology, 57(6), 1135-1170. https://doi.org/10.1093/petrology/egw035

The Kidnappers [∼1200 km 3 dense rock equivalent (DRE)] and Rocky Hill (∼200 km 3 DRE) caldera-forming events in the Taupo Volcanic Zone, New Zealand, were erupted in close succession from the Mangakino volcanic centre. They have identical radiometri... Read More about Generation and Rejuvenation of a Supervolcanic Magmatic System: a Case Study from Mangakino Volcanic Centre, New Zealand.