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15 kmMonowai Caldera (1650 m)Monowai Volcano (138 m)Monowai Caldera, Kermadec Arc
Page 1 and 2: The Role of Extension and Rifting i
Page 3 and 4: OutlineExtension and Rifting - defi
Page 5 and 6: Extension and Rifting(McKenzie and
Page 7 and 8: Seafloor Hydrothermal Vents and Rel
Page 9 and 10: Examples from Modern Geodynamic Env
Page 11 and 12: Arc-frontVolcanoesBrothers VolcanoS
Page 13: Early Arc Rifting and Proto-Backarc
Page 19 and 20: • 20 km long• 1 to 1.5 km wide
Page 21 and 22: km0 100anadad StateskeperiorAbitibi
Page 23 and 24: Examples from Modern Geodynamic Env
Page 25 and 26: Sibuet et al.,19981. Present dayand
Page 27 and 28: Sibuet et al., 1998
Page 29 and 30: Recognition of Extension-Rifting En
Page 31 and 32: Recognition of Subsidence in Ancien
Page 33 and 34: Icelandite DikePeperiteBasalt Dikes
Page 35 and 36: Basalt Pillow VolcanoBeddedTuff, La
Page 37 and 38: “Megabreccias”Evidence for Exte
Page 39 and 40: Dike SwarmCore of Subsidence Struct
Page 41 and 42: Recognition of Subvolcanic PlutonsM
Page 43 and 44: Seafloor Manifestation of Rifts: Co
Page 45 and 46: VMS deposits are located within and
Page 47 and 48: Lithostratigraphic Classification o
Page 49 and 50: Boninites (LOTI), Depleted ArcThole
Page 51 and 52: Piercey and Gibson, 2005
Page 53 and 54: Rock/Chondrites REEs-Nakamura 19741
Page 55 and 56: Kidd CreekBathurstEskay CreekFinlay
Page 57 and 58: Generation of FI- FIV RhyolitesFI F
Page 59 and 60: after Piercey and Gibson, 2005
Page 61 and 62: Fields fromPearce et al. (1984)Pier
Page 63: Final RemarkThe most valuable “ex

Criteria for Recognit

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