Miocene-Recent post-subduction alkaline magmatism along the Antarctic Peninsula II. Petrology

Research output: Chapter in Book/Report/Conference proceedingChapter

Abstract

Scattered occurrences of Miocene-Recent volcanic rocks of the alkaline intraplate association represent one of the last expressions of magmatism along the Antarctic Peninsula. The volcanic rocks were erupted after the cessation of subduction which stopped following a series of northward-younging ridge-crest‒trench collisions. Volcanism has been linked to the development of a growing slab window beneath the extinct convergent margin. Geochemically, lavas range from olivine tholeiite through to basanite and tephrite. Previous studies have emphasized the slab window tectonic setting as key to allowing melting of peridotite in the asthenospheric void caused by the passage of the slab beneath the locus of volcanism. This hypothesis is revisited in the light of more recent petrological research, and an origin from melting of subducted slab-hosted pyroxenite is considered here to be a more viable alternative for their petrogenesis. Because of the simple geometry of ridge subduction, and the well-established chronology of ridge-crest-trench collisions, the Antarctic Peninsula remains a key region for understanding the transition from active to passive margin resulting from cessation of subduction. However, there are still some key issues relating to their tectono-magmatic association, and principally, the poor geochronological control on the volcanic rocks requires urgent attention.
Original languageEnglish
Title of host publicationVolcanism in Antarctica
Subtitle of host publication200 Million Years of Subduction, Rifting and Continental Break-Up
PublisherGeological Society of London
Chapter4
Publication statusAccepted/In press - 30 Nov 2018

Publication series

NameGeological Society Memoir

Fingerprint

petrology
magmatism
slab
subduction
Miocene
volcanic rock
volcanism
melting
collision
basanite
convergent margin
tholeiite
pyroxenite
passive margin
petrogenesis
peridotite
tectonic setting
void
trench
chronology

Cite this

Hole, M. J. (Accepted/In press). Miocene-Recent post-subduction alkaline magmatism along the Antarctic Peninsula II. Petrology. In Volcanism in Antarctica: 200 Million Years of Subduction, Rifting and Continental Break-Up (Geological Society Memoir). Geological Society of London.

Miocene-Recent post-subduction alkaline magmatism along the Antarctic Peninsula II. Petrology. / Hole, Malcolm John.

Volcanism in Antarctica: 200 Million Years of Subduction, Rifting and Continental Break-Up. Geological Society of London, 2018. (Geological Society Memoir).

Research output: Chapter in Book/Report/Conference proceedingChapter

Hole, MJ 2018, Miocene-Recent post-subduction alkaline magmatism along the Antarctic Peninsula II. Petrology. in Volcanism in Antarctica: 200 Million Years of Subduction, Rifting and Continental Break-Up. Geological Society Memoir, Geological Society of London.
Hole MJ. Miocene-Recent post-subduction alkaline magmatism along the Antarctic Peninsula II. Petrology. In Volcanism in Antarctica: 200 Million Years of Subduction, Rifting and Continental Break-Up. Geological Society of London. 2018. (Geological Society Memoir).
Hole, Malcolm John. / Miocene-Recent post-subduction alkaline magmatism along the Antarctic Peninsula II. Petrology. Volcanism in Antarctica: 200 Million Years of Subduction, Rifting and Continental Break-Up. Geological Society of London, 2018. (Geological Society Memoir).
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