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Australian Journal of Earth Sciences
An International Geoscience Journal of the Geological Society of Australia
Volume 63, 2016 - Issue 4
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Original Articles

Widespread Neogene volcanism on Central Kerguelen Plateau, Southern Indian Ocean

, , &
Pages 379-392 | Received 12 May 2016, Accepted 28 Jul 2016, Published online: 30 Aug 2016
 

ABSTRACT

We report new age determinations and compositions for rocks from 18 dredge hauls collected from eight submarine areas across Central Kerguelen Plateau (CKP). Sea knolls and volcanic fields with multiple small cones were targeted over a ∼125 000 km2 region that includes Heard and McDonald Islands. Large early Miocene (22–16 Ma) sea knolls rise from the western margin of the CKP and are part of a NNW–SSE line of volcanic centres that lie between Îles Kerguelen and Heard and McDonald Islands. These are probably related to hotspot activity now underlying the Heard Island area. We see evidence of much younger activity (5 Ma to present) in volcanic fields to the north of, and up to 300 km NE of, Heard Island. Compositions include basanite, basalt and trachybasalt, which are broadly similar to plateau lava flows from nearby Ocean Drilling Program Site 1138, lower Miocene lavas at Îles Kerguelen, dredged rocks from the early Miocene sea knolls, and Big Ben lavas from Heard Island. Geochemical data indicate decreasing fractions of mantle source melting with time. We propose that a broad region of the CKP became volcanically active in Neogene time owing to incubation of plume material at the base of the relatively stationary overlying plateau. The presence of pre-existing crustal faults gave access for melts from the Heard mantle plume to rise to the surface.

Acknowledgements

The Australian Fisheries Management Authority (voyages SC26 and SC50 conducted for the Australian Antarctic Division) provided samples collected during two expeditions to CKP. Mr Richard Williams of the AAD alerted PQ to the existence of the samples and took steps to make them available for study. Jo Whittaker kindly provided and , and latest bathymetric data from the CKP. We thank Phil Robinson, Katie McGoldrick and Jay Thompson for their help with geochemical analyses. Dan Miggins provided assistance with age determinations. This research was supported by grants from the Australian Research Council and Geoscience Australia.

Disclosure statement

No potential conflict of interest was reported by the authors.

Supplementary Paper

Electronic Annex A. Complete ArArCALC data files for 40Ar–39Ar incremental heating experiments on dredged rocks from CKP.

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