Detrital-zircon geochronology of the metasedimentary rocks of north-western Graham Land

David L. Barbeau, Justin T. Davis, Kendra E. Murray, Victor Valencia, George E. Gehrels, Khandaker M. Zahid, David J. Gombosi

Research output: Contribution to journalArticle

37 Citations (Scopus)

Abstract

Metasedimentary rocks constitute an important but comparatively poorly understood part of the Antarctic Peninsula. Herein we report single-grain U-Pb detrital-zircon ages from samples of the Trinity Peninsula and Botany Bay Groups of north-western Graham Land. All studied samples are dominated by a large and narrowly defined population of late Palaeozoic zircons. Significant earlymiddle Palaeozoic and minor Neoproterozoic and Mesoproterozoic sub-populations constitute the majority of pre-Carboniferous grains. These detrital-zircon age populations are consistent with sediment derivation entirely from western Gondwana sources. Despite the clear Gondwana signatures, our data suggest that the Trinity Peninsula Group province was either a parautochthonous peri-Gondwanan terrane later accreted to the Antarctic Peninsula, or a significant topographic barrier precluded voluminous sediment contributions from the interior of Gondwana. Statistical comparisons with similar metasedimentary complexes of southern South America, the South Shetland Islands and eastern New Zealand indicate a diversity of sediment provenance not previously recognized, but may provide a means to better determine the pre-break-up configuration of western Gondwana. Although insufficient to definitively restore Antarctic Peninsula components adjacent to South American complexes, some Trinity Peninsula Group samples exhibit robust affinities to the Miers Bluff Formation in the South Shetland Islands and the Duque de York and Main Range Metamorphic Complexes of the Patagonian Andes.

Original languageEnglish (US)
Pages (from-to)65-78
Number of pages14
JournalAntarctic Science
Volume22
Issue number1
DOIs
StatePublished - Aug 2009

Fingerprint

metasedimentary rock
geochronology
Gondwana
zircon
rocks
sediments
Antarctica
Paleozoic
sediment
botany
sampling
provenance
subpopulation
terrane
land

Keywords

  • Botany Bay Group
  • Gondwana
  • Mount Flora Formation
  • Sediment provenance
  • Trinity Peninsula Group

ASJC Scopus subject areas

  • Ecology, Evolution, Behavior and Systematics
  • Oceanography
  • Geology

Cite this

Barbeau, D. L., Davis, J. T., Murray, K. E., Valencia, V., Gehrels, G. E., Zahid, K. M., & Gombosi, D. J. (2009). Detrital-zircon geochronology of the metasedimentary rocks of north-western Graham Land. Antarctic Science, 22(1), 65-78. https://doi.org/10.1017/S095410200999054X

Detrital-zircon geochronology of the metasedimentary rocks of north-western Graham Land. / Barbeau, David L.; Davis, Justin T.; Murray, Kendra E.; Valencia, Victor; Gehrels, George E.; Zahid, Khandaker M.; Gombosi, David J.

In: Antarctic Science, Vol. 22, No. 1, 08.2009, p. 65-78.

Research output: Contribution to journalArticle

Barbeau, DL, Davis, JT, Murray, KE, Valencia, V, Gehrels, GE, Zahid, KM & Gombosi, DJ 2009, 'Detrital-zircon geochronology of the metasedimentary rocks of north-western Graham Land', Antarctic Science, vol. 22, no. 1, pp. 65-78. https://doi.org/10.1017/S095410200999054X
Barbeau, David L. ; Davis, Justin T. ; Murray, Kendra E. ; Valencia, Victor ; Gehrels, George E. ; Zahid, Khandaker M. ; Gombosi, David J. / Detrital-zircon geochronology of the metasedimentary rocks of north-western Graham Land. In: Antarctic Science. 2009 ; Vol. 22, No. 1. pp. 65-78.
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