Combined apatite fission-track and single grain apatite (U Th)/He ages from basement rocks of central Dronning Maud Land (East Antarctica) — Possible identification of thermally overprinted crustal segments?

Details Combined apatite fission-track and single grain apatite (U Th)/He ages from basement rocks of central Dronning Maud Land (East Antarctica) — Possible identification of thermally overprinted crustal segments? Combined apatite fission-track and single grain apatite (U Th)/He ages from basement rocks of central Dronning Maud Land (East Antarctica) — Possible identification of thermally overprinted crustal segments?

Dec 2007

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2007e%26psl.264...72e&link_type=abstract

Earth and Planetary Science Letters, Volume 264, Issue 1-2, p. 72-88.

Physics

2

Scientific paper

Apatite fission-track (FT) and single grain (U Th)/He ages from four vertical profiles in central Dronning Maud Land (East Antarctica) range from 312 ± 20 Ma to 135 ± 11 Ma and 304 ± 28 Ma to 104 ± 8 Ma, respectively. The combined age data allows to discriminate between undisturbed cooled (due to exhumation) and thermally overprinted crustal blocks. Profiles at the Zwieselhöhe and the Conradgebirge revealed unusual apatite FT vs. elevation relationships and (U Th)/He ages older than the corresponding central apatite FT ages, possibly providing evidence for a Jurassic thermal overprint. Most probably Jurassic magmatism and associated advective heating led to total annealing of the apatite fission-tracks but helium only partially diffused. The model developed in this paper suggests that the (U Th)/He ages from the Zwieselhöhe and Conradgebirge profiles are in part relicts of the pre-Jurassic cooling history. Two thermally undisturbed vertical profiles are used to record the long-term cooling history of central Dronning Maud Land. Time-temperature paths derived from modelled apatite FT data of these profiles revealed two phases of accelerated cooling during the Late Carboniferous and the Early Jurassic. Both phases are followed by slow cooling which is also documented by the spread in apatite (U Th)/He single grain ages. The cooling at the end of the Carboniferous is most probably related to far field effects associated to the prevailing convergent tectonics. During the initial separation between East Antarctica and Mozambique erosion along an evolving rift shoulder caused the Jurassic cooling. Denudation of the basement was simultaneous with volcanism with both pre-dating (c. 20 10 Ma) sea-floor spreading in the Riser Larsen Sea (c. 155 Ma). Post Jurassic cooling was restricted to the lowest temperature sensitivity of both methods. Combined inverse modelled apatite FT data and forward modelled (U Th)/He data suggest an Eocene/Oligocene cooling step, possibly related to the flexural-isostatic response to the development of ice-sheets.

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