First record of the Late Cretaceous denudation phase in the Admiralty Block (Transantarctic Mountains, northern Victoria Land, Antarctica)

Author:

Balestrieri M.L,Bigazzi G

Publisher

Elsevier BV

Subject

Instrumentation,Radiation

Reference11 articles.

1. Uplift-denudation of the Transantarctic Mountains between the David and the Mariner Glaciers, northern Victoria Land (Antarctica): constraints by apatite fission-track analysis.;Balestrieri,1997

2. The Transantarctic Mountains: a natural laboratory for apatite fission-track analysis. Results from Italian Antarctic expeditions;Balestrieri;Radiat. Meas.,1999

3. Davey, F.J., 1987. Geology and structure of the Ross Sea region. In: Cooper, A.K., Davey, F.J. (Eds.), The Antarctic Continental Margin: Geology and Geophysics of the Western Ross Sea. Earth Science Series, 5B, Circum-Pacific Council for Energy and Mineral Resources, Houston, Texas, pp. 1–15.

4. Fission-track geochronology, tectonics and structure of the Transantarctic Mountains in northern Victoria Land, Antarctica. Chem. Geol;Fitzgerald;(Isotope Geosci. Sect.),1988

5. Uplift and denudation of the central Alaska Range; a case study in the use of apatite fission track thermochronology to determine absolute uplift parameters;Fitzgerald;J. Geophys. Res.,1995

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