Published February 2001 | Version v1
Journal article

Late Neoproterozoic to holocene thermal history of the precambrian Georgetown inlier, northeast Australia

  • 1. La Trobe University, Bundoora, VIC (Australia). VIEPS, Australian Geodynamics Cooperative Research Centre, Department of Earth Sciences
  • 2. University of Melbourne, VIC (Australia). VIEPS, Australian Geodynamics Cooperative Research Centre, School of Earth Sciences
  • 3. University of Florida, (United States). Department of Geology

Description

Carboniferous-Permian volcanic complexes and isolated patches of Upper Jurassic - Lower Cretaceous sedimentary units provide a means to qualitatively assess the exhumation history of the Georgetown Inlier since ca 350 Ma. However, it is difficult to quantify its exhumation and tectonic history for earlier times. Thermochronological methods provide a means for assessing this problem. Biotite and alkali feldspar 40Ar/39Ar and apatite fission track data from the inlier record a protracted and non-linear cooling history since ca 750 Ma. 40Ar/39Ar ages vary from 380 to 735 Ma, apatite fission track ages vary between 132 and 258 Ma and mean track lengths vary between 10.89 and 13.11 mm. These results record up to four periods of localised accelerated cooling within the temperature range of ∼ 320-60 deg C and up to ∼ 14 km of crustal exhumation in parts of the inlier since the Neoproterozoic, depending on how the geotherm varied with time. Accelerated cooling and exhumation rates (0.19-0.05 km/106 years) are observed to have occurred during the Devonian, late Carboniferous - Permian and mid-Cretaceous - Holocene periods. A more poorly defined Neoproterozoic cooling event was possibly a response to the separation of Laurentia and Gondwana. The inlier may also have been reactivated in response to Delamerian-age orogenesis. The Late Palaeozoic events were associated with tectonic accretion of terranes east of the Proterozoic basement. Post mid-Cretaceous exhumation may be a far-field response to extensional tectonism at the southern and eastern margins of the Australian plate. The spatial variation in data from the present-day erosion surface suggests small-scale fault-bounded blocks experienced variable cooling histories. This is attributed to vertical displacement of up to ∼2 km on faults, including sections of the Delaney Fault, during Late Palaeozoic and mid-Cretaceous times. Copyright (2001) Geological Society of Australia

Additional details

Publishing Information

Journal Title
Australian Journal of Earth Sciences
Journal Volume
48
Journal Issue
1
Journal Page Range
p. 9-24
ISSN
0812-0099
CODEN
AJESE7

Optional Information

Notes
65 refs., 5 tab., 8 figs.