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
INIS
- Country of Publication
- Australia
- Country of Input or Organization
- Australia
- INIS RN
- 33001024
- Subject category
- S37: INORGANIC, ORGANIC, PHYSICAL AND ANALYTICAL CHEMISTRY; S58: GEOSCIENCES;
- Resource subtype / Literary indicator
- Numerical Data
- Descriptors DEI
- APATITES; ARGON 39; ARGON 40; BIOTITE; EROSION; FELDSPARS; FISSION TRACKS; IGNEOUS ROCKS; ISOTOPE DATING; ISOTOPE RATIO; NUMERICAL DATA; PALEOZOIC ERA; QUEENSLAND; TECTONICS
- Descriptors DEC
- AGE ESTIMATION; ARGON ISOTOPES; AUSTRALASIA; AUSTRALIA; BETA DECAY RADIOISOTOPES; BETA-MINUS DECAY RADIOISOTOPES; DATA; DEVELOPED COUNTRIES; EVEN-EVEN NUCLEI; EVEN-ODD NUCLEI; GEOLOGIC AGES; INFORMATION; ISOTOPES; LIGHT NUCLEI; MICA; MINERALS; NUCLEI; PARTICLE TRACKS; PHOSPHATE MINERALS; RADIOISOTOPES; ROCKS; SILICATE MINERALS; STABLE ISOTOPES; YEARS LIVING RADIOISOTOPES
Optional Information
- Notes
- 65 refs., 5 tab., 8 figs.