Geophysical anomalies and quartz microstructures, Eastern Warburton Basin, North-east South Australia: Tectonic or impact shock metamorphic origin?
Date
2013
Authors
Glikson, Andrew
Uysal, I T
Fitz Gerald, John
Saygin, Erdinc
Journal Title
Journal ISSN
Volume Title
Publisher
Elsevier
Abstract
The Eastern Warburton Basin, Northeast South Australia, features major geophysical anomalies, including a magnetic high of near-200. nT centred on a ~. 25. km-wide magnetic low (<. 100. nT), interpreted in terms of a magmatic body below 6. km depth. A distinct seismic tomographic low velocity anomaly may reflect its thick (9.5. km) sedimentary section, high temperatures and possible deep fracturing. Scanning electron microscope (SEM) analyses of granites resolves microbreccia veins consisting of micron-scale particles injected into resorbed quartz grains. Planar and sub-planar elements in quartz grains (Qz/PE) occur in granites, volcanics and sediments of the >. 30,000. km-large Eastern Warburton Basin. The Qz/PE include multiple intersecting planar to curved sub-planar elements with relic lamellae less than 2. μm wide with spacing of 4-5. μm. Qz/PE are commonly re-deformed, displaying bent and wavy patterns accompanied with fluid inclusions. U-stage measurements of a total of 243 planar sets in 157 quartz grains indicate dominance of Π{10-12}, ω{10-13} and subsidiary §{11-22}, {22-41}, m{10-11} and x{51-61} planes. Transmission Electron Microscopy (TEM) analysis displays relic narrow ≤. 1. μm-wide lamellae and relic non-sub grain boundaries where crystal segments maintain optical continuity. Extensive sericite alteration of feldspar suggests hydrothermal alteration to a depth of ~. 500. m below the unconformity which overlies the Qz/PE-bearing Warburton Basin terrain. The data are discussed in terms of (A) Tectonic-metamorphic deformation and (B) impact shock metamorphism producing planar deformation features (Qz/PDF). Deformed Qz/PE are compared to re-deformed Qz/PDFs in the Sudbury, Vredefort, Manicouagan and Charlevoix impact structures. A 4-5. km uplift of the Big Lake Granite Suite during ~. 298-295. Ma is consistent with missing of upper Ordovician to Devonian strata and possible impact rebound. The occurrence of circular seismic tomography anomalies below the east Warburton Basin, the Poolowana Basin and the Woodleigh impact structure signifies a potential diagnostic nature of circular tomographic anomalies.
Description
Keywords
Keywords: Cooper Basin; Geothermal; Magnetic anomalies; Planar microstructures; Warburton Basin; Grain boundaries; Granite; Mineralogy; Scanning electron microscopy; Sedimentology; Seismology; Tectonics; Transmission electron microscopy; Quartz; deformation; fluid Cooper Basin; Geothermal; Magnetic anomaly; Quartz planar microstructures; Tomography anomaly; Warburton Basin
Citation
Collections
Source
Tectonophysics
Type
Journal article
Book Title
Entity type
Access Statement
License Rights
Restricted until
2037-12-31
Downloads
File
Description