
TY  - JOUR
A1  - House, M. 
A1  - Dentith, M. 
A1  - Trench, A. 
A1  - Groves, D. 
A1  - Miller, D. 
T1  - Structure of the highly mineralised late-Archaean granitoid-greenstone terrain and the underlying crust in the Kambalda-Widgiemooltha area, Western Australia, from the integration of geophysical datasets
JF  - Exploration Geophysics
JO  - Explor. Geophys.
Y1  - 1999
VL  - 30
IS  - 2
SP  - 50
EP  - 67
KW  - 
UR  - https://doi.org/10.1071/EG999050 
N2  - The highly mineralised (Au, Ni) Kambalda-Widgiemooltha area comprises typical late-Archaean granitoid-greenstone sequences, and is situated within the Kalgoorlie Terrane of the southern Norseman-Wiluna Belt in the Yilgarn Craton of Western Australia. In the Kambalda-Widgiemooltha area, high-resolution aeromagnetic data, two deep seismic reflection profiles and gravity data are available to examine the geophysical signature and three-dimensional structure of this important region of the Kalgoorlie Terrane. The Kambalda-Widgiemooltha area has previously been divided, from west to east, into three fault-bounded tectono-stratigraphic domains, the Coolgardie, Kambalda and Parker Domains. Lithological associations and structural features defined by the aeromagnetic data substantiate the division of the study area into these three north-northwest-trending domains, and indicate that each domain consists of two, approximately equal-width, sub-domains. A four-stage deformation sequence, which is recognised from the aeromagnetic data, includes early south-to-north directed recumbent folding and thrust repetition (D1), regional north-northwest folding and imbrication (D2), transcurrent movement on major north-northwest shear zones (D3), and the formation of late north-northeast and northwest-trending lineaments (D4). Two deep (20s TWT) seismic reflection profiles across the Coolgardie and Kambalda Domains reveal a three-layered crust beneath the study area. The upper layer (0 - 10 km), which includes the greenstone belt, is generally unreflective in the upper 5 km. The lower part of this layer (7.5 to 10 km) is more reflective and comprises a felsic unit which could be a continuation of the greenstone belt stratigraphy, attenuated basement, or rift-related sedimentary rocks. Domain-bounding faults are interpreted as listric structures, which have allowed the partial imbrication of the domains during regional deformation.The middle layer (10 - 27 km) is characterised by moderate to strong, variably dipping reflections. It is interpreted as an imbricate sequence of granitoids and gneisses. A more homogeneous, but weakly reflective, character is indicative of the lower crustal layer (27 - 35 km). East-dipping truncating reflectors at the western margin of the study area suggest that this layer is younger than the upper and middle layers and may, therefore, represent the late-tectonic external granitoids. The Moho is not imaged, but a general decrease in the number of reflections indicates that the crust is about 35 km thick. 
ER  -

