1. Redefined crustal structure of the Buchan Rift, northeast Victoria: evidence from potential field modelling of newly acquired land-based gravity data
- Author
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Mark McLean, Timothy J Rawling, R. A. Cayley, and T. E. Ogden
- Subjects
Gravity (chemistry) ,geography ,geography.geographical_feature_category ,Rift ,010504 meteorology & atmospheric sciences ,Potential field ,Pyroclastic rock ,Structural basin ,010502 geochemistry & geophysics ,01 natural sciences ,Devonian ,Volcanic rock ,Paleontology ,Volcano ,Earth and Planetary Sciences (miscellaneous) ,General Earth and Planetary Sciences ,Geology ,Seismology ,0105 earth and related environmental sciences - Abstract
The Buchan Rift, in northeastern Victoria, is a north–south-trending basin, which formed in response to east–west crustal extension in the Early Devonian. The rift is filled mostly with Lower Devonian volcanic and volcaniclastic rock of the Snowy River Volcanics. Although the structure and geometry of the Buchan Rift and its major bounding faults are well mapped at the surface, a discrepancy exists between the surface distribution of the thickest rift fill and its expected potential field response. To investigate this variation, two new detailed land-based gravity surveys, which span the rift and surrounding basement rocks in an east–west orientation, have been acquired and integrated with pre-existing government data. Qualitative interpretation of the observed magnetic data suggests the highly magnetic rocks of the Snowy River Volcanics have a wider extent at depth than can be mapped at the surface. Forward modelling of both land-based gravity data and aeromagnetic data supports this interpretati...
- Published
- 2016
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