Chanel DePledge
Current Organizations / Institutes
The organizations/institutes from the scholar's latest article
Research Subjects
Research Interests
Chanel DePledge has a total of 6 co-authors. Here are the top co-authors by number of shared publications:
- Amanda Buckingham
Fathom Geophysics Australia Pty Limited, P.O. Box 1253, Dunsborough, WA 6281, Australia
1 shared publication Candice Godfrey
School of Earth and Planetary Sciences, Curtin University
1 shared publication- Jane Cunneen
Applied Geology, Curtin University, Perth, Western Australia, Australia
1 shared publication - Kevin C. Hill
School of Geography, Earth and Atmospheric Sciences, University of Melbourne, Melbourne, VIC, Australia
1 shared publication - Rebecca Farrington
AuScope, School of Geography, Earth & Atmospheric Sciences, University of Melbourne, Parkville, VIC, Australia
1 shared publication - Sharon Lowe
Southern Geoscience Consultants 183 Great Eastern Highway, Belmont WA Australia
1 shared publication
Latest Publications
- 11 November 2019
- Published by Australian Society of Exploration Geophysicists in ASEG Extended Abstracts
- Vol. 2019 (1) , 1-4
The Bight Basin, Evolution & Prospectivity I: gravity, deep seismic & basin morphology
Definition of the basement architecture within the Ceduna Sub-basin is poorly understood due to the depth of the basin and limited deep crustal geophysical datasets. This study uses seismic interpretation of BightSPAN™ deep crustal seismic lines combined with 2D forward models of the gravity to define the basement architecture in the Ceduna Sub-basin. Gravity forward models identify two depocentres with maximum depths of 25 km overlying thinned continental crust. Syn-rift sedimentary packages are several km thick and underlie up to 10 km of postkinematic Cretaceous deltaic sequences. Regional Moho models contain only sparse data points offshore and isostatic residual gravity data suggests substantial local variation in the depth to Moho. This local variation in the Moho surface is interpreted as boudinage of a weak lower crust along crustal shear zones. A gradual increase in basement density towards the continent-ocean transition suggests a diffuse rather than distinct boundary between continental and oceanic crust. The results of this work are used to constrain the tectonic evolution, particularly in terms of the subsidence history and uplift and erosional pulses recorded on the seismic data in the Ceduna Delta (Hill et al., this volume) and then used as input for finite element numerical models of rifting (Farrington et al., this volume).
- 11 November 2019
- Published by Australian Society of Exploration Geophysicists in ASEG Extended Abstracts
- Vol. 2019 (1) , 1-4
The Bight Basin, Evolution & Prospectivity I: gravity, deep seismic & basin morphology
Definition of the basement architecture within the Ceduna Sub-basin is poorly understood due to the depth of the basin and limited deep crustal geophysical datasets. This study uses seismic interpretation of BightSPAN™ deep crustal seismic lines combined with 2D forward models of the gravity to define the basement architecture in the Ceduna Sub-basin. Gravity forward models identify two depocentres with maximum depths of 25 km overlying thinned continental crust. Syn-rift sedimentary packages are several km thick and underlie up to 10 km of postkinematic Cretaceous deltaic sequences. Regional Moho models contain only sparse data points offshore and isostatic residual gravity data suggests substantial local variation in the depth to Moho. This local variation in the Moho surface is interpreted as boudinage of a weak lower crust along crustal shear zones. A gradual increase in basement density towards the continent-ocean transition suggests a diffuse rather than distinct boundary between continental and oceanic crust. The results of this work are used to constrain the tectonic evolution, particularly in terms of the subsidence history and uplift and erosional pulses recorded on the seismic data in the Ceduna Delta (Hill et al., this volume) and then used as input for finite element numerical models of rifting (Farrington et al., this volume).