Hasler, C. A. and Adams, E. W. and Woods, R. A. and Dickson, J. A. D. (2008) Fine-scale forward modelling of a Devonian patch reef, Canning Basin, Western Australia. In: Analogue and Numerical Modelling of Sedimentary Systems: From Understanding to Prediction. Special Publication of the IAS, 40 (40). Wiley- Blackwell, pp. 37-64. ISBN 978-1-4051-8930-9Full text not available from this repository.
Although factors that control the distribution of carbonate sediments are relatively well understood, their interaction in producing known geometries remains poorly known. A fine-scale forward model was developed to analyse the controls on decimetre-scale heterogeneity and carbonate facies distribution within larger-scale sediment bodies. The model was tested on a Frasnian (Late Devonian) patch reef, part of the so-called Glenister Knolls reef complex in the Canning Basin, Western Australia. The evolution of Glenister Knolls was digitally reconstructed using digital surveying technologies that resulted in a high-resolution dataset containing geological information from centimetrescale to outcrop dimensions. The three-dimensional digital outcrop model of Glenister Knolls was used to evaluate predictions from the fine-scale forward modelling results. The fine-scale forward model is based on a stochastic cellular automaton that simulates the spatial distribution of carbonate facies through time. The modelled carbonate facies is based on two main factors, stromatoporoid growth and sediment transport, and it successfully predicts the distribution of the basic elements – reef fabric and sediment – that compose the patch reef. The fine-scale forward model also successful reproduces all major depositional relationships observed in the field such as backstepping, downlapping and interfingering contacts. The external structure of the reef is very sensitive to subsidence and production rates, since these directly influence accommodation space so constraining the vertical growth of the patch reef. However, the internal structure predicted by this model does not seem to be affected by one specific parameter, and displays the same sensitivity to other parameters, such as current intensity and wave amplitude.
|Item Type:||Book Section|
|Uncontrolled Keywords:||08AREP,(New to DB in 2011)|
|Subjects:||02 - Geodynamics, Geophysics and Tectonics|
|Divisions:||02 - Geodynamics, Geophysics and Tectonics|
|Page Range:||pp. 37-64|
|Depositing User:||Sarah Humbert|
|Date Deposited:||25 Aug 2011 10:52|
|Last Modified:||23 Jul 2013 10:02|
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