Improved Understanding of Fluvial Architecture Using Three-Dimensional Geological Models: A Case Study of the Westphalian a Silkstone Rock, Pennine Basin, UK
- Michael D. Blum5,
- Susan B. Marriott6,
- Suzanne F. Leclair7
Published Online: 17 MAR 2009
DOI: 10.1002/9781444304350.ch25
Copyright © 2005 International Association of Sedimentologists
Book Title

Fluvial Sedimentology VII
Additional Information
How to Cite
Keogh, K. J., Rippon, J. H., Hodgetts, D., Howell, J. A. and Flint, S. S. (2009) Improved Understanding of Fluvial Architecture Using Three-Dimensional Geological Models: A Case Study of the Westphalian a Silkstone Rock, Pennine Basin, UK, in Fluvial Sedimentology VII (eds M. D. Blum, S. B. Marriott and S. F. Leclair), Blackwell Publishing Ltd., Oxford, UK. doi: 10.1002/9781444304350.ch25
Editor Information
- 5
Baton Rouge, Louisiana, USA
- 6
School of Geography and Environmental Management, University of the West of England, Bristol BS16 1QY, UK
- 7
Department of Earth and Environmental Sciences, Tulane University, Dimwiddie Hall, New Orleans, LA 70118, USA
Publication History
- Published Online: 17 MAR 2009
- Published Print: 15 FEB 2005
Book Series:
Book Series Editors:
- Ian Jarvis
Series Editor Information
School of Earth Sciences and Geography, Centre for Earth and Environmental Science Research, Kingston University, Penrhyn Road, Kingston-upon-Thames KT1 2EE, UK
ISBN Information
Print ISBN: 9781405126519
Online ISBN: 9781444304350
- Summary
- Chapter
Keywords:
- improved understanding of fluvial architecture using three-dimensional geological models;
- Westphalian - A Silkstone Rock, Pennine Basin, UK;
- modelling methodology;
- understanding fluvial architecture using three-dimensional geological models;
- deterministic mapping of coal seams;
- Westphalian A and B of Pennine Basin - intensely studied sedimentary successions in UK;
- three-dimensional model clarifying stratal relationships
Summary
The Westphalian A and B of the Pennine Basin is one of the most intensely studied sedimentary successions in the UK owing to its economic importance in the coal and hydrocarbon industries. Previous studies of this interval have utilized the wealth of mining data available to accurately correlate sand bodies and deterministically map their regional extents in a two-dimensional framework. This paper expands on one particular study by taking the same data used by previous workers and digitally processing them into a format that is readable by an oil industry reservoir modelling programme (IRAP-RMS). A three-dimensional deterministic model has then been constructed to allow visualization and analysis of the resulting facies geometries in three dimensions, with the aim of gaining an improved understanding of the geometry and architecture of a major multistorey fluvial sandbody. Application of these techniques has allowed for enhanced visualization and interrogation of the Pennine Basin interval, previously not possible using traditional two-dimensional techniques. Understanding of the Silkstone Rock and its relationship to other facies has improved, because erosion at the base of the unit can be demonstrated to truncate coals and single-storey channel-fills that represent an earlier depositional phase. The visualization of this relationship is not possible from a single two-dimensional section, and the three-dimensional model therefore clarifies stratal relationships.
