Wadge, G. et al. (1998): Lithological classification within ODP holes using neural networks trained from integrated core-log data

Leg/Site/Hole:
ODP 126
ODP 126 792
Identifier:
1999-021018
georefid

Creator:
Wadge, G.
University of Reading, Environmental Systems Science Centre, Reading, United Kingdom
author

Benaouda, D.
University of Southampton, United Kingdom
author

Ferrier, G.
University of Wales College of Cardiff, United Kingdom
author

Whitmarsh, R. B.
author

Rothwell, R. G.
author

MacLeod, C.
author

Identification:
Lithological classification within ODP holes using neural networks trained from integrated core-log data
1998
In: Harvey, P. K. (editor), Lovell, M. A. (editor), Core-log integration
Geological Society of London, London, United Kingdom
136
129-140
Neural networks offer an attractive way of using downhole logging data to infer the lithologies of those sections of ODP holes from which there is no core recovery. This is best done within a computer program that enables the user to explore the dimensionality of the log data, design the structure for the neural network appropriate to the particular problem and select and prepare the log-and core-derived data for training, testing and using the neural network as a lithological classifier. Data quality control and the ability to modify lithological classification schemes to particular circumstances are particularly important. We illustrate these issues with reference to a 250 m section of ODP Hole792E drilled through a sequence of island arc turbidites of early Oligocene age. Applying a threshold of >90% recovery per 9.7 m core section, we have available about 50% of the cored interval that is sufficiently well depth-matched for use as training data for the neural network classifier. The most useful logs available are from resistivity, natural gamma, sonic and geochemistry tools, a total of 15. In general, the more logs available to the neural network the better its performance, but the optimum number of nodes on a single "hidden" layer in the network has to be determined by experimentation. A classification scheme, with 3 classes (claystone, sandstone and conglomerate) derived from shipboard observation of core, gives a success rate of about 76% when tested with independent data. This improves to about 90% when the conglomerate class is split into two, based on the relative abundance of claystone versus volcanic clasts.
English
Coverage:Geographic coordinates:
North:32.2359
West:140.2246East: 140.2249
South:32.2355

Oceanography; Sedimentary petrology; acoustical logging; Cenozoic; classification; clastic rocks; claystone; conglomerate; cores; data processing; electrical logging; gamma-ray methods; interpretation; Izu-Bonin Arc; Leg 126; lithofacies; lower Oligocene; marine geology; neural networks; North Pacific; Northwest Pacific; Ocean Drilling Program; ocean floors; ODP Site 792; Oligocene; Pacific Ocean; Paleogene; sandstone; sedimentary rocks; Tertiary; well-logging; West Pacific;

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