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Acoustic Travel Times for the Madison Limestone in the Williston Basin.

Authors
Marchant-LC; White-EJ
Source
For Reference Only At Bureau Libraries :15 pages
Link
NIOSHTIC No.
10010091
Abstract
An attempt was made to devise a simple method for accurately estimating rock matrix acoustic travel time for heterogeneous carbonate samples. Compressional wave travel time was measured for each of several hundred madison carbonate samples from the Williston Basin and is related to the corresponding sample porosity and bulk density. Least-squares equations for the linear plots of compressional wave travel time versus porosity and bulk density yield rock matrix travel times at zero porosity and bulk density equal to rock matrix density. However, the data are scattered enough for the authors to conclude that these relationships do not provide a reliable method for estimating rock matrix acoustic travel times.
Publication Date
19730101
Document Type
CP;
Fiscal Year
1973
Identifying No.
OFR 11-73
Source Name
For Reference Only At Bureau Libraries
Page last reviewed: April 12, 2019
Content source: National Institute for Occupational Safety and Health Education and Information Division