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Petrogrpahic Analysis of Northern Indiana Carbonate Aggregates

Please use this identifier to cite or link to this item: http://hdl.handle.net/1811/5153

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dc.creator Aughenbaugh, N. B. en_US
dc.creator Lounsbury, R. W. en_US
dc.date.accessioned 2005-10-01T01:15:19Z
dc.date.available 2005-10-01T01:15:19Z
dc.date.issued 1966-03 en_US
dc.identifier.citation The Ohio Journal of Science. v66 n2 (March, 1966), 179-187 en_US
dc.identifier.issn 0030-0950 en_US
dc.identifier.uri http://hdl.handle.net/1811/5153
dc.description Author Institution: Department of Engineering Geology, Purdue University, Lafayette, Indiana en_US
dc.description.abstract A study was made to determine those petrographic parameters that are correlative with carbonate-aggregate quality as indicated by the Los Angeles abrasion and absorption tests. Samples collected at 28 sites in northern and eastern Indiana were analyzed petrographically, chiefly for void content, grain size, grain-size variation, grain shape, and grain interlock. Most of the sampled sites are in the belt of Silurian rocks of east-central and northwestern Indiana. Though a few sites lie outside this belt, most of these have only a thin Devonian section above the Silurian. Three sites are non-Silurian and are included for comparison. Most of the samples studied are from Middle and Upper Silurian units. Both biohermal and nonbiohermal facies are included. The biohermal rocks are typically dense but vugular, finely crystalline granular dolomite. Nonbiohermal facies are porous, medium to coarsely crystalline, granular dolomite with dolomite rhombs. The Los Angeles abrasion losses ranged from 20 to 46 per cent, the rocks in the eastern part of the state showing the higher values. Absorption tests indicate the same general quality trend. Comparison of petrographic studies with Los Angeles abrasion- and absorption-test results indicate the following correlations. (1) As per cent of voids increases, quality decreases. (2) As average grain size increases, quality decreases. (3) Variations from mean grain size appear to have no effect on the quality. (4) As angularity and roughness of the grains increase, quality increases. (5) As grain-to-grain interlock increases, quality increases. Variations in the calcium-magnesium ratio have no apparent effect on aggregatequality, except as they affect the texture. en_US
dc.format.extent 1453959 bytes
dc.format.mimetype application/pdf
dc.language.iso en_US
dc.rights Reproduction of articles for non-commercial educational or research use granted without request if credit to The Ohio State University and The Ohio Academy of Science is given. en_US
dc.title Petrogrpahic Analysis of Northern Indiana Carbonate Aggregates en_US