Petrologic Studies

The 24 papers in this volume, written in honor of A.F. Buddington, cover a wide range of topics and geographic areas. H.H. Hesss History of Ocean Basins perhaps the most famous paper in the volume, introduces the concept of seafloor spreading.
Effect of Ionic Substitution on the Unit-Cell Dimensions of Synthetic Diopside*
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Published:January 01, 1962
Abstract
The writer has synthesized pure diopside and diopsides in which Na+1 and Mg+2 have been substituted for Ca+2; in which Al +3, Fe+3, Cr+3, Mn+2, Ni+2, and Ti+4 have been substituted for Mg+2; and in which Al+3 and Fe+3 have been substituted for Si+4 . The unit-cell dimensions of these synthetic clinopyroxenes have been determined. From these data, the effects of individual (e.g., Ni+2 for Mg+2) and coupled (e.g., Na+1 Al+3 for Ca+2Mg+2) ionic substitutions on the unit-cell dimensions of pure diopside have been obtained. On the basis of the assumption that the substitution of Na+1 for Ca+2 has a negligible effect on the diopside unit-cell dimensions, the effects of individual ionic substitutions (e.g., Al+3 for Mg4+2, Ti+4 for Mg+2, Al+3 for Si4+4…) are assessed. Many of the findings are i n accord with the principles of crystal chemistry (e.g., increase in the c dimension with substitution of Al+3 or Fe+3 for Si+4), but others are not. In the latter case, discrepancies are probably due to errors in the data. The probable nature and magnitude of of such errors are discussed. The unit-cell dimensions of pure diopside are: a = 9.746Å, b = 8.924Å, c = 5.247Å, β= 74°5′; a sinβ(= d100) = 9.373Å. In order of decreasing magnitude, the effects of individual ionic substitutions on these dimensions are: a sinβ decreases with substitution of Mg+2 for Ca4+2, Cr+3 for Mg+2, and Al+3 for Mg+2 and increases with substitution of Fe+3 for Si4+4; b decreases with substitution of Cr+3 for Mg+2, Al4 +3 for Mg+2, Mn4 +2 for Mg+2, Fe+3 for Si4+4, Ni4 +2 tor Mg+2, and Al+3 for Si+4; c increases with substitution of Fe+3 for Si+4 Mg+2 for Ca+2, Ti+4 for Mg+2, Al4 +3 for Mg+2, Al+3 for Si+4, and Fe+3 for Mg+2; β decreases with substitution of Mg+2 for Ca+2 and Ti+4 for Mg+2 . Effects of other individual substitutions are slight.