Abstract
Crystal-growth defects in sedimentary calcites and dolomites were examined by TEM. Dislocation densities are highly variable and distributions are heterogeneous. Growth-related stacking faults are absent in calcite but fairly common in dolomite, possibly due to its non-stoichiometry. These growth microstructures might be useful as indicators of growth conditions. -R.A.H.
| Original language | English |
|---|---|
| Pages (from-to) | 179-183 |
| Number of pages | 5 |
| Journal | Estudios Geologicos |
| Volume | 38 |
| Issue number | 3-4 |
| State | Published - 1982 |
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