Abstract
Electron microscopy of sedimentary dolomite reveals heterogeneous microstructures on a 100 ‐ 300Å scale which we interpret as compositional modulations. Electron diffraction patterns contain a new type of superstructure reflection which effectively doubles the a axis. These findings suggest the presence of a new phase in low temperature calcian dolomite rocks.
| Original language | English |
|---|---|
| Pages (from-to) | 77-80 |
| Number of pages | 4 |
| Journal | Geophysical Research Letters |
| Volume | 6 |
| Issue number | 2 |
| DOIs | |
| State | Published - Feb 1979 |
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