| |
| | Case Studies - PTTC Rockies |
 | | Here, finely crystalline euhedral-to-subhedral dolomite replaces calcareous grains and matrix (pink), leaving remnants of limestone texture shown in view A. Replacive dolomite is darker, with more inclusion material, whereas pore-filling dolomite is euhedral, inclusion-poor, and exhibits ferroan rims (arrow) in places. |
 | | General view of dolomite texture shows well-packed, finely crystalline dolomite in matrix, with coarser, euhedral dolomite filling porosity at center. |
 | | This dark area is a patch of partially dissolved and replaced, microporous chert (note remnant chert at bottom right), that was likely similar in texture to silica patch shown in A. Textures shown here suggest that pore-filling dolomite precipitated after silica. |
| www.mines.edu /research/PTTC/casestudies/lecrr/plate8.html (242 words) |
|