DOLOSTONE
Dolostone (formerly "dolomite") is a chemical sedimentary rock
composed of the mineral dolomite (CaMg(CO3)2 -
calcium magnesium carbonate). Dolostone can be jokingly described as the
"ultimate non-descript rock". It often looks like driveway gravel.
Well, there's a reason for this - a lot of driveway gravel is dolostone (at
least around where I live).
Most dolostones are grayish,
microcrystalline-textured, and have vuggy porosity. Vugs are irregularly-sized &
shaped cavities. Some dolostones are
fossiliferous. Fossiliferous dolostones usually have poorly-preserved
fossil "ghosts" (see below). Rarely, fine-grained dolostones
have soft-bodied fossil preservation.
Crystalline-textured dolostones appear secondary in
origin. They are typically interpreted
as chemically-altered fossiliferous limestones. Some dolostones look
primary, but how they formed is not entirely clear. Chemically, all
that's needed to form dolostone is the addition of magnesium (Mg) to
limestone. The details of this chemical change are not fully understood.
A few localities on Earth do have dolomite or protodolomite forming now, but
the dolomite-forming process is still
a significant unsolved problem in sedimentary geology - "the dolomite
problem".
Dolostone of Silurian age with vuggy porosity (= the irregularly-sized &
shaped holes) and fossil “ghosts” (the somewhat rounded, empty structure on the
right side is an external mold of a fossil brachiopod).