Diabase (also called dolerite) is a hard, fine-grained basic igneous rock with a composition similar to basalt and gabbro, but sitting between them in cooling rate and grain size. It is one of the most sought-after natural stones for heavy civil-engineering applications.

Origin and composition

Diabase forms where magma cools relatively quickly underground in cracks and fissures within existing rocks. Cooling is faster than for gabbro (so the grains stay finer) but slower than for basalt (so they are coarser and more crystalline). The main minerals are:

Because of these dark minerals, diabase is usually dark grey to black.

Properties

Diabase is valued for:

Applications

Because of these properties, diabase is used mainly in heavy infrastructure:

Use Reason
Railway ballast Wear resistant, dense enough to stabilise track
Asphalt for heavily trafficked roads High wear resistance and skid resistance
High-strength concrete (marine works) High strength and density
Bank protection and rip-rap Frost- and flow-resistant
Pavers and kerbs Skid-resistant and decorative
Gabions Coarsely broken diabase

Sources

Many countries lack workable diabase reserves and import the material from regions such as:

At the quarry the stone is crushed into various size fractions (e.g. 2–5 mm, 8–16 mm, 32–63 mm) and shipped by sea or rail to the user.

How diabase differs from basalt and gabbro

Rock Cooling Grain size
Basalt Fast (at surface) Very fine
Diabase Intermediate (in fissures) Fine to medium
Gabbro Slow (deep in crust) Coarse

Chemically all three are closely related: basic (silica-poor), dark and dense.

Related terms


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