Diabase is a dark, intrusive, basic igneous rock made up of plagioclasefeldspar crystals, surrounded by smaller grains of pyroxenes, such as augite and up to ten percent quartz. Diabase is formed from magna that has cooled just below the Earth's surface, and is sometimes found as intrusions in older rock. A common place to find diabase is in the neck of old volcanoes, where it has formed a plug. Research Diabase
Pentlandite is the most important industrial source of nickel and has the formulae (Fe,Ni)9S8 and a relative hardness of 4. Pentlandite was confirmed as a distinct species in 1856 and named after Joseph Pentland, the discoverer of it.
Pentlandite forms in basic igneous rocks such as diabase and gabbro through magmatic segregation. Research Pentlandite