[2] The belt is a "northeast-striking zone defined by: a Proterozoic shear zone system (McCoy, 2001); a suite of Laramide-aged plutons and related ore deposits (Tweto and Sims, 1963); a major gravity low (Isaacson and Smithson, 1976); low-crustal velocities; and high heat flow (Decker et al., 1988).

"[3] Mining districts include:[2] The belt lies within a zone[specify] that has been geologically active at intervals beginning from near the time of crustal accretion in central Colorado at least 1.6 billion years ago until the present.

Parts of the CMB follow shear zones of Precambrian age[1] and the Paleozoic and Mesozoic.

Igneous rocks intruded about 60 to 70 million years ago during the Laramide orogeny are associated with the belt and once were thought to be responsible for most of the ore deposits.

[4] Now many of the important ore deposits are thought to be[opinion] genetically related to younger magmatism, some at least as young as about 25 million years.