Different things, buddy. The Danvers pipe is a hydrothermal breccia, they mention mineralised infill.
No once-in-a-generation ore deposit is 100m x 100m x +/- 200m vertical.
Flow top breccias are formed when the basalt is erupted, and in these basalt systems, they are areas of higher porosity where the mineralising fluids collect. But they are thin and discontinuous.
Great for some 60% Cu rock chips to gee up the uninformed mug punters, though!
Ann: 105mtrs @ 2.25% Cu from 27.43m at Danvers, page-29
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