Late Devonian lamprophyric dykes in the Meguma Zone of Nova Scotia

R. M. F. Kempster, D. B. Clarke, P. H. Reynolds, A. K. Chatterjee

Canadian Journal of Earth Sciences · 1989 · 28 citations · 9 references

Concepts

Abstract

Hornblende-rich lamprophyric dykes from southeastern Nova Scotia are contemporaneous with the large peraluminous granitic batholiths (ca. 370 Ma) of the Meguma Zone and may be closely associated with their origin.

References

9