Tension cracks parallel with the axial plane
N. Edelman
Bulletin of the Geological Society of Finland · 1973
doi:10.17741/bgsf/45.1.009 (opens in a new tab)
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Abstract
Tension cracks parallel with the axial plane are rather common in the archipelago of southwestern Finland. They are filled with pegmatite or quartz. They are here attributed to secondary elastic stresses in the axial plane.
Abstract licence: CC BY-NC
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