Rjh. Jolly et Dj. Sanderson, A MOHR CIRCLE CONSTRUCTION FOR THE OPENING OF A PREEXISTING FRACTURE, Journal of structural geology, 19(6), 1997, pp. 887-892
The opening of a fracture is dependent on the fluid pressure and the l
ocal stress regime around the fracture. For a fracture to open, the fl
uid pressure must exceed the normal stress acting on the fracture. The
Mohr circle provides a useful tool allowing the visualization of thes
e relationships. This construction determines the range of fracture or
ientations that are able to open, as well as determining the opening d
irection of these fractures. This is then used to produce ratios of th
e magma pressure and the principal stresses for some dykes from the Li
zard ophiolite, U.K. (C) 1997 Elsevier Science Ltd.