This work reviews the mechanism of rifting with a focus on pre-existing
tectonic weaknesses in pre-rift and/or basement rocks, i.e., on tectonic
inheritance. The passive margins that are studied in this book are the
Norwegian Continental Shelf, the Eastern North America and the East and
West Indian Continental Margins. The continental rifts that have been
analysed are the East African Rift System, the Brazilian Continental
Rift Systems and the European Cenozoic Rift System. It states how rifts
and passive margins serve as valuable locations for hydrocarbon
exploration. Tectonic inheritance/heritage examines the influence of
pre-existing/pre-rift elements on the geometry, genesis and propagation
of rift-related faults. Such elements include anisotropies in the
shallow crustal levels, as well as the rheology of the lithosphere.
Inheritance greatly influences the architecture of rifted passive
margins including the attitude of faults and geometry of horsts, (half-)
grabens, transfer zones etc. Inheritance is also a determining factor in
the width of rifts and rift shoulder topography.