- Earth's
crust experiences both
extensive and
transtensive shear. As such,
transtensional regions are
characterised by both
extensional structures (normal faults...
- p****ive margins: map-view
formation geometry (rifted, sheared, and
transtensional),
nature of
transitional crust (volcanic and non-volcanic), whether...
- the
shear motion is oblique. Pull-apart
basins form in
extensional to
transtensional environments along fault bends or
between two
adjacent left-lateral...
- of a
depression formed between two
sides of an
active strike-slip,
transtensional or
normal fault zone. A sag pond is
formed along a strike-slip fault...
- to be
measurable and significant. Some
oblique faults occur within transtensional and
transpressional regimes, and
others occur where the
direction of...
-
parallelism with the zone itself, the
style becomes either transpressional or
transtensional depending on the
sense of deviation. Strike-slip
tectonics is characteristic...
- can
include components of
extension and/or shortening, for
example in
transtensional or
transpressional situations,
which ultimately allow for the creation...
- ISSN 0091-7613. Unruh, Jeffrey; Humphrey, James; Barron,
Andrew (April 2003). "
Transtensional model for the
Sierra Nevada frontal fault system,
eastern California"...
- 2023. Kaya,
Ersin (2014).
Structure and
Tectonics of the Late
Cenozoic Transtensional Aksu
Sedimentary Basin, SW Anatolia.
Retrieved 12
February 2023. Büyükşehir...
- Paleocene.
Sinistral motions of
Iberia relative to
France created several transtensional sub-basins (pull-apart structures).
Turbidite sedimentation in the south...
