-
potential sources of
diapirs.
Diapirs also form in the Earth's
mantle when a
sufficient m**** of hot, less
dense magma ****embles.
Diapirism in the
mantle is...
- of
relatively buoyant magma in
large m****es
called plutonic diapirs.
Because the
diapirs are
liquified and very hot, they tend to rise
through the surrounding...
- of salt
needed to form a
layer thick enough for the
formation of salt
diapirs,
indicating that a
sustained period of
episodic flooding and evaporation...
- The Añana
Diapir (Basque: Añanako diapiroa, Spanish:
Diapiro de Añana) is a
diapir in Álava,
Basque Country, Spain. Two
notable wetlands are
located within...
-
responsible for the
formation of domes, the
foremost of
which are refolding,
diapirism,
igneous intrusion, and post-impact uplift.
Structural domes can be formed...
- dome-shaped
forms called diapirs when
doing so. On Earth, salt
domes are salt
diapirs in the
crust which rise
through surrounding rock.
Diapirs of
molten low-density...
- for
later magma.
These mechanisms can
operate in tandem. For example,
diapirs may
continue to rise
through the
brittle upper crust through stoping, where...
-
evaporite deposits of Jur****ic age.
These salt
deposits formed salt dome
diapirs, and are
found in East
Texas along the Gulf coast. East
Texas outcrops...
- away from
plate boundaries has been
postulated to
arise from
upwelling diapirs from the core–mantle boundary, 3,000
kilometres (1,900 mi) deep within...
- Erin
Field westward is a
strongly folded anticline ****ociated with
shale diapirism,
which extends west
southwestward to the
Pedernales Field in southeast...
