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Famatinian orogeny
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Famatinian orogeny
The
Famatinian orogeny
is an
orogeny
that predates the
rise of the Andes
and that took place in what is now western
South America
during the
Paleozoic
, leading to the formation of the
Famatinian orogen
also known as the
Famatinian belt
. The Famatinian orogeny lasted from the
Late Cambrian
to at least the
Late Devonian
and possibly the
Early Carboniferous
, with orogenic activity peaking about 490 to 460
million years ago
. The orogeny involved
metamorphism
and
deformation
in the
crust
and the
eruption
and
intrusion
of
igneous rock
along a Famatinian
magmatic arc
that formed a chain of
volcanos
. The igneous rocks of the Famatinian magmatic arc are of
calc-alkaline
character and include
gabbros
,
tonalites
and
granodiorites
. The youngest igneous rocks of the arc are
granites
.
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