| dc.date.accessioned | 2019-03-27T15:56:50Z | |
| dc.date.accessioned | 2022-10-18T22:07:07Z | |
| dc.date.available | 2019-03-27T15:56:50Z | |
| dc.date.available | 2022-10-18T22:07:07Z | |
| dc.date.created | 2019-03-27T15:56:50Z | |
| dc.date.issued | 2014 | |
| dc.identifier | http://hdl.handle.net/10533/233623 | |
| dc.identifier | 1141139 | |
| dc.identifier.uri | https://repositorioslatinoamericanos.uchile.cl/handle/2250/4464980 | |
| dc.description.abstract | Long
and
short-‐term
tectonic
activity
plays
an
essential
role
in
the
segregation,
transport
and
emplacement
of
fluids
and
magmas
within
the
continental
crust.
Magma
ascent
and
emplacement
mechanisms
within
volcanic
arcs
are
largely
controlled
by
the
int | |
| dc.language | eng | |
| dc.relation | info:eu-repo/grantAgreement/Fondecyt/1141139 | |
| dc.relation | AGU (American Geophysical Union) Fall Meeting | |
| dc.rights | info:eu-repo/semantics/openAccess | |
| dc.title | Transtension controlling volcanic morphology: Insights from oblique-to-the arc tectonic
domains | |
| dc.type | Ponencia | |
