Cross-Scale Modeling of Mountain Building and the Seismic Cycle: From Alps to Himalaya: Springer Theses
Autor Luca Dal Zilioen Limba Engleză Hardback – 2 sep 2019
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Specificații
ISBN-13: 9783030289904
ISBN-10: 3030289907
Pagini: 156
Dimensiuni: 155 x 235 mm
Greutate: 0.43 kg
Ediția:1st ed. 2020
Editura: Springer
Colecția Springer
Seria Springer Theses
Locul publicării:Cham, Switzerland
ISBN-10: 3030289907
Pagini: 156
Dimensiuni: 155 x 235 mm
Greutate: 0.43 kg
Ediția:1st ed. 2020
Editura: Springer
Colecția Springer
Seria Springer Theses
Locul publicării:Cham, Switzerland
Cuprins
Introduction.-
Seismic
Behaviour
of
Mountain
Belts
Controlled
by
Plate
Convergence
Rate.-
Slab
Rollback
Orogeny
Model.-
Bimodal
Seismicity
in
the
Himalaya
Controlled
by
Fault
Friction
and
Geometry.-
Segmentation
of
the
Main
Himalayan
Thrust
Inferred
from
Geodetic
Observations
of
Interseismic
Coupling.-
Conclusions
and
Perspectives.
Notă biografică
Dr.
Luca
Dal
Zilio
is
the
Cecil
&
Sally
Drinkward
Post-Doctoral
Fellow
in
Geophysics
at
the
California
Institute
of
Technology
(Caltech).
After
completing
his
Bachelor’s
and
Master’s
degrees
in
Earth
Science
and
Geophysics
at
the
University
of
Padova
(Italy),
he
received
his
Ph.D.
in
Geophysical
Fluid
Dynamics
from
the
Swiss
Federal
Institute
of
Technology
(ETH
Zürich).
Dr.
Dal
Zilio’s
research
focuses
on
earthquakes
and
mountain
building
processes.
By
combining
theoretical,
computational
and
observational
approaches,
his
goal
is
to
better
grasp
the
seismic
behavior
in
orogenic
mountain
belts.
He
was
recently
selected
for
Nature
Geoscience’s
2018
Best
Geostory
Award.
Textul de pe ultima copertă
This
book
integrates
a
broad
range
of
scientific
disciplines,
from
geodynamics
and
tectonics
to
earthquake
physics,
geodesy
and
seismology.
This
holistic
approach
supports
a
detailed
investigation
of
the
deformation
and
seismicity
associated
with
mountain
building
processes
and
fault
activity
in
the
Earth’s
upper,
brittle
crust.
New
insights
into
these
deformational
processes
on
both
earthquake
cycle
and
geologic
timescales
are
subsequently
combined
to
improve
our
physical
understanding
of
seismicity
in
mountain
belts,
which
has
a
variety
of
potential
applications
in
active
tectonics
studies
and
seismic
hazard
assessments.
Caracteristici
Nominated
as
an
outstanding
Ph.D.
thesis
by
the
Institute
of
Geophysics,
ETH
Zurich,
Switzerland
Explores
the
moving
Earth,
from
the
micro
to
mega
scale
Explains
orogenesis,
the
formation
of
mountains
Sheds
new
light
on
one
of
the
greatest
unknowns
in
earthquake
modeling