Estimation of Radon Flux Density Changes in Temporal Vicinity of the Shipunskoe Earthquake with Mw = 7.0, 17 August 2024 with the Use of the Hereditary Mathematical Model
Geosciences,
Journal Year:
2025,
Volume and Issue:
15(1), P. 30 - 30
Published: Jan. 16, 2025
Using
the
data
of
radon
accumulation
in
a
chamber
with
excess
volume
at
one
points
Kamchatka
subsurface
gas-monitoring
network,
change
flux
density
due
to
seismic
waves
and
post-seismic
relaxation
medium
is
shown.
A
linear
fractional
equation
considered
be
model
equation.
The
radon-transport
intensity
changes
state
geo-environment
described
by
Gerasimov–Caputo
derivative
constant
order.
Presumably,
order
related
geosphere.
Levenberg–Marquardt
method,
optimal
values
parameters
were
determined
based
on
experimental
data:
air
exchange
coefficient
derivative,
which
allowed
solving
problems
determination.
Data
temporal
neighborhood
strong
earthquake
Mw=7.0,
occurred
northern
part
Avacha
Bay
17
August
2024,
used.
As
result
modeling,
it
shown
that
impact
subsequent
processes
led
chamber.
obtained
curves
agree
well
real
data,
estimates
theory.
Language: Английский
Comparison of Backprojection Techniques for Rupture Propagation Modelling of the Mw = 7.8 Mainshock Earthquake near Kahramanmaras and the Mw = 7.5 Second-Largest Mainshock near Elbistan, Turkey, 2023
Geosciences,
Journal Year:
2025,
Volume and Issue:
15(4), P. 146 - 146
Published: April 14, 2025
This
paper
utilises
teleseismic
Z-component
data
to
investigate
rupture
propagation,
extent,
and
velocity
for
two
very
destructive
earthquakes
in
the
East
Anatolian
Fault
Zone
(EAFZ):
Mw
=
7.8
earthquake
near
Kahramanmaras
largest
(Mw
7.5
s)
aftershock
at
Elbistan
(both
on
6
February
2023).
The
extent
of
is
modelled
with
beamforming
multichannel
signal
classification.
are
derived
from
agencies
USA
Canada.
found
be
bi-directional
towards
northeast
southwest.
Three
segments
identified
between
34.5°–37.5°
longitude
37.0°–37.5°
latitude,
another
three
36.5°–38.0°
around
38.5°
latitude.
A
total
299
km
covered
185
s
velocities
3.1
km/s
3.4
km/s.
Additionally,
mainshock’s
splay
second-largest
aftershock’s
also
bidirectional,
covering
150
within
46
s.
Five
identified,
earthquakes.
Beamforming
efficient
identifying
segments.
findings
provide
new
insights
evolution
spatio-temporal
EAFZ
may
serve
as
a
basis
long-term
hazard
planning
area
Language: Английский