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From YouTube: DISC Lab: Mexico City Afternoon
Description
DISC Lab in Mexico City: Afternoon
A
A
A
B
A
A
A
This
is
the
model
or
right
of
the
time.
This
is
the
central
line
around
this.
This
way-
and
this
is
the
sir
Fazle-
is
evolving-
and
the
the
sons
place
where
copper
is
rather
greater
than
five
thousand
million
so,
and
you
can
see,
then
the
relationship
between
the
sound
we
normally
are
related
with
local
low
resistivity.
A
So
sometimes
we
want
to
move
believing
all
models
using
additional
information
like
the
data,
our
physical
properties,
in
this
case
resistivity,
and
there
are
some
Ray's
in
the
same,
and
some
data
are
collected
from
the
course
of
the
degree.
Yes,
so
we
have,
and
then
we
have
the
related
information
of
how
is
resistivity
along
along
one
reading.
A
A
B
A
A
A
B
B
A
C
A
D
D
D
B
D
D
The
actual
in
version
and
this
this
this
model
can
make
all
the
processing
all
the
line
of
process
the
data
and
the
final,
a
inclusion
inclusion
at
a
daring
version
we
use
to
the
immersion
some
like
called
density,
the
Murphy
for
first
model
approximation
and
this
hummingbird
with
mystical
method
like
simulated
annealing
for
gravity
and
magnetic.
But
this
is
other
topic
in
this
nice
table.
We
I
talked
about
about
the
terrible
TDM
software.
D
D
D
Here
talk
about
the
structure
of
the
program
and
all
the
related
topics,
about
the
architecture
of
the
interface
and
the
course
and
a
coding
developed
for
this
this
this
platform.
Here
you
can
see
the
procedural
diagram
for
the
literal
word,
PDF
software.
You
can
start
with
all
the
related
with
the
processing
after
that
modeling
and
inversion.
The
the
first
issue
is,
you
can
hear
you
can
take
your
your
for
your
exome
data
at
the.
D
B
D
That
he
showed
before
it's
like
Cecil.
Is
this
app?
It's
like
a
program
for
open
source
access
to
immerse
your
mobile
infrared
exterminating
data
and
for
this
stage
for
mullen
NE
version,
we
use
beautiful
it's
an
algorithm
for
those
Newton
Marquardt.
Okay,
there's
in
this
algorithm!
No,
no
everyone!
The
roof
is
from
societal.
B
D
D
Of
electromagnetic
method,
this
is
algorithms,
is
open
source
and
we
make
modification
to
include
in
this
platform.
The
the
newbie
of
this
platform
is
motor
interface
and
some
more
rooms,
and
you
can
make
easy
you
can
make
a
nice
way
older.
Your
your
phrasing
data
selection
on
leaks,
make
profiles
and.
D
D
E
D
D
D
D
This
is
the
first
stage
of
the
program
you
can.
You
can
make
visualize
the
data.
If
you
only
include
the
points,
this
is
the
60
amps
that
we
entering
in
the
platform,
and
you
can
see
all
energy
slippery's
is
at
least
open
source
liveries.
You
can
see
immediately
there
your
your
racing
data,
the
six
points
of
tedium
so
needs
make
in
this
data's.
D
This
is
the
generator
first
in
winter,
Phoenix
of
the
terror
world,
TDM
platinum
here,
all
winter
Felicis
develop
in
cootie
and
the
altar
detector.
The
program
is
c++,
the
other
guy
in
charge
of
all
the
coding,
and
the
background
is
scientifically
things
he
doesn't
hear.
But
Francisco
can
talk
about
the
numerical
and
all
the
background
mathematical
analysis
to
include
this
time
of
examples
or
operation
to
processing
to
modeling
and
inverted
TDM
data
destruction
of
the
way
of
the
interface
of
the
rubber.
D
D
D
This
is
one
of
the
the
next
step
for
processing.
You
make
all
the
runs
in
the
field.
You
you
make
sure
that
the
points
that
you'll
make
sure
in
the
in
the
time
domain
for
for
lying
for
late
times,
it's
very
accurate
and
you
will
come
in
and
this
this
is
runs
to
make
a
a
new
curve
like
a
chief
screw
and
in
this
disturb
you,
you
can
eliminate
four
runs
corrected
for
game
cooks
for
the
work
for
the.
F
D
B
D
The
palings
that
we
make
in
the
in
the
decay
curve-
and
this
is
other
interface
in
interfacing-
for
processing-
you
can
the
new
mattress
and
resistivity
core,
and
you
can
make
other
kind
of
analysis
like
sensitivity,
analysis,
really.
You
can
create
a
complete
curve
for
resistivity
for
late
times
and
every
times.
D
This
is
the
religion
model,
layer,
modeling
and
you
can
put
it
in
polymer
parameters
with
the
number
of
layers,
the
width
of
the
layers-
and
this
is
the
initial
model
the
resistivity
versus
versus
then-
and
you
can
put
in
the
limits
of
death
and
the
limits
of
the
resistivity,
well
I.
Think
in
the
moment,
Paco
can
talk
about
all
the
background
analysis
that
he
he.
B
G
B
G
Some
with
some
details
about
I'd
rather
say
before:
hey
this
is
not
an
average
good,
if
not
bodies
and
make
you,
sir
I,
guess
it's
good.
That
is
because
the
another
obscure
involves
modify
your
data.
So
this
is
not
a
modified
data
from
every
every
runs
of
the
something
we
choose.
We
calculate
the
average
and
the
and
the
points
nearly
points
of
these
averages
cure
is
what
we
took
for
the
adjusted
for
a
first
at
all
and
we
are
teaching
the
the
software.
G
G
B
G
Can
take
for
every
x,
+
4
plate
times,
so
this
is
the
modelling
in
turf
the
modeling
interface.
So
we
can
see
here
the
layer
layer
model
and
we
can
choose
an
initial
initial
model
from
resistivity
versus
depth,
which
is
coming
from
the
curve
of
complete
resistivity
from
a
practice.
So
we
can
choose
this
curve
all
we
can
choose
again
mahtim.
You
see
me
space
and
we
can
choose
the
logarithmic
scale
or
linear
scale.
A
G
G
Well,
here
is
they
they
quit
the
equation
system
for
solving
for
the
welcome
they,
not
the
partial
derivatives
mattresses
and
the
Chekhov
it
so
here
is
the
an
example
of
the
current
version
of
this
tube.
Here
are
the
the
parameters
the
initial
year
of
the
finally
rule.
The
number
of
parameters
set.
A
here
is
the
layer,
the
real
model
and
in
blue
we
have.
The
inverse
mode
is
muted
important
model
here
is
the
Buell's
cognitum
mapper,
and
the
parameters
of
convergence
in
here
is
the
curve
in
blue
of
the
of
the.
G
There
is,
there
is
a
better
adjust
in
the
curves,
and
you
are
the
same
at
the
same
as
before.
Here
are
the
parameters.
Finally,
initially
so
we
can
see
with
some
benefit
of
this,
of
this
inversion
is
that
we
can
invert,
also
resistivity
and
depth
and
thickness
in
aachen.
Only
we
can
use
invert
the
resistivity.
G
G
Something-
and
here
is
the
other,
the
other
step
from
the
software
in
the
intersection
of
map
with
with
happen,
the
sunbeams
and
we
can
select
one
one
section,
one
line
section
and
we
can
select
to
the
the
sun-
is
something
but
which
we
want
to
project
into
the
line
section
it's
DC
says
easy
way,
so
we
have
the
our
section
and
we
can
choose
the
the
interpolation
could
be
linear
premium
or
other
interpolation.
We
see
that
in
this,
in
this
type
of
data
of
TDM
data
is
better,
be
linear.
G
G
We
have
yet
some
problems
with
the
color
color
theory
is
not
so
easy,
so
it's
not
so
pretty
this
section
or
we
as
I,
was
mentioning
before
we
are
working
yet
in
this
over
well,
because
we
have
to
before
to
commercialize
and
other
things.
We
have
to
perfection
this,
and
this
is
the
section
of
the
commercial
software
and
we
have
a.
G
G
E
I
C
C
E
E
I
C
C
F
C
C
So
here
I
think
it's
an
interesting
question
that
has
been
raised,
but
we
need
to
think
both
about
the
question
and
the
answer,
but
sometimes
these
are
the
things
that
are
really
informative.
So
suppose
you,
you
have
a
loop
system
and
then
you
look
at
the
very
early
time
and
you
find
that
it's,
the
behavior
is
different
than
what
you
might
expect
so
that
that's
at
some
point
things
are
going
to
kind
of
decay
with
a
particular
race.
But
if
you're
in
very
near
field,
very
early
things
might
change
over
and
ask
Muto
I.
C
Think
that's
the
question
and
the
way
to
make
really
good
use
of
this
is
to
first
of
all
have
a
numerical
example
that
chosen
and
then
to
start
trying
to
promote
it's
a
question
of.
Why
is
that
and
then,
ultimately,
that
has
to
go
back
to
the
formulas,
so
you
could
look
at,
for
instance,
a
dipole
in
in
a
hole
spacer
over
over
a
spit,
perhaps
space,
and
you
find
that
there's
actually
many
terms.
C
If
you
look
in
the
book
by
weight,
then
you
know,
there's
there's
a
lot
of
terms
in
there
and
at
some
point
this
term
is
useful
at
some
point.
That
term
is
useful
and
you
can
use
those
astronautics
to
kind
of
understand
what
the
nature
of
that
curve
is,
and
by
doing
that
by
linking
the
mathematics
with
the
numerix
with
the
visual
calculation.
Those
things
turn
out
to
be
really
powerful
understanding,
I
think.
B
F
C
I
I
I
Commerce
forties
use
the
overworld
from
so
with,
with
with
the
dreamer
Shama,
I
I
suggest
you
limit
of
the
promise.
That
is
the
magenta
line
unless
we
are
going
to
do
four
empty
profiles
and
in
this
world
a
person
that
is
one
that
is.
This
is
one
more
here
that
is
from
Puerto
peñasco
Sonora
to
aquaris
one.
B
I
I
I
B
C
I
B
A
B
I
I
B
B
B
I
F
B
F
So
I
mean
enough
not
what
we
use
it's
the
natural
source,
as
we
saw
yesterday,
it's
our
first
magnetic
field
of
the
earth,
their
interaction
and
also
the
Lightning's.
So
we
have
all
of
that.
We
have
a
lot
of
energy
around
the
earth
and
if
we
use
that
one
limitation
of
the
of
this
metal
business,
if
we
have
some
wonderful
song
very
close
to
here
nearby
with
a
cup
to
anything
because
it's
gross
and
then
the.
F
F
F
F
C
F
F
F
B
F
F
F
F
F
F
F
B
F
F
F
F
But
we
were
in
the
right
direction,
so
the
next
step
was
making
very
big
loop
by
loop,
seven
point
four
meters,
and
at
that
time
engineering
decided
to
do
the
same
secret.
He
looks
for
the
base
as
well.
We
saw
40
around
empty,
we
did
some
bass
and
we
need
some
state
moving
station.
In
this
case
same
would
have
two
days.
F
F
For
the
air
balloon,
we
have
three
BS
one,
two,
three
with
us,
a
quick.
Yes,
we
can
control
all
the
time
they
have
to
love
the
system
coos,
but
we
that
we're
missing
it's
the
components,
and
this
is
because
the
of
the
middle
they
are
magnetic
in
that
one
there
is
no.
There
is
no
response.
If
all
be
wrong,
if
we
have
space
is
homogeneous,
so
you
don't
have
any
response,
but
it's
not
going
to
happen
in
the
earth
near
Carol
and
discontinuities.
F
F
F
The
second
iteration
of
a
bases
that
were
used
for
polishing
selling
service-
and
this
is
the
notify
everyone
bloop,
it's
told
by
90
others.
Okay,
it's
very
long,
so
we
need
experienced
pilots
flight
experience
very
long,
the
tow
cable,
but
it's
possible
to
control
by
the
pilots
inside
but
long
because
we
need
to
keep
the
the
machine
out
of
the
as
far
as
possible
of
the
loop
to
reduce
the
noise.
F
F
In
general,
the
most
reliable
you
are
from
360
to
34
radiance
with
60
Hertz
power,
and
it's
2
into
the
filtering
that
we
use
here
is
a
sample
of
a
perfect
record
with
only
X.
My
clothes
and
the
burqa
is
the
airborne
and
those
ones
are
from
from
the
base
we
can
get
one
for
every
station
leaves
and
we
have
the
power
spectrum.
We
can
see
that
we
have
lots
of
energy
here
and
then,
because
almost
0
to
0
man
gives
the
same
way
for
higher
frequencies.
So
that's
a
problem.
We
can
go
I.
F
F
F
F
F
F
F
F
G
F
So
at
the
top
there
is
the
the
admiration
song
at
the
peaks
a
and
over
some
granite,
and
in
here
we
have
to
run
a
new
song,
say
something
everything
and
because
of
the
depth
of
the
sandstone,
that
it's
over
boarding
be
in
conformity.
So
this
one's
our
be
the
models
for
the
area
and
we
can
see
the
operation
achieve.
B
A
F
F
F
F
A
F
F
Well
after
that
station
that
I
show
me
2.5
meters.
We
went
to
three
and
three
calls
for
three
components
for
the
base
station.
That
one
was
the
two
meters
which
on
each
side
they
were
square,
and
then
we
were
trying
to
fly
with
that.
It
was
brought
that
impractical
to
do
the
fact
that
it's
very
much
it's
very
difficult
to
fly,
3
3
goals,
2
meters
and
with
keeping
the
noise
level
slope.
So
we
decided
to
be
back
to
the
girls,
one
girl,
the
American
gold
and
for
thee
for
the
stations.
F
Now
we
have
a
some
course
of
3
meters
in
length.
They
are,
they
have
a
core
iron
core
and
they
need
to
be
calibrated
because
it
was
a
matter
how
we
try
to
do
it
there.
So
there
are
small
difference
of
us
on
both
points,
so
we
can
equate
the
base
and
we
can
break
the
final.
That's
not
that
much
problem,
because
it's
a
current
error.
So
there
is
no
problem,
but
we
can
program
on
that,
but
you'll
at
once.
F
F
F
F
H
C
C
C
G
C
C
About
an
hour
so
Lindsey's
going
to
take
you
on
a
walk
through
sempai
show
you
the
site,
talk
a
little
bit
about
the
software
and
how
to
access
the
apps
and
yeah.
That's
that's
going
to
open
up
a
portal
to
you,
so
we
won't
be
able
to
talk
about
everything.
But
at
least
you'll
have
a
net
have
a
vision
for
what
is
there
and
then
you
can
use
that
and
communicate
and
get
conversations
going
so
that
lets
see
Thanks.
H
H
To
other
contributors,
so
there's
a
few
different
things,
and
one
of
them
that
I
want
to
point
out
here
is
this
is
called
the
GP
gene.
So
this
is
it
like
a
basically
a
web-based
textbook
that
has
been
created
for
introductory
applied
to
your
business,
so
we've
been
using
this
at
UBC
for
an
undergraduate
geophysics
course.
It's
mostly
geologists
and
geologic
engineers
who
take
this
course.
So.
H
All
of
the
Chi
of
mythical
methods,
we
introduce
everything,
gravity
and
net
excitement
GPR
DC.
So
this
is
meant
to
be
a
useful
resource
for
an
introduction
to
Keough.
Business
is
open
source
and
it's
meant
to
be
something
st..
You
can
add
to
and
edit
things
in
Alta.
So
if
there's
examples
of
you're
teaching
a
course
and
makes
an
example,
they
have
that
you
really
like
it
would
like
having
good.
We
can
work
with
you
to
make
sure
that
the
colleges
there's
already
a
professor
in
California
we've
started
adopting
this.
H
H
To
point
out
here
is
the
case
histories,
so
these
are
all
these
are
bright.
Ups
that
accompany
some
of
the
cases
trees
of
induction
of
gas
today,
they're
all
broken
down
into
that
same
seven
step
framework,
so
we've
all
got
fairly
similar
looking
field
and,
for
the
most
part,
they're
based
on
published
paper.
So
this
is
the
high.
H
Broken
down
into
those
seven
steps,
and
then
we
reference
the
original
paper.
If
you
want
to
go
back
and
see
all
the
details
and
in
particular,
if
you
have
a
case
history,
that
you
would
like
to
contribute
as
well,
but
something
that
we
can
work
with
you
to
get
that
it's
exciting
to
see
this
go
and
see
applications
in
different
areas.
They're
meant.
B
H
H
So
if
you
come
here,
you'll
see
that
there
are
two
different
styles
of
apps,
so
we
have
the
EMS,
and
these
are
really
a
meant
to
be
like
beauty,
style
interactions
with
Maxwell's
equations.
So
you
don't
really
see
any
code.
All
your
going
to
do
is
run
through
your
notebook
and
I'll.
Show
you
this
in
a
minute
and
then
you'll
get
some
widgets
and
some
vineyards
and
that's
it
on
the.
B
H
Style
I'll
show
you
these
as
well.
These
are
the
simulation
of
notebooks,
and
so
what
these
are
is.
These
are
examples
that
will
actually
show
you
how
to
use
open
source
software
like
attached
to
run
the
EEM
forward
simulation
or
an
inversion,
and
it
shows
you
all
of
the
code.
So
if
you
want
to
see
all
the
details
of
how
to
actually
code
up
and
run
them
forward
simulation
by
this
is
where
to
go.
So,
let's
take
a
look.
H
H
By
looking
at
Microsoft
Azure,
it's
supposed
to
look
here,
so
what
this
is
is
this
is
actually
a
cloud
service
that
microsoft
offers
for
free
for
small
notebooks,
where
we
can
actually
just
get
this
running
on
the
way.
So
here
this
is
what
you'll
see
when
you
click
on
that
link
at
first
and
you'll
notice
that
the
Run
button
is
grayed
out
so
right
now
we're
not
actually
logged
in.
So
we
just
need
to
sign
in
and
so.
H
F
H
H
H
B
B
H
Tasking
we
want
to
replace
that
and
we
can
update
it
so
please
and
then
now
we
can
actually
receive
it.
The
run
is
live
so
we're
good
to
go
so
you'll
see,
there's
there's
three
pages
of
notebooks,
and
so
what
we've
tried
to
do
is
name
them
by
method.
First,
so
we've
got
a
whole
bunch
with
DC
Istanbul.
B
H
So
what
this
is
doing
when
I
clicked
on
this,
we
spun
of
the
server
summer,
crucio,
Microsoft
and
so
they're
launching
a
new
notebook
if
you're
not
familiar
with
Jupiter,
it's
an
interactive
computing
environment.
It's
really
been
used
a
lot
in
the
Python
community,
but
it
actually
it
doesn't
care
what
language
you
use
and
it
can
interoperate
with
a
lot
of
different
programming.
H
This
business
there's
two
ways
you
can
run.
Did
you
clear
a
book?
So
each
of
these
cells
is
like
a
code
cell,
so
you
can
do
shift
enter
to
run
them
one
at
a
time.
The
other
thing
you
can
do
for
these
apps.
If
you
just
go
to
cell
run,
all
it'll
just
run
them
all
or
it
that's
fine
for
the
apps,
because
there's
like
three
three
cells
of
code,
so
what's
happening
here,
is
we're
installing
a
package
built.
H
H
They
were
going
to
import
some
standard
Python
packages
as
well
as
REM
acts,
and
then
we've
got
a
short
little
write-up
and
a
couple
of
questions.
So
we
show
you
what
the
setup
looks
like
what
each
of
the
parameters
are
and
then
here
now
we
have
our
app
where
we
can
go
and
play
with
the
cylinder
and
the
sphere
and.
H
We
have
a
resistant
layer,
so
two
tiers
question
earlier
today.
The
comment
that
came
up
is
that
we
were
looking
at
currents
versus
electric
fields.
Let's
forget
about
the
cylinder.
For
now,
we've
got
this
resistive
layer.
We
can
see
what
the
currents
are
getting
so
in
this
case
they're
they're
bunching
up
mostly
in
this
top
layer.
H
H
H
We
have
a
couple
of
frequency
domain
examples,
and
so,
if
you
remember
yesterday
seeing
the
example
of
the
occurrence
in
the
sphere
these
diesel-run
not
for
you,
so
you
can
actually
go
and
reproduce
some
of
the
figures
that
you
saw
yesterday
and
then
the
other
thing
that
I'll
walk
through
in
a
moment
is
this
empty
tutorial.
So
recently
we
broke
a
short
leading-edge
article
that
basically
builds
up
before
a
simulation
for
a
1d.
They
neither
telluric
problem
and.
B
H
Go
in
and
investigate
and
shows
the
important
choices
that
you
make
in
the
inversion,
and
so
this
serves
a
couple
purposes.
It
shows
what
those
important
choices
are.
So
looking
at
things
like
picking
off
curve,
you're
stopping
criteria,
you're
twisting
data
that
your
choice
of
parameters
and
your
regularization,
somehow
smaller.
H
H
Is
is
to
actually
bring
all
of
the
geophysical
methods
into
one
place
so
that
you
can
have
a
consistent
way
to
access
them
play
around
with
conversions,
and
one
of
our
big
goals
has
really
been
to
give
you
hooks
and
the
ability
to
play
with
all
of
the
disease
so
that
if
you
want
to
go
in
and
look
at
the
fields
and
closes
and
where
the
currents
are,
when
you
solve
it
in
this
case
simulation
I,
you
can
easily
do
that
in
an
intuitive
way.
Rather
than
coming
back
around.
H
Moving
back
as
an
open
source
project
is
a
my
team
license
you're
free
to
use
it
I,
do
what
you
like
with
it
there's
two
papers
about
it.
There's
links
in
some
of
slides
from
yesterday's,
so
there's
one
paper
describing
the
overall
simulation
framework
and
then
there's
one
papers
specific
to
electromagnetics
and
that
also
breaks
down
how
we're
thinking
about
the
problem.
H
There
easily
but
I
think
it's
gonna
be
very
nice.
We
also
have
slack
on
so
that
is
one
way
that
you
can
get
in
touch
with
us
and
have
a
conversation,
and
so
that
you
can.
Actually
you
know
if
you've
got
questions
and
things
like
that
that
come
up
you
can
get
in
touch
with
the
real
solution
and
that's,
what's
the
what
they
stood
to
start
is
really
looking
at
the
examples.
H
H
H
H
Actually,
a
field
data
center,
also
physical
examples
with
DC
frequency
domain,
iam
natural
source
time
domain,
there's
fluid
flow
field.
You
may
know
some
we've
got
regions
equation
in
there.
It's
a
little
bit
of
seismic.
It's
just
straight
way
of
smog
Rafi.
So
if
that's
something
you're
interested
in
and
interested
in
contributing,
and
then
it
could
be
utilities.
H
So
we
walk
through
starting
through
Maxwell's
equation.
What
is
the
system
that
we're
going
to
actually
disparate
eyes
and
solve
because
we're
in
1d
we
can
take
advantage
of
that
cemetry
really
reduce
this
down.
I'll
show
you
where
things
are
at
district
highest.
So
what
is
it?
What
does
it
know?
What's
an
edge
so.
E
H
In
discrete
growth,
and
then
here
we
actually
show
you
what
the
district
ID
system
should
look
like
and
then
below
we'll
build
that
up
in
same
thing,
so
we
design
a
mesh,
get
our
operators
and
then
we're
going
to
go
ahead
and
build
up
that
system.
So
if
here
we're
just
defining
a
bunch
of
years,
but
then
this
is
the
system
that
we
want
to
solve.
So
we
then
go
ahead
and
show
okay.
These
are.
H
H
H
H
H
H
And
then
this
here
are
going
to
do
with
this
empty
for
simulation
last
bit
code
that
we
wrote
in
the
last
notebook.
So
that's
our
script
that
runs
at
one
p
answer
problem,
so
we're
going
to
do
here
instead
of
a
half
space
model
and
the
thing
that
we're
going
to
look
at
is
mesh
design.
So
we're
going
to
compare
what
goes
on
if
we
make
art
our
finest
it
sells
to
be
order
for
your
katakana.
H
So
one
of
the
things
that's
really
important
to
consider
when
you're
designing
a
mesh
is
that
we're
capturing
the
highest
frequencies
properly.
So
the
rapid
changes
near
surface.
We
need
to
make
sure
that
our
finest
selves
are
fine
enough
to
capture
badly.
So
the
thing
to
look
at
there
is
the
skin
depth,
and
so
our
sort
of
rule
of
thumb,
this
one
make
sure
at
least
you
know
four
cells
for
your
phone
for
your
tallest
skin
depth.
H
And
then
you
need
to
also
make
sure
that
your
mesh
extends
far
enough,
because
the
boundary
condition
on
the
bottom
basically
says
we're,
assuming
that
our
fields
indicate
as
we
need
to
make
sure
that
you
know
here.
A
couple
of
index
pass
your
lowest
frequency,
and
so
here
all
we
do
is
based
on
our
hundred
immediate
half
space,
and
the
frequency
ranges
that
you
chose.
I
will
print
out
our
index
and
we're
going
to
design
a
match
to
make
sure
that
our
finest
cells
are
by
enough
and
our.
H
H
H
H
Are
we
matching
the
analytic
so
in
this
case
we're
doing
a
good
job
on
both
can't
resist
Indiana
babies,
but
one
of
the
things
that
you
might
want
to
look
at
it's
okay,
how
far
you
mean
push
that
so
what
we've
done
in
this
notebook
is.
There
is
a
couple
of
way
to
get
to
where
we
conclude
the
minimum
cell
size
and
the
domain
instant.
H
H
H
H
H
H
B
H
H
You
see
that
it
would
be
extremely
difficult
to
actually
try
and
tease
apart
which
model
we
actually
have
as
services.
We're
bringing
in
things
like
a
primary
information
is
really
important
if
you
know
how
deep
your
layer
is
or
how
thick
your
layers
or
perhaps
conductive
your
leadership,
those
pieces
of
information
and
then
actually
help
specify
which
model
should
be
looking
for
us
at.
H
H
And
so
here
we
didn't
free
and
bring
the
packages
that
we
need.
The
way
that
we
set
up
the
inverse
problem
is
as
an
optimization.
So
this
is
a
fairly
typical
keeping
off
style
bridge
the
two
pieces
here.
So
there's
our
datum,
which
fit,
which
is
this
by
team
and
then
there's
our
model
regularization,
which
we
call
fly-in
and
then
in
between
them.
There's
a
trade
off
grammar,
basically.
H
E
H
F
I
H
Here
we
set
up
a
match
so,
as
we
said
before,
we
want
to
make
sure
that
it
goes
far
enough,
and
so
this
little
utility
basically
builds
us
on
extras.
That
is
reasonable.
For
this
install
and
soo
Plagueis
is
written
in
Python,
which
is
an
object-oriented
language.
So
what
that
means
is
you
can
create
objects
like
a
mesh
and
it
actually
has
methods.
H
I
H
H
H
Of
details,
so
I'm
not
going
to
go
into
that
now,
but
it
is
included
in
the
right
up
here
and
you're
welcome
to
get
in
touch
with
us
with
questions,
and
so
this
is
the
this
to
pay
frameworks
to
set
up
and
how
we
really
are
thinking
about
the
inverse
problem,
and
so
what
I
mentioned
before
these
inversion
elements?
That's
really
what
we're
going
to
focus
on.
In
this
example,
it's
the
database
a
bit
in
the
vaporization
I.
H
So
all
we've
written
here
is
a
simple
function
to
actually
go
ahead
and
run
the
MT
inversion.
So
this
is
a
lot
of
inputs,
but
these
are
all
different
things
that
you
can
play
with
in
the
inversion,
and
so
we
walk
through
and
playing
with
a
couple
parameters,
but
we've
tried
to
set
up
so
that
you
can
go
in
and
teach
with
everything.
H
H
H
So
there's
a
few
things
that
are
inside,
so
we
print
out
the
value
of
beta
I
will
print
out
the
5d.
So
what's
our
getting
a
biscuit
and
the
regularization,
and
so
then,
in
this
case
let's
say
version
is
finished.
We
can
plug
off
our
Tegan
off
curves,
and
so
in
this
case,
what
we're
going
to
do
is
we're
gonna,
show
we've
got
five
e,
Phi,
M
and
then
fighting
forces.
So
this
is
what
we've
marked
as
the
star
here.
B
H
E
H
I
H
H
H
H
H
C
C
C
H
H
H
H
H
E
C
B
C
Actually
make
one
one
comment
here:
that's
that's
actually
a
good
way
to
find
people
are
always
worried
about
depth
of
the
investigation
right
so
that
that
one
way
of
doing
that
is
to
actually
change
your
reference
model.
Okay-
and
you
end
up
with
two
different
reference
models,
then
you
look
at
the
back
end
and
that
smallest
term
will
take
it
down
to
that
reference
model
and
when
it
does.
H
B
H
H
B
C
Yes,
I'll
just
echo
that
we're
actually
hoping
that
this
is
actually
going
to
be
a
start
of
a
longer
communication
and
some
people
have
already
offered
to
contribute
to
EMGs
I
tell
us
what
IP
membrane
polarization
is.
This
is
good
and
yeah.
Maybe
we
can
use
Deiters
program,
wrap
it
up
in
some
apps
and
make
that
useful.
So
it's
been
really
good
to
get
it
an
insight
as
to
what
the
problems
are.
We
can't
really
thank
you
for
putting.