127
sodium
taken
london
load
rotation
diagonal
S11
rearranged
elsevier
shown
ruoff
reduce
studied
insight
godwal
26ds11
placed
s33
presence
setting
thank
elasticity
interesting
worked
estimate
smith
2002
situation
angew
cauchy
nature
supported
there
appreciable
intercept
loaded
cesmec
jephcoat
thl2
appropriate
dependence
180
matter
importance
d2s11
cmmac
discontinuity
duffy
breslin
dhklth21
treated
perpendicular—
source
front
measuring
3gdhklth
occur
varying
separating
powder
polycrystal
inter
few
extensively
reducing
show
planetary
york
instrum
even
1975
ltd
contact
1991
should
discus
plane
4686
calculated
los
tungsten
uniaxial
interest
polakowsky
rheological
spend
uncompressed
resulting
349
sci
differently
dhklth
knowledge
d18th
immersed
137
square
off
708
wavelength
known
tmin
additional
nonhydro
asm0
equality
position
1944
ﬁnancial
assumption
deal
relying
symmetry
freezing
lite
line
neighboring
fisher
result
keyword
142
delay
wa
disadvantage
real
set
1988
C33
correcting
cij
detail
mao
ceased
earth
daymond
could
expression
interface
23d1
suggesting
laboratorie
computed
research
15063
center
geophysical
considering
klotz
257
sight
application
2ds11
sensitive
both
rheology
applicable
important
rev
comparison
inaccessible
englewood
mainly
all
M1
dispersion
peak
enclosing
bend
inade
manghnani
vaughan
itie
development
limitation
1984
support
polycrystalline
d8th
factor
quasicrystalline
get
anisotropic
murnaghan
d17th
335
smax
complete
concomitantly
third
mgo
agree
geophy
deviate
wood
discrepancy
33199
constituent
1976
cubic
below
during
butterwoth
continuity
encountered
stixrude
greatly
approach
elsewhere
5338
kavner
equally
2dm
recently
jianu
rather
revised
difﬁcult
goetze
volume
higher
1943
van
d9th
distributed
ﬂuid
modulu
valid
relative
—geometry
dij
derive
extended
magnitude
geometric
equation
‘differential
exist
908
right
attributed
compression—some
extraction
easily
aksingh
handled
tail
d1th
coincide
slope
miami
four
slippage
crystal
gallardo
micro
priesmeyer
validation
pfarr
undergo
topic
represented
ﬁne
region
homogeneou
plastic
simple
predicted
419
vol
suggest
leak
d5th
grima
ethanol
continuously
hill
recording
commonly
radiation
tmax
expected
consisting
calculate
main
nicula
1998
calculation
modiﬁcation
boron
mail
cliff
S12
causing
bangalore
many
merkel
conventional
4956
dhklth
subject
kqhkll
numerical
moment
permanent
1257
energy
d11th
system
noyan
conden
syono
exact
provide
way
model
static
national
739
145
1974
hdhklthedhklth
remaining
understanding
3sgdhklth
rigorou
1972
highly
ignore
d10bth
measured
strictly
friction
possibility
voigt
USC
presented
accessible
study
description
gasket
case
singh
observation
alone
aligned
ripling
combination
surface
309
1963
conﬁrmed
slip
about
extrapolate
824
axial
stressed
parameter
prove
relation
1987
complexity
ellipticity
mag
2296
investigate
shen
017
von
fei
soc
791
cold
normal
beryllium
suggested
compressed
wherein
doi
2001
temp
possible
symbolically
chem
later
operation
recognizing
topsoe
derivative
gdhklth
opposing
4dtmax
length
metal
bassett
varied
–31
containing
yield
427
iron
understood
2sgdhklth
introduced
thick
23M1
inhomogeneou
pﬃﬃ
deﬁnition
examine
achieved
1982
inﬂuenced
under
2hklth
preferred
mezouar
1589–1596
lehrbuch
distinct
differential
1592
earlier
1933
1thd2gv
d15th
sdhklth
determined
satisfactory
anvil
W33
FIU
cthgdhklth
detection
collection
velocity
face
compression
group
accessed
angle
large
florida
accepted
der
compute
anisotropy
2157
ast
boundary
deformation
permit
origin
bulk
respective
theory
strain
wilson
simul
S44
267
great
reus
inﬁnite
formalism
without
than
determine
force
moduli
measure
become
initial
deform
earliest
strike
cryst
isotropic
electro
yagi
symbol
calcu
tion
technology
careful
several
effort
cos21
propertie
texture
strength
2000
zero
image
1979
attracted
1929
lead
PTM
effectivenes
plate
record
practice
order
following
weaver
indistinguishable
tend
data
orient
basal
d13ath
corresponding
after
discussion
water
gradient
meade
india
–71
shear
1147
acknowledgement
engineering
instrumental
meng
second
difference
1997
bound
repeat
deviatoric
magnetic
universitie
insensitive
reported
174
work
302
chen
1940
641
dhklth1d
new
conducted
2S11
funamori
044
three
reviewed
respectively
develop
reference
yielding
ponkratz
prediction
1593
cth1
mathematical
enhance
conclusion
two
bras
athd2gv
wide
each
243
d13cth
753
technique
W11
hausermann
hashin
experi
attention
it
taneou
differ
crystallite
plot
generated
helium
1990
special
weight
full
describe
ultrasonic
changed
half
close
niobium
2691
limit
amorphou
consistent
probability
physic
shieh
however
appl
compared
consequently
eq
obviou
misalignment
one
detector
minimum
relationship
did
averaged
method
molybdenum
teubner
any
more
material
ultra
let
among
epoxy
considered
iment
detailed
most
analyse
transparent
stop
information
neumann
164
3269
560
particle
measurement
cs
d6th
s22
relevant
still
978
kinsland
direction
kristalphysik
will
phase
much
PMT
pascoe
chloride
kqdhklthl
average
proﬁle
d2gv
synchrotron
experiment
fact
seen
gpa
cause
quite
sample
only
very
13c
C13
usually
d16ath
problem
homo
recorded
aggregate
structural
produced
d10ath
component
park
reorientation
align
ref
eisenforsch
into
107
liepzig
–45
good
ambient
journal
dependent
then
luo
formu
edhklth
thicknes
state
ds11
ring
0022
8071
reserved
interference
773
205
dxth
behavior
hkl
involving
diffracting
493
speziale
1591
isotropy
increa
ndwth
hemley
ﬁeld
depending
dhklth1
1993
due
V0
analyzing
introduction
151
1977
increased
1952
independent
FWHM
received
mathie
1242
extreme
quacy
often
intensity
parallelism
stresse
similar
3337
1995
methanol
circle
toward
value
displacement
contain
evaluated
rotating
indicate
shu
science
free
make
mitt
assuming
saxena
allow
gerward
tds11
spacing
passing
empirically
badro
larger
gaussian
cohen
property
termed
transition
cupping
mise
M0
hyderabad
datths
applied
some
function
steinle
processe
unrestricted
B11
quadrant
raised
constant
spread
respect
expressed
non
5892
given
qdhklth
analysi
lipson
130
principal
sayer
article
xia
begin
soderlind
between
aspect
2ap
stress’
likely
uchida
276
parallel
3523
justiﬁcation
elastic
pillinger
detected
justiﬁed
positive
lation
though
incident
434
hanﬂand
variation
nelli
plausible
axi
5920
wenk
TH
ﬁlled
les
modeling
offer
mixture
C44
oriented
gauthier
465
solidiﬁe
shift
publication
eos
doe
controlled
struges
verify
lating
d7th
pattern
hundred
bunge
studying
anil
consider
theoretically
DC
equivalence
freeze
variou
lower
design
studie
solidi
ser
path
using
interpreting
single
da21
1928
balasingh
since
1996
gigapascal
orthogonal
hydrostatic
ing
involved
nonhydrostatic
ed
corrected
other
prentice
term
investigator
perpendicular
except
d2th
university
upper
compare
literature
another
view
TH21
limited
versu
kroner
integral
radial
obtained
katahara
stres
proc
obtain
curve
washington
6729
proceeding
2004
partial
2TH
generate
choice
processing
moriarty
well
3thd1
d16bth
hexagonal
because
recent
condition
chemistry
AIP
ksn
lattice
inviting
variance
subscript
symmetric
NJ
level
1596
axe
pres
followed
diffraction
smaller
ds33
phy
occurring
d16cth
1978
harmonic
gillet
beam
wilh
birch
burkel
wider
22GX
suitable
cos2
4278
weidner
1971
d10cth
3TH1
orientation
decrease
marker
straight
slightly
early
1016
fig
experimental
equal
nicol
d13bth
continuou
form
vary
longer
28–
give
render
unique
3830
used
jpc
precision
cthqdhklth
young’
examined
lie
when
derived
TH2
july
technol
3697
1999
twist
may
re
2217
hall
different
diamond
d14th
mid
addres
convention
1992
thu
pressurized
creep
solid
pressur
mode
besson
lett
1389
further
change
379
1386
november
width
number
abrupt
randomly
summary
geneou
called
6gkqdhklthlf
initially
–21
produce
statu
elastically
286
ﬂow
superscript
s11
scale
best
therefore
ernet
having
rhenium
dat
cease
interpretation
13b
vohra
denote
point
hand
pressure
carried
far
3261
4327
carbide
overestimate
required
also
compliance
AGU
distribution
related
but
2st
small
over
passe
found
tensor
criterion
agreement
miner
sonic
instead
nacl
W22
assume
boundarie
correspond
like
dh2
aerospace
ha
hartley
stoke
nearly
low
1594
176
cth
satisﬁed
easy
through
succes
while
theoretical
caused
akahama
takemura
take
loading
cthqdhklth
axis—1
extrapolation
linear
residual
1371
generalized
depend
1994
device
unit
made
strikman
3TH
morup
redundant
surrounded
du0
estimation
687
such
wang
equivalent
FL
intersect
edge
example
discussed
2S44
d4th
present
these
grain
mech
see
deﬁned
isolation
–309
ray
time
C12
208
ment
acros
sponsored
exhibit
quantitie
springer
either
detect
d12th
1962
1958
review
585
1TH
geometry
correct
general
maximum
additive
complex
restrict
nth
agreed
cell
bridge
showed
kawamura
international
relaxation
jeanloz
represent
out
reason
inst
macro
probe
sij
stage
size
vely
math
setup
side
908TH
2S12
solving
compressibility
enough
balance
langford
radially
kennedy
exper
short
use
despite
398
5S44
temperature
1595
255507
physik
822
arise
mineralogy
4smax
343
504
suitably
conference
1966
13a
investigation
2hkl
transparency
respecti
hdhklth
2d0
require
transmitting
broadening
sung
houtte
1590
typical
dispersive
broaden
establish
scientiﬁc
microscopic
observed
pointed
axially
noted
d20th
d3th
DAC
established
d19th
mean
phenomena
terra
simultaneou
along
not
interpreta
remain
onset
division
drop
2dp
range
planet
medium
effect
beta
philo
62–67
7567
standard
homogenou
1629
abstract
compressive
major
primary
high
USA
simpliﬁed
destroy
tokyo
kimura
thin
structure
heinz
kdsn
2003