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o
p
q
r
s
t
u
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w
x
y
z
##e
##f
##o
##r
##m
##a
##t
##i
##n
##l
##s
##d
##h
##y
##w
##v
##g
##c
##u
##k
##z
##b
##p
##x
##5
##0
##3
##j
##7
##q
##6
##he
##on
the
##re
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of
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and
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##ith
##osphe
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cr
in
lith
con
lithosphe
is
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th
##eo
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craton
##ve
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re
to
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##ation
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it
pro
##ical
##ou
##id
##ric
##the
lithosphere
are
##che
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su
gr
geo
mant
##ow
##if
##ess
lithospheric
mantle
by
##am
##ly
##chean
fro
##og
##ts
##ies
##ure
from
##th
##il
bel
te
##et
##om
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##ig
##eral
##cti
##ec
##ist
cont
co
for
ma
##hen
##est
##ite
gran
st
##ev
##ere
##od
##ab
as
ev
neo
##oc
##han
##cess
##ur
##ust
##per
##ate
##ich
##osit
##ction
crust
conve
that
##ogical
contin
ast
ex
ear
ind
par
##ter
##dc
##ce
##one
##archean
##ens
##ism
process
##henosphe
asthenosphe
sou
##ot
##se
##war
##gm
cratons
continent
asthenosphere
an
low
pre
wh
##ep
##oz
##oic
##har
##ud
##ick
thick
##ctive
comp
which
##ozoic
at
bas
dif
dhar
er
gre
or
pl
with
##eat
##fere
##ov
##mal
##nt
##hi
##ul
##uction
##ature
##eri
##erature
##osion
##ins
##cton
##isc
##mperature
temperature
neoarchean
differe
dharwar
erosion
ar
imp
on
und
we
##ew
##fer
##mov
##ay
##ia
##ness
##um
##us
##ication
##ary
##enst
##ely
cons
remov
##thern
sub
geol
belts
tecton
magm
##ock
part
##terozoic
greenst
archean
under
greenstone
al
dest
ga
ke
mo
other
rel
sc
sev
tr
up
var
visc
wdc
##ra
##ac
##tion
##ties
##hy
##ved
##cre
##ong
##atic
##and
##ally
int
##ents
proper
##ctiv
granul
stud
evol
##osition
convective
earth
india
southern
continental
lower
thickness
different
geological
tectonic
##ocks
keel
several
properties
bou
gen
late
met
mec
nor
she
som
ter
##ri
##ak
##ast
##ted
##im
##vid
##ge
##ges
##pro
ther
##ated
##ity
##arg
##ndary
##stand
##ory
this
its
##ification
form
composition
##hib
weak
understand
vari
granulite
boundary
mechan
shear
some
##proterozoic
ac
bu
ben
can
du
dec
dens
edc
fig
hig
hist
lay
mod
peri
ro
rhe
wid
##iz
##ive
##sical
##duction
##ces
##ates
##ern
##ans
##ites
##ost
##ell
##ort
##ork
cratonic
rec
sug
grad
##ogy
##ists
##able
##osity
exhib
processes
pres
##eath
import
consists
removal
viscosity
into
north
mechanism
beneath
due
figure
high
history
layer
modification
period
rheol
exhibit
am
be
bl
bec
col
chan
di
dy
dep
east
heat
li
man
mes
marg
oce
rocks
sg
sep
was
zon
zone
##fic
##ration
##ruction
##mical
##most
##ave
##iev
##nam
##lm
##ho
##gest
##und
##ution
##by
##pre
##qu
##here
there
##ics
##ass
refer
provid
geod
##ill
below
believ
mafic
granite
str
##ered
neoproterozoic
crustal
parts
plum
destruction
moho
sclm
trans
##hysical
##ctively
studies
evolution
general
terra
accre
recent
suggest
important
deple
lik
many
meso
sgt
separ
zones
thereby
believed
plume
ad
activ
bet
ch
che
de
dat
det
dur
fur
few
fac
gl
how
km
ka
le
lab
loc
mat
min
ov
rig
rich
so
sh
smal
when
where
will
##em
##een
##ft
##fle
##oy
##ob
##mom
##av
##au
##ap
##act
##ail
##agm
##iv
##ior
##ld
##led
##sed
##yp
##ynam
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##ween
##vent
##gh
##ci
##ch
##can
##uct
##kes
##ph
##50
these
##red
##espre
##ities
##ale
##nding
##osed
##ine
##ions
##ional
##orph
incre
cond
than
##asom
rework
##ous
##chem
sur
##amb
##amorph
##iliz
granites
stable
events
convection
earl
south
##sequ
continents
base
plate
##erial
temperatures
one
consid
subduction
magma
scale
upper
study
evolved
keels
metasom
metamorph
thermal
thermom
formed
weaken
buoy
density
root
widespre
present
rheological
exhibits
blocks
dykes
eastern
ocean
referred
geodynam
struct
transfer
terrains
depleted
like
mesoarchean
between
chemical
data
during
further
glob
material
mineral
rigid
soft
small
##flect
##ause
##agmatic
increas
##sequent
thermomagmatic
widespread
structure
37
active
amal
age
bo
cl
cre
del
dist
disc
ef
en
fr
fi
fl
fin
fund
has
have
kar
long
mel
mass
nw
nu
num
ou
phan
pass
physical
res
rif
se
sy
sw
sin
tre
typ
used
vi
ver
vol
war
wor
west
xen
##eas
##ectively
##op
##other
##ry
##rit
##rad
##ms
##mot
##ain
##amp
##ture
##tered
##ian
##ially
##la
##les
##so
##der
##dration
##well
##val
##ga
##gn
##gam
##cl
##cle
##camb
##uid
##ber
##ple
##physical
##posed
##ond
##ating
##atism
##icating
##erozoic
##erved
##itic
##itrad
##ence
##inn
##inal
##inate
##stem
##round
##iths
##cting
##eld
init
inter
conduction
convent
##ental
thus
thinn
ret
reg
rehy
reflect
toge
##ations
##ational
##ology
##oliths
proterozoic
promot
##oup
##ough
##idence
##rich
areas
super
suture
geother
geochem
geophysical
##own
##amew
##aminate
##amental
##lying
##iest
##ilt
##omes
##ads
##erall
##istry
cool
forces
##ever
##abiliz
evidence
##urga
convecting
continu
examp
exposed
early
indicating
##termost
any
anci
another
prev
precamb
basal
basins
order
differen
removes
subsequent
magmatic
magmatism
underlying
along
altered
also
destabiliz
more
relat
releas
upwell
viscus
##rian
##vided
compositional
understanding
variation
but
wide
grade
gradu
mechanisms
periods
rheology
amou
among
being
because
becomes
cold
chang
changes
dire
divided
margins
provides
generally
accretion
accreted
separated
separates
activity
chitrad
detail
facies
however
kaap
leads
overall
shown
whereas
##ively
condu
reworking
surround
earliest
consider
metasomatic
metamorphism
weakening
buoyant
oceanic
geodynamic
transfers
globe
mineralogical
increases
amalgam
both
delaminate
eff
framew
fluid
finally
fundamental
massif
nucle
outermost
phanerozoic
passive
seism
system
trending
view
volcan
world
western
xenoliths
conventional
rehydration
together
geochemistry
ancient
precambrian
destabilizing
released
upwelling
chitradurga
kaapval
framework
fluids
13
250
35
350
40
56
550
60
af
aw
ab
act
amp
ages
bh
bar
bro
bab
bhi
brit
cal
cam
char
cud
cause
coup
des
dis
dev
deri
dri
dim
et
ep
emp
eac
ecl
fe
fo
fol
fast
fact
go
gn
gh
gas
hy
hyp
id
kal
kil
kom
kim
kamb
lat
lid
lim
larg
line
mw
mar
mos
med
mid
mad
mig
mov
most
non
not
new
ol
os
oc
ob
oro
our
oper
old
pr
pu
per
pal
peo
pow
pod
phy
position
past
pain
ran
red
ris
rid
sl
sil
sig
sec
shi
sim
sarg
schem
tw
ton
tan
tens
tim
table
trich
tilt
vel
wy
wat
wit
were
way
well
wave
yil
##eg
##eed
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##equ
##fa
##for
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##filt
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##othe
##ots
##ron
##ran
##rst
##raton
##rce
##rins
##rates
##ma
##mb
##mer
##min
##ment
##mation
##ments
##ah
##aic
##ains
##ti
##tic
##tin
##tle
##tical
##tens
##tac
##tiliz
##tational
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##ip
##ier
##ied
##iation
##ium
##ients
##iated
##iates
##iitic
##nif
##nts
##not
##lin
##lis
##lant
##low
##lite
##lication
##lac
##land
##lim
##lian
##ses
##sis
##sol
##soc
##sics
##ssed
##served
##dd
##dit
##dro
##dap
##hj
##ys
##yc
##yar
##vic
##ver
##van
##ves
##ven
##gi
##gre
##gar
##gen
##gered
##cy
##ced
##cis
##ccess
##cur
##cum
##cri
##crit
##uric
##uity
##uces
##ugh
##utational
##kal
##zan
##zation
##be
##bed
##blication
##por
##pectively
##00
##jor
##onents
##ontin
then
they
##reas
##regn
##relian
##rever
##ats
##atical
##ately
##atiz
##atiitic
##ica
##icant
##ers
##erist
##erate
##erous
##ermin
##erves
##ani
##ance
##ancy
##esy
##ition
##itates
##itational
##alite
##allow
##ose
##osep
##enrich
##ina
##ined
##inct
##inci
##sts
##stab
##stra
##stell
##roved
##roys
##rovic
##cted
##ctory
##elop
##ors
##org
##orth
infer
incl
infilt
incis
instab
lithology
consequent
constra
isot
island
##ented
##entif
though
those
##eous
##eoproterozoic
##assical
##isod
##inges
refra
reenrich
tool
##olite
##ological
probe
##idot
##idus
##rican
##chemical
such
sudd
success
grav
geoch
geotecton
geochemical
##ogites
##ilar
##ilities
##ilitates
belt
##ety
##etic
##etot
##eters
##oming
##ometers
##ada
##ades
##adgi
##adition
##iginal
##iggered
content
contra
contact
core
cohere
coorg
magn
major
granod
##abud
asce
asse
assoc
even
##ocities
##hanced
##osites
convectively
exot
expre
extens
indication
indian
indeed
##ensation
##ensch
##ensions
asthenospheri
source
##sected
##ward
anorth
prevent
##udes
composed
complim
computational
components
atlant
basin
based
greensch
original
play
plac
##ntly
##hip
##ulation
##ults
impregn
improved
impinges
only
##nessed
removed
subsol
geology
tectono
magmas
partially
alkal
destroys
moyar
others
relate
related
relations
trond
tradition
triggered
upward
varies
integ
intrins
granulites
lowermost
differentiation
tectonics
generate
genetic
northern
terran
terti
##rier
##gests
forms
compositionally
##hibolite
weaker
weakens
variant
variable
various
variety
mechanical
accum
cannot
canada
deccan
decoup
decraton
decreas
decades
denser
densification
role
roots
##ization
##elluric
recyc
suggests
gradients
preserved
preserves
importance
highly
exhibited
block
colla
collis
dynam
margin
marginal
oceans
refertiliz
provide
provided
geodesy
##illation
strong
mohorovic
transpor
terrain
suggested
depletion
likely
mesoproterozoic
adequ
addit
advan
activities
china
deflect
defor
degre
determin
facilitates
karelian
leave
local
located
locations
over
shallow
##emite
##avu
##avani
##acterist
##ails
##ivine
##iorite
condensation
reworked
surfa
earlier
considered
uppermost
metasomatiz
metamorphic
buoyancy
presented
geodynamics
chemically
global
softens
increase
closep
classical
creep
cretac
distinct
distillation
discip
discontin
enough
enhanced
field
first
karur
karwar
melt
melts
number
numerous
respectively
results
rift
rifts
sink
since
types
typical
very
vertical
warms
warmer
##ope
##ained
##lages
##berlite
##ondary
initially
initiates
interior
interstell
thinner
thinning
retains
retained
region
regions
reflects
promote
promotes
superior
supercrit
sutured
geothermal
geotherms
continuation
continuous
example
examples
prevents
prevails
basalts
basaltic
difference
differences
relative
relatively
gradual
gradually
amount
amounts
changed
changing
direct
direction
details
detailed
conductive
conductively
surrounded
surrounding
amalgamation
amalgamated
effectively
effect
massifs
nuclei
nucleus
seismic
seismology
volcanism
volcanics
1300
african
away
above
amphibolite
bhavani
barrier
brough
bababud
bhima
brittle
called
came
characterist
cuddap
coupled
descri
dissected
develop
derived
driven
dimensions
etc
episod
emplac
each
eclogites
forever
fold
factors
good
gneis
ghats
hydro
hypothe
identif
kaladgi
kilometers
komatiitic
kimberlite
kambam
lateral
limit
largest
linear
mwm
mark
mosaic
medium
made
migration
moves
olivine
occur
observed
orogen
operation
oldest
princi
publication
peridot
paleoproterozoic
people
power
pods
physics
painavu
range
reduces
rising
ridges
slab
silica
signif
secondary
shield
similar
sargur
schematical
two
tonalite
tanzan
time
trichur
tilting
velocities
wyoming
water
witnessed
yilgar
##ronological
##mblages
##lines
##hjemite
includes
infiltration
incisive
instabilities
consequently
constrained
isotope
refractory
reenrichment
tools
sudden
successively
gravitational
geochronological
geotectonic
##etotelluric
contrasts
coherently
magnetotelluric
granodiorite
ascending
assemblages
associated
exotic
expressed
extensive
asthenospherization
anorthosites
preventing
complimented
atlantic
greenschist
plays
places
impregnation
subsolidus
alkaline
relationship
trondhjemite
traditionally
integrates
intrinsic
terranes
tertiary
accumulation
decouples
decratonization
decrease
recycled
collage
collisional
dynamic
refertilization
mohorovicic
transported
adequately
additions
advances
deflected
deformation
degree
determining
shallows
surface
metasomatized
closepet
cretaceous
distinctly
disciplines
discontinuity
fields
interstellar
supercritical
brought
bababudan
characteristics
cuddapah
described
developments
episodes
emplaced
gneisses
hydrous
hypothesis
identified
occurs
orogenic
principle
publications
peridotitic
significant
schematically
tanzania
yilgaran
magnetotellurics