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Ion beam analysis techniques: a powerful set ge tools for identification and sourcing of ancient gems

Abstract

Gemstones are defined as rare minerals having a high clarity, a high hardness and showing a bright colour and a nice shining. The most important gems are diamond, sapphire and emerald. These gems are callad precious stones. Gems have fascinated man since the earliest times. They have always been sought out by man for their aesthetic and symbolic valué. Due to their scarceness and high '^alue, gems were appreciated by the mighty ones as a sign of their power (emperors ^nd kings, dignitaries of religions ...). Their high hardness and henee strong resismnce to deterioration symbolised the everlastingness of their reign. This last property is interesting from an archaeological point of view: gemstones travel through time without noticeable alteration, even buried in aggressive environment. On the other hand, gems oiay be used several times on different jewels, possibly cut and polished again. Like spices and other precious and sought-after items, gems were brought back from long distance. Accordingly, they are good tracers for ancient trading routes and influence of civilisations. Each civilisation had its own favourite gemstones: lapis lazuli in Egypt; amber and emerald in the Román Empire; gamet in early Middle Ages westem civil isations; jade, ruby and sapphire in Far-East cultures. Moreover, the provenance of some ancient gems such as emeralds or gamets is still debated. For all these reasons, the study of gems kept in museum collections is a promising research fíeld.

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Ion beam analysis techniques: a powerful set ge tools for identification and sourcing of ancient gems

Author: Calligaro, T.; Dran, J.C; Poirot, J.P; Querré, G.
Publisher: Universidad de Sevilla
Year: 1999
Source: https://idus.us.es/bitstreams/3c3d86b5-272a-4865-a44d-8fbba6a00275/download
ION
BEAM
ANALYSIS
TECHNIQUES:
A
POWERFUL
SET
GE
TOOLS
FOR
THE
IDENTIFICATION
AND
SOURCING
OF
ANCIENT
GEMS
T.
C(i¡li{*a o'".
J.C.
D an'".
J.P.
Poi o "
anci
G.
Que é
INTRODUCTION
Gems ones
a e
de ined
as
a e
mine als
ha ing
a
high
cla i y,
a
high
ha dness
and
showing
a
b igh
colou
and
a
nice
shining.
The
mos
impo an
gems
a e
diamond,
sapphi e
and
eme ald.
These
gems
a e
callad
p ecious
s ones.
Gems
ha e
ascina ed
man
since
he
ea lies
imes.
They
ha e
always
been
sough
ou
by
man
o
hei
aes he ic
and
symbolic
alué.
Due
o
hei
sca ceness
and
high
'^alue,
gems
we e
app ecia ed
by
he
migh y
ones
as
a
sign
o
hei
powe
(empe o s
^nd
kings,
digni a ies
o
eligions
...).
Thei
high
ha dness
and
henee
s ong
esismnce
o
de e io a ion
symbolised
he
e e las ingness
o
hei
eign.
This
las
p ope y
is
in-
e es ing
om
an
a chaeological
poin
o
iew:
gems ones
a el
h ough
ime
wi hou
no iceable
al e a ion,
e en
bu ied
in
agg essi e
en i onmen .
On
he
o he
hand,
gems
oiay
be
used
se e al
imes
on
di e en
jewels,
possibly
cu
and
polished
again.
Like
spices
and
o he
p ecious
and
sough -a e
i ems,
gems
we e
b ough
back
om
long
dis ance.
Acco dingly,
hey
a e
good
ace s
o
ancien
ading
ou es
and
in luence
o
ci ilisa ions.
Each
ci ilisa ion
had
i s
own
a ou i e
gems ones:
lapis
lazuli
in
Egyp ;
ambe
and
eme ald
in
he
Román
Empi e;
game
in
ea ly
Middle
Ages
wes em
ci il
isa ions;
jade,
uby
and
sapphi e
in
Fa -Eas
cul u es.
Mo eo e ,
he
p o enance
o
some
ancien
gems
such
as
eme alds
o
game s
is
s ill
deba ed.
Fo
all
hese
easons,
he
s udy
o
gems
kep
in
museum
collec ions
is
a
p omising
esea ch
í
eld.
2.
ANALYSIS
OF
GEMSTONES
Usually,
he
iden i ica ion
o
gems
elies
on
he
measu emen
o
op ical
and
me-
chanical
p ope ies:
e ac i e
index
n,
bi e ingence,
isible
op ical
spec um,
speci ic
g a i y
p
[1]-
When
gems ones
a e
se
on
a
jewel,
hese
measu emen s
a e
no
always
Cen e
de
Reche che
e
de
Res au a ion
des
Musées
de
F ance.
Palais
du
Lou e.
Pa ís
CNRS
UMR-171
.
198
T.
Cmjmíako.
J.-C.
Dhw.
J.-P.
Po/koi
>
CJ.
eadily
ca ied
ou .
Dismoun ing
hem
om
he
se ing
o
sampling
is
o
cou se
p o-
hibi ed.
The
p o enance
o
gems,
ha
means
he
geog aphical
loca ion
o
he
deposi ,
is
o en
in e ed
by
iden i ying
speci ic
inclusions.
Ano hc
possibili y
is
he
chemical
cha ac e isa ion
o
gems ones.
In
his
case,
gems
a e
di ccily
idcn i ied
by
means
o
hei
majo
chemical
cons i uen s.
Fo
ins ance,
diamond
is
a
pu c
ca bón
c ys al;
niby
is
an
AI2O3
c ys al
colou ed
by
less
han
1%
C ;
sapphi e
is
also
an
ALO*
c ys al
bu
i s
blue
colou
is
due
o
ace
amoun
o
Ti
and Fe;
eme aid
is
a
bc yl
o
o mula
Be3Al2(Si03)6
colou ed
by
a
small
amoun
o
C .
The
ace
clcmen
con cn
o
gems
also
ca ies
aluable
in o ma ion.
Indeed,
some
o
hese
ace
elemen s
come
om
he
su ounding
ocks,
being
inco po a ed
du ing
he
génesis
o
he
c ys al.
Being
linked
o
he geological
con ex
( ype
o
e ain
and
ock- o ming
his o y)
ace
elemen
con-
en
may
ac
as
a
inge p in
o
he
occu cnce
o
a
gems one.
A
wide
ange
o
ech-
niques
ha e
been
applied
in
iew
o
pe o m
chemical
analysis:
EMPA.
XRF,
NAA,
ICP/MS,
SIMS.
Table
I
summa ises
some
ea u es
o
he.se
analy ical
echniques.
O
cou se,
ca e ul
obse a ion
o
he
gems
and
hei
in e nal
ea u es
using
con en ional
gemmological
means
has
o
be
pe o med
p io
o
p oceeding
o
hese
chemical
analy
sis.
Mo eo e ,
se e al
analy ical
echniques
ha e
o en
o
be
combined
o
in e ing
unambiguously
he
p o enance
o
a
gem.
Table
1.
Fea u es
o
se e al
analy ical
echniques
used
o
he
chemical
cha ac
e isa ion
o
gems
EMPA
EDXRF
NAA
LA-ICP/MS
SIMS
IBA
Elemen
ange
>
Na
>
Na
Selec ed
all
all
all
LOD
>1.000
ppm
1-1.000
ppm
<
1
ppm
<
1
ppm
<
1
ppm
1-1.000
ppm
P obé
size
pm
mm
whole
sample
10-//m
//m
10-//
m
Des uc i e
no
no
ac i a ion
P-
des uc i e
P-
des uc i e
no
P epa a ion
yes
/
coa ing
no no
no
yes
/
coa ing
no
Iso opic
in o
no
no
no
possible
yes
no
Sample
size
cm
any
cm
any
cm
any
EMPA:
elec ón
mic op obe
analysis.
EDXRF:
ene gy-dispe si e
X- ay
luo esccnce.
NAA:
neu ón
ac i a ion
analysis.
LA-ICP/MS:
lase -ahla ion
lon-coupled-pla.sma
mass
spec ome y.
SIMS:
seconda y
ion
ma.is
spec ome y.
IBA:
ion
beam
analysis.
3.
IBA
TECHNIQUES:
PIXE
AND
PIGE
APPLIED
TO
THE
STUDY
OF
GEMS
I
is
no
he
place
he e
o
gi e
a
comple e
desc ip ion
o
Ion
Beam
Analysis
(IBA)
echniques;
nume ous
books
and
e iew
pape s
will
ul il
his
equi emen
[2
and
3].
Le
us
jus
ecall
ha
IBA
echniques
ely
on
he
same
p ocess:
iden i ica ion
o
ele-
Til
199
CoNcRi.so
Naciiiwi
OI
AKQi
i-(nnn"RlA
den al
cons i uen s
by
de ec ing
p oduc s
o
in e ac ion
o
he
ion
beam
and
he
a ge
(••e.
gems one).
Among
hem,
PIXE
(pa icle
indiiced
X- ay
emission)
is
qui e
simila
XRF,
being
based
on
he
de ec ion
o
X- ay
emi ed
by
he
a ge
a oms,
subsequen
o
an
inne -shell
ionisa ion.
The
only
di e ence
s ems
om
he
exci a ion
sou ce
which
a
cha ged
pa icle
beam
ins ead
o
a
X- ay
beam.
Fo
he
PIGE
echnique,
ac onym
o
pa icle
induccd
y- ay
emission.
he e
is
no
coun e pa .
PIGE
elies
on
a
nuclea
eac ion
subsequen
o
he
collision
be een
an
inciden
pa icle
and
a
a ge
nucleus.
Pollowing
his
eac ion,
he
nucleus
migh
emi
a
y- ay
ha ing
a
speci ic
ene gy.
On
he
o he
hand,
IBA
echniques
canno
be
used
o
iso opic
a io
de e mina ion
ño
<^oes
i
gi e
in o ma ion
on
chemical
bonds.
F om
he
poin
o
iew
o
gemmology,
he
IBA
echniques
exhibi
se e al
Ín e es
ing
ea u es.
Fi s ,
in-ai
IBA
echniques
allow
in
si i
and
non-des uc i e
analysis
o
8cms
wi hou
sample
p epa a ion.
This
haimlessness
is
a
mus
o
he
s udy
o
a
luable
obje s
such
as
his o ical
jewels.
Using
simul aneously
he
PIXE
and
PIGE
me-
hods
i
is
possible
o
de e mine
a
wide
ange
o
elemen s.
PIXE
gi es
he
composi ion
o
elemen s
anging
om
Na
o
U,
while
PIGE
use ully
ex ends
he
ange
o
i-,
e
ones;
F,
Be,
Li,
B.
Secondly,
he
high
sensi i i y
o
hese
echniques
pe mi s
inea-
^u emen
o
elemen s
down
o
a
low
le el
o
concen a ion
(e.g.
—
ppm
w
)
ansi ion
me áis
in
co undum).
Finally,
he
use
o
a
mic obeam
wi h
a
size
o
ess
han
20-^m
allows
selec ion
o
inclusions
o
hei
iden i ica ion.
Such
a
small
spo
is
also
use ul
o
analysing
a
egión
ee
o
inclusions.
Indeed,
when
using
a
b oade
spo
size,
he e
is
always
he
isk
o
including
an
inclusión
in
he
analysed
a ea
^a
may
bias
he
ace
composi ion
o
he
c ys al
(e.g.
an
Fe-con aining
inclusión
migh
lead
o
a
w ong
Fe
ace
con en
in
a
uby).
F om
he
poin
o
iew
o
he
IBA
echniques,
gems ones
a e
ideal
samples
when
compa ed
o
o he
objec s
o
cul u al
he i age
such
as
pain ings
o
ce amics.
They
ha e
3
simple,
homogeneous
composi ion.
The
sample
has
a
polished
and
o en
ía
su
ace.
Owing
o
hei
e y
s able
c ys al
s uc u e,
gems
a e
nea ly
insensi i e
o
beam
e -
ec s
(no
al e a ion).
Cha ging
o
hese
usually
non-conduc i e
a ge s
is
a oided
when
using
an
ex e nal
beam
se up.
4.
EXPERIMENTAL
SETUP
The
expe imen al
se up
and
i s
successi e
imp o emen s
ha e
been
ho oughly
des-
c ibed
[4].
Only
he
s iking
ea u es
will
be
ecalled
he e.
The
analy ical
sys em
is
based
on
an
ex emal
beam
line
o
he
AGLAE
accele a-
o
acili y
( igu e
1).
The
usual
3-MeV
p o on
beam
is
ocused
down
o
30
pm
size
using
magne ic
lenses
(3
MeV
is
p o ed
o
be
an
op imum
ene gy
o
analysing
geo
logical
samples).
This
beam
is
b ough
on
he
sample
by
passing
h ough
a
e y
hin
SÍ3N4
oil.
The
de ec ion
o
X- ays
is
achie ed
using
wo
de ec o s.
A
i s
one
is
dedi-
ca ed
o
ligh
elemen s,
which
a e
he
majo
cons i uen s
o
he
gems
( om
Na
o
Fe).
I
has
a
low
solid
angle,
and
a
minimal
il e ing
using
an
ul a
hin
window
combined
200
T.
Cmjj(íaho,
J.-C.
Dk.w.
J.-P.
Poikoi
>
G.
Qi'e é
Figu e
I.
View
o
he
ex e na!
beam
Une
o
he
AGLAE
accele a o -based
IBA
acili y.
P
I
wi h
a
helium
low.
The
second
ene
is
dedica ed
o
hea y
elcmen s
( om
Ca
o
U)
a
a
low
le el
con ení.
I
has
a
high
solid
angle
and
a
ll e
chosen
in
o de
o
emo e
ma ix
X- ays.
Gamma- ays
a e
collec ed
using
a
High
Pu i y
Ge manium
de ec o .
The
beam
is
moni o ed
using
a
signal
emi ed
by
he
exi
oil:
backsca e ed
p o ons
o
X- ay
line
o
Si,
acco ding
o
expe imen al
equi emen s.
5.
applica ion
o
gems ones
We
will
desc ibe
some
ecen
applica ions
o
he
PIXE
and
PIGE
echniques
o
an-
cien
gems
om
museums
pe oimed
wi h
he
AGLAE
se up
o
he
Cen e
de
Reche che
e
de
Res au a ion
des
musées
de
F ance.
I
should
be
emphasised
ha
all
gems ones
s udied
he e
a e
well
documen ed
and
ha e
aceable
his o y.
So
we
a e
con iden
ha
hese
gems
a e
he
o iginal
ones.
5.1.
Ruby:
Ish a 's
s a ue e
This
s a ue e
which
may
ep esen
Ish a ,
a
goddess
equi alen
o
Aph odi e,
is
a
pe ec
illus a ion
o
a
IBA
s udy
o
gems ones
( igu e
2).
The
sculp u e
is
a
naked
woman
ca ed
in
alabas e ,
he
eyes
and
na el
inlaid
wi h
ubies.
This
ema kable
piece,
which
joined
he
Lou e
collec ions
in
1866,
was
exca a ed
in
he
incini y
o
Babylon
in
Mesopo amia
[5].
Po
s ylis ic
and
ypological
easons
i
is
a ibu ed
o
he
Pa hian
pe iod
(2nd
cen u y
B.C.
o
he
la e
2nd
cen u y
A.D.).
We
we e
able
o
con i m
ha
he
cabochons
we e
indeed
na u al
ubies
and
no
colou ed
glass,
as
had
been
belie ed
e en
qui e
ecen ly,
as
he
wo
main
cons i uen s
o
ubies
we e
e ealed:
99%
alumina
(AhOd.
associa ed
wi h
less
han
1
%
ch omium,
he
elemen
esponsible
o
he
cha ac e is ic
ed
colou
o
uby.
Se e al
ace
elemen s
III
CoNGRluSO
N
a(
U)N
1
DI
ARGIH)MI
TRlA
201
Figu e
2.
Ish a
in
being
analysed
using
he
ex e na!
beam
sys e n
( e
cuade niUo
a
co!o .
pág.
^.
we e
also
measu ed,
including
i anium,
anadium,
i on,
coppe ,
gallium,
all
being
cha ac e is ic
o
na u al
s ones
( igu e
3).
The
simila
aspec
and
chemical
composi-
ion
o
he
h ee
inlays
sugges
he
use
o
a
single
ba ch
o
s ones
o
he
s a ue e.
In
o de
o
de e mine
he
geog aphical
o igin
o
his
s a ue e's
ubies,
we
unde -
ook
a
compa a i e
s udy
wi h
con empo a y
ubies
o
known
p o enance
[6].
A
o al
o
o e
500
analyses
was
ca ied
ou
on
ubies
om
he
main
exis ing
deposi s:
A ghanis an,
Myanma
(Bumia),
Cambodia,
India,
Kenya,
Madagasca .
S i
Lanka,Thai-
land
and
Vie nam.
The
ace
elemen
con en s
o
he
s ones
a e
qui e
di e en
de-
pending
on
hei
p o enance
and
a e
homogeneous
wi hin
a
gi en
deposi ,
a
ea u e
absolu ely
needed
o
a
p o enance
s udy
based
on
geochemis y.
Mul i a ia e
s a is-
1e5
10000
1000
100
high
ene gy
X- ay
de ec o
spec um
low
ene gy
X- ay
de ec o
spec um
TI,,
Vk
C K
Fe
10
15
X- ay
ene gy
(keV)
Figu e
3.
X- ay
spec a
o
maja
and
ace
eiemen s
eco ded
on
a
ed
eye
o
he
s a ue e.
202
T.
Caujc.a o.
J.-C.
D w.
J.
P.
Poi oi
>
G.
Qi'EKR^
ical
me hods
we e
used
( ac o
analysis,
hie a chical
classi ica ion
and
disc iminan
analysis),
inco po a ing
all
he
chemical
ace
elemen s
(Ti,
V,
C ,
Fe,
Ga).
All
hese
analyses
con e ge
and
show
ha
he
s a ue e's
ubíes
ha c
a
composi ion
e y
cióse
o
ha
o
ubíes
om
Bu ma
( igu e
4).
The
esul s
o
he
geochemícal
s udy
we e
con i med
by
classícal
gcmmological
obse a íons
conduc ed
concu en ly;
ín
pa icula ,
he
u ile
inclusions
obsc ed
in
he
eyes
and
he
na el
a e
consis en
wi h
a
Bu mese
o igin.
Resea ch
ca ied
ou
on
he
ubíes
o
he
Pa hian
s a ue e
om
he
Lou e
com-
bining
obse a ion
o
he
gems
and
hei
geochemícal
cha ac e ísa íon
by
he
PIXE
me hod
has
led
o
a
be e
ínsígh
ín o
hís
wo k
o
a
by
ídcn í yíng
í s
cons í uen
ma e ials.
In
addí íon,
í
has
p o íded
he
oppo uní y
o
es ablísh
a
da a
base
on
he
composí íons
o
he
main
uby
deposí s.
Fínally,
hanks
o
s a ís ícal
analysis,
a
p o e-
nance
o
he
s a ue e's
ubíes
could
be
p oposed:
Bu ma.
I
can
hus
be
concluded
ha
he
gems
om
he
Pa hian
s a ue e
a e
e ídence
o
ade
o
exchange
o e
se e al
housand
kilome es
be ween
Mesopo amía
and
Sou h-Eas
Asía
du íng
he
Pa hian
pe iod.
As
a
as
we
know,
hís
ís
he
ea líes
use
o
ubíes
íden í íed
lo
da e
ín
hís
egión.
Thís
i
gu e
o
Ish a
ís
ema kable
o
í
combines
ín luences
de í íng
om
h ee
ci ílísa íons:
Mesopo amía
( he
ímage
o
he
naked
woman
as
a
é ilí y
sym-
bol),
G eece
( he
Hellenís íc
ealísm
o
he
body),
and
ínally
Asía
( he
p esence
o
he
ubíes).
10000
S
s
Ó
1000
100
10
g oup
III
g oup
I
10
X
:
Ish a
A:
A ghanis an
B
;
Bu ma
C
;
Cambodia
K;
Kenya
M
;
Madagasca
S
:
S í
Lanka
T
:
Thaíiand
g oup
100
1000
10000
Fe
(ppm)
Figu e
4.
Plo
o
C
s
Fe
con ení
o
he
ubíes
o
he
s a ue e
and
e e ence
ubíes.
III
CoNíikl
SO
N
ac
lONM
DI
ARyi
loMMKlA
203
Figu e
5.
Royal
o i e
c own
being
analysed
wi h
he
e. e nal
beani
( e
cuade nillo
a
colo ,
pdg.
i)-
5.2.
Emií ald:
hi-:
Visigo hic
easu e
We
epo
he e
an
applíca íon
o
he
analysis
o
eme alds
o
he
Gua aza
easu e
( igu e
5).
Thís
amous
se
o
o i e
oyal
c owns,
made
o
gold
wi h
ínlaid
gem-
s ones,
da es
om
he
Visigo hic
pe iod
(7*^-8"'
cen u ies).
I
was
exca a ed
in
1858
nea
Toledo
and
is
now
splí
ín o
wo
main
pa s
kep
a
he
Na ional
A chaeological
museum
ín
Mad id,
Spain
and
he
Na ional
Middle-Ages
museum
in
Pa ís,
F ance
[7].
The
sou ces
o
eme alds
used
in
ancien
Egyp
and
he
Román
Empi e
a e
qui e
well
documen ed;
i
is
no
so
o
he
ea ly
Middle-Ages.
This
wo k
aimed
a
companng
an
cien
eme alds
o
hose
o
a ious
o igins
epo ed
in
ancien
li e a u e
(Egyp ,
Aus
ia,
A ghanis an,
Ou al),
on
he
basis
o
chemical
analysis
[8].
PIXE
and
PIGE
ech-
niques
pe mi ed
o
iden i y
gems ones
by
means
o
hei
composi ion
in
majo
elemen s
(Be,
Al,
Si)
and
o
de e mine
hei
ace
elemen
con en s
( igu e
6).
P o enance
de-
e mina ion
elies
on
he
compa ison
o
hese
con en s
o
hose
o
e e ence
eme alds
cons i u ing
a
da a
base
o
geochemical
composi ion.
The
mos
disc imina ing
elemen s
we e
Li,
Na,
V,
Rb
and
Zn.
The
measu ed
con en s
in
hese
ancien
eme alds
a e
only
compa ible
wi h
Egyp ian
(Jebel
Zaba a)
o
Aus ian
(Habach al)
deposi s
( igu e
7).
Since
i
pe mi ed
o
disca d
al é na e
assump ions
(e.g.
U al,
A ghanis an
o
Pakis án),
his
wo k
p o ided
a
new
insigh
in o
he
ade
ou es
o
gems ones
a
he
ime
o
he
G ea
In asions.
5.3.
Ga ne :
jewels
o
he
i s
Kings
o
F ange
Game s
belong
o
a
amily
o
gems
ha ing
a iable
composi ion.
The
mos
com-
mon
ype
is
he
py alspi e
amily
wi h
he
chemical
o mula
X*^3AP^*2(Si04)í,
X
be-
204
T.
CMJJdAKO,
J.-C.
D W.
J.-P.
Po/KOI
>
G.
QdERRÉ
Figu e
6.
Gamma- ay
spec um
o
an
eme ald.
Figu e
7.
Sun ay
plo
o
ace
elemen s
con ení
o
ancien
and
e e ence
eme alds.
10
10
10
10^1
10'
10'
iiAL-j
kJJ
SI
I
'
I
'
'
■
'
I
'
'
'
■—I
'
■—■—'
I
'
■
' '
I
PIGE
spec a
o
an
e oe ald
Bo
3662
koV
iil
Li
478
keV
F
197
keV
500
1000
1500
2000
2500
3000 3500
4000
GaoMa
ay
Ene gy
(keV)
S a islical
p ocessing
;
Sun ay
plo
o
ace
elemen s
I
/|
A ghanís an
Pakis án
^Gallo-Roman
Columbia
_
Zambia
("S
Egyp
J
Wlsigo h
Zimbabwe
ladagasca
No /ay
B azil
''Ja
/
Mg
o
Rb
Ca
Re
/
C
^
V
Vaiiaules
ing
ei he
Fe
(almandin
game ),
Mg
(py ope
game )
o
Mn
(spessa i e
game ),
o
a
combina ion
o
hem.
The
ques ion
o
he
na u e,
o igin,
cu ing
and
se ing
echniques
o
he
game s
used
in
Eu ope
du ing
he
Ea ly
Middle
Ages
is
highiy
deba ed.
A
í
s
a emp
o
apply
IBA
echniques
o
Ea ly
Middle
Ages
game s
has
been
pe -
o med
in
he
C2RMF
[9].
This
wo k
deal
wi h
he
iden i ica ion
o
game s
moun ed
on
Me o ingian
jewelle y
om
Lou es-en-Pa isis.
The
conclusión
was
ha
hese
a -
chaeological
game s
had
a
majo
composi ion
compa ible
wi h
game s
om
S i
Lanka
(almandine-py ope
ype).
We
a e
cu en ly
de eloping
a
new
esea ch
p og am
on
he
Me o ingian
game s.
The
aim
o
his
wo k
is
o
include
ace
elemen
and
nea -su ace
analysis
o
he
gems.
III
Conc; i_s()
Nac
iowi
di
A (,)1
i-.omi- Ia
205
Figu e
8.
Me o ingian
jewei
wi h
ga ne s
se
in
cloisonné
s yle
( e
cuade nillo
a
colo ,
pág.
i).
These
ga ne s
a e
se
on
he
cloisonné
jewels
( igu e
8)
om
he
oyal
easu e
o
Sain
Denis,
F ance,
comp ising
he
amous
jewels
o
Queen
A egonde
[10].
This
wo k
will
be
ex ended
wi h
he
analysis
o
game s
exca a ed
om
a ious
a chaeological
si es
in
Eu ope.
6.
CONCLUSION
IBA
echniques
and
speci ically
he
PIXE/PIGE
combina ion
in
ai
appea
as
a-
luable
ools
o
analysing
gems
moun ed
on
his o ical
jewels.
They
use ully
comple-
men
classical
gemmological
in es iga ions.
The
main
ad an ages
a e
1)
comple ely
non-des uc i e
analysis,
2)
b oad
ange
o
elemen s
de ec ed,
3)
0- 4m
size
spa ial
esolu ion
4)
ppm
le el
sensi i i y
and
5)
good
accu acy.
They
we e
applied
o
de e
mine
he
na u e
and
p o enance
o
ancien
mbies.
Fo
Middle
Ages
eme alds
and
ga
ne s,
he
esul s
al eady
ob ained
a e
p omising.
Mo e
e e ence
da a
a e
needed
and
he
combina ion
wi h
o he
analy ical
echniques
has
o
be
ied.
7.
REFERENCES
[1]
Ande son,
B.W.
and
Jobbins,
E.A.,
1990,
Gem
es ing,
Bu e wo hs,
London.
[2]
Bi d,
J.R.
and
Williams,
J.S.,
1989,
Ion
beams
o
ma e ials,
Academic
P ess,
London.

206
T.
Caumíamo.
J.-C.
Dka.s.
J
-I*.
I^oihoi
>
G.
Que é
[3]
Campbell,
J.L.
and
Malmq is ,
K.G.,
1995,
Pa icle-induced
X- ay
spccí ome y
(PIXE),
John
Wiley
&
Sons,
Lxjndon.
[4]
Calliga o,
T.,
D an,
J.-C.,
Hamon,
H.,
Moigna d,
B.
and
Salomón,
J..
1998,
An
exlemal
milli-beam
o
a chaeome ic
applica ions
on
ihe
AGLAE
IBA
acili y
o
he
Lou e
mu-
seum.
Nucí.
Ins .
and
Me h.
B
136/138,
339-343.
[5]
Tallen,
F.,
1999,
Ac es
du
colloque:
Comaline
c
pie cs
p ccieu.scs
-
1995,
Musée
du
Lou e,
Pa is.
[6]
Calliga o,
T.,
Mossmann,
A.,
Poi o ,
J.-P.
and
Que é,
G.,
1998,
P o enance
s udy
o
u
bíes
om
a
Pa hian
s a ue e
by
PIXE
analysis.
Nucí,
hus .
and
Me h.
B
136/138,
846-
850.
[7]
Pe ea,
A.
and
Balmaseda,
LJ.,
1999,
Las
es
his o ias
del
eso o
de
Gua aza
y
el
p oyec o
Au,
Re is a
de
a queología
221,
37-45.
[8]
Calliga o,
T.,
D an,
J.-C.,
Poi o ,
J.-P.,
Que é,
G.,
Salomen,
J.
and
Zwaan,
J.C.,
2000,
PDCE/PIGE
cha ac e isa ion
o
eme alds
using
an
ex emal
mic obeam.
Nucí.
In.s .
and
Me h.
B161/163,
769-774.
[9]
Fa ges,
F.,
1998,
Mine alogy
o
he
Lou es
Me o ingian
game
cloisonné
jewel y:
O i-
gins
o
he
gems
o
he
i s
kings
o
F ance,
Am.
Mine al
83,
323-330.
[10]
Fleu y,
M.
and
F ance-Lano d,
A.,
1998,
Les
é.so s
mé o ingiens
de
la
basilique
de
Sain -Denis,
Gé a d
Klopp
eds,
Woippy,
F ance.
APROXIMACIÓN
AL
ESTUDIO
DE
PROCEDENCIA
Y
TECNOLOGÍA
DE
FABRICACIÓN
DE
LAS
CERÁMICAS
CAMPANIFORMES
DEL
YACIMIENTO
DE
LA
EDAD
DEL
COBRE
DE
LOS
MILLARES
Jose a
Capel''',
Fenia ido
Molina'",
T inidad
Náje a*",
José
Lina es'-'
V
F ancisco
Hue as'"
Resumen
En
es e
abajo
se
lle a
a
cabo
el
es udio
analí ico
median e
Espec ome ía
de
Masas,
Di acción
de
Rayos-X
y
Mic oscopio
Es e eoscópico
de
un
conjun o
de
asijas
ce ámicas
de
es ilo
campani o me
p oceden es
del
yacimien o
de
la
Edad
del
Cob e
de
Los
Milla es.
El
análisis
químico
se
ha
cen ado
en
el
es udio
de
los
elemen os
denominados
ie as
a as
que
cons i uyen
un
indicado
exce
len e
del
o igen
de
los
ma e iales.
El
es udio
mine alógico
así
como
la
obse a
ción
óp ica
han
apo ado
in o mación
sob e
p ocesos
ecnológicos
de
manu ac-
u ación.
Palab as
cla e:
ce ámica.
Edad
del
Cob e,
p ocedencia,
manu ac u ación.
1.
INTRODUCCIÓN
Los
abajos
sob e
la
mo ilización
de
elemen os
químicos
du an e
los
p ocesos
de
hid ólisis
y
al e ación
de
ocas
ocupa
un
impo an e
campo
en
la
in es igación
desa
ollada
en
el
ámbi o
de
las
ciencias
del
suelo
y
ciencias
de
la
Tie a
en
gene al.
La
mayo
o
meno
mo ilidad
de
es os
elemen os,
en
el
caso
de
los
mine ales,
es á
in
l
uenciada
po
la
es uc u a
del
c is al.
Es
igualmen e
ob io
que
exis en
nume osos
ac o es
isicoquímicos
ales
como
pH,
empe a u a
y
p esión
de
la
solución,
ex u a
y
pe meabilidad
de
los
sólidos,
á ea
supe icial,
e c.,
que
in luyen
de
igual
o ma.
No
obs an e
un
mismo
elemen o
puede
compo a se,
dependiendo
de
su
posición
c is alo-
Dp o.
de
P ehis o ia
y
A queología.
Facul ad
de
Le as.
Campus
Uni e si a io
de
Ca uja,
18071
G anada
Dp o.
de
Ciencias
de
la
Tie a
y
Geoquímica
Ambien al.
Es ación
Expe imen al
del
Zaidín,
CSIC.
P o eso
AIba eda,
s/n,
18008
G anada.