SYNTHESIZED TARANAKITE 
Laboratory Formation of Taranakite — Liu, Sherman, and Swindale 
501 
u 
VO o 
'-I o 
VO VO XT' C\ 'sr 
xr (N t-h oo vq 
1T\ tr Vf Cfl fO 
ocv rri ovrowovroovfva 
ia m ovoor'i^t^vovoA 
rn A cfi cf 1 MN(N(NMN(N(N 
-» -> <- 
-> -> -» -» -> -> 
r-~ o 
GV rCi VO O 
\q 
c<v oq 
i/> 
(n t-h vo xr 
CO> 
id vd 
VT\ 
"d 'd cd cc-, 
t-i r- 
oo r^ 
d <n 
it- 
o 
cC> 
GV 
m 
VO 
cn 
o 
CA 
j 
t-H 
r- 
rA 
oo 
i r\ 
CN 
rH 
vq 
\r\ 
H 
q 
cv 
oq 
d 
vd 
\r\ 
'd 
fT> 
cn 
rA 
cn 
d> 
<N 
(N 
(N 
-> <r <- <r <- <r 
cOi 
m 
GV 
cTi 
r- 
0 
m 
'sT 
t-H 
\r\ 
CN 
H 
\T\ 
-q 
Gv 
oq 
oq 
d 
v r\ 
'd 
co 
rO 
rn 
CN 
<N 
<N 
GV 
<TV 
t-H 
r- 1 
\ '- h 
rOi 
o 
CC> 
<N 
o I 
m 
t-H 
t-h 
oq 
oq 
'sr 
oq 
i r\ 
COl 
t-j 
oq 
\r\ 
q 
g\ 
oq 
oq 
\r\ 
cO> 
d 
rd 
\r\ 
\T\ 
I'd 
cd 
crv 
cO 
<d 
rO 
CN 
<N 
CN 
■» -> 
-> 
rA CO fT, M M M M 
* Change in intensity. 
** Visual estimates of peak intensities. 
Note: Prominent peaks of dehydrated taranakite are underlined. 
