A POSSIBLE NEW MINERAL SPECIES, “FERROGATEHOUSEITE”
(Fe,Mg) (PO ) (OH) FROM CONT
5
4 2
4
U PEGMATITE, ROMÂNIA
1
2
2
1
1
2
N. CALIN , A-M. FRANSOLET , M. BAIJOT , S. MARINCEA , D-G. DUMITRAS , F. HATERT ,
1
1
M.A. ANASON , A.M. IANCU
Phosphates belonging to the triphylite - lithiophilite series
generally occur as nests in the spodumene and feldspar
masses. They from granular masses of greenish gray
color that turns locally into dark or black, due to the
weathering. Both optical and scanning electron microscope
studies show that triphylite abundantly contains inclusions
of wolfeite and of a gatehouseite - like phase, the later
occurring
on
the (001) perfect cleavage plane of triphylite.
X-ray powder data were obtained on a representative sample
and indexed according to ICDD file 01-070-0516, belonging
to gatehouseite. These data allow the refinement of the
unit-cell parameters, in the space group P2 2 2 (19)
1 1 1.
The
refined parameters are:
a = 9.103(3)
Å
, b = 18.019(6)
Å
and
c = 5.685(9)
Å
.
The a and b parameters are slightly larger
while c is slightly smaller
compared to those of gatehouseite,
given by Pring and Birch
(1993), i.e., a = 9.097(2)
Å
,
b = 18.002(3)
Å
and c = 5.693(2)
Å
.
Table 1. Unit-cell parameters for triphylite
Table 2. Representative electron-microprobe
analysis of triphylite
Table 3. Unit-cell parameters for ferrisicklerite
Table 4. Representative electron-microprobe
analysis of ferrisicklerite
Table 5. Unit-cell parameter for heterosite
Table 6. Representative electron-microprobe
analysis of heterosite
Tab
le
7.
Unit-cell parameters for gatehouseite
Table 9. Representative electron-microprobe analysis of ferrogatehouseite
Table 8. Chemical structural formulas of
ferrogatehouseite
Photomicrograph of ferrisicklerite in
association with feldspars. Plane polarized
light. Crossed nicols.
To achive this the goals of this work, a series of analytical
methods were used as follows:(1)optical study with Leica and
Jenapol-U polarizing microscopes; (2) X-ray powder diffraction
using a Bruker D8 Advance diffractometer (Ni-filtred Cu Ka
radiation,
= 1.54060Å, accelerating voltage 40 Kv, beam
current 40 mA); (3) electron-microprobe analyses, using
CAMECA SX 50 device in wavelength-dispersive mode.
ferrisicklerite
fe
rri
sic
kle
rit
e
albite
albite
albite
B
ack-scattered image
of ferrogatehouseite in triphylite.
“ferrogatehouseite”
triphylite
Photomicrograph of ferrogatehouseite
( 30 µm in length, 20µm in width) on cleavage .
triphylite
“ferrogatehouseite”
This research was supported by the Executive Agency for Higer Education, Research,
Development and inovation Funding (UEFISCDI), Ministry of National Education in Romania,
through the projects IDEI PN-II-ID-PCE-2013-3-0023 and ERA-MIN PT 339, 25.03.2014.
720
1. Department INI, Geological Institute of Romania, 1 Caransebes Str. , RO-012271, Bucharest, Romania,
[email protected]
2. Université de Liège, Laboratoire de Minéralogie, B18, Sart Tilman, 4000, Belgique.
Geological map of Romania
0
50
100Km
1 =
schists and muscovite-bearing gneisses
;
2 =
kyanite schists
; 3 =
staurolit schists
;
4 =
garnet-bearing schists
;
5 =
a
m
ph
ibolite
s
,
gneisses
and schist
s
;
6 = pegmatite
s quartzo-feldspathic
;
7 =
albite and spodumene-bearing pegmatites
;
8 = graphic
pegmatites.
phosphate
muscovite
quartz
feldspar
muscovite
phosphate
albite
phosphate
quartz
albite
muscovite
feldspar
muscovite
phosphate
quartz
Hand specimens of pegmatites from Contu
ferrisicklerite
fe
rri
sic
kle
rit
e
albite
albite
albite
Photomicrograph of triphylite sample with inclusion of
ferrogatehouseite. Plane polarized light. Crossed nicols.
ferrogatehouseite
triphylite
triphylite
ferrogatehouseite
Photomicrograph showing the association ferrisicklerite - heterosite - quartz.
Heterosite has an obvious pleochroism in tints of mauve and yellow, whereas ferrisicklerite has more
evident pleochroism in tents.
ferrisicklerite
heterosite
ferrisicklerite
heterosite
quartz
Gatehouseite, Mn
5
(PO
4
)
2
(OH)
4
,
is a rare Mn-bearing
phosphate, since this mineral is only reported in a
sedimentary iron ore deposit in Australia (Pring and
Birch, 1993). Like in many Mn-bearing phosphates
structures, Fe may replace Mn and a complete solid
solution often exists between the Mn- and Fe-bearing
end-members. One more time, our work leads us to
consider the existence of an hypothetic new species,
“ferrogatehouseite”, which would be the iron
dominant equivalent species of gatehouseite.
During the research on the Li-bearing pegmatites from
Contu (Cibin Mountains, South Carpathians, Romania) a
rich phosphate association, including heterosite –
purpurite, lithiophilite – triphylite, sicklerite –
ferrisicklerite, fluorapatite, vivianite, monazite, wolfeite
was identified. Other associated minerals include
spodumene, quartz, muscovite, K-feldspar, plagioclase,
beryl, cassiterite, columbite group minerals, lepidolite,
rutile, scarce schorl, uraninite, topaz, spessartine,
sillimanite, titanite. Pegmatites from Contu are hosted
by micaschists and gneisses related to the Sebes - Lotru
Series.
Electron-microprobe analyses of this mineral, identified as iron-rich
gatehouseite (sample 14/c4), yielded (in wt.% oxides): P
2
O
5
= 26.76, FeO
= 38.97, MnO = 27.15, MgO = 0.41, CaO = 0.05, H
2
O (calculated for charge
balance) = 6.79, total =100.13. The crystal-chemical formula which
results from this composition is: (Fe
2.877
Mn
2.030
Mg
0.053
Ca
0.004
)(PO
4
)
2
(OH)
4
,
which is related to the one of gatehouseite but with Fe > Mn. Chemical
analyses on two other samples yielded similar empiric formulae, i.e.,
(Fe
3.083
Mn
1.855
Mg
0.021
Ca
0.009
)(PO
4
)
2
(OH)
4
and (Fe
2.735
Mn
1.717
Mg
0.042
Ca
0.003
)
(PO
4
)
2
(OH)
4
(samples 13/c4 and 17/c4, respectively).
Further investigations by FTIR and micro-Raman are needed to acquire
more details about the H
2
O content of this potential ferrous homologue
of gatehouseite. The petrographic texture indicates that
“ferrogatehouseite” as well as wolfeite, partially replaced triphylite
along its cleavage plane during the hydrothermal stage.
Acknowledgements
A
NDERSSON
, A. S., K
ALSKA
, B., H
ÄGGSTRÖM
, L. and T
HOMAS
, J. O. (2000): Lithium extraction/insertion in LiFePO
4:
An X – ray diffraction and Mössbauer spectroscopy study. Solid State Ionics, 130, 41 – 52.
L
OSEY
, A., R
AKOVAN
, J. and H
UGHES
, J. M., F
RANCIS
, C. A., D
YAR
, M. D. (2004): Structural variation in the
lithiophilite – triphylite series and other olivine group structures. The Canadian Mineralogist, Vol. 42, pp.
1105 – 1115.
P
RING
, A.,
AND
B
IRCH
, W. D. (1993): Gatehouseite, a new manganese hydroxy phosphate from Iron Monarch,
South Australia. Mineral. Mag., 57, 309 – 313.
S
ABAU
, G., I
LINCA
, G., M
ARINCEA
, S., R
OBU
, L. (1990): Evaluation of the lithium potential of the Romanian
pegmatites and of the possibilities of use. I. South Carpathians (Cibin Mountains). Unpubl. Report,
Geological Institute of Romania, 65 pp.
References:
IGR
1906
Sample
a(Å)
b(Å)
c(Å)
N 113
5.841(9) 9.765(5)
4.765(4)
N 107 b
5.829(2) 9.749(4)
4.773(6)
29 B
5.837(4) 9.757(8)
4.768(9)
N 109
5.835(3) 9.756(6)
4.770(3)
N 114 A
5.824(3) 9.748(1)
4.777(2)
N 128
5.833(6) 9.718(7)
4.772(3)
Ci_1d
5.810(5) 9.758(3)
4.783(6)
Ce. 1C
5.810(4) 9.742(4)
4.773(2)
Ce. 2D
5.844(5) 9.778(6)
4.773(2)
N 129
5.857(1) 9.811(9)
4.776(2)
N 122
5.824(9) 9.775(2)
4.773(6)
N 120
5.821(3) 9.763(1)
4.782(8)
Mean
5.830(5)
9.76(5)
4.774(4)
Sample
a(Å)
b(Å)
c(Å)
23C1
4,719(1)
10,368(6)
6,035(5)
65CI
4,718(4)
10,366(3)
6,031(2)
9E
4,712(4)
10,379(6)
6,039(10)
29B
4,718(1)
10,378(3)
6,033(4)
Ci 1D
4,712(8)
10,375(7)
6,047(6)
Ci 1D1
4,713(7)
10,380(6)
6,038(7)
Mean
4,715(4)
10,374(5)
6,037(6)
Sabau et.al. (1990)
4,698(4)
10,365(5)
6,034(9)
Anderson et al. (2000) 4.6908(2) 10.3290(3) 6.0065(2)
Losey et al. (2004)
4,7138(6) 10,3826(1) 6,0499(5)
Sample
a(Å)
b(Å)
c(Å)
N 103
5,945(6) 10,076(8) 4,793(1)
Ce 59
5,941(7) 10,061(5) 4,791(8)
23C1
5,943(9) 10,056(8) 4,796(2)
N 112
5,945(4) 10,061(9) 4,797(7)
Mean
5,944(7) 10,064(8) 4,794(5)
ICDD 00-033-0802
5,946
10,063
4,793
Triphylite
9/c2
10/c2
11/c2
19/c4
20/c4
39/c12 40/c12
%
%
%
%
%
%
%
P
2O
545.94
45.98
45.79
45.93
46.51
46.26
46.18
FeO
30.73
30.9
30.46
30.23
30.8
29.64
29.45
MnO
15.04
15.14
15.23
15.21
15.1
15.65
16
MgO
0.3
0.28
0.29
0.24
0.25
0.25
0.25
CaO
0.01
0.04
0.02
0.06
0.04
0.07
0.04
Li
2O
9.66
9.66
9.62
9.64
9.64
9.70
9.70
Total 1
92.02
92.34
91.79
91.67
92.7
91.87
91.92
Total 2
101.68 102.00 101.41 101.31 102.34 101.57 101.62
Triphylite
94/c9
159/c1 160/c1 161/c1 166/c1 167/c1 171/c1
%
%
%
%
%
%
%
P
2O
546.14
46.11
46.11
46.07
45.31
46.59
46.12
FeO
30.88
29.29
29.29
29.32
26.38
26.75
26.45
MnO
15.31
16.82
16.82
16.6
19.47
19.37
19.26
MgO
0.29
0.14
0.14
0.14
0.06
0.07
0.06
CaO
0.04
0.04
0.04
0.03
0.05
0.03
0.03
Li
2O
9.69
9.68
9.69
9.68
9.51
9.79
9.69
Total 1
92.66
92.4
92.4
92.16
91.27
92.81
91.92
Total 2
102.35 102.08 102.09 101.84 100.78 102.60 101.61
Triphylite
9/c2
10/c2
11/c2
19/c4
20/c4
39/c12 40/c12
1PO
41PO
41PO
41PO
41PO
41PO
41PO
4P
1
1
1
1
1
1
1
Fe
2+0.660
0.663
0.657
0.65
0.654
0.633
0.63
Mn
0.327
0.329
0.332
0.331
0.324
0.338
0.346
Mg
0.011
0.010
0.011
0.009
0.009
0.009
0.009
Ca
0
0.001
0
0.001
0.001
0.001
0.001
Li
0.999
0.998
0.998
0.997
0.998
0.995
0.997
Triphylite
94/c9
159/c1 160/c1 161/c1 166/c1 167/c1 171/c1
1PO
41PO
41PO
41PO
41PO
41PO
41PO
4P
1
1
1
1
1
1
1
Fe
2+0.660
0.627
0.627
0.628
0.575
0.567
0.566
Mn
0.332
0.364
0.364
0.360
0.429
0.416
0.419
Mg
0.011
0.005
0.005
0.005
0.002
0.002
0.002
Ca
0.001
0.001
0.001
0
0.001
0
0
Li
0.998
0.998
0.998
0.998
0.997
0.998
0.998
Ferrisicklerite 42/c1 43/c1 47/c1 56/c3 57/c3 59/c3 60/c3 71/c6
% % % % % % % %
P2O5 44,67 43,95 43,28 45,14 44,54 43,98 42,87 41,79 FeO 30,00 31,03 30,17 30,69 30,94 30,9 31,68 32,11 MnO 18,83 18,78 19,61 18,36 18,49 18,73 19,36 19,72 MgO 0,10 0,11 0,1 0,1 0,11 0,11 0,11 0,11 CaO 0,52 0,37 0,66 0,28 0,29 0,36 0,46 0,53 Li2O 9,13 9,06 8,76 9,35 9,22 9,07 8,78 8,52 Total 1 94,12 94,24 93,82 94,57 94,37 94,08 94,48 94,26
total 2 103,25 103,30 102,58 103,92 103,59 103,15 103,26 102,78
Ferrisicklerite 72/c6 79/c7 81/c7 84/c10 125/c9 158/c1 174/c6 175/c6
% % % % % % % %
P2O5 45,13 43,3 44,14 44,31 42,93 45,21 43,66 42,56 FeO 30,65 31,13 30,39 30,77 30,15 29,76 29,42 30,12 MnO 18,58 18,96 18,71 18,65 19,77 17,74 19,71 20,04 MgO 0,09 0,12 0,12 0,1 0,09 0,15 0,08 0,06 CaO 0,25 0,74 0,44 0,38 0,27 0,79 0,42 0,53 Li2O 9,37 8,72 9,20 9,13 8,89 9,10 8,97 8,68 Total 1 94,7 94,25 93,8 94,21 93,21 93,65 93,29 93,31
total 2 104,07 102,97 103,00 103,34 102,10 102,75 102,26 101,99
Ferrisicklerite 42/c1 43/c1 47/c1 56/c3 57/c3 59/c3 60/c3 71/c6 PO4 PO4 PO4 PO4 PO4 PO4 PO4 PO4
P 1 1 1 1 1 1 1 1
Fe 0,663 0,697 0,688 0,671 0,687 0,693 0,729 0,758 Mn 0,421 0,427 0,453 0,406 0,415 0,426 0,451 0,472 Mg 0,003 0,004 0,003 0,003 0,004 0,004 0,004 0,004 Ca 0,014 0,010 0,019 0,007 0,008 0,010 0,013 0,015 Li 0,970 0,978 0,961 0,984 0,983 0,979 0,973 0,968
Ferrisicklerite 72/c6 79/c7 81/c7 84/c10 125/c9 158/c1 174/c6 175/c6 PO4 PO4 PO4 PO4 PO4 PO4 PO4 PO4
P 1 1 1 1 1 1 1 1
Fe 0,670 0,710 0,679 0,685 0,693 0,650 0,665 0,699 Mn 0,411 0,438 0,424 0,421 0,460 0,392 0,451 0,471 Mg 0,003 0,004 0,004 0,003 0,003 0,005 0,003 0,002 Ca 0,006 0,021 0,004 0,010 0,007 0,021 0,012 0,015 Li 0,986 0,957 0,990 0,978 0,984 0,956 0,975 0,968
Heterosite 44/c1 45/c1 48/c1 58/c3 61/c3 62/c3 63/c3
% % % % % % %
P2O5 46,65 45,42 46,75 46,85 46,87 46,79 47,19 Fe2O3 33,09 33,16 31,95 32,70 32,76 33,47 33,17 Mn2O3 20,33 20,58 19,99 19,90 20,018 19,38 20,10 MgO 0,11 0,08 0,12 0,11 0,07 0,10 0,07 CaO 0,23 0,33 0,38 0,28 0,23 0,35 0,18 Total 100,41 99,578 99,19 99,85 99,95 100,09 100,72
Heterosite 64/c3 65/c3 70/c6 74/c7 75/c7 76/c7 77/c7
% % % % % % %
P2O5 47 46,14 46,25 47,08 47,42 46,21 47,69 Fe2O3 33,18 33,16 32,69 32,24 32,72 32,26 33,15 Mn2O3 19,70 20,60 19,52 19,49 19,50 19,18 19,57 MgO 0,08 0,06 0,1 0,09 0,09 0,08 0,09 CaO 0,17 0,27 0,53 0,59 0,42 0,52 0,16 Total 100,14 100,24 99,10 99,49 100,16 98,25 100,66
Heterosite 78/c7 80/c7 83/c10 149/c1 153/c1
% % % % %
P2O5 47,17 47,22 46,27 44,95 45,63 Fe2O3 32,58 33,36 34,61 31,49 32,35 Mn2O3 19,38 19,85 19,72 19,55 18,90 MgO 0,09 0,09 0,09 0,14 0,12 CaO 0,29 0,14 0,14 2,01 0,58 Total 99,51 100,66 100,84 98,14 97,58
Heterosite 44/c1 45/c1 48/c1 58/c3 61/c3 62/c3 63/c3 1PO4 1PO4 1PO4 1PO4 1PO4 1PO4 1PO4
P 1 1 1 1 1 1 1
Fe3+ 0,630 0,649 0,607 0,620 0,595 0,635 0,624 Mn3+ 0,391 0,407 0,384 0,381 0,368 0,372 0,383 Mg 0,004 0,003 0,004 0,004 0,002 0,003 0,002 Ca 0,006 0,009 0,010 0,007 0,005 0,009 0,004
Heterosite 64/c3 65/c3 70/c6 74/c7 75/c7 76/c7 77/c7 1PO4 1PO4 1PO4 1PO4 1PO4 1PO4 1PO4
P 1 1 1 1 1 1 1
Fe3+ 0,627 0,638 0,628 0,608 0,613 0,620 0,617 Mn3+ 0,377 0,401 0,379 0,372 0,369 0,373 0,368 Mg 0,003 0,002 0,003 0,003 0,003 0,003 0,003 Ca 0,004 0,007 0,014 0,015 0,011 0,014 0,004
Heterosite 78/c7 80/c7 83/c10 149/c1 153/c1 1PO4 1PO4 1PO4 1PO4 1PO4
P 1 1 1 1 1
Fe3+ 0,614 0,627 0,665 0,622 0,630