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METALS AUSTRALIA LTD Capital/Financing Update 2014

Jun 30, 2014

65344_rns_2014-06-30_b5e55159-6a31-4207-9562-89570e943a89.pdf

Capital/Financing Update

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A S X A N N O U N C E M E N T 1 J u l y 2 0 1 4 M ILE 72 U R ANI U M D RILLING R ESU L TS

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Drilling at Mile 72 in May 2014

HI G HLIGH T S

  • Drilling completed at Mile 72; confirmation of primary Rössing-style uranium mineralisation hosted by alaskitic pegmatites in southeast of licence.

  • 53 RC drillholes completed for 2,688m in a campaign of widely-spaced drilling to assess large areas of the licence.

  • Assays received for 7 holes show 7 Significant Intercepts[1] , including an intercept of 2m@690ppm U3[O] 8[in MS] RC0037 and 2m@226ppm U3O8 in MSRC0047.

  • Confirmation of previously identified multiple anomalous uraniummineralised zones showing strike continuity of up to 2km in drilling and trenching.

  • Primary mineralised zones confirmed under sand cover, including mineralised calcrete channels (secondary mineralisation).

  • Radon Cup anomalism in northwest of licence shown by drilling to be near surface and localised in nature, underlain by areas of barren schist.

  • Further exploration will focus on identifying the extent of trap sites in southeastern uranium mineralised zones.

1 Si g nificant Intercept being 1 m>50ppm U 3O8

Met a ls Australi a Ltd (ABN 38 0 08 982 474) www.metals a ustralia.com. a 1[st] Flo o r, 8 Parliament P lace, West Perth, WA 6005 ▪ PO B ox 1618, West Perth, WA 6872 ▪ t : +61 8 9481 78 3 3 ▪ f: +61 9481 7 8 35 ▪ e: mls@me t alsaustralia.com. a

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DRILLING PROGRAM CO M PLETED

Met a ls is pleas e d to announce the co m pletion of a second pha s e of reverse circulation (RC) drilling at its Mile 72 Project north o f Swakopmund in Nami b ia (Figure 1). Initial res u lts from th e first progr a m in Nove m ber 2013 c onfirmed the existence o f alaskite-h o sted urani u m minerali s ation at Mil e 72. The pr o grams carried out by t h e Compan y are the first ever to t e st this are a for urani u m minerali s ation at sig n ificant dept h below surf a ce.

The November 2 013 program focused o n a series o f priority out c ropping ta r gets testin g the Da m aran schis t -granitepeg m atite/alask i te sequenc e where it c o rrelated wit h surface geo c hemical, radiometric, a n d aeromag n etic anom a lies. The pri m ary objecti v e of the in i tial progra m was met, with the ide n tification of multiple stri k e-persisten t pegmatitic horizons con t aining ano m alous uranium minerali s ation, withi n 85m of surf a ce at Mile 7 2.

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Figure 1 – L o cation of the M ile 72 uraniu m project, Namib i a.

Thi s most rece n t program was design e d to targe t blind mineralised ura n ium horizo n s that are hid d en under s hallow bla n keting san d s. These s andy plain s host a n u mber of R adon Cup ano m alies in th e undrilled n o rtheast of t h e Mile 72 li c ence area w hich require d testing.

AS S AYS RECEI V ED

Lab o ratory ass a ys have b e en receive d from 7 ho l es of the 53 hole pro g ram. Inters e ctions are sho w n in Tabl e 1, and ex p lained in f u rther detail in Appendix 1 of this release. T h e drillhole loc a tions are s h own in Fi g ure 2. A f u ll list of th e hole loca t ions in the program is shown in Appendix 2.

The most signifi c ant assay i n tercepts from the progr a m included;

2m at 690ppm U3[O] 8[in MSR] C0037 from 3m including 1m at 737ppm U3O82m at 226ppm U3[O] 8[in MSR] C0046 from 3m including 1m at 312ppm U3O8

Als o of significa n ce was an intersection of 1m at 136ppm U3O8 from 30m i n MSRC0054, in which a p e gmatite is h osted withi n a medium grained gra n ite. These n ew results a re consist e nt with the res u lts of the first drill pro g ram, furth e r validating the presen c e of continuous prima r y uranium min e ralisation a t Mile 72.

A c a lcrete pala e ochannel h o sts an inte r section of 5m at 62ppm U3O8 from surface in MSRC055 including 1m at 106 ppm U3O8 , (se c ondary La n ger Heinrich style of m ineralisation) .This is con s idered pro m ising for the accumu l ation of surface mineralisation so u rced from hard rock sou r ces already identified at the Project.

Table 1 include s all sample s taken duri n g the progr a m that wer e sent for la b oratory analysis. Each of t h e 53 drillh o les in the p rogram wa s assayed i n the field on a metre- b y-metre ba s is using a RS125 spectro m eter and a h andheld X R F machine. Significant a nomalism i n either spec t rometer or XR F samples w ere sent fo r assay. This significan t ly reduced a ssay costs to the Co m pany. The spe c trometer a n d XRF res u lts have an excellent c o rrelation to mineralisati o n and uranium grade, and are considered a valid sample selec t ion guide.

2

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Table 1: U3O8 values d e termined by X-Ray Fluoresce n ce Spectromet r y.

Hole
ID
C
ollar coordin
ates
C
ollar coordin
ates
Inter
cept
Inter
cept
Inter
cept
U3O8
**ppm **
C
omments
H
ole direction
E
asting
N
orthing
D
ip
Azimuth
(mag)
From To Interval
MSRC
0037
4
09610
7
581851
-6
0
133 3
4
4
5
1
1
737
643
2m
at 690ppm
MSRC
0041
4
09521
7
581673
-6
0
133 13 14 1 200 1m
at 200ppm
MSRC
0046
4
09555
7
581685
-6
0
133 3
4
4
5
1
1
312
141
2m
at 227ppm
MSRC
0047
4
09504
7
581720
-6
0
133 7 8 1 94 1m
at 94ppm
MSRC
0054
4
10153
7
582939
-6
0
133 30 31 1 136 1m
at 136ppm
MSRC
0055
4
10043
7
583019
-6
0
133 0
1
2
3
4
1
2
3
4
5
1
1
1
1
1
106
35
29
88
53
5m
at 63ppm
MSRC
0056
4
09991
7
583056
-6
0
133 17 18 1 218 1m
at218ppm
  • The November 2 013 results included significant ass a y intercepts including:  3m at 1,192ppm U3O8 in MSRC0042 from 13m, including 1m at 3,407ppm U3O8 .  6m at 158ppm U3O8 in MSRC0031 from 9m , including 3m at 265ppm U3[O] 8[from ] 12m and including 1m at 572ppm U3O8

  • 3m a t 106ppm U 3[O] 8[in MSR] [C] 0004 from 11m, including 1m at 14 1 ppm U3O8  3m a t 102 U3O8 in MSRC00 4 3 from 45 m , including 1 m at 147p p m U3O8

  • 3m a t 96ppm U 3 O8 in MSR C 0009 from 32m , includi n g 1m at 15 9 U3O8

  • 3m a t 88ppm U 3 O8 in MSR C 0001 from 9 6m, includi n g 1m at 10 6 ppm U3O8

  • 7m a t 82ppm U 3 O8 in MSR C 0026 from 2m , includin g 2m at 144 p pm U3O8

3

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Fig u re 2 – Loca t ion of deep e r RC drillin g at Mile 72. D rilling has intercepted a laskite-host e d uranium mi n eralisation in several dr i llholes in th e Southeast terrane, defining a serie s of uranium trends up to 2km lon g . The drilling in the Nor t hwest terra n e defined a large area underlain by s chist

RA D ON CUP A NOMALIE S TESTED

Thi s most rece n t drill progr a m was desi g ned to test a number of targets lo c ated under s and cover as w ell as othe r s identified by radon cup anomalis m . The first 1 8 holes of t he program tested the ext e nsions of pr e vious uranium trends i d entified in t h e Novembe r 2013 drillin g program, s uch as the res u lts at MSR C 0031, whic h identified m ineralisation under sand cover. Th e presence o f multiple, nar r ow uraniu m -enriched h orizons wi t hin a sequence of s chist-granit e -pegmatite/ a laskite is con f irmed by t h e drilling around MSRC 0031, a n d includes the results from MSR C 0037 and

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MS R C0046. Th e se uranium-mineralise d zones repr e sent an on g oing oppor t unity for th e southeast of t h e project to host signific a nt primary a nd/or seco n dary uraniu m mineralis a tion.

Of the program , 35 holes t a rgeted highly anomalo u s radon cu p highs loca t ed in a radiometrically bar r en region i n the cent r e and nor t hwest of t h e licence. Localised a nomalous radon cup ano m alism was seen to b e potentiall y representative of buri e d primary o r seconda r y uranium min e ralisation. T he drilling f o und this no t to be the c a se, with the central and northwest a reas being und e rlain by pelitic schist wi t h sporadic p egmatites ( b arren) and underlain b y deeper granite bodies (als o barren). The schist-gr a nite-pegm a tite/alaskite geological t e rrane of th e southeast is in stark con t rast to the s chist dominated northw e st, separat e d by a maj o r geologic a l structure ( S ee Figure 2).

The drill progr a m was ter m inated early when it became evident that a l l of the n o rthwestern sub s urface targ e ts were bar r en of urani u m mineralis a tion. Explo r ation will re - focus on th e southeast terr a ne where p revious dril l ing has be e n successf u l at identif y ing both n e ar surface a nd buried zon e s over sign i ficant distances.

In a ddition, the identificatio n of mineral i sed calcret e palaeochannels in th e southeastern terrrane ope n s up furthe r opportuniti e s for preser v ed second a ry uranium m ineralisati o n at Mile 72.

FU R THER EXP L ORATION

Thi s most rece n t drilling, w hile sterilisi n g a signifi c ant portion of the proj e ct area, allows future exp l oration to f o cus on the most prospective area s and possi b le trap zon e s in the s o utheastern terr a ne. As well as primary Rossing-st y le uranium m ineralisation, this prog r am has co n firmed the pre s ence of cal c rete-hosted uranium at M ile 72.

For further information please contact: Vin c ent Algar or Matthew P a inter +61 8 948 1 7833 Or consult our website: w ww.metals a

w ww.metals a ustralia.co m .au

Competent Person Declaration

The i n formation in thi s release relating to the geology a nd exploration r e sults of the projects owned by MMetals Australia L td is based on infor m ation compiled b y Dr Matthew P a inter, who is a c o nsultant to Met a ls Australia. Dr P ainter is a membber of The Austr a lian Institute of Geos c ientists, a Reco g nised Professio n al Organisation b y the Australasian Joint Ore Re s erves Committeee, and has sufficient experience relev a nt to the style of mineralisation a n d types of depo s its under consid e ration and to the activity which is bbeing undertake n to qualify as a Com p etent Person as d efined in the 2012 Edition of the J o int Ore Reserve s Committee (JO R C) Australasian CCode for Reportin g of Exploration Results. Dr Painter co n sents to the inclu s ion in this report of the matters based on his inform a tion in the form aand context in which it appears. Forward-Looking Statements

This d ocument may include forward-lo o king statements. Forward-looking statements inclu d e, but are not limmited to, statem e nts concerning Metal s Australia Ltd’s planned exploration programme a n d other statem e nts that are not h istorical facts. WWhen used in this document, the word s such as "coul d ," "plan," "estim a te," "expect," "i n tend," "may”, " p otential," "shoul d ," and similar eexpressions are forward-looking state m ents. Although M etals Australia L td believes that i ts expectations r e flected in these forward-looking sstatements are reasonable, such state m ents involve ris k s and uncertaint i es and no assur a nce can be giv e n that actual results will be consiistent with these forward-looking state m ents.

5

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JO R C TABLE 1

Section 1 – Sa m ple Techniques and Da t a

Crit
eria
Explana
tion
Samp
techn
ling
iques
Exploratio
appropriat
samplesa
analysis.
Spectrome
for more p
All drill sa
riffle splitte
are thenp
by X-Ray
Bureau Ve
n results are ba
e quality assura
re collecteda
Each 1m split
ter. Anomalou
recise analysis.
mples submitte
r to obtain a s
repared by mix
FluorescenceS
ritas Laboratory
sed on industr
nce quality co
s 1m compos
sample is an
s samples are
d to the labora
ub-fraction whic
ing with a spec
pectrometry (X
in Swakopmu
y best practice
ntrol (QAQC)m
ite samples th
alysed with a
submitted toB
tory are dried t
h is then pulve
ial wax and pr
RF). Samplep
nd, Namibia.
s, including sam
easures. Reve
rough a cyclon
handheld XRF
ureau Veritas
hen crushed.A
rised with a vib
essing to form
reparation and
pling, assaym
rse circulation
e which arer
analyser and
Laboratory inS
sample is the
rating pulveris
a solid buttona
analysis areu
ethods, and
(RC) drilling
iffle split for
an RS125
wakopmund
n split with a
er. Samples
nd analysed
ndertaken at
Drilli
ng techniques
RC drilling
coordinate
is completed
s are quoted in
by a 5 ¼ inch
WGS84 datum
diameter hole
unless otherwi
drilled with af
se stated.
ace samplingh
ammer. All
Drill
reco
sample
very
The qualit
logging of
field duplic
The quality
with certifi
that results
y of RC drilling
various criteria
ates to measur
of analyticalr
ed standards,d
are representa
samples is op
designed to re
e sample precis
esults is monito
uplicates andb
tive and within
timised by the
cord sample siz
ion.
red by the use
lanks and statis
acceptable ran
use of riffle an
e, recovery an
of internal labo
tical analysiso
ges of accuracy
d/or cone split
d contamination
ratory procedu
n a monthly ba
and precision
ters and the
, and use of
res together
sis to ensure
.
Logg
ing
All logging
intervalsa
standard
database
validation
Detailed in
mineralisa
is completeda
nd stored inp
Metals/Datashe
and validated.
and interpretatio
formation on lit
tion are collecte
ccording to ind
lastic chip tra
d logging tem
Once validate
n.
hology, sample
d in a series of
ustry best prac
ys for future r
plate. The res
d, the data is
quality, structu
detailed self-va
tice. RC drillc
eference. Log
ulting data is
exported tom
re, geotechnica
lidating logging
hips are wets
ging is comple
uploaded to
odelling softwa
l information,a
templates.
ieved on 1m
ted using a
a Datashed
re for visual
lteration and
Sub-
techn
samp
sampling
iques and
le preparation
RC sample
splitting ta
For all sam
is conside
Field dupl
control re
duplicates
Sample siz
s are riffle split
kes place.
ple types, the
red suitable as
icates are take
ports are unde
.
es are appropr
on 1m interva
nature, quality
per industry bes
n every 20 sam
rtaken routine
iate to the grain
ls when dry.W
and appropriat
t practice.
ples to ensure
ly to monitor
size of the ma
hen wet, sampl
eness of the sa
the samples
the performan
terial being sam
es are dried ou
mple preparati
are representa
ce of field sta
pled.
t before riffle
on technique
tive. Quality
ndards and
Qual
data
tests
ity of assay
and laboratory
The samp
crushing th
3kg sub-fra
Samplesa
analysedb
Field Stan
and blank
batch.
les have been
e whole sampl
ction which ha
re then prepar
y X-Ray Fluore
dards and Blan
s at random in
sorted, dried,c
e. The samples
s then been pu
ed by mixingw
scence Spectro
ks are inserted
tervals, but sev
rushed and pu
have been spl
lverised in a vib
ith a special wa
metry (XRF) to
every 10 sam
eral are insert
lverised. Prima
it with a riffle sp
rating pulverise
x and pressing
determine Ua
ples. Laborato
ed per batch re
ry preparation
litter, if require
r.
to form a soli
nd Th contents
ry inserts its ow
gardless of th
has been by
d, to obtain a
d button and
.
n standards
e size of the

6

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Verif
samp
assa
ication of
ling and
ying
All signific
release to
No adjustm
original for
All data is
then carrie
ant intercepts
the market.
ents are mad
mat.
validated using
d out by senior
are revieweda
e to the raw a
the QAQCr rep
staff members
nd confirmed
ssay data. Da
orter validation
.
by at least thre
ta is imported
tool with Datas
e senior pers
directly to Data
hed. Visual va
onnel before
shed in raw
lidations are
Loca
point
tion of data
s
Holes are
licenced s
set out usinga
urveyor on com
handheld 12 c
pletion of the h
hannel GPS.A
ole.
ccurate collarl
ocations are pi
cked up by a
Data
distr
spacing and
ibution
Data spac
type ands
data spaci
ing and distribu
tyle under cons
ng and density
tion used to de
ideration. Wh
is decided and
termine geolog
ere a mineral re
reported by the
ical continuityi
source is to be
competent per
s dependent o
estimated, the
son.
n the deposit
appropriate
Orien
in rel
geolo
tation of data
ation to
gical structur
e
Orientation
and interp
If structure
general str
If the relat
is conside
considered
Drilling is
known inte
of sampling is
retation of thed
and geometry
ike of stratigrap
ionship betwee
red to havei
material.
at an angle to
rpretation of th
as unbiased a
eposit geometr
is not well und
hy and/or regio
n the drilling or
ntroduced as
surface and i
e strike of previ
s possible base
y.
erstood, sampl
nal structure.
ientation and th
ampling bias,
s drilled to ma
ously intersecte
d on the domin
ing is orientated
e orientationo
this would be
ximise perpend
d mineralisatio
ating mineralis
to be perpend
f key mineralise
assessed and
icular intersec
n.
ed structures
icular to the
d structures
reported if
tion with the
Samp
le security
All sample
field collec
s remain in the
tion to laborato
custody of co
ry drop-off.
mpany geologi
sts, and are fu
lly supervised
from point of
Audi
ts and reviews
None yetu
ndertaken fort
his dataset.

Section 2 – Reporting of Ex p loration Re s ults

Crit
eria
Explana
tion
Mine
and l
statu
ral, tenement
and tenure
s
The Comp
3308 is cu
licence re
pending st
the area.
The Comp
any metal
impedimen
current en
any controls an
rrently pending
ports and expe
atus. There are
any maintains
production.T
ts. The licence
vironmental cle
Exclusive Pro
renewal by th
nditure are al
no known imp
a 100% interes
here are no kn
is located in
arance certifica
specting Licenc
e Namibian Mi
l in good stan
ediments with r
t in EPL3308,a
own native title
the Dorab Par
te to operate in
e (EPL) at Mile
nistry of Minera
ding at the tim
espect to renew
nd a 3% gove
interests, histo
k recreationala
the Park.
72, namely EP
ls and Energy,
e of reporting
ing the licence
rnment royalty
rical sites ore
rea. The Com
L3308. EPL
however the
, despite the
to operate in
is in place on
nvironmental
pany holds a
Explo
other
ration done b
parties
y
Prior to th
recorded
deposit, lo
Appraisal
becausev
has had to
e exploration
in the area. His
cated on adjace
of previous wo
ery limited data
re-collect thed
completed by
torical explora
nt ground and
rk has therefo
are available
ata.
Metals on EPL
tion in the are
not within EPL3
re been limited
in either digital
3308, no reco
a focused ont
308.
to high level
or hardcopy fo
rd of moderne
he nearby Mile
reviews of hist
rmat. In most
xploration is
72 Uranium
orical reports
cased Metals
Geol
ogy
The geolo
mineralisa
the schists
gy consists of
tion is alaskite-
, and supergen
a sequence
hosted uranium
e uranium mine
of Damaran s
(Rössing-style
ralisation.
chists, granites
uranium), with
and alaskites
potential for u
. The target
ranium within
Drill
infor
hole
mation
All relevan
t drillhole inform
ation is supplie
d in appendix
1 of the announ
cement.
Data
meth
aggregation
ods
All explora
of high gra
tion results are
de material rec
reported by a
eive less weigh
length weighte
ting than longe
d average. Thi
r lengths of low
s ensures that
grade material
short lengths
.

7

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No high gr
ade cut-offs are
applied.
Relat
betw
mine
width
lengt
ionship
een
ralisation
s and interce
hs
pt
Mineralisa
betweena
these have
All holesd
intersectio
be close to
tion seen atM
magnetic bea
been exposed
rilled to dated
n as practicable
true thickness
ile 72 is curre
ring of 020° an
in numerous t
ip at 50° and
to the above
.
ntly interpreted
d 045°. Dips o
renches across
60° and drilled
orientation. Int
to be largely
f the various un
the project
at orientations
ercept lengths,
strata bound
its are close to
that result ina
therefore, are
and oriented
vertical and
s high angle
interpreted to
Diag
rams
A series o
f relevant diagra
ms are include
d in the body o
f the announce
ment.
Balan
ced reporting
Informatio
laboratory
XRF arer
and XRFd
n relating to ge
assay resultsa
ecorded andu
ata are not inc
ophysical andg
re excluded.S
sed to selects
luded in the rele
eochemical tes
amples taken i
amples for labo
ase.
twork is include
n the field with
ratory assay.
d in the annou
handheld Spec
The handheld
ncement. No
trometer and
Spectrometer
Furth
er work
Plans forf
urther work are
outlined in the
body of the ann
ouncement

8

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Appendix 2 – Mile 72 RC Drilling

Hole No Easting Northing F
inal Depth
(m)
Dip (
**O) **
A
(
zimuth
Omag)
MSRC0036 409529 7581909 45 -60 133
MSRC0037 409610 7581851 50 -60 133
MSRC0038 409492 7581689 50 -60 133
MSRC0039 409411 7581747 50 -60 133
MSRC0040 409330 7581806 50 -60 133
MSRC0041 409521 7581673 21 -60 133
MSRC0046 409555 7581685 15 -60 133
MSRC0047 409504 7581720 15 -60 133
MSRC0048 409595 7581821 15 -60 133
MSRC0049 409634 7581833 15 -60 133
MSRC0050 409566 7581877 15 -60 133
MSRC0051 410036 7582777 50 -60 133
MSRC0052 409876 7582895 15 -60 133
MSRC0053 409849 7582915 50 -60 133
MSRC0054 410153 7582939 50 -60 133
MSRC0055 410043 7583019 50 -60 133
MSRC0056 409991 7583056 45 -60 133
MSRC0057 409830 7583174 50 -60 133
MSRC0058 410109 7583218 50 -60 133
MSRC0059 409947 7583336 50 -60 133
MSRC0060 410065 7583498 50 -60 133
MSRC0061 409903 7583615 50 -60 132.83
MSRC0062 409741 7583733 50 -60 132.83
MSRC0063 410020 7583777 50 -60 132.83
MSRC0064 409859 7583895 50 -60 132.83
MSRC0065 409697 7584012 50 -60 132.83
MSRC0066 409535 7584130 50 -60 132.83
MSRC0067 409411 7583976 50 -60 132.83
MSRC0068 409192 7584260 100 -60 120.83
MSRC0069 409030 7584096 100 -60 120.83
MSRC0070 408991 7584318 50 -60 120.83
MSRC0071 410778 7583968 50 -60 132.83
MSRC0072 410616 7584086 50 -60 132.83
MSRC0073 410895 7584130 50 -60 132.83
MSRC0074 410733 7584248 50 -60 132.83

9

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MSRC0075 410292 7584321 50 -60 132.83
MSRC0076 410130 7584439 50 -60 132.83
MSRC0077 409969 7584556 50 -60 132.83
MSRC0078 409760 7584677 100 -60 3
00.83
MSRC0079 409692 7584489 100 -60 3
00.83
MSRC0080 409851 7584394 87 -60 3
12.83
MSRC0081 409624 7584301 100 -60 3
00.83
MSRC0082 409673 7584383 50 -60 120.83
MSRC0083 409814 7584174 50 -60 3
12.83
MSRC0084 408590 7584677 50 -60 120.83
MSRC0085 408684 7584643 50 -60 3
00.83
MSRC0086 408778 7584609 50 -60 3
00.83
MSRC0087 408872 7584574 50 -60 3
00.83
MSRC0088 409060 7584506 50 -60 3
00.83
MSRC0089 408496 7584711 50 -60 3
00.83
MSRC0090 408608 7586480 50 -60 3
00.83
MSRC0091 408796 7586411 50 -60 3
00.83
MSRC0092 408727 7586223 50 -60 3
00.83

10