ASX ANNOUNCEMENT



9 June 2015

EXTENSIVE ZONE OF SEDIMENT HOSTED HIGH-GRADE COPPER OUTLINED AT McARTHUR RIVER PROJECT, NT

Sampling outlines large continuous stratiform zone with assays up to 47.8% Cu, 68g/t Ag, 2220 Bi

HIGHLIGHTS

Extensive copper-silver-bismuth anomalous area outlined by mapping and sampling

A minimum of 600 x 400m area delineated with average of >10% Cu in rock samples plus high Ag and Bi

Maximum assay results of 47.8% Cu, 68 g/t Ag and 2220 ppm Bi

25% of samples analysed returned values of greater than 10% Cu and 10 g/t Ag, with seven samples grading over 40% Cu and 40 g/t Ag

Area remains open down-dip to the east and to the south and represents an outstanding drill target

These results confirm the prospectivity of the McArthur River Project, which has been included in the spin-off of TNG's non-core base metal assets via Todd River Resources

TNG continues to focus on its flagship Mount Peake Vanadium Project, where the Feasi bility Study is in its final stages and progressing according to plan

Australian strategic metals company TNG Limited (ASX: TNG) is pleased to announce that it has delineated an extensive zone of high-grade surface copper mineralisation from mapping and rock chip sampling undertaken at its 100%-owned McArthur River Project in the Northern Territory (Figure 1).
The work was carried out while TNG continues its primary focus on the completion of the Feasibility Study on its flagship Mount Peake Vanadium Project, which is continuing to progress on schedule and according to plan. Updates on this work, including the TIVAN® pilot testwork, are expected with the completion of each phase and after assessment and review of results.
A program of field mapping, soil sampling and rock chip sampling was conducted at the McArthur River Project to follow up the high grade 48% copper analysis located during earlier reconnaissance sampling (see ASX Announcement - 16 February 2015). This work was conducted as part of the ongoing background assessment of the assets, which have been included in the recently approved demerger of Todd River Resources.
The field work has confirmed the very high prospectivity of the McArthur River Project, with these results indicating a newly discovered zone of sedimentary-hosted stratiform copper-silver mineralisation which represents a significant exploration target and potential new mineralisation style for this area.
Sediment-hosted stratiform copper deposits are an important and economically attractive, world-class mineral deposit style. Examples of these are demonstrated by the super-giants of the Kupfershiefer in north-central Europe and the Copper Belt of Central Africa.
The McArthur River Project is located 60km south-west of the world-class McArthur River Zinc Mine, operated by Glencore, and within the Batten Fault Zone, which hosts several other base metal resources including the recently outlined Teena deposit (Rox/Teck).

ASX CODE: TNG

REGISTERED OFFICE

T +61 8 9327 0900

W www.tngltd.com.au

ABN 12 000 817 023

Level 1, 282 Rokeby Road

Subiaco, Western Australia 6008

F +61 8 9327 0901

E corporate@tngltd.com.au



The tenements are highly prospective and are being explored for both McArthur River-style zinc mineralization as well as stratiform and/or structurally-controlled copper mineralization within the Wollogorang Formation sequence, which is exposed over 17km of strike within the tenement package.

Figure 1. McArthur River Project location plan. McArthur River Sampling Program

Detailed geological mapping at 1:2500 scale was completed by TNG geologists year over an area of approximately
3 square kilometres (as shown in Figure 1). Systematic Portable XRF (pXRF) and -80# soil sampling and rock chip sampling was also undertaken with details outlined in Appendix 2.
48 rock samples were collected with all samples analysed for a 33-element suite. Results of greater than 1%
copper are shown in Table 1 and results of all significant elements and sample coordinates are listed in Appendix
1. Significant copper results >40% Cu are shown in Table 2. Laboratory analysis of the rock samples returned a total of seven samples with >40% Cu, 12 samples greater than 10% Cu and 19 samples above 1% Cu. These results enhance and confirm the extent of the potential copper horizon.
2

Table 1. Significant rock chip sample results (>1% Cu.

Table 2. Multi-element anomalism for the two sampling areas.

Copper

Results

Silver

Gold

Bismuth

Molybdenum

>40%

>10%

>1%

>10 g/t

>0.05 g/t

>250ppm

>=30ppm

Original Site

No. Samples (23)

4

7

11

8

2

8

7

Maximum Value

47.80%

68

0.09

1220

50

Northern Breakaway

No. Samples (18)

3

5

8

5

3

4

0

Maximum Value

45.80%

48

0.10

2220


All anomalous samples came from a shale band in the lowermost Wollogorang Formation (Figure 2). This shale (Pto1) is approximately ten metres thick and bound below by the Settlement Creek Dolerite and above by a dolomite subunit within the Wollogorang Formation (Pto2).
The dolomite exposures are prominent, forming low (2-10m) breakaways with the shale poorly exposed on the scree slope below the breakaway (Plate 1). Stratigraphy in the area displays variable but shallow dips (0-20 degrees), mostly dipping towards the east.
Copper anomalism was found in two main areas (see Figure 2). A total of 23 samples were taken in the vicinity of the original sample at approximately 593,373mE 8,109,079mN. These samples were spread over an area of 150m by 120m and returned four (five including the original sample) assays of greater than 40% Cu. Seven samples returned values of greater than 10% Cu, while the eight samples showing more than 1% Cu were spread over an area of 30m by 50 metres.
An exposure of the shale along a NNE facing breakaway some 300-500m to the north returned three rock samples with >40% Cu results. The anomalous samples were all taken from the same stratigraphic shale unit and were spread over 250m of strike exposure along the breakaway.
The copper is present as malachite (green hydrated copper carbonate) and chalcocite (black supergene copper sulphide) in all samples with more than 1% Cu (see Plate 2). Significant tenorite (black high-grade copper oxide) and/or native copper may also be present (as there is insufficient sulphur present to generate the high copper grades as sulphide).

3

TNG LlMITED

593200 593300 593400 593500 593600

TNGLIMITED

.o ...

_,

, '

McArthur Rlver Project

Copper Anomalous Zone

Rock Chip Sampllng,Copper Resutts

$..

o....

Sample No. eu o1o

MC15536 45.1

MC15537 45.8

MC1SS38 44.6

MC15540 11.0

,

l

...

o o o...... o

8 8

N

o o...

;;; EL 27711

El30085

8

l

/. t

'... ... ...

' ...

Sample No. Cu%

MC15001 48.3 8

o; t MC15501 47.8 t c;;

o...

---

MC15502 45.6 ... - o

)---"

t'

l l

MC15505 47.7

MC15506 44.3

MC15507 35.9

MC15508 37.2

MC15509 15.3

+ t

.,.---/-- .......

2fl ... ... ...

...

...

;;;

593200

N

Metres

o 25 50 75 100

593300 593400

Wollogorang Formatton CJPT03 Ovold Beds CJPT02 Lower Dolomite

CJ PTOl Sl'lale

593SOO

Sample LocatJon

t l%Cu

+ > 1% Cu

t > tO% eu

593600

Olp/Strlke / 2ff

Stratigraphic

Contact ., '

"

Projtetlon:e.g GOA94 MGA Zone 53 SettJement Creek Dolerite

1.3,000 CJ

Fault ,

Figure 2.

Portion of the mapped area showing the locations of the rock chip samples in Table 1.

4



Plate1. Photograph showing the some of the rock chip sampling (MC15535-15538) in the basal shale unit exposed below the dolomite breakaway. Note the poorly exposed outcropping and sub - cropping shale, the coarse dolomite scree, and the kapok trees growing on the dolomite.

Plate 2. Detailed photograph showing the some of the shale material sampled (MC15541). Note the rubbly nature of the outcrop and the green (malachite) and black (chalcocite) fragments of copper mineralisation.

5

There is a distinct multi-element association which is displayed by these samples in Cu-Bi-Ag-Au-Mo. The multi- element anomalism for the two areas is outlined in Table 2.

Silver correlates well with copper and is highly anomalous with ten samples returning over 40 g/t Ag and 13 above 10g/t, with a maximum value of 68 g/t. Gold was analysed only in 18 samples and, of those, five results exceeded 0.05 g/t, with a maximum value of 0.10 g/t Au. All anomalous gold results came from samples with

>40% copper.

Bismuth is also highly anomalous, with results to 2220 ppm Bi, while the background is Molybdenum (Mo) is elevated in the copper anomalous samples with a maximum value of 50ppm in sample MC15502 which has 45.6% Cu (Table 1).

TNG has been active in this area since 2011, although most work to date has been directed towards the zinc potential higher in the stratigraphy (see ASX Announcements - 16 September 2013, 20 August 2014, and 14
October 2014). Late in 2014, NTGS-sponsored diamond drilling was completed on two combined geochemical and
geophysical zinc targets.
Sampling of this drill core provided numerous sulphides in an organic and sulphide rich portion of the Ovoid Beds subunit of the Wollogorang Formation (Pto3) and returned results of over 0.2% for both zinc and copper (see ASX Announcement - 18 December 2014). The zinc was associated with pyrite and sphalerite fine sulphides in the most organic rich portion of the stratigraphy. Very high (to 7% TOC) organic content is seen in this interval of core.
The extreme high copper grades seen (10-48% Cu) are a result of supergene enrichment in the weathered profile and likely persist to around 100m below surface. The likely original chalcopyrite hypogene copper has been upgraded to supergene sulphide species (chalcocite, bornite, native copper) which were then replaced by carbonate/oxide species (malachite, tenorite) resulting in the extreme grades seen.
These results indicate a new sedimentary hosted stratiform layer of copper mineralisation has been outlined over an area in excess of 600m by 400m. It is several metres thick and persistent under very thin dolomite cover covering an area of at least 0.5 square kilometres. The horizon dips to the east and would be present over a couple of square kilometres at less than 100m depth below surface and reappears to the south of the area mapped. Soil sampling (see ASX Announcement - 16 September 2013) also highlights the copper potential in the south.
It would be unusual if the mineralised zone was not continuous as is normal with sedimentary hosted stratiform layers but further work is required to establish this.
The McArthur River Project is part of a portfolio of non-core base metal assets held by TNG in the Northern Territory which have been included in the demerger of Todd River Resources. This is consistent with TNG's focus on advancing its world-class Mount Peake Vanadium-Titanium-Iron Project to development.
The further evaluation of this prospect will be determined by Todd River Resources once the demerger has been completed, and future work programs would be likely to include trenching and geophysics to determine the full extent of copper anomalism before undertaking drill testing.
TNG's Managing Director, Mr Paul Burton, said the copper results from McArthur River were encouraging and demonstrated the prospectivity of the project.
"This has the early indications of very large and potentially significant copper exploration target," Mr Burton said. "In many respects this vindicates our decision to include this asset with our other significant Northern Territory mineral exploration assets with the demerger into Todd River Resources - which will be able to pursue an appropriate exploration strategy to unlock their full value for shareholders.
6

"TNG shareholders will continue to have significant exposure to these assets through the proposed in-specie distribution of shares once the demerger has taken place. A timetable for this is anticipated soon and I expect to be able to provide an update on this following our Feasibility Study results from Mount Peake," he said.
Paul E Burton
Managing Director
9 June 2015
Inquiries:
Paul E Burton Nicholas Read
Managing Director + 61 (0) 8 9327 0900 Read Corporate + 61 (0) 8 9388 1474

About TNG

TNG is building a world-scale strategic metals business based on its flagship 100%-owned Mount Peake Vanadium-Titanium-Iron Project in the Northern Territory. Located 235km north of Alice Springs, Mount Peake will be a 20-year plus project producing a suite of high-quality, high-purity strategic metals products for global markets including vanadium pentoxide, iron oxide and titanium dioxide. The project, which will be a top-10 global producer, has received Major Project Facilitation status from the NT Government.
The Mount Peake Feasibility Study is well advanced and due for completion by mid-2015, paving the way for
project financing and development to proceed. An integral part of TNG's emerging strategic metals business its
100% ownership of the unique and patented TIVAN® hydrometallurgical process, which offers significantly lower capital and operating costs, lowers risk and successfully extracts two other valuable metals from the resource in addition to vanadium - titanium dioxide and high-purity iron oxide.
Vanadium is a highly strategic metal which is used as an alloy in steel. It is also in strong demand for use in energy storage, with vanadium redox batteries used to store electricity generated by solar and wind power, and lithium- vanadium ion batteries used to power hybrid cars.

Competent Person Statement

The information in this report that relates to Exploration Results and Exploration Targets is based on, and fairly represents, information and supporting documentation compiled by Exploration Manager Mr Kim Grey B.Sc. and M. Econ. Geol. Mr Grey is a member of the Australian Institute of Geoscientists, and a full time employee of TNG Limited. Mr Grey has sufficient experience relevant to the style of mineralisation and type of deposit under consideration and to the activity which he is undertaking to qualify as a Competent Person as defined in the 2012
Edition of the 'Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves'. Mr Grey consents to the inclusion in the report of the matters based on his information in the form and context in which it appear.

Forward-Looking Statements

This announcement has been prepared by TNG Ltd. This announcement is in summary form and does not purport to be all inclusive or complete. Recipients should conduct their own investigations and perform their own analysis in order to satisfy themselves as to the accuracy and completeness of the information, statements and opinions contained.
This is for information purposes only. Neither this nor the information contained in it constitutes an offer, invitation, solicitation or recommendation in relation to the purchase or sale of TNG Ltd shares in any jurisdiction.
7

This does not constitute investment advice and has been prepared without taking into account the recipient's investment objectives, financial circumstances or particular needs and the opinions and recommendations in this presentation are not intended to represent recommendations of particular investments to particular persons. Recipients should seek professional advice when deciding if an investment is appropriate. All securities transactions involve risks, which include (among others) the risk of adverse or unanticipated market, financial or political developmen ts.

To the fullest extent permitted by law, TNG Ltd, its officers, employees, agents and advisers do not make any representation or warranty, express or implied, as to the currency, accuracy, reliability or completeness of any information, statements, opinions, estimates, forecasts or other representations contained in this announcement. No responsibility for any errors or omissions from this arising out of negligence or otherwise is accepted.

This may include forward looking statements. Forward looking statements are only predictions and are subject to risks, uncertainties and assumptions which are outside the control of TNG Ltd. Actual values, results or events may be materially different to those expressed or implied.

8

SAMPLE LOCATION LAB Au-AA24 ME-ICP61a ME-ICP61a ME-ICP61a Cu-OG62 ME-XRF15c Consolidated ME-ICP61a ME-ICP61a

NUMBER

EASTING

NORTHING

BATCH

Au

Ag

Al

As

Ba

Bi

Ca

Cu

Cu

Cu

Cu

Fe

Mg

Mn

Mo

P

Pb

S

Sb

U

Zn

MGAZ53

MGAZ53

ppm

ppm

%

ppm

ppm

ppm

%

ppm

%

%

%

%

%

ppm

ppm

ppm

ppm

%

ppm

ppm

ppm

MC15001

593373

8109079

AS15012084

0.031

68

0.2

1860

1050

0.12

>100000

>40

48.3

48.3

5.72

0.15

210

30

180

40

1.76

100

MC15001D

593373

8109079

AS15012084

47.9

47.9

MC15501

593375

8109090

AD15061369

0.089

41

0.39

5270

1120

0.43

>100000

>40

47.8

47.8

3.63

0.24

210

30

220

40

0.21

110

MC15502

593372

8109088

AD15061369

N.D.

57

0.49

5710

1220

0.26

>100000

>40

45.6

45.6

5.07

0.43

350

50

200

40

0.92

50

140

MC15503

593372

8109090

AD15061369

0.006

4

2.88

11800

160

7.39

50100

5.01

2.71

3.71

4760

10

670

30

0.27

20

MC15504

593370

8109085

AD15061369

N.D.

1

3.02

10200

30

8.02

15400

1.54

1.8

4.27

5510

450

0.26

MC15505

593373

8109086

AD15061369

0.074

57

0.3

7360

1290

0.29

>100000

>40

47.7

47.7

5.59

0.29

380

30

210

40

0.91

150

MC15506

593376

8109081

AD15061369

0.037

46

0.38

6200

1050

1.19

>100000

>40

44.3

44.3

7.15

0.48

500

30

170

40

0.83

160

MC15507

593375

8109080

AD15061369

N.D.

46

1.09

11250

1000

1.49

>100000

35.9

35.9

5.4

1.3

960

30

280

50

1.17

130

MC15508

593380

8109093

AD15061369

0.039

45

0.8

6030

970

2.38

>100000

37.2

37.2

3.96

0.76

1850

30

260

20

0.47

110

MC15509

593376

8109106

AD15061369

N.D.

18

1.26

6270

420

7.85

>100000

15.25

15.25

2.85

3.98

5230

10

410

0.18

50

MC15510

593372

8109098

AD15061369

0.009

9

2.03

7990

180

8.3

60200

6.02

2.76

3.36

5970

10

840

20

0.23

50

MC15511

593498

8109393

AD15061369

N.D.

39

2

10050

240

3

>100000

17.95

17.95

5.53

2.5

2260

20

360

50

0.7

70

30

MC15512

593508

8109397

AD15061369

4.15

3340

11.95

2080

0.208

1.65

4.49

4080

530

30

MC15513

593520

8109385

AD15061369

N.D.

3.57

5700

6.21

800

0.080

3.44

3.18

3970

10

610

20

0.13

20

MC15514

593494

8109397

AD15061369

N.D.

2.32

11750

8.67

430

0.043

1.79

5.01

4540

250

0.28

MC15515

593468

8109409

AD15061369

N.D.

3.64

9120

2.44

510

0.051

1.42

2.03

1850

350

0.21

20

MC15516

593751

8109821

AD15061369

N.D.

1.59

10600

18.55

150

0.015

1.84

4.82

4140

350

0.25

MC15517

593670

8109760

AD15061369

N.D.

2.43

2220

11.1

170

0.017

2.26

4.71

4620

630

20

20

MC15518

593637

8109838

AD15061369

N.D.

2.03

11400

15.6

120

0.012

2.11

3.64

4340

420

0.27

MC15519

593623

8109691

AD15061369

N.D.

6.94

2540

1.49

190

0.019

5.95

2.64

910

1430

20

0.08

70

MC15520

593693

8109654

AD15061369

N.D.

7.09

2520

0.9

120

0.012

5.24

2.62

950

1400

80

MC15521

593345

8109070

AD15061369

2.91

10750

11.9

100

0.010

2.02

2.2

3530

560

20

0.24

20

MC15522

593340

8109081

AD15061369

N.D.

1.67

7530

22.4

50

0.005

1.63

3.45

1780

340

0.17

MC15523

593325

8109100

AD15061369

N.D.

2.82

4490

18.6

50

0.005

1.37

3.24

1480

390

0.09

MC15524

593311

8109129

AD15061369

N.D.

7.84

2180

0.33

10

0.001

4.83

2.2

520

610

20

30

MC15525

STD

AD15061369

N.D.

3

6.16

60

1070

3.97

3570

0.357

5.43

1.64

830

60

980

2010

0.39

1120

MC15526

593354

8109078

AD15061369

3

3.46

9020

120

4.02

41500

4.15

2.36

2.59

3680

640

0.21

20

MC15527

593358

8109055

AD15061369

N.D.

3.7

8850

4.69

190

0.019

3.31

3.59

6550

530

0.18

20

MC15528

593374

8109023

AD15061369

N.D.

2.82

9510

4.88

90

0.009

1.94

2.4

4470

380

0.22

MC15529

593411

8109026

AD15061369

0.76

4150

33.3

270

0.027

0.48

0.41

2180

440

0.1

20

MC15530

593415

8109044

AD15061369

1

0.89

590

31.9

30

0.003

0.46

0.43

2080

420

20

MC15531

593409

8109072

AD15061369

N.D.

1.6

2710

15.3

690

0.069

1.47

2.73

5590

600

20

0.08

30

MC15532

593412

8109107

AD15061369

N.D.

1.82

3160

11.55

140

0.014

1.04

1.84

2340

520

20

0.07

70

MC15533

593375

8109112

AD15061369

N.D.

2.6

10850

5.17

120

0.012

2.16

2.55

6430

1320

0.23

20

MC15534

593369

8109143

AD15061369

N.D.

2.45

3440

16.4

350

0.035

1.11

3.26

2910

380

20

0.07

20

MC15535

593256

8109516

AD15061369

N.D.

2.55

4700

26.3

30

0.003

1.65

1.35

560

370

20

0.1

20

MC15536

593268

8109518

AD15061369

0.076

48

0.89

14150

2220

0.28

>100000

>40

45.1

45.1

3.77

0.38

100

150

30

1.53

130

MC15537

593273

8109512

AD15061369

0.068

48

0.75

16100

2140

0.96

>100000

>40

45.8

45.8

4.02

0.4

120

130

30

1.61

110

MC15538

593273

8109508

AD15061369

0.099

47

0.73

14950

2220

2.01

>100000

>40

44.6

44.6

3.6

0.45

130

170

30

1.57

120

MC15539

593286

8109531

AD15061369

N.D.

2

2.68

7610

150

19.4

25100

2.51

1.95

1.9

970

360

0.28

MC15540

593276

8109535

AD15061369

N.D.

12

1.49

6380

840

22

>100000

10.95

10.95

1.62

1.2

930

180

20

0.61

60

MC15541

593281

8109544

AD15061369

0.011

3

1.79

7440

170

22.9

19900

1.99

1.37

2.14

2450

270

30

0.26

MC15542

593291

8109543

AD15061369

N.D.

5

1.99

6380

230

21.3

41000

4.10

2.37

2.14

920

290

30

0.27

MC15543

593308

8109532

AD15061369

N.D.

2.97

10300

20

11.75

2610

0.261

2.49

4.4

3760

420

0.24

20

MC15544

593372

8109517

AD15061369

N.D.

1

1.46

1480

28.6

1470

0.147

0.88

2.53

200

180

MC15545

593365

8109501

AD15061369

N.D.

2.27

5660

15.8

220

0.022

1.83

3.56

3000

700

20

0.11

20

MC15546

593398

8109423

AD15061369

N.D.

3.47

2330

1.67

170

0.017

0.92

1.69

680

170

0.06

MC15547

593499

8109277

AD15061369

N.D.

0.98

150

21.5

170

0.017

0.74

7.69

4150

360

30

MC15548

593744

8109151

AD15061369

1.15

10250

22

350

0.035

1.18

4.78

3390

370

20

0.25

MC15549

593702

8109146

AD15061369

0.005

1.66

270

15.65

1710

0.171

1.46

5.91

3730

10

620

30

90

MC15550

STD

AD15061369

N.D.

15

2.32

60

70

30

0.31

24500

2.45

11.1

1.21

800

100

29600

7.5

16150

MC15551

STD

AD15061369

N.D.

2

6.26

60

1080

3.95

3550

0.355

5.43

1.67

830

60

990

2020

0.38

1120


APPENDIX 2 - MCARTHUR RIVER PROJECT

JORC TABLE - Section 1 Sampling Techniques and Data

Criteria JORC Code explanation Commentary

Sampling techniques Nature and quality of sampling (eg cut channels, random chips, or specific specialised industry standard measurement tools appropriate to the minerals under investigation, such as down hole gamma sondes, or handheld XRF instruments, etc). These examples should not be taken as limiting the broad meaning of sampling.

Include reference to measures taken to ensure sample representivity and the appropriate calibration of any measurement tools or systems used.

Aspects of the determination of mineralisation that are Material to the

Public Report.

Drilling techniques Drill type (eg core, reverse circulation, open-hole hammer, rotary air blast, auger, Bangka, sonic, etc) and details (eg core diameter, triple or standard tube, depth of diamond tails, face-sampling bit or other type, whether core is oriented and if so, by what method, etc).

Drill sample recovery Method of recording and assessing core and chip sample recoveries and results assessed.

Measures taken to maximise sample recovery and ensure representative nature of the samples.

Whether a relationship exists between sample recovery and grade and whether sample bias may have occurred due to preferential loss/gain of fine/coarse material.

Logging Whether core and chip samples have been geologically and geotechnically logged to a level of detail to support appropriate Mineral Resource estimation, mining studies and metallurgical studies.

Whether logging is qualitative or quantitative in nature. Core (or costean, channel, etc) photography.

The total length and percentage of the relevant intersections logged.

The samples reported here were collected from outcrop and subcrop of shale and dolomite in the lower Wollogorang Formation. Sampling was selective, with copper colours (green malachite, black chacocite) collected in many samples,

and hence are not representative of the full stratigraphy.

Not relevant

Not relevant

The rock samples reported here is geologically described in the report

Sub-sampling techniques and sample preparation

Quality of assay data and laboratory tests

Verification of sampling and assaying

If core, whether cut or sawn and whether quarter, half or all core taken. If non-core, whether riffled, tube sampled, rotary split, etc and whether sampled wet or dry.

For all sample types, the nature, quality and appropriateness of the sample preparation technique.

Quality control procedures adopted for all sub-sampling stages to maximise representivity of samples.

Measures taken to ensure that the sampling is representative of the in situ material collected, including for instance results for field duplicate/second-half sampling.

Whether sample sizes are appropriate to the grain size of the material being sampled.

The nature, quality and appropriateness of the assaying and laboratory procedures used and whether the technique is considered partial or total.

For geophysical tools, spectrometers, handheld XRF instruments, etc,

the parameters used in determining the analysis including instrument make and model, reading times, calibrations factors applied and their derivation, etc.

Nature of quality control procedures adopted (eg standards, blanks, duplicates, external laboratory checks) and whether acceptable levels of accuracy (ie lack of bias) and precision have been established.

The verification of significant intersections by either independent or alternative company personnel.

The use of twinned holes.

Documentation of primary data, data entry procedures, data verification, data storage (physical and electronic) protocols.

Discuss any adjustment to assay data.

Rock chip samples from insitu material. Sample preparation by ALS using PUL23 method to crush and pulverize the entire sample - industry standard and appropriate.

No field duplicates taken.

Sample size (>1kg) appropriate for the grainsize of ore minerals.

Sample analysed at ALS in Perth by techniques ME-ICP61a - a four acid "total" digest for a suite of 33 elements. Selected samples for Au by Au-AA24 a 50g Fire Assay. High grade copper (>10% Cu) was reanalysed by OG62 (upper DL of 40%

Cu) and then as required (if >40% Cu) by ME-XRF15c - a Lithium metaborate fusion decomposition with XRF determination.

Sampling was conducted by the

Exploration Manager

No adjustments have been made to the primary assay data

Locations of data points Accuracy and quality of surveys used to locate drill holes (collar and down-hole surveys), trenches, mine workings and other locations used in Mineral Resource estimation.

Specification of the grid system used.

Quality and adequacy of topographic control.

The samples were picked up using a standard GPS device, with accuracy of better than 3 metres for Northing and Easting, and around 5 metres for RL.

All coordinates data for the project are in

MGA_GDA94 Zone 53.

Data spacing and distribution

Data spacing for reporting of Exploration Results.

Whether the data spacing and distribution is sufficient to establish the degree of geological and grade continuity appropriate for the Mineral Resource and Ore Reserve estimation procedure(s) and classifications applied.

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Sampling was of an exploratory and reconnaissance nature and spacings are insufficient to establish continuity or define Resources.

No compositing has been applied to the


Whether sample compositing has been applied. exploration results.

Orientation of data in relation to geological structure

Whether the orientation of sampling achieves unbiased sampling of possible structures and the extent to which this is known, considering the deposit type.

If the relationship between the drilling orientation and the orientation of key mineralised structures is considered to have introduced a sampling bias, this should be assessed and reported if material.

The samples come from the lower portion of the Wollogorang Formation, subunits PTO1 and PTO2. These units were mapped at a scale of 1:2500, and so

there is excellent geological control on positions.

Sample security The measures taken to ensure sample security. All samples were under company supervision at all times prior to freighting to ALS laboratories in Alice Springs

Audits or reviews The results of any audits or reviews of sampling techniques and data. No sampling audits have been completed to date at the McArthur River Project


Section 2 Reporting of Exploration Results

Criteria JORC Code explanation Commentary

Mineral tenement and land tenure status

Type, reference name/number, location and ownership including agreements or material issues with third parties such as joint ventures, partnerships, overriding royalties, native title interests, historical sites, wilderness or national park and environmental settings.

The security of the tenure held at the time of reporting along with any known impediments to obtaining a licence to operate in the area.

The McArthur River Project comprises two tenements EL 27711 and EL 30085, held by Enigma Mining Ltd, a wholly owned subsidiary of TNG Limited.

The samples reported here come from both EL 27711 and EL 30085.

The tenements are in good standing with no know impediments

Exploration done by other parties

Acknowledgment and appraisal of exploration by other parties. The most significant previous work looking for base metals in the area was completed in the late 1960's by AGPL and is available on NTGS open file

Geology Deposit type, geological setting and style of mineralisation. The main target for this project is Zn-Pb- Cu-Ag mineralisation of a similar style to that found at the McArthur River Mine, some 60km NNE of the project location. This sample displays strong stratabound copper mineralisation

Drill hole Information A summary of all information material to the understanding of the exploration results including a tabulation of the following information for all Material drill holes:

o Easting and northing of the drill collar

o Elevation of RL (Reduced Level - elevation above sea level

in metres) of the drill collar

o Dip and azimuth of the hole

o Down hole length and interception depth

o Hole length

Not relevant

Data aggregation methods

Relationship between mineralisation widths and intercept lengths

In reporting Exploration Results, weighting averaging techniques, maximum and/or minimum grade truncations (eg cutting of high grades)

and cut-off grades are usually Material and should be stated.

Where aggregate intercepts incorporate short lengths of high grade results and longer lengths of low grade results, the procedure used for such aggregation should be stated and some typical examples of such aggregations should be shown in detail.

The assumptions used for any reporting of metal equivalent values should be clearly stated.

These relationships are particularly important in the reporting of

Exploration Results.

If the geometry of the mineralisation with respect to the drill hole angle is known, its nature should be reported.

If it is not known and only the down hole lengths are reported, there should be a clear statement to this effect (eg 'down hole length, true width not known').

No data aggregation has been applied.

The strongly copper anomalous samples are from a known stratigraphic subunit, which has been mapped in detail, but the extent of this mineralisation under cover and down dip is not known

Diagrams Appropriate maps and sections (with scales) and tabulations of intercepts should be included for any significant discovery being reported These should include, but not be limited to a plan view of drill hole collar locations and appropriate sectional views.

Balanced reporting Where comprehensive reporting of all Exploration Results is not practicable, representative reporting of both low and high grades and/or widths should be practiced to avoid misleading reporting of Exploration Results.

Refer to Figures 1 and 2 in the body of the report

All laboratory results are presented.

Other substantive Other exploration data, if meaningful and material, should be reported Information relating to this area appeared

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Criteria JORC Code explanation Commentary

exploration data including (but not limited to): geological observations; geophysical survey results; geochemical survey results; bulk samples - size and method of treatment; metallurgical test results; bulk density,

groundwater, geotechnical and rock characteristics; potential deleterious or contaminating substances.

Further work The nature and scale of planned further work (eg tests for lateral extensions or depth extensions or large-scale step-out drilling). Diagrams clearly highlighting the areas of possible extensions, including the main geological interpretations and future drilling areas, provided

this information is not commercially sensitive.

in the ASX releases on 16 September

2013, 27 June 2014, 20th August 2014,

14th October 2014, 18 December 2014, and 16 February 2015.

Further step out geological mapping, rock sampling and soil (pXRF and lab ICP) sampling will be required, and trenching is being considered. Drilling would follow thereafter.


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