PETRATHERM LIMITED

ACN 106 806 884

ASX: PTR

www.petratherm.com.auadmin@petratherm.com.au

ASX ANNOUNCEMENT

20/04/2022

Drilling uncovers major High-Value Rare Earth Discovery at Comet in the Northern Gawler Craton

HIGHLIGHTS

  • Petratherm redefines the mineral prospectivity of the Northern Gawler Craton of South Australia after Greenfield's regional RAB drilling supported by South Australian Government Exploration Initiative Co-Funding uncovers significant rare earth (REE) occurrences.

  • Shallow RAB drilling tested the top 3 metres of the prospective clay horizon. Mineralisation encountered, includes impressive concentrations of high-value REE's which remain open at depth below and out into surrounding areas.

  • Notable drill intercepts include:

    High Value

    Hole

    Interval

    Magnet Rare Earths*

    703

    3m @ 2,819 ppm TREO from 15m - 18m (EOH)

    743 ppm

    704

    3m @ 2,660 ppm TREO from 15m - 18m (EOH)

    702 ppm

    590

    3m @ 2,701 ppm TREO from 15m - 18m (EOH)

    1,016 ppm

    799

    3m @ 1,813 ppm TREO from 12m - 15m (EOH)

    456 ppm

    931

    3m @ 1,705 ppm TREO from 12m - 15m (EOH)

    382 ppm

    T14_RC10

    4m @ 3,042 ppm TREO from 36m - 40m

    814 ppm

    (* Magnet Rare Earths = Pr6O11, Nd2O3, Tb4O7 & Dy2O3)

  • All 44 holes assayed returned significant results with 23 holes returning TREO > 1,000ppm.

  • REE intercepts in clays show striking similarities and comparable grades to the ion-absorption rare earth deposits of China which are a major world supplier.

  • Deeper RC drilling into crystalline basement rock below REE enriched clays at the Target 14 Prospect intersected zones of primary REE mineralisation. This may represent a potential source rock for the mineralisation and petrological analysis of the REE enriched basement rock is underway.

  • 10,000 metre RAB drilling program scheduled to start in three weeks to test extent of mineralisation. Initial JORC resource potentially defined within six months.

  • Petratherm has a strong ground position in the Northern Gawler Craton, totalling 1,885 Km2. There is large upside for further important new REE Prospects in surrounding un-explored areas.

INTRODUCTION

Petratherm Limited (ASX: PTR) is pleased to announce assay results of Rare Earth (REE) drill intersections from the Comet Project Area (EL 6443 & EL 6633) in the Northern Gawler Craton of South Australia. Samples from 44 shallow RAB drill holes returned significant REE mineralised clay intersections outlining several regionally significant Prospect Areas. The results presented are for the most part 3 metre composite bottom hole samples taken from the Company's ongoing regional RAB geochemical sampling program and the mineralisation encountered remains open at depth and out into surrounding areas.

Full suite REE analysis of the 44 drill holes was undertaken following recognition of anomalous light REE (cerium and lanthanum) and other REE path finder elements from the Company's initial assay work. In addition to the 44 holes presented herein, a further 111 drill holes of the 993 shallow RAB holes drilled thus far contain evidence for elevated REEs. These samples are now undergoing analysis to better characterise the extent of REE mineralisation in the region.

First pass drilling was completed on a 400 metre X 400 metre spaced grid and the newly defined REE Prospect areas have been shown to be regionally extensive extending several kilometres (Figure 1).

REE 1 Anomaly - Area 1 is a broad northeast trending anomaly extending over an approximate 9 kilometre by 2-kilometre area (Figure 1). The 10 holes sampled to date in this area have returned a top of clay 3 metre composite Total Rare Earth Oxide (TREO) grade ranging between 703 ppm to 2,819 ppm. The area includes the Target 14 Gold Prospect where REE assaying of the crystalline basement rock below the clay interval has also returned highly anomalous REE's, with drill hole T14_RC10 intercepting 4m @ 3,042 ppm TREO from 36m - 40m. The presence of primary REE mineralisation in fresh rock below the REE clays is highly encouraging, confirming the presence of local REE source rocks.

Drill Hole 703 records 3m @ 2,819 ppm from 15m to end of hole and Hole 704 which is the adjacent hole 400m to east, returned 3m @ 2,660 ppm TREO from 15m to end of hole. These holes contain exceptional high value Magnet REE grades of 743 ppm and 702 ppm respectively. Another 50 drill holes with anomalous REEs and/or REE pathfinder elements from within Area 1 are with ALS laboratories undergoing analysis.

REE2 Anomaly - Area 2 REE anomaly extends over an approximate 3 kilometre by 1.5-kilometre area and broadly overlies a prominent magnetic basement rock complex (Figure 2). Research is underway to determine if the magnetic complex is the source of the REE mineralisation in the area. A further 37 drillholes at REE2 have returned anomalous samples which are now with ALS for analysis.

Other Early Stage REE Anomalies - Several single and multi-hole regional spaced drill holes (Figure 1) have returned highly significant REE grades including:

Hole 590

3m @ 2,701 ppm TREO from 15m - 18m (EOH) of which 1,016 ppm are High-Value Magnet REEsand

Hole 931

3m @ 1,705 ppm TREO from 12m - 15m (EOH)

Comet Project - Table of all REE Intercepts

Drill HoleFromToIntervalTREO

metresmetres

metres

ppm

High Value Magnet Rare Earths

Praseodymium

Neodymium

Pr6O11

Nd2O3

Terbium Tb4O7

Dysprosium

Dy2O3

ppm

% TREOppm

% TREOppm

% TREOppm

% TREO

280

18

22

4

980

36.25

3.70

109.76

11.20

1.13

0.12

6.5

0.66

358

8

12

4

972

42.65

4.39

137.05

14.11

2.22

0.23

12.9

1.33

400

8

12

4

877

52.80

6.02

177.29

20.23

1.58

0.18

9.3

1.06

404

9

12

3

1322

67.66

5.12

205.29

15.53

1.98

0.15

10.6

0.80

428

14

18

4

654

29.12

4.45

92.03

14.08

1.01

0.15

6.8

1.03

475

6

9

3

1088

53.76

4.94

194.21

17.85

2.57

0.24

16.4

1.51

484

8

12

4

1205

76.84

6.38

261.27

21.68

3.25

0.27

17.3

1.44

493

9

15

6

868

42.17

4.73

152.62

17.58

2.52

0.29

15.1

1.74

567

9

12

3

1030

61.86

6.00

212.87

20.66

2.52

0.24

14.5

1.41

586

18

21

3

550

23.74

4.31

72.20

13.12

0.61

0.11

2.9

0.53

590

15

18

3

2701

216.27

8.01

744.16

27.55

10.08

0.37

45.2

1.67

TG14RB01

28

30

2

906

48.81

5.39

177.88

19.63

1.51

0.17

8.2

0.90

638

9

12

3

1013

66.09

6.52

229.20

22.62

3.02

0.30

14.2

1.40

639

12

15

3

1140

74.30

6.52

244.94

21.49

3.60

0.32

18.9

1.66

703

15

18

3

2819

149.21

5.29

562.20

19.95

4.71

0.17

27.1

0.96

704

15

18

3

2660

141.36

5.31

530.71

19.95

4.47

0.17

25.7

0.97

707

19

22

3

1225

71.65

5.85

246.11

20.09

4.38

0.36

21.1

1.72

710

12

15

3

1081

59.56

5.51

199.45

18.46

3.19

0.29

15.9

1.47

733

24

27

3

848

35.16

4.15

124.22

14.65

1.62

0.19

7.9

0.93

744

18

21

3

1142

77.20

6.76

278.77

24.41

3.62

0.32

16.9

1.48

750

20

24

4

1165

67.90

5.83

258.94

22.22

5.72

0.49

30.3

2.60

757

12

15

3

568

36.49

6.43

137.64

24.24

1.76

0.31

7.8

1.37

785

5

15

10

710

33.04

4.65

120.02

16.90

2.50

0.35

13.4

1.89

790

12

15

3

626

21.87

3.49

78.15

12.48

2.09

0.33

12.3

1.96

799

12

15

3

1813

88.80

4.90

333.59

18.40

5.80

0.32

27.9

1.54

800

8

12

4

1121

53.64

4.79

212.87

18.99

4.63

0.41

22.6

2.01

804

8

14

6

780

40.60

5.20

155.13

19.88

2.58

0.33

11.3

1.44

808

10

14

4

1248

65.00

5.21

242.61

19.45

2.62

0.21

11.5

0.92

and

22

24

2

728

37.09

5.10

137.05

18.83

1.91

0.26

8.1

1.11

822

10

15

5

758

37.51

4.95

132.68

17.51

2.18

0.29

11.6

1.53

855

9

12

3

1418

67.66

4.77

251.94

17.77

4.94

0.35

25.7

1.81

875

15

17

2

1041

63.91

6.14

236.78

22.74

2.81

0.27

14.2

1.36

877

9

15

6

712

37.21

5.23

132.97

18.67

2.05

0.29

10.6

1.49

886

15

18

3

728

41.68

5.72

144.05

19.78

1.83

0.25

9.9

1.36

901

15

18

3

495

22.65

4.58

76.87

15.53

1.35

0.27

7.6

1.54

931

12

15

3

1705

83.49

4.90

286.93

16.83

1.98

0.12

9.5

0.56

953

8

12

4

682

29.36

4.31

105.21

15.43

1.89

0.28

10.4

1.53

961

15

18

3

873

46.64

5.34

147.55

16.90

1.58

0.18

8.4

0.96

21T14RC03

12

16

4

1298

72.37

5.58

271.77

20.94

1.14

0.09

5.9

0.45

and

44

48

4

1179

65.00

5.51

246.11

20.87

1.09

0.09

5.8

0.50

21T14RC08

8

16

8

962

52.13

5.42

186.92

19.44

0.65

0.07

2.9

0.30

21T14RC10

12

16

4

817

44.34

5.42

155.71

19.05

0.68

0.08

3.4

0.42

and

36

40

4

3042

169.15

5.56

640.35

21.05

1.00

0.03

3.4

0.11

and

52

56

4

829

46.27

5.58

174.38

21.03

0.66

0.08

3.5

0.42

21T14RC12

20

24

4

1147

62.71

5.47

239.11

20.84

1.53

0.13

8.6

0.75

21T14RC13

36

40

4

604

31.41

5.21

118.97

19.71

0.88

0.15

4.8

0.79

21T14RC14

8

12

4

749

40.23

5.37

146.97

19.63

0.58

0.08

2.7

0.37

and

24

28

4

727

38.30

5.27

139.38

19.16

0.89

0.12

4.9

0.67

and

32

36

4

1361

74.91

5.50

276.44

20.31

0.66

0.05

2.4

0.18

and

44

48

4

1295

74.06

5.72

276.44

21.34

0.76

0.06

3.2

0.25

21T14RC18

24

28

4

804

34.19

4.25

132.97

16.53

3.01

0.37

18.3

2.28

Table 1 Comet Project - Summary Table of all REE drill intersections analysed

Figure 1 Comet Project REE Results Overview Map

(*Anomalous Drillhole = anomalous Ce and/or La and/or REE path finder element(s) Th, Sr & P)

It is important to note that sample results are for the most part single 3 metre composite samples of the top of the interpreted clay (saprolite) zone. Up hole sampling has not occurred and the mineralised intervals remain open at depth and laterally into surrounding areas. Samples from adjacent drill holes currently not recording significant REEs may be due to the sample interval being taken above or below potential mineralisation. Ionic Clay hosted REE occurrences typically show vertical and horizontal grade and depth variability within a saprolite clay profile. Better determination of these unknowns will come from the up-coming drilling scheduled to start in 3 weeks' time.

Commenting on these results Petratherm's Exploration Manager, Mr Peter Reid said:

"These are highly encouraging early results and a validation of the Company's long standing frontier exploration approach, working in under-explored terrains and trialling new exploration methods. The results provide strong evidence that the Northern Gawler Craton of South Australia is fertile for ionic clay hosted rare earth mineralisation."

Figure 2 REE2 Prospect, TREO values and REE anomalous drill holes.

(*Anomalous Drillhole = anomalous Ce and/or La and/or REE path finder element(s) Th, Sr & P)

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Petratherm Ltd. published this content on 19 April 2022 and is solely responsible for the information contained therein. Distributed by Public, unedited and unaltered, on 19 April 2022 23:04:04 UTC.