High Grade Tarcoola Assays Confirm Additional Open Pit Gold

Interval (m)

Grade (g/t Au)

Depth (m)

5m

@

5.94

from

11m

4m

@

10.4

from

32m

6m

@

6.17

from

39m

5m

@

6.07

from

99m

7m

@

9.63

from

67m

Interval (m)

Grade (g/t Au)

Depth (m)

4m

@

10.4

from

32

4

@

1.4

from

50

5

@

5.94

from

11

7

@

9.63

from

67

6

@

6.17

from

39

and

3

@

2.65

from

62

and

3

@

2.83

from

74

and

5

@

6.07

from

99

Activity

Competent Person

Membership

Status

Aspects of the determination of mineralisation that are Material to the Public Report. In cases where ‘industry standard' work has been done this would be relatively simple (e.g. "RC drilling was used to obtain 1 m samples from which 3 kg was pulverised to produce a 30 g charge for fire assay"). In other cases, more explanation may be required, such as where there is coarse gold that has inherent sampling problems. Unusual commodities or mineralisation types (e.g. submarine nodules) may warrant disclosure of detailed information

The RC drilling by Barton Gold used a face-sampling 5 ¾" RC drilling techniques undertaken by Profile Drilling. Profile Drilling used an air delivery systems comprising primary and auxillary compressor plus booster, delivering nominal air capacities of approximately 1000psi/2000cfm.

Historic drilling has taken place over numerous periods since the mid- 1980s as follows:

• 1987-1989 BHP Gold/Aberfoyle JV (RC and HQ3 DD)
• 1991-1994 Queens Road Mines/Grenfell Resources(RC)
• 1996-1998 Grenfell Resources (RC, RCD, HQ3 DD)
• 2001-2002 AngloGold/Gravity Capital (RC/RCD)
• 2008 LIDDS (NQ DD)
• 2012 Tunkillia Gold (RC and HQ3 DD)
• 2016-2018 Tarcoola Gold (RC).

Drilling recoveries were qualitatively described for each drilled interval in the field database along with an estimation of moisture content. In general recoveries were good in the order of 30-40kg for each one-metre interval of RC drilling and less than 1% of intervals noted any moisture content. Samples submitted to the laboratory were weighed on a dry, as-received basis and reported along with assay results.

No relationship between grade and recovery has been identified.

Drilling recoveries prior to 2012 were not recorded for both RC chips and diamond core. Some earlier reports noted difficult drilling. Grenfell noted that care was taken to maximise recoveries and minimise contamination and wet drilling conditions were not often encountered. AngloGold noted no major problems with drilling conditions.

TGL RC drilling programmes noted good recoveries, with weights of 30-40kg achieved in fresh material. Within the weathered zone, sample weights were more variable. Holes collared in the Quaternary overburden yielded poor or no recovery from the upper unconsolidated cover sequence, which does not host gold mineralisation.

Diamond core recoveries were recorded by TGL. Local zones of core loss were noted in the oxide zone however core recoveries were generally good.

The RC drilling was closely monitored by the site geologist to ensure optimal recovery and that samples were considered representative.

Historically, HQ triple tube (HQ3) drilling was used for some holes to maximise core recovery. Re-entry holes were not triple-tubed as they were drilled straight into fresh bedrock. Drilling rates were controlled, and short drill runs were often used through the oxide zone to maximise core recovery.

The RC drilling program electronically logged a number of parameters direct into a database including: Stratigraphy, lithology, weathering, primary and secondary colour, texture, grainsize, alteration type-style-intensity and mineralisation type-style-percentage.Logging practices varied over the project's history, however AngloGold attempted to standardize the logging by relogging holes in 2002. Approximately 17,000m of diamond and RC drilling and conversion of historical data into a consistent coding system. Some inconsistency in the logging is evident in the current database, however significant mapping has been completed in the pit which, in conjunction with the logging, provides a sound geological basis to prepare a Mineral Resource estimate.Logging from drilling is generally qualitative in nature.All diamond core and RC drilling has been geologically logged.

SADME (1964) - Diamond holes were quarter-cored by Grenfell.

Aberfoyle (1979-1985) - Samples of open holes TP001-021 were collected in a PVC bag via a cyclone, and then split downto approximately 1.5kg.

Newmex Exploration Limited/Tarcoola Gold Ltd (1987-1988) - RC samples from TRC001-TRC025 were collected over 1m intervals via a cyclone with an incorporated splitter.

Approximately 3kg was collected for analysis. RC samples from TRC026-TRC138 were collected over 1m intervals and riffle split to collect a sample. The weight of the sample was approximately 2kg.

BHP (1987-1989) - RC holes were sampled at 1m intervals with rock chips homogenized via a cyclone before being split and sampled. A 4m composite sample weighing approximately 2.5kg was initially submitted for analysis. The 1m samples were only submitted if the original 4m sample returned a value of >0.5 g/t Au. Diamond core was apparently half-cored, with samples generally taken at 1m intervals.

Grenfell (1991-1993) - RC holes were sampled at 1m intervals were collected in full in plastic bags. The plastic bags were rolled several times to help ensure mixing prior to collecting a 1-2kg sample using a short plastic tube inserted diagonally several times into the material. A 4 m composite was initially submitted for analysis. 1m samples were only submitted if the original 4m sample returned a value of >0.3 g/t Au. Diamond core was apparently half-cored, with samples generally taken at 1m intervals.

Grenfell (1995-1997) - RC holes were sampled at 1m intervals were collected in full in a plastic bucket, and then poured through a three-tier riffle splitter. Buckets were emptied through the splitter at 0.5m intervals. A 3kg sample was collected in a calico bag for assay, and the remaining sample collected in a large plastic bag. Poor sample recovery was apparently only noted within a small number of drillholes.

Diamond core was apparently half-cored, with samples generally taken at 1m intervals.AngloGold (2001-2002) - RC holes were sampled at 1m intervals. Detail surrounding the RC subsampling techniques was not provided to CSA Global. Diamond core was apparently half- cored, with samples generally taken at 1m intervals.Subsampling is performed during the preparation stage according to the assay laboratories' internal protocols.During the RC drilling program primary samples were collected from a shute on the cyclone splitter. Field duplicates were obtained from a secondary shute on the splitter.To the best of the Competent Persons knowledge, no RC field duplicates were taken prior to 1995. After 1995, field duplicates have generally been inserted in the sample stream at a rate of one in every 20 samples. No data was provided for the AngloGold drilling program however (2001-2002). Results generally give confidence in sampling procedures .Sample sizes are considered to be appropriate to the grain size of the material being sampled.

Analytical techniques have varied somewhat over the projects history and are summarised below.

SADME (1964) - Diamond holes were sent to Amdel in Adelaide for analysis by Aqua Regia digest flame AAS with a 0.02 detection limit. Any samples returning grades >1 g/t Au were re-assayed by fire assay with an AAS finish.

Aberfoyle Exploration (1985-1987) - Samples were submitted to Classic Laboratories in Perth for fire assay using a 50g charge.

Newmex Exploration Limited, Tarcoola Gold Limited (1987- 1988) - Samples from TRC001-TRC025 were submitted to Genalysis in Perth for analysis using Aqua Regia digest and AAS finish after roasting to oxidise sulphides. Fire assay was carried out on all samples containing >1 g/t Au determined following Aqua Regia. Samples from TRC026-TRC138 were submitted to Classic Comlabs, Adelaide for analysis by fire assay.

BHP Gold (1988-1991) - Samples were submitted to Amdel Laboratories in Adelaide for analysis. The analytical method is not known.

Queens Road Mine/Grenfell Resources (1992-1994) - Samples were submitted to Amdel for digest by Aqua Regia (two parts hydrochloric acid to one-part nitric acid), followed by extraction into organic solvent (D.I.B.K.). A 50g subsample was then analysed by AAS with a 0.02 g/t Au detection limit.

Grenfell Resources (1996-1998) - Earlier samples were submitted to Amdel for analysis by Aqua Regia digest with AAS finish. Any samples returning grades >1 g/t Au were re-assayed by fire assay with and AAS finish. Later holes were submitted to Aqua Regia digest with graphite furnace AAS.

AngloGold, Gravity Capital Limited (2001-2002) - Earlier holes (up to TCRC0029) were submitted to Genalysis in Adelaide.

Sample preparation was completed in Adelaide, and then sample analysis was completed in Perth via a 50g fire assaywith AAS finish (Method FA50/AAS). Later holes were submitted to Analabs in Perth for analysis by fire assay.

Low Impact Diamond Drilling Services (2008) - Two core holes were submitted to Onsite Laboratory Services, Bendigo for analysis by 25g fire assay with AAS finish. Subsampling techniques are not known.

Tunkillia Gold (2012) - Au analysis was completed by IntertekGenalysis in Adelaide, via a 50 g lead collection fire assay with AAS finish to a 0.005 ppm detection limit (Method FA50/AA).

Tarcoola Gold (2016-2017) - Samples were dried at 90 ̊C to eliminate the impact of moisture on sample processing. After drying samples are crushed via a Boyd Crusher to <10mm in size then split through a rotary splitter to produce a sub-sample. The crusher is cleaned regularly and has barren bricks crushed between sample groups to prevent contamination. Analysis is through the pulverising and leach (PAL) process. This process reflects the site mill extraction process where: each process is pulverised in aqueous solution with cyanide bearing assay tabs and a collection of assorted sized ball bearings.

Each sample is pulverised for an hour, resulting in an Au-CN complex bearing solution and remnant pulverised sample, and the pulverised material is 95% passing 75 microns. Following PAL processing, samples are decanted, centrifuged and prepared for analysis in an AAS with a solvent separation with a DIBK and residence time of 20 minutes. The sample is then aspirated through the AAS to produce a reading.

Barton Gold (2020) - 2-4kg splits were sent to MinAnalytical in Perth for preparation and analysis using photon assay techniques for gold and ICPOES/MS for multielement geochemistry. The received samples used MinAnalytical's PAP3502R method for preparation which included weighing before drying and crushing to 3mm. A 500g charge was split for analysis using MinAnalytical's PAAU2 photon assay method for gold which is a fully automated technique designed for the analysis of ores. It uses high energy x-rays to excite the atoms so liberation from the surrounding material is not required. The ~500g single-use jars allows for bulk analysis with no chance of cross contamination between samples.

Barton Gold (2021) - 2-4kg splits were sent to Intertek Genalysis in Adelaide for preparation and analysis using 50g fire assay techniques for gold and ICPOES/MS for multielement geochemistry. Whilst preparation and some fire assays were undertaken in Adelaide Intertek also sent some batches to their Perth laboratories for analysis. Intertek's FA50/OE04 method uses a 50 g lead collection fire assay with ICP-OES / MS finish to a 0.005 ppm detection limit. Multielement samples were analysed using Intertek's method 4A/MS48 which is a 4-acid digest followed by analysis using ICP-OES and MS for 48 elements.

Barton Gold (2022-present) - 2-4kg splits were sent to Bureau Veritas in Adelaide for preparation and analysis using a 40g fire assay technique for gold. Bureau Veritas' FA1 method uses a 40 g lead collection fire assay with AAS finish to a 0.01 ppm detection limit.

No geophysical studies were used in this latest drilling program.

Barton Gold's RC drilling program included a comprehensive QAQC component with Field Duplicates, Certified Standards (selection of OREAS CRM's considered most appropriate for expected grade and composition) and coarse blanks collectively inserted at ratio of approximately 1 in 17 primary samples. The sequencing of QC samples is tailored on the basis of preliminary (field) assaying to maximise the effect of QA. Additionally, the laboratories provided their internal QAQC which included check samples, CRM's, blanks and repeats.

Analysis of the duplicate samples was variable but considered acceptable given the nature of gold mineralization associated with this project. Some significant variation was noted however this is considered consistent with the interpreted high nugget style of mineralisation.

Bureau Veritas' analysis for gold using fire assay performed well with all batches falling within the +/-3SD test of the expected value for the given standards (3 OREAS CRM's).

Historically, the amount of sampling and analytical QC data that has been collected has varied over the project's history.

Limited sampling and analytical QC data is available to support drilling programs completed prior to 1992, which represents a relatively minor portion of the dataset.

Between 1992 and 1994, the only meaningful QC data appears to be a comparison of spear and riffle split sampling results. No significant bias was noted between the methods.

Between 1996 and 1998, standard results indicate no significant bias, and blank results suggest no issue with carry-over contamination. Field duplicate results reveal a reasonable amount of scatter, which implies poor sample precision, however no bias was noted. Check (umpire laboratory) assay results also revealed considerable scatter but no significant bias which further attests to the accuracy of the analytical data.

It is understood no QC samples were submitted between 2001 and 2008.

Tunkillia Gold used blanks to monitor carry-over contamination and no significant issues were detected. Field duplicates were used to assess sample precision, while CRMs were used to assess analytical accuracy. Some pulps were also sent to an umpire laboratory as a further check on analytical accuracy.

Field duplicate results provide some confidence sample precision. The scatter which is observed is understandable given the moderate to high nugget effect evident at Tarcoola. The CRMs reasonably demonstrated the accuracy of the laboratory. Pulp repeats were higher than the original results, which did cause some concern however, given the CRM results the Competent Person had reasonable confidence in the accuracy of the primary laboratory.

Tarcoola Gold collected field duplicates to monitor sample precision and submitted one main CRM to monitor analytical accuracy. The field duplicate results give some confidence in sample precision, with the scatter which is observed likely a consequence of the high-nugget nature of the mineralisation. Although only one CRM was used, no bias was noted.

Alternative company personnel have verified significant intersections.

No twinned holes were used in the course of this program.

All data collected in the reported program including collar details, drilling records, sampling records and geological logs are recorded directly into spreadsheets in the field which includes comprehensive interval validation processes.

Gyro downhole surveys and Assay results were provided in digital format.

All relevant historical data was entered into a DataShed database where various validation checks were performed. Data was exported into an Access Database.

No adjustments were made to any assay data in this release.

All 2024 RC collars were sited using a Garmin hand-held GPS system, with all drill collars also picked up using a Leica DGPS system post-drilling (<0.1m accuracy). The RL was generated from the LiDAR survey collected at the completion of drilling.

All Barton RC holes were downhole surveyed using an Axis Champ-Gyro system which provided measurements at 20m intervals up and down hole.

Collar location and downhole survey methods have varied somewhat over the project's history. Almost all hole collars have been surveyed by GPS, DGPS or total station methods, with checks completed against the topographic DTM.

Downhole survey methods have varied somewhat over the projects history and are summarised below.

Aberfoyle (1979-1985) - Holes not surveyed. Set-up positions were used and are well documented.

BHP (1987-1989) - Holes not surveyed. Set-up positions were used and are well documented.

Grenfell (1991-1997) - A single shot Eastman camera was used, with surveys taken every 30-50m (GP, GL series). Early generation holes completed by Grenfell/Queens Road were not surveyed at the time of the drilling. Grenfell conducted a campaign of Eastman surveys for open historical holes, using Fugro Survey as a contractor.

AngloGold (2001-2002) - A single shot Eastman camera was used, with surveys taken every 30-50m (TCD, TCRC series).

Tunkillia Gold (2012) - A reflex Ezi-shot downhole camera was used, with readings taken every 30m for diamond holes (TADD series) and end-of-hole for RC holes (TARC series). TGL completed validation checks on the downhole surveys including consistency checks on available databases, comparison of digital databases against hard copy records, and against original Eastman camera discs, cross checks on grid to magnetic conversions and visual review.

Tarcoola Gold (2016-2017) - In February 2017, Kinetic Technologies was engaged to perform a downhole optics survey for a geotechnical review. A total of seven holes were downhole surveyed for deviation using a directional survey probe.

Readings were taken at 10m downhole intervals. Results showed minor lifting in holes deeper than 28m. The majority of grade control holes are drilled to 23m; hence hole deviation is not considered to be significant

All site data is reported in Geocentric Datum of Australia 1994 (GDA94) and Vertical Datum in Australian Height Datum (AHD). The map projection is MGA Zone 53. Historic Survey Data has been converted to GDA94.

In March 2020 Barton gold engaged Aerometrex to collect LiDAR and high-resolution ortho-imagery over the entire Tarcoola Mining Lease. All datasets are levelled to the LiDAR survey.

An internal peer review of the exploration data processes has been completed by Barton Gold which has included a detailed review of the assay, survey and QAQC data.

MacArthur carried out a review of sampling techniques and data in 2013.Mining Plus undertook a comprehensive audit of the historical drilling database in 2020 and have in part rebuilt the database using original assay results and incorporated significant supporting metadata.

The Tarcoola deposit has been subject to sporadic exploration by numerous parties since alluvial gold was first discovered in 1893. Companies who have undertaken drilling include: Newmex Exploration, BHP, Grenfell Resources, AngloGold, Stellar, Hiltaba Gold, Tunkillia Gold and Tarcoola Gold.

The Tarcoola Project covers a portion of the north-western Gawler Craton centred over the historic Tarcoola goldfield, where Archaean and Proterozoic rocks form the basement to an extensive cover of Phanerozoic sediments. The Archaean basement has been extensively deformed, whereas the Proterozoic rocks have been weakly to moderately deformed.

At Perseverance (current Tarcoola open pit mine), gold mineralisation is hosted within sedimentary rocks of the Tarcoola Formation and granite, both of Proterozoic age. The granite is variably in fault contact with or unconformably overlain by the sediments, which consists of conglomerate, limestone, sandstone, siltstones, and shale. A suite of later intrusions (Lady Jane Diorite) cut both the sedimentary rocks and the granite.

Mafic high level intrusives associated with the 1590Ma Hiltaba Magmatic Event are considered to control the spatial setting of both gold and base metal mineralisation.

Three deformation events have been recognised in the area. D1 is characterised by open folding and NNW-directed thrusting, responsibly for the southerly dip of the sedimentary package at Perseverance. Steeply dipping NW and NE trending brittle faults developed during D2. These structures host and control the gold mineralisation in the Tarcoola Ridge area. The third deformation event (D3) is represented by the late E-W trending barren quartz veins.

Gold has locally been remobilised and enriched in the weathering profile. The base of complete oxidation occurs typically 10-40m below surface, and the base of partial oxidation occurs at a depth of ~20-60m.

Within the primary zone, sericite-quartz-pyrite alteration zones are spatially associated with the mineralisation and overprint earlier hematite-magnetite alteration. An outer halo of chlorite (+/-leucoxene and pyrite) is developed. Pyrite, galena and sphalerite are the main associated sulphide minerals, with subordinate amounts of chalcopyrite bornite and/or arsenopyrite noted.

Veins can be discrete or form wider stockwork zones and are surrounded by broader quartz-sericite alteration envelopes which can host lower grade background halos of mineralisation. Dispersed supergene mineralisation in the oxide zone can be largely detached from veining.

For more detail see: Budd, A & Skirrow, R, 2007. The Nature and Origin of Gold Deposits of the Tarcoola Goldfield and Implications for the Central Gawler Gold Province, South Australia. Economic Geology, 2007.

A summary of all information material to the understanding of the exploration results including a tabulation of the following information for all Material drillholes:

• Easting and northing of the drillhole collar
• Elevation or RL (Reduced Level - Elevation above sea level in metres) of the drillholecollar
• Dip and azimuth of the hole
• Downhole length and interception depth hole length.
• Hole length

If the exclusion of this information is justified on the basis that the information is not Material and this exclusion does not detract from the understanding of the report, the Competent Person should clearly explain why this is the case.

A tabulation of the drilling program including the details of historic holes mentioned in this Announcement are presented in Tables 2 to 5.

In reporting Exploration Results, weighting averaging techniques, maximum and/or minimum grade truncations (e.g. 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.

• Reported intervals have been determined by applying a 0.5g/t Au cut-off (minimum 1gram-metre accumulation, ie the multiple of the interval in metres and the weighted average grade) and allowing for a maximum of two consecutive intervals of dilution
• No high-grade cut-offs were applied
• Zones of anomalous mineralisation presented on drill sections have been determined by applying a 0.1g/t Au cut-off , with a minimum width of two metres and allowing for a maximum two consecutive intervals of dilution.

No metal equivalents were calculated

These relationships are particularly important in the reporting of Exploration Results.

If the geometry of the mineralisation with respect to the drillhole 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 (e.g. "downhole length, true width not known").

The relationship between mineralisation width and intercept lengths is unknown. Mineralisation elsewhere in the broader project area where there is greater levels of geological confidence is steeply dipping.

See figures included in the body of this announcement

Balanced reporting of Exploration Results is presented. Historical drilling has been undertaken across all recently drilled areas and is presented only where applicable at the scale of diagrams provided.

Other exploration data, if meaningful and material, should be reported 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.

No substantive exploration data not already mentioned in this table has been used in the preparation of this Announcement.

There are however extensive geological, geophysical, geochemical, geotechnical and metallurgical datasets available for this project area

Barton Gold is planning further work which will be focused on testing for dip extensions and strike extensions and to confirm grade and geological continuity implied by the current results.

Diagrams have been included in the body of this Announcement

Hole ID

Easting

Northing

RL

DIP

TAZ

Total Depth (EOH)

Type*

Completion

Target

TBM0205

454951

6602904

90

-78

272

84

RC

19/7/2024

SE Pit Floor

TBM0206

454916

6602871

89

-50

172

60

RC

19/7/2024

SE Pit Floor

Perseverance Fault

TBM0207

454920

6602877

90

-67

136

84

RC

20/7/2024

SE Pit Floor

Perseverance Fault

TBM0208

454919

6602888

90

-60

095

96

RC

20/7/2024

SE Pit Floor

Granite Fault East

TBM0209

454866

6602790

85

-67

123

108

RC

21/7/2024

Granite Fault East

TBM0210

454877

6602807

85

-59

126

60

RC

21/7/2024

Granite Vein South

TBM0211

454883

6602816

85

-65

105

66

RC

21/7/2024

Perserverance Fault

Peela Contact

Granite Deeps

TBM0212

454890

6602823

85

-50

77

54

RC

22/7/2024

Perserverance Fault

Granite Fault East

TBM0213

454930

6602863

90

-54

304

138

RC

22/7/2024

Peela Contact

Granite Vein South

TBM0215

454879

6602822

85

-79

330

132

RC

22/7/2024

Granite Vein South

24

27

3

1.44

31

38

7

0.66

2

4

2

0.93

13

14

1

3.53

26

32

6

0.69

36

38

2

1.8

42

44

2

2.13

9

10

1

1.11

26

27

1

1.06

40

41

1

1.19

27

28

1

2.34

38

40

2

1.86

46

49

3

0.76

32

36

4

10.4

0

1

1

2.25

6

7

1

4.2

25

26

1

2.55

13

14

1

2.93

50

54

4

1.4

58

63

5

0.44

11

16

5

5.94

24

25

1

1.6

2

3

1

2.14

67

74

7

9.63

86

87

1

1.36

39

45

6

6.17

62

65

3

2.65

74

77

3

2.83

83

86

3

1.59

99

104

5

6.07

Hole ID

Easting

Northing

RL

DIP

TAZ

Total Depth (EOH)

Type*

Completion

Target

454793

6602749

164

-58

65

279

15/04/1996

454807

6602872

157

-61

113

274.2

10/03/1997

454911

6602769

164

-90

0

144

1/01/1993

454835

6602820

161

-90

0

60

16/04/1993

454898

6602740

164

-60

331

125

20/04/1993

454903

6602860

160

-61

235

80

18/08/1993

454817

6602786

165

-57

32

77

13/09/1993

454773

6602927

152

-60

133

318

18/08/2020

454834

6602804

135

-60

0

23

1/07/2017

Grade Control

454839

6602799

135

-60

0

23

1/07/2017

Grade Control

454839

6602809

135

-60

0

23

1/07/2017

Grade Control

454903

6602784

120

-60

270

45

1/01/2018

Grade Control

454904

6602776

100

-60

270

24

1/06/2018

Grade Control

454897

6602781

100

-60

270

26

1/06/2018

Grade Control

454922

6602821

100

-60

270

32

1/06/2018

Grade Control

454907

6602826

100

-60

270

23

1/06/2018

Grade Control

454847

6602806

100

-90

0

42

1/06/2018

Grade Control

454843

6602796

163

-60

106

100

1/09/1991

183

185

2

1.64

190

191

1

11.85

138

148

10

6.47

160

161

1

1.17

166

177

11

0.95

101

102

1

3.65

44

45

1

3.6

46

47

1

4.1

101

103

2

13.32

75

79

4

4.27

57

59

2

0.8

206

207

1

2.36

17

21

4

1.04

21

23

2

2.29

17

18

1

1.11

40

43

3

0.77

17

20

3

1.22

18

26

8

8.93

26

27

1

1.75

20

22

2

0.81

20

21

1

2.13

90

99

9

5.57