Highly Encouraging VTEM Results at Wongan Hills

“We are very encouraged by the detection of bedrock conductors within an area prospective for VHMS deposits, where supported by strongly anomalous laterite geochemistry comparable to that of Golden Grove. We anticipate several drill targets to be refined from modeling of the VTEM data and follow- up ground EM.” ~Cullen’s Managing Director, Chris Ringrose

Published: August 14, 2018

WONGAN HILLS, E70/4882 and ELA70/5162, ~180 km north-east of Perth, base metals and gold project (Cullen 90% – Tregor Pty Ltd 10%).

HIGHLIGHTS

  • Cullen Resources Limited (Cullen or the Company) has received an interpretation of the preliminary data of its VTEMTM max survey at Wongan Hills from geophysical consultants “Newexco”.
  • The results highlight multiple clusters and trends of interpreted bedrock conductors.
  • In particular, five clusters of interpreted bedrock conductors, over strike lengths of ~0.4 to 1.5km which are coincident with significant CHI-3 geochemical index anomalies now define priority VHMS targets.
  • None of the multiple geochemical anomalies with interpreted bedrock conductors has been the target of previous drill testing.
  • The laterite geochemistry alone shows some similarities to that of the 50Mt Golden Grove VHMS system (as shown here by the CHI – 3 geochemical index).
  • In Cullen’s opinion, Wongan Hills has several high priority targets for Volcanic-Hosted Massive Sulphides deposits (VHMS) of the Golden Grove – type.

AIRBORNE GEOPHYSICAL SURVEY

In June 2018, Cullen completed a helicopter-borne, Versatile Time – Domain Electromagnetic geophysical survey (VTEMTM Max) to advance its exploration at Wongan Hills. The survey was flown by UTS Geophysics Pty Ltd (266 line km on east-west lines spaced at 150m, with a sensor height of 30m) and was centred on the geochemical anomalies previously reported by Cullen. The objective of the survey is to test for bedrock conductive responses typical of massive sulphide deposits, particularly where they coincide with geochemical anomalies.

INTERPRETED BEDROCK CONDUCTORS – GEOCHEMICAL ANOMALIES

The multiple interpreted bedrock conductors (Category 1 and Category 2 – the most significant in a three range classification) have been overlain on an air mag image (Fig.1) to show their relationship to stratigraphic trends, and/or other more discrete magnetic features, and importantly, on the geochemical anomalies (Fig. 3). This has enabled the prioritising of targets.

Fig.1 Category 1 and 2 interpreted bedrock conductors shown as white dots

Fig.1 Category 1 and 2 interpreted bedrock conductors shown as white dots

Cullen’s laterite sample assays for E70/4882 (ASX: CUL – 5 July 2017; 24 April 2018; 3 May 2018) and compilation of historical geochemical data are summarised in Cullen’s ASX announcement of 18 July 2018. Using these data, Cullen has plotted the CHI – 3 geochemical index for Cullen’s laterite sample assays from Wongan Hills and compared it to a plot of the CHI – 3 geochemical index, as presented by Smith and Perdrix, 1983, for the Golden Grove VHMS deposits (Fig. 2), using the same contouring intervals.

CHI – 3 values in laterite over the Scuddles (blind) and Gossan Hill (outcropping) orebodies at Golden Grove, are shown where:

CHI – 3 = As +3Sb+10Bi+10Cd+10In+3Mo+30Ag+30Sn

Cullen concludes that this comparison is in itself compelling evidence for the good prospectivity of the Wongan Hills project for VHMS deposits. This is reinforced by the overlay of interpreted bedrock conductors from Cullen’s VTEM survey on the Wongan Hills CHI – 3 geochemical index plot. There are five priority clusters of conductors which are embedded in the most anomalous CHI – 3 geochemical zones or their strike extension – four on the west and one on the east ranging from approximately 0.4 to 1.5km in strike length (Fig. 3). Some historical drilling has occurred in the general area of the eastern priority cluster – all other priority clusters are untested by any drilling.

Other interpreted bedrock conductor trends are outside of the highest level of geochemical anomalies where defined by CHI – 3 = “297”. Some are broadly related to historical MMI geochemical anomalies (see ASX:CUL 18 July 2018), and at this stage there is limited geochemical and/or geological data on other trends, however, all are worthy of further investigation. Note, no bedrock VTEM data is available for the general area of the “Louise” geochemical anomaly in the western margin of the geophysical survey, due to the interference of conductive, near-surface, salt water.

Fig. 2: Plot of CHI - 3 geochemical index values, laterite samples.

Fig. 2: Plot of CHI – 3 geochemical index values, laterite samples.

Fig. 3: Prioritised clusters of interpreted bedrock conductors plotted on CHI - 3 geochemical index values for laterite samples at Wongan Hills.

Fig. 3: Prioritised clusters of interpreted bedrock conductors (1-6) plotted on CHI – 3 geochemical index values for laterite samples at Wongan Hills.

SUMMARY

Cullen concludes that the Wongan Hills project presents:

  • A favourable geological setting for Volcanic-Hosted Massive Sulphides deposits (VHMS) in an Archaean greenstone belt with known Cu-Au mineralisation (Figures 4 and 5) – several VHMS targets now defined by significant, coincident geochemical anomalies and interpreted bedrock conductors;
  • Compelling laterite geochemistry with some similarities to that of the 50Mt Golden Grove VHMS system (as shown herein by CHI – 3 geochemical index e.g.);
  • Five clusters of bedrock conductors, over strike lengths of ~0.4 -1.5km , are entirely coincident with significant CHI-3 geochemical index anomalies; and,
  • None of the geochemical anomalies with interpreted bedrock conductors has been the target of any previous drilling.

NEXT STEPS

Modelling of the VTEM conductors by Newexco, together with a field review will further prioritise targets planned for ground EM surveys next Quarter.

However, it is envisaged that several of the targets within E70/ 4882 warrant drilltesting and as most of these are located on freehold, arable farm land, a compensation agreement with the landowner(s) is required to permit further exploration. Cullen plans to negotiate the required agreements to permit access and/or drilling as soon as possible.

Cullen’s Managing Director, Chris Ringrose commenting on the results said:

“We are very encouraged by the detection of bedrock conductors within an area prospective for VHMS deposits, where supported by strongly anomalous laterite geochemistry comparable to that of Golden Grove. We anticipate several drill targets to be refined from modeling of the VTEM data and follow- up ground EM.”

Wongan Hill Project - Aeromagnetics Image

Fig. 4. The approximate centre of the western CHI – 3 geochemical index anomaly is shown (yellow star) as is the approximate trend of the “Louise” geochemical anomaly (white arrow).

Fig. 5. Geological interpretation of the Wongan Hills greenstone belt and Cullen’s tenure

Fig. 5. Geological interpretation of the Wongan Hills greenstone belt and Cullen’s tenure – map modified from Karajas, J, 2005 – see References. Note that Caravel Minerals’ Calingiri Project, lies to the south where 250Mt @ 0.34% Cu (Consolidated Indicated and Inferred Resource Estimate at 0.25% cut-off) has been delineated (www.caravelminerals.com.au).

REFERENCES

  1. Cornelius, M., Robertson, I.D.M., Cornelius, A.J., and Morris, P.A., 2007. Laterite geochemical database for the western Yilgarn Craton, Western Australia: Western Australia Geological Survey, Record 2007/9, 44p.
  2. Smith, R.E., and Perdrix, J.L., 1983. Pisolitic laterite geochemistry in the Golden Grove, Massive Sulphide District, Western Australia.
    Journal of Geochemical Exploration, 18, 131-164.
  3. Karajas, J., 2005. Swancove Enterprises Pty Ltd. Combined annual mineral exploration report – E70-2437 and E/70-2443, Wongan Hills. For the Year to 14 January, 2005. WAMEX report A70056.
  4. Red River Resources Ltd, 2007. Partial Surrender Report E70/2437 & E70/2443 GSWA Ref No 12242, WAMEX report A74956.
  5. Smith, R.E., Birrell,R.D. , and Brigden,J.F., 1989: The implications to exploration of chalcophile corridors in the Archaean Yilgarn Block, Western Australia, as revealed by laterite geochemistry. In: Jenness et al. (Editors), Geochemical Exploration 1987, J Geochem . Explor., 312 : 169-184.

ASX: CUL Announcements

Quarterly Report to June 30 2018 (18-7-2018).
Further Geochemical Results (3-5-2018);
Quarterly Report to 31March 2018 (24-4-2018); and,
Quarterly Report to June 30 2017 (5-7-2017).

Note : The 2012 JORC Code Table 1 data has previously been presented in each of the abovementioned ASX announcements by Cullen for its laterite sampling, and is included herein for the 102 sample assays forming part of this report’s summary compilation, together with the relevant 2012 JORC Code Table 1 data for the geophysical survey.

ATTRIBUTION: Competent Person Statement

The information in this report that relates to exploration activities is based on information compiled by Dr. Chris Ringrose, Managing Director, Cullen Resources Limited who is a Member of the Australasian Institute of Mining and Metallurgy. Dr. Ringrose is a full-time employee of Cullen Resources Limited. He has sufficient experience which is relevant to the style of mineralisation and types of deposits under consideration, and to the activity which has been undertaken, to qualify as a Competent Person as defined by the 2012 edition of the “Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves”. Dr. Ringrose consents to the report being issued in the form and context in which it appears.

Information in this report may also reflect past exploration results, and Cullen’s assessment of exploration completed by past explorers, which has not been updated to comply with the JORC 2012 Code. The Company confirms it is not aware of any new information or data which materially affects the information included in this announcement.

FORWARD – LOOKING STATEMENTS

This document may contain certain forward-looking statements which have not been based solely on historical facts but rather on Cullen’s expectations about future events and on a number of assumptions which are subject to significant risks, uncertainties and contingencies many of which are outside the control of Cullen and its directors, officers and advisers. Forward-looking statements include, but are not necessarily limited to, statements concerning Cullen’s planned exploration program, strategies and objectives of management, anticipated dates and expected costs or outputs. When used in this document, words such as “could”, “plan”, “estimate” “expect”, “intend”, “may”, “potential”, “should” and similar expressions are forward-looking statements. Due care and attention has been taken in the preparation of this document and although Cullen believes that its expectations reflected in any forward looking statements made in this document are reasonable, no assurance can be given that actual results will be consistent with these forwardlooking statements. This document should not be relied upon as providing any recommendation or forecast by Cullen or its directors, officers or advisers. To the fullest extent permitted by law, no liability, however arising, will be accepted by Cullen or its directors, officers or advisers, as a result of any reliance upon any forward looking statement contained in this document.

ABOUT CULLEN: Cullen is a Perth-based minerals explorer with a multi-commodity portfolio including projects managed through a number of JVs with key partners (Fortescue, Hannans Reward, and Matsa) and a number of projects in its own right. The Company’s strategy is to identify and build targets based on data compilation, field reconnaissance and early-stage exploration, and to pursue further testing of targets itself or farm-out opportunities to larger companies. Projects are sought for most commodities mainly in Australia but with selected consideration of overseas opportunities.

REGISTERED OFFICE: Unit 4, 7 Hardy Street, South Perth WA 6151.
Telephone: +61 8 9474 5511
Facsimile:+61 8 9474 5588
CONTACT: Dr. Chris Ringrose, Managing Director.
E-mail: cringrose@cullenresources.com.au
www.cullenresources.com.au

Data description as required by the 2012 JORC Code – Section 1 and Section 2, Table 1 Laterite sampling at Wongan Hills – EL 70/4882 (Bureau Veritas, Laser Abalation)

Section 1 Sampling techniques and data

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

A total of 102 reconnaissance samples of lateritic residuum i.e. ferruginous gravel and ferruginous duricrust.

The VTEM survey was flown by UTS Geophysics Pty Ltd (266 line km on east-west lines spaced at 150m, with an EM sensor height of 30m) and was centred on the geochemical anomalies previously reported by Cullen.

Include reference to measures taken to ensure sample representivity and the appropriate calibration of any measurement tools or systems used Samples were handpicked of available material at surface and a handheld GPS was used to determine the sample locations. Coordinates are in grid GDA94 Z50
Aspects of the determination of mineralisation that are Material to the Public report Notes of colour, roundness, regolith setting and topography were made for each sample.
In cases where ‘industry standard’ work has been done this would be relatively simple (e.g. ‘reverse circulation drilling was used to obtain 1m samples from which 3kg was pulverised to produce a 30g 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 (eg submarine nodules) may warrant disclosure of detailed information. Samples were collected by hand from an area measuring approximately 5m x 5m. Where material is scarce, a larger area was sampled (10m x 10m) to obtain sufficient sample.
Drilling techniques Drill type (e.g. core, reverse circulation, open-hole hammer, rotary air blast, auger, Bangka, sonic etc.) and details (e.g. 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.). Not applicable – no drilling used
Drill Sample recovery Method of recording and assessing core and chip sample recoveries and results assessed Not applicable – no drilling used
Measurements taken to maximise sample recovery and ensure representative nature of the samples. Not applicable – no drilling used
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. Not applicable – no drilling used
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. Laterite samples were examined and described for all features and the geology, topography and surface type noted. Photographs were taken of sub-crop, landform and setting where appropriate.
Whether logging is qualitative or quantitative in nature. Core (or costean, channel etc) photography. Logging is qualitative only
The total length and percentage of the relevant intersections logged Not applicable – no drilling used
Sub-sampling techniques and sample preparation If core, whether cut or sawn and whether quarter, half or all core taken. No subsampling or sieving is done in the field. The total sample is submitted to the laboratory and all sample preparation is done there.
If non-core, whether riffles, tube sampled, rotary split, etc. and whether sampled wet or dry. All samples were collected dry by hand.
For all sample types, quality and appropriateness of the sample preparation technique. All sample preparation is carried out at Bureau Veritas (BV) laboratory and is considered appropriate and to industry standard, to the best of our knowledge.
Quality control procedures adopted for all sub-sampling stages to maximise representivity of samples. Laboratory international standards and duplicate splits were inserted by BV.
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. No field duplicates were collected.
Whether sample sizes are appropriate to the grain size of the material being sampled. Samples are considered adequate in size for the type of material sampled
The nature, quality and appropriateness of the assaying and laboratory procedures used and whether the technique is considered partial or total. The assaying is industry standard in quality and total, and appropriate for the objectives of the sampling. Laboratory QA/QC involves the use of internal lab standards using certified reference material, blanks, splits and duplicates. Samples were submitted to Bureau Veritas Minerals (BVM) in Perth sorted, dried and whole sample crushed and pulverize to 85% passing – 75μm. A barren flush was pulverised between each sample. The samples were analysed by laser ablation ICPMS using XRF beads. Gold and some other elements were analysed following an Aqua Regia digest.
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. Not applicable – no such instruments used in the field.
Quality of assay data and laboratory tests Nature of quality control procedures adopted (e.g. standards, blanks, duplicates, external laboratory checks) and whether acceptable levels of accuracy (i.e. lack of bias) and precision have been established. No control procedures or external checks done. Laboratory QA/QC involves the use of internal lab standards using certified reference material, blanks, splits and duplicates. Samples dried, pulverized with 85% passing -75μm established.
Verification of sampling and assaying The verification of significant intersections by either independent or alternative company personnel Not applicable – no drilling used
The use of twinned holes Not applicable – no drilling used
Documentation of primary data, data entry procedures, data verification, data storage (physically and electronic) protocols. Not applicable – no drilling used
Discuss any adjustment to assay data. Not applicable – no drilling used
Location of data points Accuracy and quality of surveys used to locate drill holes (collar and downhole surveys), trenches, mine workings and other locations used in Mineral Resources estimation. Samples located using a handheld GPS.
Specification of the grid system used. GDA94 Z50
Quality and adequacy of topographic control. No topographic control.
Data spacing and distribution Data spacing for reporting of Exploration Results. Samples are irregularly spaced and of a reconnaissance nature
Whether the data spacing and distribution is sufficient to establish the degree of geological and grade continuity appropriate for the Mineral Reserve and Ore Re4serve estimation procedure(s) and classifications applied. Not applicable – no drilling used
Whether sample compositing has been applied. No compositing applied.
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. Sampling is at a very early stage of exploration.
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. Not applicable – no drilling used
Sample security The measures taken to ensure sample security. All samples were collected, bagged and transported to the laboratory by Cullen staff and consultants.
Audits or reviews The results of and audits or reviews of sampling techniques and data. No reviews or audits of techniques and data.

Section 2 Reporting of exploration results

Type, reference name/number, location and ownership including agreements or material issues with third parties such as joint ventures, partnerships, overriding royalties, native title interest, historical sites, wilderness or national park and environmental settings. The samples were taken on E70/4882 which is held in the name of Cullen Exploration Pty Ltd. – 90%; and Tregor Pty Ltd -10%.
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. Tenement is approved with a heritage agreement in place with Native Title Party. The tenement includes private land and a compensation agreement will be required to be signed with key landowners to allow progress to any drill testing.
Exploration done by other parties Acknowledgement and appraisal of exploration by other parties. Previous work by others has included soil and laterite sampling and some drilling – as referenced in this report.
Geology Deposit type, geological settings and style of mineralisation The sampling targets Archaean volcanic hosted massive sulphide base metal deposits and gold deposits.
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:

  • Easting and northing of the drill hole collar
  • Elevation or RL (Reduced levelelevation above sea level in metres) and the drill hole collar
  • Dip and azimuth of the hole
  • Down hole length and interception depth Hole length
Not applicable – no drilling used
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. Not applicable – no drilling used
Data aggregation methods In reporting Exploration results, weighing 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. No averaging or aggregation techniques have been used. No top cuts and no metal equivalent values have been used in this report.
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. Not applicable – no drilling used
The assumptions used for any reporting of metal equivalent values should be clearly stated. Not applicable – no metal equivalent values have been used in this report.
Relationship between mineralisation widths and intercept lengths These relationships are particularly important in the reporting of Exploration Results. Not applicable – no drilling used
If the geometry of the mineralisation with respect to the drill hole angle is known, its nature should be reported. Not applicable – no drilling used
If it is not known and only the down hole lengths are reported, there should be a clear statement to this effect (e.g. ‘down hole length, true width not known’) Not applicable – no drilling used
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. Not applicable – a general location figure depicting the geological setting of the laterite anomalies is appropriate and included.
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. All relevant pathfinder elements of the whole sample suite are reported.
Other substantive exploration data 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 containing substances. From ground examination there does not appear to have been any previous drilling or exploration in the area of the historic geochemical anomaly reported in the YLA and referenced in this report, or in the western half of the EL.
Further work The nature and scale of planned further work (e.g. tests for lateral extensions or depth extensions or large-scale step-out drilling). Further programmes, including drilling, are anticipated and will be possible once the required land access agreements are in place and cropping is concluded this season.
Diagrams clearly highlighting the areas of possible extensions, including the main geological interpretations and future drilling areas, providing this information is not commercially sensitive. Figures included showing location and geological setting of the geochemical results and sampling. No drilling used.

TABLE 1 (following): Cullen Laterite samples – E70/4882

Note 1: The CHI – 6 and CHI – 3 geochemical indices are calculated for positive values only. Negative ones (below detection) were substituted with a half or a third the detection limit. 2: All values used for the indices with the exception of Se are based on the laser ablation/MS analyses. Selenium and gold analyses are by Aqua Regia/ICPMS. All values in ppm except for gold in ppb.

CHI – 6 = (As +3.65Sb+10Bi+3Mo+30Ag+30Sn+10W+3.5Se)

CHI – 3 = (As +3Sb+10Bi+10Cd+10In+3Mo+30Ag+30Sn)

The use of geochemical indices was discussed in Smith, R.E., and Perdrix, J.L., 1983 as a guide to interpretation.

Sample MGAz50 E MGAz50N Ag As Au Bi Cd Cu In Mo Sb Se Sn W Zn CHI-6 CHI-3
217040001 465311 6590699 0.2 19.6 3.6 0.6 0.05 54 0.35 2.4 1.4 0.5 2 1 35 116 107
217040002 464947 6590664 0.2 12 1.6 1.26 0.05 12 0.35 4.8 4.4 0.5 7.4 3.5 2.5 319 284
217040003 464927 6591077 0.1 14 0.2 0.74 0.05 30 0.3 4.6 3.5 0.5 6 1.5 10 247 232
217040004 464556 6591193 0 29 0 1 0 10 0.03 4 5 1 10 5 3 414 368
217040005 464556 6591193 0 21 1 1 0 16 0.03 6 6 1 12 7 10 514 441
217040006 464637 6591662 0.2 47.8 0.2 0.5 0.05 108 0.3 3.6 4.9 0.5 4.6 1.5 10 242 226
217040007 464637 6591662 0.2 38.6 0.2 0.42 0.05 82 0.35 2.6 4 0.5 3.4 2 10 195 175
217040008 464671 6592506 0 85 0 1 0 12 0.4 4 5 1 5 4 10 315 283
217040009 464671 6592506 0 349 5 0 0 76 0.45 3 5 1 2 2 10 471 451
217040010 465212 6592314 0.1 128 0.1 0.46 0.05 30 0.25 3.8 5.8 0.5 2.2 1 10 245 233
217040011 465526 6591910 0.05 69.6 0.1 0.76 0.05 22 0.25 3.6 3.2 0.5 2.4 1 2.5 185 174
217040012 465635 6591713 0.2 177 0.1 1.42 0.05 54 0.25 4.2 5.6 0.5 2.6 1.5 10 324 308
217040013 465341 6591210 0.2 10.6 0.6 0.46 0.05 20 0.2 4.4 3.3 0.5 4.6 2 2.5 206 185
217040014 465348 6590142 0.3 14.8 0.1 0.52 0.05 80 0.2 2.4 1.7 0.5 2.6 0.25 15 125 122
217040015 464235 6594173 0.1 24 1.4 0.56 0.05 242 0.1 1.6 1.9 0.5 3.4 1 20 158 147
217040016 463895 6593112 1.1 107 3.2 10.4 0.05 172 0.2 4.4 5.9 0.5 117 56.5 10 4355 3787
217040017 463895 6593112 0.2 149 2.2 5.44 0.05 370 0.15 3.2 4.5 0.5 68.2 32 25 2603 2281
217040018 463454 6592642 0.1 55 1.2 0.9 0.1 154 0.2 2.8 5.6 0.5 13 4.5 20 532 485
217040019 464881 6593972 0.1 62.4 0.4 0.94 0.1 56 0.25 2.6 2.2 0.5 4.4 4 10 264 225
217040020 465641 6594407 0.1 1050 2.8 2.5 0.05 200 0.3 5.4 5.7 0.5 4.2 3.5 35 1277 1241
217040021 463791 6593802 0.05 101 0.1 2.36 0.05 18 0.15 5.2 2.4 0.5 39.6 17.5 10 1515 1339
217040022 468230 6588326 0.2 22.6 0.1 0.2 0.1 28 0.3 2.8 1.4 0.5 2.6 2 15 144 125
217040023 465458 6588445 0.2 22.2 0.4 1.36 0.05 84 0.15 2.2 7.3 0.5 4.4 2 2.5 228 204
217040024 465285 6589198 0.1 19.8 0.6 1.56 0.05 62 0.15 2.8 3 0.5 8.2 3.5 15 340 304
217040025 463821 6590413 0.05 14 0.4 0.48 0.05 42 0.15 3.4 1.8 0.5 3.8 2 2.5 173 152
217040026 462429 6599412 0.05 15.2 0.1 0.4 0.3 12 0.25 6.2 0.6 0.5 3.2 2.5 10 164 143
217040027 467810 6604826 0.05 27.4 0.1 0.7 0.2 6 0.1 7.8 1.1 0.5 5.4 2.5 2.5 252 228
217040028 469391 6602712 0.05 20 0.1 0.34 0.2 42 0.2 3.6 0.7 0.5 5 1.5 2.5 205 192
217040029 462448 6601779 0.05 11.2 0.1 0.86 0.1 10 0.15 4.2 0.6 0.5 2.4 1.5 10 125 110
217040030 460330 6595438 0.05 24.2 0.1 0.26 0.05 1 0.1 5.2 0.6 0.5 2.4 1.5 2.5 135 119
217040032 467326 6588382 0.2 21 0.1 0.22 0.05 50 0.2 2.4 8.2 0.5 1.6 1.5 15 130 112
217040033 471061 6591776 0.05 32.2 0.1 0.38 0.2 4 0.2 6.2 1.2 0.5 4.4 1 2.5 204 196
213091451 464249 6593934 0.1 112 0.1 2.24 0.05 44 0.4 4.2 5.5 0.25 26.4 6 2.5 1022 963
213091452 464249 6593934 0.1 68.2 1.8 2.7 0.05 170 0.3 2.4 2.9 0.25 6.2 2 15 323 304
213091453 464388 6593919 0.2 130 0.1 1.7 0.05 52 0.3 3.8 4.4 0.25 17.2 9.5 2.5 792 697
213091454 464388 6593919 0.3 150 0.8 1.3 0.05 58 0.25 4.8 4 0.25 15.6 9.5 2.5 765 669
213091455 464453 6593499 0.6 57.2 0.1 0.4 0.05 382 0.2 2.4 4.1 0.25 2.8 1 15 196 185
213091456 464331 6593466 0.2 76.6 0.1 0.8 0.05 84 0.35 5.8 5 0.25 10.2 4.5 10 478 433
213091457 464331 6593466 0.1 43.8 1.8 0.7 0.05 64 0.3 3.2 2.3 0.25 5.2 3.5 15 263 230
213091458 464415 6593269 0.05 76.2 0.1 0.8 0.05 38 0.3 3.6 4.7 0.25 5.6 2.5 2.5 307 282
213091459 464415 6593269 0.2 189 0.1 1.1 0.05 94 0.3 7.2 6.2 0.25 10.4 3.5 10 598 562
213091460 464441 6593037 0.2 74.4 0.1 0.92 0.05 34 0.4 3.8 5.6 0.25 7.8 4.5 2.5 401 356
213091461 464441 6593037 0.2 48.2 3.2 0.82 0.05 32 0.3 3.8 5.9 0.25 8.8 5 2.5 410 359
213091462 463978 6593105 0.7 14.6 1.6 0.2 0.05 514 0.05 0.4 2.9 0.5 3.6 1 50 169 157
213091463 463919 6593131 1 25.6 5.2 0.42 0.05 270 0.025 0.8 0.8 0.5 4.2 6 645 253 191
213091464 463920 6593102 0.1 112 1.8 6.36 0.05 58 0.2 5.4 4.1 0.25 91.8 34.5 2.5 3309 2964
213091465 463869 6593056 0.2 184 18.6 13.3 0.05 126 0.25 2.6 2.8 0.25 36.8 13 2.5 1576 1446
213091466 463869 6593056 0.5 117 2.2 15.2 0.05 180 0.3 1.8 9.6 0.25 56.2 11.5 10 2125 2008
213091467 463984 6590355 0.05 7.8 0.1 0.34 0.05 32 0.25 3.8 1.2 0.25 5.6 3.5 2.5 232 199
213091468 463972 6592583 0.3 158 0.1 1.68 0.05 90 0.35 5.6 5.2 0.25 28.4 10.5 2.5 1177 1072
213091471 464243 6592257 0.2 46.2 3.6 0.56 0.05 226 0.2 2.8 7.8 0.25 6.4 2.5 20 312 284
213091472 464243 6592257 0.6 62 18.2 0.52 0.05 190 0.25 4.8 11.1 0.25 5.8 2 10 334 310
213091473 464209 6591220 0.3 25.4 0.1 0.98 0.05 138 0.2 2.6 4.5 0.25 8 2 20 329 308
213091474 464131 6590995 0.2 17.2 0.1 1.2 0.05 58 0.25 8 2.1 0.25 8 4.5 2.5 353 309
213091475 464131 6590995 0.5 23.2 0.1 0.78 0.05 64 0.3 5.8 2.9 0.25 7.2 3 10 321 292
213091477 464047 6591423 0.4 52.2 26.6 0.5 0.05 110 0.15 2.6 3.5 0.25 8.6 2.5 10 373 348
213091478 464103 6592072 0.4 37.8 5 2.8 0.05 82 0.2 2 4.5 0.25 14 3.5 2.5 556 520
213091479 464057 6592253 0.6 129 3.2 2.06 0.05 204 0.25 1.6 4.1 0.25 17 4.5 10 743 698
560151 463192 6592186 0.3 22.6 14.2 0.62 0.033 74 0.3 4.8 1.6 0.25 5.2 6.5 10 279 216
560152 463192 6592186 0.3 24.8 0.6 0.58 0.033 160 0.2 2.2 1.9 0.25 5 7.5 15 279 204
560153 462918 6591965 0.2 10 0.6 0.38 0.033 156 0.15 1.8 2.4 0.25 4.6 8 20 252 172
560154 463077 6591880 0.2 34.6 -0.2 0.86 0.2 136 0.3 5.8 3.1 0.25 8.6 19 35 526 339
560155 463077 6591880 0.2 39.6 2 0.94 0.033 50 0.3 7.6 3.4 0.25 8.2 8.5 -5 421 337
560156 463480 6591894 0.1 12 -0.2 1.86 0.033 50 0.45 4.4 1.3 0.25 8.8 7.5 40 391 320
560157 463943 6595147 0.033 9.4 4.8 0.88 0.033 28 0.25 4.8 2.5 0.25 6.4 15 -5 385 236
560158 463787 6595689 0.1 11.2 0.4 1.56 0.033 36 0.25 7.4 1.3 0.25 5.6 11 10 335 227
560159 465721 6596672 0.033 3.8 1.8 0.3 0.1 18 0.025 0.067 0.7 0.25 1 0.17 -5 43 41
560160 465753 6596632 0.3 55 7 0.4 0.033 94 0.25 2.2 2.3 0.25 1.6 2.5 20 156 132
560161 465753 6596632 0.5 80.6 2.2 0.34 0.033 76 0.25 2.8 3.2 0.25 1.8 3 15 203 174
560162 464292 6594342 0.2 74.8 3 0.42 0.033 72 0.4 3.2 1.7 0.25 2.4 1.5 -5 188 176
560163 465505 6593557 0.1 377 69.4 0.84 0.033 258 0.15 0.8 3.5 0.25 1.4 0.17 20 448 445
560164 465556 6593581 0.1 196 5.2 0.9 0.033 96 0.35 6.6 2.8 0.25 4.2 2 20 384 366
560165 466138 6595850 0.7 50.4 10.4 0.48 0.2 116 0.3 1.8 6.2 0.25 2.4 1 130 186 177
560166 466107 6596573 0.2 88.8 10 0.04 0.033 218 0.025 0.067 1 0.25 0.4 1 95 122 111
560167 464677 6595802 0.2 16 -0.2 1.14 0.033 130 0.4 3.8 1.1 0.25 3.6 3.5 15 192 160
560168 465115 6595615 0.1 8.6 11.6 0.64 0.033 60 0.3 3.2 1.6 0.25 3.8 4 10 188 150
560169 464490 6594507 0.2 206 0.4 0.8 0.033 22 0.35 5.8 4.1 0.25 5.6 3.5 -5 456 422
560170 464490 6594507 0.2 54.6 -0.2 0.5 0.033 116 0.3 2.2 1.8 0.25 2.8 1.5 15 178 165
560171 464814 6594149 0.2 29.4 -0.2 0.4 0.033 118 0.2 3.2 2.4 0.25 3.4 2.5 -5 185 161
560172 464814 6594149 0.1 45.8 -0.2 0.52 0.033 74 0.25 3 2.6 0.25 3.4 2.5 10 200 176
560173 465297 6594430 0.2 137 2.2 1.46 0.033 46 0.3 5.4 2.6 0.25 5.6 5.5 15 407 353
560174 465297 6594430 0.1 120 1 1.68 0.033 26 0.4 4.2 2.6 0.25 5.8 5 15 386 339
560175 465886 6595117 0.4 116 2 0.56 0.033 100 0.25 3.8 3.7 0.25 3 1.5 20 264 249
560176 465658 6595440 0.033 80.4 5.2 0.06 0.033 176 0.1 0.4 0.3 0.25 1 0.17 155 117 115
560177 464439 6594962 0.1 16 0.4 0.46 0.033 82 0.25 2.8 1.6 0.25 2.6 3.5 10 151 118
560178 464443 6594972 0.6 6.6 -0.2 0.26 0.033 278 0.2 0.6 1.6 0.25 1 1 20 75 66
560179 465397 6596190 0.4 17 33.4 0.18 0.033 226 0.25 2 1 0.25 1.4 0.17 10 85 85
560180 465820 6595740 0.2 16.2 61.8 0.26 0.8 112 0.3 3.4 1.1 0.25 2.8 1.5 -5 138 133
560181 465536 6595859 0.033 5.4 2 0.0067 0.033 1390 0.2 0.067 0.2 1 0.6 0.17 555 31 28
560182 465529 6595880 0.3 35.4 26.2 0.56 0.033 110 0.3 3.4 2.1 0.25 3.2 1.5 15 179 166
560183 465529 6595880 0.3 51.6 13.2 0.52 0.033 86 0.3 5 2.8 0.25 3.6 2 10 219 201
560184 464828 6595453 0.033 0.4 1.2 0.18 0.033 54 0.025 0.4 0.5 0.25 1 0.17 25 38 36
560185 464849 6595394 0.033 1.6 3 0.16 0.033 40 0.025 0.067 0.7 0.25 0.6 0.17 25 27 25
560186 464475 6595552 0.1 0.6 0.4 0.58 0.033 90 0.025 0.6 1.8 0.25 1.2 0.17 10 56 53
560187 462761 6591439 0.1 18 -0.2 1.02 0.033 18 0.25 6.8 1.8 0.25 6.4 8 -5 331 252
560188 462761 6591439 0.1 30.6 -0.2 0.74 0.033 16 0.25 10.4 2 0.25 6 8 10 340 261
560191 463915 6593144 0.033 90.4 1.2 3.38 0.1 36 0.2 10.6 9.3 0.25 56 19.5 -5 2066 1868
560194 463810 6592814 0.033 34.2 0.2 1.14 0.033 22 0.25 3.6 4.2 0.25 19 5.5 -5 698 643
560195 463744 6591658 0.033 13.8 0.2 0.42 0.033 22 0.2 4.2 2.1 0.25 6.2 5.5 -5 281 226
560196 463801 6592044 0.033 82 0.2 1.32 0.033 40 0.25 3.6 5.4 0.25 20.6 8 -5 825 744
560197 463830 6592198 0.2 61.8 0.2 1.18 0.033 60 0.2 2.8 3.6 0.25 12.2 4 -5 507 467
213091264 464973 6593870 0.2 178 3 0.88 0.033 50 0.25 3.2 2.6 0.25 2.4 2.5 10 309 285

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