Historic Surface Drilling Results on the Novales Zinc Trend
Released
Released
Announcement PDF
ASX Announcement | 11 May 2026
Variscan Mines Limited (ASX:VAR)
HIGH-GRADE HISTORIC SURFACE DRILLING RESULTS ON THE
NOVALES ZINC TREND
Highlights
• Recent exploration has focused on two historical mines; Emilia and Margarita, which
are situated 2.3 km North-East from the San Jose mine
• Acquisition of 109 historic drillholes for 6,720 metres, delivering multiple +20% zinc
(Zn) and lead (Pb) intercepts at the Emilia mine, including:
o S-37: 2.00m @ 11.29% Zn; 1.50m @ 6.27% Zn;
o S-50: 0.85m @ 23.47% Zn; 0.90m @ 17.43% Zn
o S-60: 1.50m @ 14.22% Zn; 3.00m @ 4.46% Zn
• High-grade sample results from drives and faces at the Emilia mine include:
o Sample Z-3: 2.85m @ 33.50% Zn, 0.52% Pb
o Sample Z-7: 2.75m @ 22.50% Zn, 0.31% Pb
o Sample Z-9B: 2.00m @ 28.00% Zn, 1.52% Pb
• High-grade sample results from drives and faces at the Margarita mine include:
o Sample D-M1: 3.55m @ 26.50% Zn, 2.99% Pb
o Sample D-M2: 3.85m @ 24.50% Zn, 11.76% Pb
o Sample D-M3: 3.30m @ 16.20% Zn, 14.07% Pb
Variscan Mines Limited (ASX:VAR) (“Variscan” or the “Company”) is pleased to publish previously
unreported assay results from historical underground drilling and face sampling at the former
producing Emilia and Margarita mines, situated within the Novales-Udias Project, located in
Cantabria, northern Spain.
• Newly acquired, historic drilling results and face samples are outside the current Mineral
Resource Estimate of the Novales-Udias Project supporting a larger, longer-term, district-scale
Zinc exploration and development opportunity along the ‘Novales Zinc Trend’
• 3D survey of underground workings at Emilia and Margarita also completed
• Newly integrated historic drilling data provides significant time and cost saving
• Project drilling database now consists of 1,484 drillholes for 113,733 m
• Total batch of 70 face samples compiled over distance of nearly 1 km
• Drilling results and sampling will support and guide the definition of high-priority targets for
forthcoming surface drilling over step-out areas to be conducted in 2026
2
Exploration Manager Dr Mike Mlynarczyk beside a large mineralised lens in the Emilia mine.
Acquisition of Historic Surface Drilling Data at the Emilia Mine
The Emilia Mine is located 2.3 km from the portal of the San Jose Mine,on the high-grade San Jose-Udias
zinc trend which runs SW-NE for over 12 km.
Variscan has conducted a thorough review of historical data at the School of Mines and Energy
Engineering at Torrelavega (University of Cantabria) and compiled an extensive batch of historical
underground drilling and face sampling assay results, which were subsequently surveyed in the field by
Variscan geologists and precisely located on the newly obtained high-resolution 3D laser surveys of the
Emilia and Margarita mine workings.
3
This newly documented area is mostly undeveloped, which is very promising considering that historical
drilling, as well as Variscan’s previously completed surface drilling in this area (refer ASX
Announcement 2 March 2023) has yielded significant zinc intercepts confirming the overall continuity
of mineralization along trend. The zinc-dominant character of mineralisation intercepted together with
the textures and geological structures observed underground confirm that this area is an integral part
of the San Jose-Udias mineral system. Importantly, this high-grade zinc mineralisation is very shallow,
occurring at depths between 0 and 105 m.
The area was intermittently explored by the Real Compania Asturiana de Minas (RCAM) from the late
1950s to the early 1980s. Variscan have compiled drill collar and assay data from historical drilling
conducted at the Emilia Mine between 1957-1962 by RCAM. Based on the historical records, it appears
that there were well in excess of one hundred underground holes drilled, however, the drill collar
records are incomplete and the assay data were only preserved for the “higher grade” mineralisation,
with low-grade and trace zinc assay results not located in the archives (see tables in Appendices 1 and
2).
There is evidence of limited mining operations within the historical mines targeting shallow zinc non-
sulphidemineralisation inthelate 19th
and early 20th
century.Historicalsources report adozenartisanal
mines, which Variscan has verified and located on the ground; all but Emilia and Margarita were very
small.
The acquisition of the historic drilling data saves significant time and financial resources for Variscan
and provides valuable data to support and guide future drilling programmes over these licence areas
more efficiently and effectively. The area in question straddles the San Jose mining permit and the
Buenahora and Esperanza exploration permits, all of which are in good standing.
4
Figure 1. Map of historical mines and historical surface drilling results reported along the north-east
extension of the Novales-Udias zinc trend overlain on Variscan Mines land tenure in Cantabria
(refer also ASX announcements 2 March 2023 and 16 September 2025).
Figure 2. Simplified geological cross-section showing connectivity and continuity between the San
Jose mine and the Margarita and Emilia mines to the northeast.
5
Figure 3. Plan view of historical underground drilling and face sampling results from the upper levels
of the Emilia mine.
High grade sampling results from the Emilia and Margarita Mines
Batches of 35 face sampling assay results dating from 1983 conducted by RCAM have been identified
for each of the Emilia and the Margarita mines. The underground Emilia and Margarita mines have both
recently been surveyed by Variscan with a high-resolution 3D laser. Drill collars and face samples were
inspected and located in situ. The inspection of historical drives and stopes confirm the past
exploitation of calamine ores and the presence of very high-grade zinc sulphide mineralisation, which
owing to the lack of suitable ore processing technology pre-1930 was subject to only very limited mining
activity.
Variscan is in the processof conducting its own channel sampling at the Emilia mine, in order to confirm
these excellent historical results.
6
Figure 4. Vertical section of the 3D laser survey model of the Emilia mine.
District Scale Opportunity
The Cantabria region is a proven multi-deposit zinc district. So-called ‘Mississippi Valley Type’ (MVT)
zinc-lead deposits usually occur in extensive districts consisting of several to as many as 400 deposits1.
The newly acquired drilling results add scale and upside with mineralisation identified stepping out
from the San Jose Mine in a northeasterly direction on the 12 km mineralised ‘Novales Zinc Trend’,
which hosts multiple zinc ore deposits.
This presents a district-scale advanced exploration and development opportunity over multiple mines
and proven mineralised areas which are typically high-grade, as well as very prospective under-
explored targets.
Future drilling will test step-out targets NE of San Jose Mine
The highly encouraging drilling and sampling data reported in this announcement is augmented by
historical surface drillhole data already compiled and reported by Variscan for the area north-east and
south-west of Novales.
The drilling and the sampling indicate that there is excellent continuity of mineralisation extending,
along strike, in a broad north-easterly direction from the San Jose mine for over 4 km and linking with
the Emilia and Margarita mines.
1
US Geological Survey (2010) ‘A Deposit Model for Mississippi Valley Type Lead-Zinc Ores’ Scientific Investigations Report 2010-5070-A
7
Figure 5. High-level plan view of future surface and underground drilling and survey priority areas.
The style of zinc mineralisation is identical to that found at the San Jose Mine and consists of multiple
stacked lenses of high-grade zinc sulphide mineralization that occur at a consistent elevation (i.e., with
very little vertical offset). Furthermore, the area hosts the thickest dolomitisation of the whole district
(200-350m in the vertical dimension) a feature that in most MVT zinc districts exhibits a strong positive
correlation with the grade and tonnage of associated zinc mineralisation, making it Variscan’s prime
exploration target for future drilling.
Variscan continues to acquire and review historic data to refine planning of the forthcoming surface
drilling in the area north-east of the San Jose mine, with drilling permits for the San Jose and Buenahora
mineral permits already in hand, and that for the Esperanza mineral permit being processed. This area
has not yet been drill-tested by Variscan and is expected to contribute significantly to the Project’s
growing Mineral Resource Estimate (MRE).
8
Next Steps & Way Forward
The San Jose/Novales-Udías Project continues to progress, with the following primary activities:
• Assay results from underground drilling
• Continuation of underground drilling program at Udias
• Development of an expanded Surface drilling program
ENDS
To ask questions directly to the Variscan management team and access media content, visit our
interactive investor website at: https://variscan.com.au/s/aa7e61
This ASX announcement has been approved by the Board and authorised for issue by Tony Wehby, Chairman,
Variscan Mines Limited
For further information, please contact:
Variscan Mines Limited (ASX:VAR)
Tony Wehby
Chairman
E: info@variscan.com.au
Media & Investor Enquiries
Jane Morgan Management
Chloe Hayes / Jane Morgan
E: chloe@janemorganmanagement.com.au / jm@janemorganmanagement.com.au
P: + 61 (0) 458619317/ +61 (0) 405 555 618
About Variscan Mines Limited (ASX:VAR)
To learn more, please visit: www.variscan.com.au
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9
Project Summary
The Novales-Udias Project is located in the Basque-Cantabrian Basin, some 30 km southwest from the regional
capital, Santander. The project is centred around the former producing San Jose underground mine with a large
surrounding area of brownfield exploration opportunities which include a number of satellite underground and
surface workings and areas of zinc anomalism identified from recent and historic geochemical surveys. Variscan
has delineated a significant 9km mineralised trend and a sub-parallel 3km trend from contemporary and historical
data across both the Buenahora exploration and Novales mining permits.
The San Jose Mine is nearby (~9 km) to the world class Reocin mine which is the largest known strata-bound
carbonate-hosted Zn-Pb deposit in Spain2
and one of the world’s richest MVT deposits3
. Further, it is within
trucking distance (~172 km) from the San Juan de Neiva zinc smelter operated by Asturiana de Zinc (100% owned
by Glencore). Significantly, the Novales-Udias Project includes a number of granted mining tenements4.
Figure 6. Map of Novales-Udias Project Licence areas.
2
Velasco, F., Herrero, J.M., Yusta, I., Alonso, J.A., Seebold, I. and Leach, D., (2003) ‘Geology and Geochemistry of the Reocin
Zinc-Lead Deposit, Basque-Cantabrian Basin, Northern Spain’ Econ. Geol. v.98, pp. 1371-1396.
3
Leach, D.L., Sangster, D.F., Kelley, K.D., Large, R.R., Garven, G., Allen, C.R., Gutzner, J., Walters, S., (2005) ‘Sediment-
hosted lead-zinc deposits: a global perspective’. Econ. Geol. 100th Anniversary Special Paper 561 607
4
Refer to ASX announcement of 29 July 2019
10
Figure 7. Map of Novales-Udias Project Licence areas and local infrastructure.
11
Mineral Resource Estimate for Novales-Udias Project
JORC Mineral Resource Estimate for San Jose mine and north-eastern Udías by deposit and
classification reported above at 2% Zn+Pb cut-off (ASX announcement 9 December 2024)
Competent Person Statement
The information in this document that relates to exploration results is based on and fairly represents information
and supporting documentation compiled and reviewed by Dr. Mike Mlynarczyk, Principal of the Redstone
Exploration Services, a geological consultancy acting as an external consultant for Variscan Mines. Dr. Mlynarczyk
is a Professional Geologist (PGeo) of the Institute of Geologists of Ireland, and European Geologist (EurGeol) of
the European Federation of Geologists, as well as Fellow of the Society of Economic Geologists (SEG). With over
14 years of full-time exploration experience in MVT-style zinc-lead systems in several of the world’s leading MVT
provinces, Dr. Mlynarczyk has sufficient experience which is 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 December 2012 edition of the “Australasian Code for Reporting of Exploration Results, Mineral
Resources and Ore Reserves” (‘JORC Code’). Dr. Mlynarczyk consents to the inclusion in the report of the matters
based upon the information in the form and context in which it appears.
Where reference is made to previous releases of exploration results and mineral resource estimates in this
announcement, the Company confirms that it is not aware of any new information or data that materially affects
the information included in those announcements and all material assumptions and technical parameters
underpinning the exploration results and mineral resource estimates included in those announcements continue
to apply and have not materially changed.
Where information in this document relates to previous exploration results that was prepared pre-2012 JORC
code. It is the opinion of Variscan that the exploration data is reliable. Although some of the data is incomplete,
nothing has come to the attention of Variscan that causes it to question the accuracy or reliability of the historic
exploration.
Forward Looking Statements
Forward-looking statements are only predictions and are not guaranteed. They are subject to known and unknown
risks, uncertainties and assumptions, some of which are outside the control of the Company. Past performance
is not necessarily a guide to future performance and no representation or warranty is made as to the likelihood of
achievement or reasonableness of any forward-looking statements or other forecast. The occurrence of events in
the future are subject to risks, uncertainties and other factors that may cause the Company’s actual results,
performance or achievements to differ from those referred to in this announcement. Given these uncertainties,
recipients are cautioned not to place reliance on forward looking statements. Any forward-looking statements in
this announcement speak only at the date of issue of this announcement. Subject to any continuing obligations
under applicable law and the ASX Listing Rules, the Company, its directors, officers, employees and agents do
not give any assurance or guarantee that the occurrence of the events referred to in this announcement will occur
as contemplated.
12
JORC Table 1, Sections 1 and 2
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
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
representativity and the
appropriate calibration of any
measurement tools or systems
used.
• Aspects of the determination of
mineralisation that are Material
to the Public News release.
• In cases where ‘industry
standard’ work has been done
this would be relatively simple
(e.g., ‘reverse circulation 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 sample data referenced in this report relates to
historical exploration undertaken by Real Compania
Asturiana de Minas (RCAM) – one of the mining companies
operating the Project from 1855 till 1983, when it was taken
over by Asturiana de Zinc SA (AZSA) - previously a
subsidiary of Xstrata / Glencore.
• The historical underground drilling was conducted in 1957-
1962, whereas the face sampling was conducted in 1983
(the year of change in project ownership), and the data in
paper format is held at the School of Mines and Energy
Engineering at Torrelavega, a faculty of the University of
Cantabria. No drill core has been preserved.
• The underground drilling is understood to have been core
drilling, with assaying conducted at RCAM´s in-house
laboratory in Torres, but it is not known whether full core or
half core was assayed. It has been assumed that all
reported assays are representative of technology available
at the time, but no reliance has been put on it.
• Based on historical records, the number of holes drilled at
the Emilia mine exceeds one hundred, however only assay
data for the “better mineralized” holes have been
preserved in the archives, with low-grade and trace zinc /
barren assay results missing from the records. Appendix 1
lists drill collar data and Appendix 2 lists all of the available
assay results.
• Due to the incomplete nature of the historic drill data and
records, including procedures, a comment on the samples’
representability or calibration of measurement tools or
systems used by historic workers cannot be made. Further
comment regarding specific components of the historic
drilling is provided in subsequent sections of this table. The
data cannot be considered ‘industry standard’ by modern
standards.
• The underground “face sampling” consisted of a manual
collection of rock chips along vertical profiles in the walls
of the galleries and stopes of the Emilia and Margarita
mines, ranging in length between 28 cm and 3.85 m
(average 2.0 m). The sampling was similar to vertical
channel sampling, yet the rock chips were not taken
continuously along the profile but from multiple spots
separated by distances in the order of 10-30cm, and the
given profile length corresponds to the distance between
the top and bottom sampling spots.
13
Criteria JORC Code explanation Commentary
• Based on the physical review of the underground sampling
sites these cannot be considered “true” channel samples
and do not fulfil the present-day industry standard
requirements for systematic sampling. Nevertheless, they
provide very useful, semi-quantitative information on grade
distribution over wide areas of the Emilia and Margarita
mines.
• The sampling sites were marked on the mine walls with
yellow paint, highlighting the location of the sampling
profiles and the sample number, and they were reported on
detailed mine plans available in paper format. A
representative number of sampling sites was checked in
situ and was found to visually match the metal grades
listed in the historical records, both in terms of zinc versus
lead content and in terms of sulphide versus non-sulphide
mineralogy.
• A total of 66 face samples are listed in Appendices 3
(Emilia mine) and 4 (Margarita mine), and the bulk of them
have assay data for zinc (sulphide), lead (sulphide), as well
as zinc and lead in non-sulphide (‘oxide’) form. The ‘zinc
meters-%’ column was added by Variscan Mines, solely as
a means of assessing the spatial variation of zinc grade in a
very approximative manner, and should ‘not’ be relied on,
as these were not ‘true’ channel samples.
• Due to the incomplete nature of the historical sampling
methodology and historical records, including details of
the procedures implemented and QAQC control, a
comment on sample representativeness or calibration of
measurement systems used by historical workers cannot
be made. The historical data cannot be considered JORC-
compliant nor ‘industry standard’ by modern standards. It
has been assumed that the assays are representative of
technology available at the time, but no reliance has been
put on it.
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).
• The historic underground drilling reported here is
understood to be all core drilling. No details of the drilling
techniques employed have been identified in the historic
data. This includes reference to core diameter, core
orientation methods, nor downhole survey data.
• Historical drilling referenced within this document refers to
109 underground drillholes from between 1957 and 1962.
• It is assumed that no core orientation has taken place for
these holes as no structural data exists in the core logs. No
records of the type of drill rig used have been identified.
14
Criteria JORC Code explanation Commentary
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.
• No records of core recovery have been identified from the
historic data. Given the absence of core recovery data nor
the actual physical drill core, it is not possible to assess
the potential of a relationship between sample recovery
and grade.
• The absence of drill recovery data means that reported
grades may be subject to either over or underreporting. No
assessment or estimation of these effects has been made
due to the lack of data.
• Face samples collected at the Emilia and Margarita mines
have had no recovery recorded, moreover, the rock chips
were not taken continuously along the vertical sampling
profiles but from multiple spots separated by distances in
the order of 10-30cm, and the given profile lengths
correspond to the distance between the top and bottom
sampling spots. Therefore, these are not “actual” channel
samples and only give a semi-quantitative assessment of
zinc and lead distribution along both mines.
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 historical logs available for the underground drillholes
are very basic, presumably prepared by the drillers and not
geologists. No geotechnical logs have been identified. In
the absence of detailed data, no comment on whether the
logging, where observed, is qualitative or quantitative has
be made. No core photography has been identified.
• Of the 109 underground drillholes reported, only 55 have
complete drill collar data and of them only 16 have assay
data, which are limited to “higher grade” intervals, with
low-grade and trace zinc / barren assay results missing
from the records.
• Regarding face samples, no geological sample
descriptions have been identified in the historical records,
but in-situ visual inspection of selected sampling profiles
matches well the mineralogy and metal grades reported.
No logging has taken place along the vertical profiles of
face sampling. Only sample intervals were recorded, with
the profile lengths corresponding to the distance between
the top and bottom sampling spots.
Sub-
sampling
techniques
and sample
preparation
• If core, whether cut or sawn and
whether quarter, half or all core
taken.
• If non-core, whether riffled,
tube sampled, rotary split, etc.
• Historic approach to sampling drill core appears selective,
guided by geological observation, and no “apparent” waste
was sampled (or the records were not preserved). No
details of the sub-sampling or sample preparation
techniques have been identified from the historic records,
and no supporting sampling procedures have been
identified. It is not known whether half core or whole core
15
Criteria JORC Code explanation Commentary
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
representativity 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.
was submitted for analysis. In the absence of this data and
other data related to the sub-sampling techniques and
sample preparation, one cannot comment on the
appropriateness of the sample preparation techniques.
• No evidence of Quality Control procedures nor results have
been identified for the historical drilling campaign. This
includes evidence of field duplicates or other current
industry standard quality control procedures, such as
Certified Reference Materials and blanks.
• In the absence of sample size data, no comment on
whether the sample size is appropriate to the grain size of
the sampled material can been made.
• The historical approach to face sampling cannot be
considered ‘industry standard’ by modern standards as the
full length of the sampling profiles had not been sampled,
instead focusing on a succession of multiple sampling
spots, from which larger rock chips were taken. Therefore,
there is significant uncertainty over sampling
representativeness and any possible bias, and the assay
data are semi-quantitative at most and cannot be relied
upon.
• No details of the sample preparation techniques, sampling
procedures, and QAQC measures have been identified so
far in the historical records pertaining to the face sampling
campaign.
Quality of
assay data
and
laboratory
tests
• 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
• No details of Quality Control procedures (such as
duplicates, Certified Reference Materials and blanks) and
whether they were used at the time of drilling or face
sampling have been identified from the historical records,
and no supporting sampling procedures have been
identified. It is inferred that the techniques used were total
and representative of technology available in the late
1950s to early 1980s. No comment can be made on
whether acceptable accuracy or precision of results have
been established.
16
Criteria JORC Code explanation Commentary
accuracy (ie lack of bias) and
precision have been
established.
Verification
of sampling
and assaying
• 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.
• Due to the historical nature of the results reported and the
lack of preserved drill core, it has not been possible to
verify significant drilling intersections. It is not known
whether verification of intersections was undertaken by
previous operators at the time of drilling.
• The historical data does not include any twinned holes. It
is understood that Variscan may consider twinning historic
drill holes as part of the company’s upcoming exploration
plans.
• No documentation or records of primary data, data entry
procedures, data verification, data storage (physical and
electronic) protocols have been identified.
• Historic records consist solely of handwritten drillhole
summaries. This data was identified and transcribed to
Microsoft Excel © and then imported into Leapfrog Geo for
drill hole database validation, significant intersections, and
3D viewing. Variscan intend to transfer this data to an
industry standard drillhole database during the ongoing
exploration on the project.
• Given the absence of detailed historical information
relating to the assay data, no adjustment to the assay data
has been made. The data has been reported as it was
recorded in the original documentation. Variscan have no
reason to disbelieve the data as presented in the historical
drill logs, however, understand the limitations of the data
for use in reliable and classified mineral resource
estimations going forward until assay verification has been
achieved to a satisfactory standard.
• A representative selection of historical face sampling sites
has been reviewed in situ by Variscan Mines geologists and
found to visually match the metal grades listed in the
historical records, both in terms of zinc versus lead
content, and in terms of sulphide versus non-sulphide
mineralogy.
• Full verification of the sampling representativeness would
require executing proper channel sampling at the locations
of historical sampling profiles, an exercise that is being
planned and will supersede historical data but has not yet
been carried out. The principal uncertainty at this stage
regards sample representativ
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