CASCATA- POTENZIELLE ENTDECKUNG VON VULKANOGENEM MASSIVSULFID

^
DGAP-News: Conico Ltd. / Schlagwort(e): Sonstiges
CASCATA- POTENZIELLE ENTDECKUNG VON VULKANOGENEM MASSIVSULFID (News mit
Zusatzmaterial)

31.08.2021 / 10:01
Für den Inhalt der Mitteilung ist der Emittent / Herausgeber verantwortlich.

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ACN 119 057 457, AUSTRALIAN SECURITIES EXCHANGE ANNOUNCEMENT, 31 August 2021

HIGHLIGHTS

- Das Prospektionsgebiet Cascata ist eine neue Entdeckung, bei der es sich
wahrscheinlich um vulkanogenes Massivsulfid (VMS) handelt. Auf einer
Streichenlänge von über 6 km wurden durchgängig Sulfide an der Oberfläche
entdeckt. Das interessierende Gebiet ist etwa 15 km2 groß und liegt
vollständig innerhalb der bestehenden Ryberg-Lizenz des Unternehmens. Mit
den Bohrungen wurde begonnen.

- SODD003 (Sortekap-Prospekt) ist abgeschlossen und durchteufte auf 78 m
aussichtsreiche Quarzadern mit Sulfidmineralisierung innerhalb von
Amphibolit. Das Ziel ist Gold, wobei frühere Oberflächenproben in der Nähe
einen Gehalt von bis zu 2,7 g/t Gold aufweisen.

- SODD002 (Sortekap-Prospekt) ist abgeschlossen und durchteufte ~6%
vereinzeltes Chalkopyrit + Pyrrhotit über 7,1m aus 188,5m Bohrlochtiefe. Es
wurden auch Zonen mit vereinzeltem Pyrit angetroffen.

- 1 x Bohrgerät wurde zu einem elektromagnetischen Ziel auf dem
Miki-Prospekt mobilisiert

Conico Limited (ASX: CNJ) ("Conico" oder "das Unternehmen") und seine
hundertprozentige Tochtergesellschaft Longland Resources Ltd ("Longland")
freuen sich bekannt zu geben, dass eine neue Entdeckung, die als
wahrscheinliches vulkanogenes Massivsulfid (VMS) interpretiert wird,
entdeckt wurde und eine Bohrung begonnen hat. Die Bohrungen SODD002 und
SODD003 wurden bei Sortekap und die Bohrung MIDD008 auf dem Miki-Prospekt
abgeschlossen.

Thomas Abraham-James, CEO von Longland, sagte:

"Die Entdeckung eines potenziellen neuen VMS-Vorkommens bei Cascata ist ein
typisches Beispiel dafür wie chancenreich die Exploration in Grönland ist.
Unser Team hat mehr als 6 km des Streichens zu Fuß abgewandert, wobei
Lithologien mit Aussicht auf VMS und eine konsistente Sulfidmineralisierung
beobachtet wurden, was eine sofortige Bohrung rechtfertigt. In der
Zwischenzeit sehen wir weiterhin Mineralisierungen in den Bohrlöchern bei
Miki und Sortekap."
Das neu entdeckte Prospektionsgebiet Cascata

Im Rahmen der Erkundungsexploration wurden auffällige Kupfer- und
Eisensulfide identifiziert, die als Cascata-Prospekt bezeichnet werden
(Abbildung 1). Die Mineralisierung liegt in Form von Pyrit, Chalkopyrit und
Bornit in massiven, halbmassiven, stockförmigen und vereinzelten Formen vor
und steht in Zusammenhang mit Schwarzschiefer, rhyolitischem Vulkanismus und
darunter liegendem Amphibolit (Abbildungen 2-7). Die bisher durchgeführten
Felduntersuchungen deuten darauf hin, dass es sich bei Cascata
möglicherweise um ein vulkanogenes Massivsulfidvorkommen (VMS) handelt,
wobei eine Streichenlänge von mehr als 6 km zu Fuß abgeschritten wurde und
ein Gebiet von Interesse von ~15 km2 identifiziert wurde.

Die Bohrungen bei Cascata haben begonnen und befinden sich am oberen Ende
der Stratigraphie. Das Projekt befindet sich innerhalb der bestehenden
Ryberg-Lizenz und ist leicht zugänglich, nur 6 km von der Küste entfernt und
verfügt über reichlich Süßwasserquellen.

Prospektionsgebiet Sortekap: Bohrloch SODD003

Das Bohrloch SODD003 zielte auf eine Goldmineralisierung in Amphibolit
(Abbildung 9) ab und wurde so positioniert, dass es senkrecht zu Quarzadern
gebohrt wurde, in denen frühere Oberflächenproben Gehalte von bis zu 2,7 g/t
Gold ergaben.

Das Bohrloch durchteufte erfolgreich 78 m aussichtsreichen quarzhaltigen
Amphibolit, beginnend an der Oberfläche (Abbildung 8). Die Quarzadern
enthielten häufig Spurensulfide bzw. disseminierte Sulfide, was insofern
ermutigend ist, als die veröffentlichte Literatur über die Goldvorkommen bei
Sortekap besagt, dass die Goldmineralisierung mit dem Vorhandensein von
Spurensulfiden (insbesondere Arsenopyrit) im Amphibolit in Zusammenhang
steht. Die angetroffenen Sulfide umfassen Arsenopyrit in Verbindung mit
Pyrit und Chalkopyrit (Abbildungen 10-11).

Das Bohrloch wurde im Serpentinit beendet und das Bohrgerät wurde inzwischen
zum nächsten Bohrloch auf dem Miki-Prospekt verlegt, um eine
elektromagnetische (EM) Anomalie zu erbohren, die bei der EM-Untersuchung
2020 identifiziert wurde.

Prospektionsgebiet Sortekap: Bohrung SODD002

Das Bohrloch SODD002 befand sich im Sortekap-Prospekt und zielte auf eine
aufladbare Anomalie durch induzierte Polarisation (IP) ab. Das Bohrloch
durchteufte erfolgreich eine Sulfidmineralisierung über mehrere Abschnitte,
wobei der bedeutendste Abschnitt 7,1 m lang ist, der bei 188,5 m
Bohrlochtiefe beginnt und aus ~6 % verstreutem Chalkopyrit und Pyrrhotit
besteht. Tiefer im Bohrloch gibt es Zonen mit bis zu 20 % verstreutem Pyrit
(Abbildung 12).
Die Bohrung wurde auf eine Gesamttiefe von 356 m verlängert, um den in
Bohrung SODD001 entdeckten Serpentinit zu durchteufen. Dadurch wird die
Geologie der beiden Sortekap-Bohrungen miteinander verknüpft, was zu einem
besseren Verständnis der regionalen Stratigraphie führt.

Miki Prospektionsgebiet: Bohrung MIDD008

Dieses Bohrloch zielte auf magmatische Sulfide ab, die mit dem Miki Fjord
Macrodyke verbunden sind (Abbildung 16). Von 78,9 m bis zum Ende des
Bohrlochs (312 m) durchteufte MIDD008 eine
Quarz-Kalifeldspat-Glimmer-Assemblage (Abbildungen 13 bis 14), die Adern mit
Molybdänit (zwischen 1 und 2 %, wenn sie angetroffen wurde) und Spuren von
Chalkopyrit (~ 2 %, wenn sie angetroffen wurde, Abbildung 15) enthält.

Die Entdeckung einer solchen Mineralisierung ist unerwartet, aber nicht
überraschend, wenn man die Nähe zu bekannten Systemen wie dem 38 km westlich
gelegenen Porphyr-Molybdän-Projekt Flammefjeld bedenkt.

Das Bohrloch wurde in 312 m Bohrtiefe beendet, als es sich noch im
alterierten Gestein befand, und das Bohrgerät wurde zum Prospektionsgebiet
Cascata umdisponiert.

Im Auftrag des Vorstandes.

/
Guy T Le Page, FFIN, MAusIMM
Executive Director

COMPETENT PERSONS STATEMENT

The information contained in this report relating to exploration results
relates to information compiled or reviewed by Thomas Abraham-James, a
full-time employee of Longland Resources Ltd. Mr. Abraham-James has a B.Sc.
Hons (Geol) and is a Chartered Professional (CPGeo) and Fellow of the
Australasian Institute of Mining and Metallurgy (FAusIMM). Mr. Abraham-James
has sufficient experience of relevance to the styles of mineralisation and
the types of deposit under consideration, and to the activities undertaken
to qualify as a Competent Person as defined in the 2012 edition of the Joint
Ore Reserve Committee (JORC) "Australasian Code for Reporting of Exploration
Results, Mineral Resources and Ore Reserves". Mr. Abraham-James consents to
the inclusion in this report of the matters based on information in the form
and context in which it appears.

FORWARD-LOOKING STATEMENTS

This announcement contains forward-looking statements that involve a number
of risks and uncertainties. These forward-looking statements are expressed
in good faith and believed to have a reasonable basis. These statements
reflect current expectations, intentions or strategies regarding the future
and assumptions based on currently available information. Should one or more
of the risks or uncertainties materialise, or should underlying assumptions
prove incorrect, actual results may vary from the expectations, intentions
and strategies described in this announcement. No obligation is assumed to
update forward-looking statements if these beliefs, opinions and estimates
should change or to reflect other future developments.

Annex 1

    Hole ID Easting Northing  Elevation Dip Azimuth Length
    MIDD001 565,714 7,571,884   298m    -80   215   217.0m
    MIDD002 565,840 7,571,990   312m    -80   355   313.5m
    MIDD003 565,734 7,571,883   298m    -80   215   180.0m
    MIDD004 565,715 7,571,897   299m    -80   290   36.0m
    MIDD005 565,797 7,571,960   311m    -70   285   381.0m
    MIDD006 565,728 7,571,889   298m    -75   290   153.0m
    MIDD007 566,497 7,573,151   386m    -70   290   278.0m
    MIDD008 566,880 7,573,889   567m    -80   290   312.0m
    MIDD009 565,910 7,571,891   318m    -90   000    N/A
    SODD001 567,481 7,601,155  1,319m   -80   355   287.0m
    SODD002 567,518 7,600,827  1,240m   -85   095   356.0m
    SODD003 567,496 7,600,712  1,203m   -70   290   117.0m
    CADD001 593,237 7,585,297   795m    -70   290    N/A
All coordinates are displayed in WGS84 UTM Zone 25N

Annex 2

JORC Code, 2012 Edition
Section 1: Sampling Techniques and Data

   Cri-    JORC Code Explanation              Commentary
   te-
   ria
   Sam-    Nature and quality of sampling     * Sampling of MIDD008,
   pli-    (e.g., cut channels, random        SODD002 & SODD003 was
   ng      chips, or specific specialised     conducted using standard
   tec-    industry standard measurement      industry practices with
   hni-    tools appropriate to the           diamond drilling. Magnetic
   que-    minerals under investigation,      readings were taken using a
   s       such as down hole gamma sondes,    Reflex EZ-Trac downhole
           or handheld XRF instruments,       survey tool.
           etc.). These examples should
           not be taken as limiting the
           broad meaning of sampling.
           Include reference to measures      * Drill-holes MIDD008,
           taken to ensure sample             SODD002 & SODD003 were angled
           representivity and the             to optimally intersect the
           appropriate calibration of any     interpreted contact with an
           measurement tools or systems       IP conductor or adjacent to
           used.                              lithologies of interest.
           Aspects of the determination of    * Mineralisation in
           mineralisation that are            drill-holes MIDD008, SODD002
           Material to the Public Report.     & SODD003 has not been
           In cases where 'industry           quantitively determined and
           standard' work has been done       is awaiting assay. The
           this would be relatively simple    determination in this report
           (e.g., 'reverse circulation        is qualitative, based on
           drilling was used to obtain 1 m    visual observation made by
           samples from which 3 kg was        the Competent Person who is a
           pulverised to produce a 30 g       geologist on site.
           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.
   Dri-    Drill type (e.g., core, reverse    * Wireline diamond drilling
   lli-    circulation, open-hole hammer,     using a 56.5mm diameter drill
   ng      rotary air blast, auger,           bit and standard tube. The
   tec-    Bangka, sonic, etc) and details    core has not been orientated
   hni-    (e.g., core diameter, triple or    but has been surveyed using a
   que-    standard tube, depth of diamond    Reflex EZ-Trac multi-shot
   s       tails, face-sampling bit or        tool. The drill rig is a CDI
           other type, whether core is        500 heli-portable fly rig
           oriented and if so, by what        operated by Cartwright
           method, etc.).                     Drilling Inc.
   Dri-    Method of recording and            * All drill core has been
   ll      assessing core and chip sample     geotechnically logged with
   sam-    recoveries and results             core recovery measured per
   ple     assessed.                          drill core run (3m).
   re-
   co-
   ve-
   ry
           Measures taken to maximise         * The drill crew was notified
           sample recovery and ensure         of the target depth and
           representative nature of the       likelihood of intersecting
           samples.                           sulphides, accordingly they
                                              eased pressure on the drill
                                              bit from that depth onward to
                                              minimise the chance of core
                                              destruction. All drill core
                                              was then placed in trays with
                                              lids to ensure that no core
                                              was lost during
                                              transportation from the drill
                                              site to core logging
                                              facility. The drill core was
                                              then reconstructed into
                                              continuous runs on an angle
                                              iron cradle by the geologist.
                                              Depths were checked against
                                              depths indicated on the core
                                              blocks.
           Whether a relationship exists      * Not applicable as no assays
           between sample recovery and        have been conducted to date.
           grade and whether sample bias
           may have occurred due to
           preferential loss/gain of
           fine/coarse material.
   Log-    Whether core and chip samples      * All drill core has been
   gin-    have been geologically and         geologically and
   g       geotechnically logged to a         geotechnically logged by a
           level of detail to support         qualified geologist to a
           appropriate Mineral Resource       level of detail that supports
           estimation, mining studies and     appropriate Mineral Resource
           metallurgical studies.             estimation, mining studies
                                              and metallurgical studies.
           Whether logging is qualitative     * The logging is qualitative.
           or quantitative in nature. Core    All drill core was
           (or costean, channel, etc.)        photographed.
           photography.
           The total length and percentage    * Drill-holes MIDD008,
           of the relevant intersections      SODD002 & SODD003 have been
           logged.                            logged in full.
   Sub-    If core, whether cut or sawn       * No sampling has been
   -sa-    and whether quarter, half or       undertaken.
   mp-     all core taken.
   lin-
   g
   tec-
   hni-
   que-
   s
   and
   sam-
   ple
   pre-
   pa-
   ra-
   ti-
   on
           If non-core, whether riffled,      * Not applicable as the
           tube sampled, rotary split, etc    drill-hole is core.
           and whether sampled wet or dry.
           For all sample types, the          * Not applicable as no
           nature, quality and                sampling has been undertaken.
           appropriateness of the sample
           preparation technique.
           Quality control procedures         * Not applicable as no
           adopted for all sub-sampling       sampling has been undertaken.
           stages to maximise
           representivity of samples.
           Measures taken to ensure that      * Not applicable as no
           the sampling is representative     sampling has been undertaken.
           of the in-situ material
           collected, including for
           instance results for field
           duplicate/second-half sampling.
           Whether sample sizes are           * Not applicable as no
           appropriate to the grain size      sampling has been undertaken.
           of the material being sampled.
   Qua-    The nature, quality and            * Not applicable as no
   li-     appropriateness of the assaying    assaying has occurred.
   ty      and laboratory procedures used
   of      and whether the technique is
   ass-    considered partial or total.
   ay
   da-
   ta
   and
   la-
   bo-
   ra-
   to-
   ry
   tes-
   ts
           For geophysical tools,             * Downhole magnetic readings
           spectrometers, handheld XRF        were taken using a Reflex
           instruments, etc., the             EZ-Trac. Readings were taken
           parameters used in determining     every 3m at completion of
           the analysis including             drilling, with the survey
           instrument make and model,         beginning at bottom of hole
           reading times, calibrations        and working up. The tool
           factors applied and their          protruded beyond the drill
           derivation, etc.                   string by 3m to ensure no
                                              interference from the rods.
                                              The magnetic roll is 0 to 360
                                              with an accuracy of ±0.35 .
                                              The magnetic range is 0 to
                                              100,000 nT with an accuracy
                                              of ±50 nT.
           Nature of quality control          * Not applicable as no
           procedures adopted (e.g.,          sampling or assaying has
           standards, blanks, duplicates,     occurred.
           external laboratory checks) and
           whether acceptable levels of
           accuracy (i.e., lack of bias)
           and precision have been
           established.
   Ve-     The verification of significant    * Consultants utilised by the
   ri-     intersections by either            Company have verified the
   fi-     independent or alternative         findings of the on-site
   ca-     company personnel.                 geologists.
   ti-
   on
   of
   sam-
   pli-
   ng
   and
   ass-
   ay-
   ing
           The use of twinned holes.          * Not applicable as no
                                              twinned holes have been
                                              drilled.
           Documentation of primary data,     * All logging data was
           data entry procedures, data        entered into a computer on
           verification, data storage         site, with daily backups
           (physical and electronic)          taken and stored on hard
           protocols.                         drives and the cloud.
           Discuss any adjustment to assay    * Not applicable as no
           data.                              assaying has occurred.
   Lo-     Accuracy and quality of surveys    * Drill-holes MIDD008,
   ca-     used to locate drill holes         SODD002 & SODD003 were
   ti-     (collar and down-hole surveys),    located using a handheld
   on      trenches, mine workings and        Garmin GPS with an accuracy
   of      other locations used in Mineral    of ±4m.
   da-     Resource estimation.
   ta
   poi-
   nts
           Specification of the grid          * UTM WGS84 Zone 25N.
           system used.
           Quality and adequacy of            * Topographic information was
           topographic control.               sourced from the Greenland
                                              Mapping Project (GIMP)
                                              digital elevation model (30m
                                              accuracy).
   Da-     Data spacing for reporting of      * Not applicable as the
   ta      Exploration Results.               drill-holes are targeting
   spa-                                       specific geological and IP
   cin-                                       targets.
   g
   and
   dis-
   tri-
   bu-
   ti-
   on
           Whether the data spacing, and      * Not applicable as the
           distribution is sufficient to      drill-holes are targeting
           establish the degree of            specific geological and IP
           geological and grade continuity    targets.
           appropriate for the Mineral
           Resource and Ore Reserve
           estimation procedure(s) and
           classifications applied.
           Whether sample compositing has     * Not applicable as no
           been applied.                      sampling has occurred.
   Ori-    Whether the orientation of         * The strike and dip of
   ent-    sampling achieves unbiased         drill-holes MIDD008, SODD002
   ati-    sampling of possible structures    & SODD003 were designed to
   on      and the extent to which this is    intersect an IP
   of      known, considering the deposit     target/lithological unit at
   da-     type.                              an adjacent angle, not along
   ta                                         strike. Therefore, the
   in                                         sampling conducted by the
   re-                                        drill-hole is considered
   la-                                        unbiased.
   ti-
   on
   to
   geo-
   lo-
   gi-
   cal
   str-
   uc-
   tur-
   e
           If the relationship between the    * There are no known biases
           drilling orientation and the       caused by the orientation of
           orientation of key mineralised     drill-holes MIDD008, SODD002
           structures is considered to        & SODD003.
           have introduced a sampling
           bias, this should be assessed
           and reported if material.
   Sam-    The measures taken to ensure       * The drill core is stored
   ple     sample security.                   onboard the Company's charter
   se-                                        vessel which is considered
   cu-                                        highly secure.
   ri-
   ty
   Au-     The results of any audits or       * No audits or reviews have
   dit-    reviews of sampling techniques     been carried out at this
   s       and data.                          time.
   or
   re-
   vie-
   ws


Section 2: Reporting of Exploration Results

   Cr-    JORC Code           Commentary
   it-    explanation
   er-
   ia
   Mi-    Type, reference     * The Ryberg Project is wholly within Mineral
   ne-    name/number,        Exploration Licences 2017/06 and 2019/38,
   ra-    location and        located on the east coast of Greenland. They
   l      ownership           are held 100% by Longland Resources Ltd, a
   te-    including           wholly owned subsidiary of Conico Ltd.
   ne-    agreements or
   me-    material issues
   nt     with third
   an-    parties such as
   d      joint ventures,
   la-    partnerships,
   nd     overriding
   te-    royalties,
   nu-    native title
   re     interests,
   st-    historical
   at-    sites,
   us     wilderness or
          national park
          and
          environmental
          settings.
          The security of     * The tenure is secure and in good standing
          the tenure held     at the time of writing. There are no known
          at the time of      impediments.
          reporting along
          with any known
          impediments to
          obtaining a
          licence to
          operate in the
          area.
   Ex-    Acknowledgment      * Previous work mentioned (2017 VTEM survey)
   pl-    and appraisal of    was planned and managed by Longland Resources
   or-    exploration by      Ltd, a wholly owned subsidiary of Conico Ltd.
   at-    other parties.      * Historic rock-chip sampling was conducted
   io-                        by Platina Resources Ltd and University of
   n                          Leicester.
   do-
   ne
   by
   ot-
   he-
   r
   pa-
   rt-
   ie-
   s
   Ge-    Deposit type,       * Deposit types: Magmatic & VMS. * Geological
   ol-    geological          setting: The project area is located within
   og-    setting and         the North Atlantic Igneous Province (NAIP), a
   y      style of            Tertiary volcanic centre that covered an area
          mineralisation.     of approximately 1.3 million km2 in
                              continental flood basalts (6.6 million km3 in
                              volume), making it one of the largest
                              volcanic events in history. Volcanism is
                              associated with the opening of the North
                              Atlantic, and presence of a mantle plume
                              (what is now the Icelandic hotspot). The
                              project area represents an erosional
                              interface where the flood basalts have been
                              removed, revealing the basement geology
                              beneath. The project area is adjacent to a
                              triple junction (failed rift) and consists of
                              Archaean orthogneiss, Tertiary gabbro/flood
                              basalt, and Cretaceous-Tertiary sediments
                              (rift valley basin). Approximately 70% of the
                              geology within the sedimentary basin has been
                              intruded by Tertiary sills that are feeders
                              to the overlying plateau basalts. There are
                              also feeder dykes and layered mafic
                              intrusions - it is likely that there is also
                              a large ultramafic body present at depth,
                              evidence for this is in the form of
                              ultramafic xenoliths brought to surface by
                              magma conduits. * Style of mineralisation:
                              magmatic copper and nickel sulphides with
                              appreciable cobalt, palladium and gold.
   Dr-    A summary of all    * Refer to Annex 1.
   il-    information
   l      material to the
   ho-    understanding of
   le     the exploration
   In-    results
   fo-    including a
   rm-    tabulation of
   at-    the following
   io-    information for
   n      all Material
          drill holes: -
          easting and
          northing of the
          drill hole
          collar -
          elevation or RL
          (Reduced Level -
          elevation above
          sea level in
          metres) of the
          drill hole
          collar - dip and
          azimuth of the
          hole - down hole
          length and
          interception
          depth - hole
          length.
          If the exclusion    * This is not the case.
          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.
   Da-    In reporting        * Not applicable as no sampling or assaying
   ta     Exploration         has occurred.
   ag-    Results,
   gr-    weighting
   eg-    averaging
   at-    techniques,
   io-    maximum and/or
   n      minimum grade
   me-    truncations
   th-    (e.g., cutting
   od-    of high grades)
   s      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     * Not applicable as no sampling or assaying
          used for any        has occurred.
          reporting of
          metal equivalent
          values should be
          clearly stated.
   Re-    - These             * The geometry of the mineralisation with
   la-    relationships       respect to the drill-hole angle is not known.
   ti-    are particularly    All reported lengths are in reference to
   on-    important in the    down-hole length, true width not known.
   sh-    reporting of
   ip     Exploration
   be-    Results. - If
   tw-    the geometry of
   ee-    the
   n      mineralisation
   mi-    with respect to
   ne-    the drill hole
   ra-    angle is known,
   li-    its nature
   sa-    should be
   ti-    reported. - If
   on     it is not known
   wi-    and only the
   dt-    down hole
   hs     lengths are
   an-    reported, there
   d      should be a
   in-    clear statement
   te-    to this effect
   rc-    (e.g., 'down
   ep-    hole length,
   t      true width not
   le-    known').
   ng-
   th-
   s
   Di-    Appropriate maps    * Refer to Figures 1,4, 5, 6, 7 and 10.
   ag-    and sections
   ra-    (with scales)
   ms     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.
   Ba-    Where               * Not applicable as no sampling or assaying
   la-    comprehensive       has occurred.
   nc-    reporting of all
   ed     Exploration
   re-    Results is not
   po-    practicable,
   rt-    representative
   in-    reporting of
   g      both low and
          high grades
          and/or widths
          should be
          practiced to
          avoid misleading
          reporting of
          Exploration
          Results.
   Ot-    Other               * Previous exploration results are detailed
   he-    exploration         in: Conico Ltd press release on the 11th of
   r      data, if            December 2020, entitled 'EM Survey Reveals
   su-    meaningful and      Highly Prospective Chonolith at Ryberg'.
   bs-    material, should    Conico Ltd press release on the 29th of July
   ta-    be reported         2020, entitled 'Conico to acquire East
   nt-    including (but      Greenland projects via acquisition of
   iv-    not limited to):    Longland Resources'. Holwell et al,
   e      geological          Mineralium Deposita, 2012, 47:3-21.
   ex-    observations;
   pl-    geophysical
   or-    survey results;
   at-    geochemical
   io-    survey results;
   n      bulk samples -
   da-    size and method
   ta     of treatment;
          metallurgical
          test results;
          bulk density,
          groundwater,
          geotechnical and
          rock
          characteristics;
          potential
          deleterious or
          contaminating
          substances.
   Fu-    The nature and      * Diamond drilling testing for lateral
   rt-    scale of planned    extensions of mineralisation, and large-scale
   he-    further work        step-out drilling.
   r      (e.g., tests for
   wo-    lateral
   rk     extensions or
          depth extensions
          or large-scale
          step-out
          drilling).
          Diagrams clearly    * Refer to Figures 1, 5 & 10.
          highlighting the
          areas of
          possible
          extensions,
          including the
          main geological
          interpretations
          and future
          drilling areas,
          provided this
          information is
          not commercially
          sensitive.


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Zusatzmaterial zur Meldung:

Datei:
https://eqs-cockpit.com/c/fncls.ssp?u=1e90043d37741b552a3403a674c59591
Dateibeschreibung: Pressemitteilung Conico Ltd.

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31.08.2021 Veröffentlichung einer Corporate News/Finanznachricht,
übermittelt durch DGAP - ein Service der EQS Group AG.
Für den Inhalt der Mitteilung ist der Emittent / Herausgeber verantwortlich.

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   Sprache:        Deutsch
   Unternehmen:    Conico Ltd.

                   6000 Perth
                   Australien
   Internet:       www.conico.com.au
   EQS News ID:    1230053



   Ende der Mitteilung    DGAP News-Service
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1230053 31.08.2021

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