NORANDA MINES LIMITED (GECO DIVISION) ASSESSMENT …...The claims are held by Noranda Mines Limited...
Transcript of NORANDA MINES LIMITED (GECO DIVISION) ASSESSMENT …...The claims are held by Noranda Mines Limited...
42F03NWM07 2.4730 FOCH LAKE 010
NORANDA MINES LIMITED (GECO DIVISION)
ASSESSMENT WORK REPORT
Area l
MAN1NG
NORANDA MINES LIMITED (GECO DIVISION)
ASSESSMENT WORK REPORT
Geological Report
To accompany the geological maps for Area l (Maps l to 5), Claims
TB 565565 to TB 565613 inclusive; TB 565615 to TB 565660 inclusive;
TB 565665; TB 565667 to TB 565713 inclusive; TB 578061 to TB 578089 inclusive;
TB 578091 to TB 578119 inclusive; TB 578121 to TB 578142 inclusive and
TB 578151 to TB 578183.
Location and Access
The survey area is located approximately 22 kilometers northeast of
Manitouwadge, Ontario (Figure 1). The claim block consists of 256 contiguous
claims forming a rough rectangle some 1.5 kilometers by 19 kilometers long.
The area is accessible via gravel road maintained by Ontario Paper
Company Limited. Access is excellent with the exception of the southeastern
portion of map sheet 5. This portion was covered by traversing from Ice Lake
which is accessible by float plane.
Ownership
The claims are held by Noranda Mines Limited with Head Offices in
Toronto, Ontario. The claims were staked in two stages with an inner core
of 143 claims staked in May, 1980 and an additional 113 claims in August, 198C.
Nature of Work
This report is submitted by the Geology Department of Noranda Mines
Limited, Geco Division and is a follow-up survey to a Horizontal Loop EM
and magnetometer survey conducted by Noranda Exploration Company between
January to April, 1981. It is the result of work carried out during May to
July, 1981 under the supervision of Mr. R. Friesen, Chief Geologist.
The geological mapping was done by Mr. R. Kusins, a B.Se. graduate of
McMaster University and Mr. J. Campbell, a B.Se. graduate of Acadia University
assisted by Mr. K. Allaty and Mr, F. Fueten, third year students at McMaster
University. All men were employed by Noranda Mines Limited, Geco Division at
the time of the survey.
The survey was run on a grid cut by M. Lampron of Amos, Quebec during
the fall and winter of 1980-81. Approximately 445.5 kilometers of line were
cut and pickets erected at 25 meter intervals. Mapping was carried out along
these lines and all outcrop was tied into this grid system. Five geological
maps covering Area l v;ere prepared at a scale of 1:5000.
- 2 -
Topography
The area covered by the claims consists of low ridges and hills
interspersed between small lakes and swamps. The western half of the
property has been largely cut over with subsequent growth of small trees
and brush. A large portion of map sheet 3 has been reforested with jackpine.
Map sheets 4 and 5 are largely untouched with mature spruce and jackpine
occurring on ridges and occasional eskers in the northern and southern porticus
of these map sheets. A large swamp with stunted trees and little undergrowth
covers the central portion of these map sheets.
Gravel and sand overburden covers the majority of the property but is
most abundant on map sheets 2, 3 and A.
DESCRIPTION OF THE PRINCIPAL ROCK TYPES MAPPED IN THIS CLAIM BLOCK(No Order Implied)
Granite - A medium grained, equigranular, felsic intrusive rock with a
poorly developed foliation often present. It often takes on a migmatitic
appearance and may have been formed by the in situ melting of the surrounding
rock types. The dominant minerals are quartz, plagioclase, potash feldspar
and lesser biotite. Magnetite is a common accessory mineral and may comprise
up to 57, of the rock.
Pegmatite - A coarse grained, white to pink, felsic intrusive rock. The
dominant minerals are potash feldspar, plagioclase and quartz with lesser
amounts of biotite.
Diabase - A fine to medium grained, equigranular, mafic intrusive with
approximately equal amounts of pyroxene, amphibole and plagioclase. Pyrite
is a common accessory mineral usually found in trace to minor amounts.
Quartz-Feldspar-Biotite Gneiss - A fine to medium grained, tan to gossan
coloured rock in outcrop with a well developed foliation. It is typically
comprised of quartz, plagioclase and potash feldspar with up to 2C7o biotite.
Garnets are occasionally found and may comprise up to 307. of the rock.
Granitized equivalents are very common and usually contain magnetite.
Biotitic Quartzite - A well banded, fine to medium grained, grey to white
coloured rock. It is comprised of quartz with lesser^ amounts of plagioclase,
potash feldspar and biotite; minor magnetite is a common accessory.
Quartz-Feldspar Gneiss - A grey to white, fine to medium grained rock with
a well developed foliation. It is intermediate between the quartz-feldspar-
biotite gneiss and biotitic quartzite containing near equal amounts of
quartz and plagioclase with usually about 107. biotite.
- 3 -
Hornblende-Biotite Gneiss - A medium grained, black coloured rock with a
well developed foliation. The major constituents of this rock are hornblende,
biotite and plagioclase with subordinate quartz. Granitized equivalents of this
rock type are common and tend to be enriched in plagioclase and potash
feldspar with a corresponding drop in hornblende and biotite content.
GEOLOGICAL OVERVIEW
Two major units cover the majority of Area 1. From north to south
these are a metasedimentary unit (Grey Gneiss Group) and a metavolcanic unit
(Hornblende Schist Group). These two groups are the eastward extension of
the Mine Series which hosts the Geco and Willroy orebodies. Missing fron
the Mine Series in Area l are rock types belonging to the Granite Gneiss
Group, an altered metavolcanic unit which may have become too thin to be
outlined in outcrop. A third, poorly exposed sequence of metavolcanic and
metasedimentary migmatites'outcrops along the northern portion of maps l to 2.
This sequence has been named the Migmatite Group for the convenience of this
report. Although often covered by overburden along their length, these groups
have been extended across the survey area with the aid of the magnetometer
survey. The groups are commonly granitized and have been intruded by
numerous intrusives, namely granite, pegmatite and diabase.
The Migmatite Group consists of two members which from north to south are:
1) Metasedimentary migmatite and 2) Hornblende-biotite gneiss. The
metasedimentary migmatite member is comprised of quartz-feldspar-biotite
gneiss which have been granitized. These granitized rocks may contain
magnetite particularly on map sheet 3. The hornblende-biotite gneiss member
is best exposed on map sheet l and is comprised of hornblende-biotite
gneiss, hornblende schist and quartz-feldspar-biotite gneiss. Interbedding
of this member with quartz-feldspar-biotite gneiss and the lack of outcrop
exposure does not allow this unit to be outlined on sheets 2 and 3. A zone
of garnetiferous quartz-feldspar-biotite gneiss occurs at the contact
between the two members on map sheet 1. The narrow magnetic high signature
over this zone and the association of this rock type with iron formation
elsewhere suggests that this horizon may be a poorly developed iron formation.
Outcrops of garnetiferous quartz-feldspar-biotite gneiss and poorly developed., . . formation
siliceous ironAContaining magnetite within this group may represent a
similar type of horizon on map sheet 3.
The Grey Gneiss Group can be subdivided into four mapable members which
may occur in different stratigraphic positions. The typical section from
north to south is comprised of 1) Granitized metasediment with magnetite,
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2) Garnetiferous metasediment, 3) Siliceous metasediment and 4) Interbedded
metasediment and metavolcanic. Interbedding and granitization of rock types
representative of the members was common.
The granitized metasediment with magnetite member extends from map l
to map 4, where it eventually trends north of the grid. On map sheet l this
member consists of quartz-feldspar-biotite gneiss and biotitic quartzite
which has been granitized to produce a metasedimentary migmatite containing
minor to 17, magnetite. Outcrop exposures of this member become more
granitized from the eastern half of map sheet l to map sheet 4. In this
area the dominant rock type is a granitic migmatite containing magnetite
with occasional remnants of quartz-feldspar-biotite gneiss and hornblende-
biotite gneiss.
The garnetiferous metasediment member is found to extend across the
central portions of maps l and 3. This horizon is poorly exposed with
outcrop restricted to limited areas on maps 1,3 and 4. The zone is found
to consist of quartz-feldspar-biotite gneiss, biotitic quartzite and iron
formation, all of which may be garnetiferous. Siliceous iron formation is
found exposed in the western section of map sheet 4 and contains 2-37. pyrite,
pyrrhotite and magnetite. Drilling in the vicinity of L119E/103+OON by
Marlhill Mines Limited in 1958 intersected two zones of iron formation
within this member. The exact location of this drilling was not determined
by the present survey. Similar drill results were obtained by Falconbridge
Nickel Mines Limited in 1965 on this horizon in the vicinity of
L225E/203+25N. Seventy-five meters to the east of this station, a cache
of core was located as well as the drill casing for hole number 1-3.
The siliceous metasediment member can be extended across maps 3 and 4,
although little outcrop information is available from map sheet 3. This
member contains a wide range of rock types including biotitic quartzite,
quartz-feldspar gneiss, quartz-feldspar-biotite gneiss and hornblende-
biotite gneiss. Interbedding of these rock types creates problems in
outlining this unit for any distance. The unit is best developed about
the eastern edge of map sheet 3 becoming less siliceous and more difficult
to outline towards map sheets 2 and 5. In places, this siliceous
metasedimentary horizon contains rocks which may be felsic metavolcanics.
The interbedded metasediment and metavolcanic member extends across
the full width of Area l, occurring in r.he central, portion of the map
sheets. On maps l and 2 the member forms a single horizon, while on
sheets 3 to 5 thickening of the siliceous and garnetiferous metasedimentary
horizons has resulted in the splitting of the unit into two horizons.
- 5 -
Typically the member is comprised of quartz-feldspar-biotite gneiss and
biotite-hornblende gneiss which locally may be granitized.
The Hornblende Schist Group outcropping along the southern section of Area l
has not been subdivided into members. The unit is quite extensive with only
the northern portion of the group exposed on Area 1. In the map area it is
typically comprised of a metavolcanic migmatite often containing remnants of
hornblende-biotite gneiss and hornblende schist. Occasional outcrops of
quartz-feldspar-biotite gneiss may also occur within this group.
Intrusives were commonly observed on the claim block. Granite and granite
migmatites were very common and appear to be the product of regional
granitization of the surrounding metasedirnents and metavolcanics. Remnants
of the parent material were usually found within the granite and a poor
foliation was often preserved. Intrusive contacts were not generally
observed although zones of granitization were outlined. Outcrops of granite
of intrusive origin were observed in the northeastern corner of map sheet 5.
Pegmatites showed a wide range in width from a few inches to outcrop
size. Their erratic nature and often limited size did not allow individual
pegmatites to be traced for any distance on this scale of mapping.
Diabase dikes were commonly found in the map area. The three major
trends are north, northeast and northwest. These trends were coincident
with the major fault trends for the map sheets. The dikes occasionally had
a magnetic response often occurring as isolated highs or cross-cutting trends
on the magnetometer survey maps. This feature was useful in extending contacts
between isolated outcrops of diabase.
GEOLOGY OF AREA l
Map Sheet l
The Migmatite, Grey Gneiss and Hornblende Schist Groups are exposed
on this map sheet, trend easterly, with dips of approximately 60 S. Increased
granitization of these groups has occurred towards the eastern portion of
the sheet.
In addition to the garnetiferous metasediment horizon containing
Anomalies lA and B as well as the zone in the Migmatite Group, a lesser zone
is exposed on L107+OOE along the contact between the Grey Gneiss and
Hornblende Schist Groups. This lesser zone may represent a poorly developed,
iron formation horizon similar to those found along this contact about the
Manitouwadge Syncline.
- 6 -
An outcrop of biotite-anthophyllite gneiss at L111E/106+50N may
possibly be the extension of the Granite Gneiss Group into Area l, although
additional rock types typical of this group were not located.
Map Sheet 2
A continuation of the major groups extends onto map sheet 2 from
sheet l, although the metavolcanic member of the Migmatite Group and the
garnetiferous metasediment member of the Grey Gneiss Group have pinched out.
Outcrop is sparse with the majority of outcrop found on the eastern half of
the sheet. In this area a number of felsic outcrops of quartz-feldspar
gneiss and biotitic quartzite form a siliceous member within the Grey Gneiss
Group. Foliation is easterly trending with dips of about 70 S. No
mineralization or geophysical anomalies were located on this map sheet.
Map Sheet 3
The Migmatite Group is exposed along the northern edge of the map
trending beyond the grid in the eastern portion of the map sheet. Outcrops
of garnetiferous metasediment and poorly developed siliceous iron formation
indicative of an iron formation horizon were located within the group
although no geophysical responses were detected in these areas.
The Grey Gneiss Group is poorly exposed with gravel overburden
covering the central portion of the sheet. Outcrop is limited to the
extreme eastern portion of the map and along the contact with the Migmatite
Group. A string of EM conductors occurs within the garnetiferous metasediment
menber, the most significant being Anomaly 3B. This anomaly has been tested
with 8 holes by Falconbridge Nickel Mines Limited which outlined two zones
of pyrite and pyrrhotite mineralization within iron formation. An outcrop
of weakly mineralized, garnetiferous iron formation was located within this
member at L246E/205+60N.
Foliations trend easterly with dips overall being somewhat flatter
than observed on sheets l and 2. A number of fold features are evident. A
Z-shaped drag fold has warped the Grey Gneiss-Hornblende Schist contact in
the southeastern part of the map sheet.
Shallow southerly to shallow northerly dips along the edge of the
sheet may represent an easterly trending, anticlinal fold axis.
Map Sheet 4
The Migmatite Group and the granitized metasediment member of the
Grey Gneiss Group are not outlined on the remaining map sheets due to their
trend which have extended the units to the north of the grid. The garnetiferous
metasediment horizon of the Grey Gneiss Group has been extended across the
- 7 -
western half of the map until poor outcrop exposure and poor magnetic
signature did not allow the unit to be outlined. An outcrop of siliceous
iron formation was located between lines 305E and 306E at 305+25N within
this member and anomaly 4B may represent a conductive extension of this zone.
The siliceous metasediment member has become interbedded with quartz-
feldspar-biotite gneiss creating problems in outlining this unit. This
member appears to have pulled away from its contact with the garnetiferous
metasediment member and a zone of quartz-feldspar-biotite gneiss now
separates the two units. A minor zone of garnetiferous metasediment occurs
within this member in the vicinity of L312E/300+OON and anomaly 4C. This
zone has been folded into a Z-shaped drag fold having a northeasterly trending
fold axis.
Anomalies 4A, D, E and F occur in the interbedded metavolcanic and
metasediment member of the Grey Gneiss Group in close proximity to the
Hornblende Schist contact. Little outcrop information is available in these
areas.
The Hornblende Schist Group is extensively granitized with pegmatite
intrusions being common. A broad z-shaped drag fold is outlined by the Grey
Gneiss-Hornblende Schist contact in the eastern portion of the map sheet.
Foliations on this map are generally easterly trending with dips
ranging from 70 S to locally horizontal. Dips for the most part continue to
show a shallowing from map sheet 3.
Map Sheet 5
The Grey Gneiss Group largely consists of quartz-feldspar-biotite
gneiss in various degrees of granitization. Occasional outcrops of
siliceous metasediments occurs in the northern portion of the map sheet,
but extensive interbedding of rock types makes the separation of the group
into members somewhat questionable.
The Hornblende Schist Group covers the southern half of the sheet
and is comprised of metavolcanic migmatites.
Dips where located, were variable ranging from 80 to near horizontal
and generally maintained a southerly attitude. Foliations were usually
easterly trending. No mineralization or geophysical anomalies were located
on this map sheet.
- 8 -
Conclusions and Recommendations
No economic mineralization was located during the present survey.
Mineralization that was encountered consisted of pyrite, pyrrhotite and
magnetite often contained within iron formation. Two major zones of
garnetiferous metasediment were outlined which host anomalies 1A, IB, 3A,
AB and a string of lesser anomalies. These zones are intimately associated
vrith iron formation horizons, with the anomalies detected representing
local accumulations of conductive sulfides. A detailed drill program should
be carried out on these zones with the objective of systematically testing
the horizon as well as the anomalies detected.
Anomaly AC is situated in close proximity to a diabase dike and has a
similar orientation. The anomaly may be caused by a zone of remobilized
sulfides along the diabase contact as it passed through an iron formation.
A closer examination is required before recommendations can be made on this
anomaly.
Anomalies AA, 4D, AE and AF are located adjacent to the contact between
the Hornblende Schist and Grey Gneiss Groups. Limited outcrop information is
available in these areas and drilling of the anomalies is suggested in
determining their economic potential.
Manitouwadge, Ontario
March 2A, 1982
)l
1l
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al*
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nch
* 2
mil*
* • fi*
.10'
.CLAIM NUMBERS FOR AREA ^
TB565565 to TB565613 inclusive
TB565615 to TB565660 inclusive
TB565665
TB565667 to TR565713 inclusive
TB578061 to TB578089 inclusive
TB578091 to TB5781I9 inclusive
TB578121 to TB578142 inclusive
TB578151 to TB578183 inclusive
42F83NW8M7 2.4739 FOCH LAKE 900
,.,. P.O.
Bay, OntaHe
Dear Madam
ME: tooloflcalftrvey on Mining Claim TB W5565 at al 1n tne Areas of Loken Uke and Foch Lake.
Tht Geological Survey assessment work credits as shown on the ttachtd statement have been approved as of the above date.
PI MM Infora the recorded holder of these mining clala* and so Indicate on your records.
Yours very truly,
E.F. AndersonDirectorLand Management Branch
Whitney Block, Room 6450Quean's ParkToronto, OntarioN7A 1W3Phone: 416/965-1380
A. Barr:se
cc: Horanda Mines Limited Manitouwadge, Ontario
cc: Horanda Mines Limited Toronto, Ontario
cc: Resident Geologist Thunder Bay, Ontario
Ministry of Natural
r u rees
Technical Assessment Work Credits
File
2.4730
Recorded Holder
NORANDA MINES LIMITEDTownship or Area
LOKEN LAKE h FOCH LAKE AREAS
Type of survey and number of Assessment days credit per claim
GeophysicalElectromagnetic
Magnetometer
Radiometric
Induced polarization ,.
Section 86 (18)
Geological 20
Geochemical
Man days Q Airborne
Special provision Gr Ground
Q Credits have been reduced because of coverage of claims.
D Credits have been reduced because of coire to work dates and figures of applicant.
days
days
days
days
days
days
days
D 3*
partial
ctions
Mining Claim* Amiud
TB 565565 565615 565665 565667 578061 578091 578121 578151
to 13 Inclusive to 60 Inclusive
to 713 Inclusive to 89 Inclusive to 119 Inclusive to 42 Inclusive to 83 Inclusive
Special credits under section 86 (15a) for the following mining claims
No credits have been allowed for the following mining claims
not sufficiently covered by the survey l l Insufficient technical data filed
The Mining Recorder may reduce the above credits if necessary in order that the total number of approved assessment days recorded on each claim does not exceed the maximum allowed as follows: Geophysical — 80; Geological — 40; Geochemical — 40; Section 86(181-60:
828
Ontario
Ministry ofNaturalResources
Notification of recording
of assessment work credits
v. Lands Administration Branch "~~/ Mining Lands Section f Ministry of Natural Resources
Room 161.7. Whitney Block Queen's Park, Toronto
M7A 1W3
RE*" w w ir
MINING
Date of recording of work:.
Recorded holder: ————
Address: ____
Township or Area: ————
April 21,1982
Noranda Mines LimitedP.O. Box 45
MSL 1B6
Loken Lake Area (M2381) Foch Lake Area (M5)
Type of survey and number of Assessment days credit per claim
GeophysicalElectromagnetic- days
Magnetometer.
Radiometric _
-days
-days
Induced polarization ——-—
Section 86 (18)
Geological.____20
-days
-days
-days
' Geoeh'^mieal. -days
Man days CD
Special provision jtJ
Airborne LJ
Ground Dx
Mining claims
/TB565565-613X/TB565615-660 incl.^"
V/TB565665,' TB56566~7-713 inclK TB578061-089 incl.*,X/TB578091-119i^B578121-42 i
N/TB578151-83 incl.
Notice to recorded holder:
(H Survey reports and maps in duplicate be submitted to the Lands Administration Branch. Toronto with in 60 days from the date of recording of this work.
H Reports and maps are being forwarded to the Lands Administration Branch with this letter.
792 (6/77J
Mining recorder
c.c.
Noranda Mines LimitedP.O. Box 45, Toronto,Ontario
Noranda Mines LimitedP.O. Box 100, Manitouwadge,Ontario
LA. O6S
Ministryof GeotechnicalNatural ppnnrtResources RePOrt ,
Ontario Approval
Mining Lands Comments
To: Geophysics
Comments
Approved Wish to see again with correctionsDate Signature
o: Geology - ExpendituresComments
r*./["^Approved Wish to see again with corrections
To: Geochemistry
Comments l ~"*V
Approved Q Wish to see again with correctionsSignature
(To: Mining Lands Section, Room 6462, Whitney Block. (Tel: 5-1380)
1593 (81/10)
1982 OS ^p * 2.4730
Mining RecorderMinistry of Natural ResourcesP.O. Box 5000Thunder Bay, OntarioP7C 566
Dear Sir:
He have received reports and naps for a Geological Survey submitted under Special Provisions (credit for Performance and Coverage) on Mining Claims TB 565565 et al In the Areas of Loken Lake and Foch Lake.
This Material will be examined and assessed and a statement of assessment work credits will be Issued.
Yours very truly.
E.F. AndersonDirectorLand Management Branch
Whitney Block. Room 6450Queen's ParkToronto, OntarioM7A 1U3Phone: 416/965-1316
J. Skura/amc
cc Noranda Mines Limited Toronto, Ontario
cc Noranda Mines Limited Manitouwadge, Ontario
J ZO a
bo
Ontario
Ministry of Natural Resources
GEOPHYSICAL - GEOLOGICAL - GEOCHEMICAL TECHNICAL DATA STATEMENT
File.
TO BE ATTACHED AS AN APPENDIX TO TECHNICAL REPORTFACTS SHOWN HERE NEED NOT BE REPEATED IN REPORT
TECHNICAL REPORT MUST CONTAIN INTERPRETATION, CONCLUSIONS ETC.
GeologicalType of Survey(s) __Township or Aro. Loken Lake (M2381) and Foch Lake (M5)
Claim Hnlrier(s) Moranda Mines Limited __________
P.O. Box 100, Manitouwadge, Ontario
Survey r^^ny Noranda Mines Limited __________
Author of Report Robert Kusins and Joseph Campbell
Address of A,,thnr P.O. Box 100, Manitouwadge, Ontario
Covering Dates of Snrv. August 1980 - December 1981
Total Miles of Line P.nt 280 ' 0(linecutting to office)
SPECIAL PROVISIONS CREDITS REQUESTED
ENTER 40 days (includes line cutting) for first survey.ENTER 20 days for each additional survey using same grid.
Geophysical—Electromagnetic.—Magnetometer_—Radiometric———Other.——.—.
DAYSper claim
Geological.Geochemical.
20
AIRBORNE CREDITS (Special provision credits do not apply to airborne survey*)
Magnetometer. .Electromagnetic. . Radiometric(enter days per claim)
-; l Jf H01- SIGNATURE:.Author of Report or Agent
Res. Geol.. . Qualifications p/.
Previous Surveys File No. Type Date Claim Holder
MINING CLAIMS TRAVERSED List numerically
see attached list'(prefix) (number)
TOTAL CLAIMS 256
837 (5/79)
'-iApplied to the following Contiguous Claims
No.
123456789
1011121314151617181920212223242526272829303132333435363738394041424344454647484950515253545556
Claim No.
5655655655665655675655685655695655705655715655725655735655745655755655765655775655785655795655805655815655825655835655845655855655865655875655885655895655905655915655925655935655945655955655965655975655985655995656005656015656025656035656045656055656065656075656085656095656105656115656125656L3565615565616565617565618565619565620565621
Days
2020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020
No.
57585960616263646566676869707172737475767778798081828384858687888990919293949596979899
100101102103104105106107108109110111112
Claim No.
565622565623565624565625565626565627565628565629565630565631565632565633565634565635565636565637565638565639565640565641565642565643565644565645565646565647565648565649565650565651565652565653565654565655565656565657565658565659565660565665565667565668565669565670565671565672565673565674565675565676565677565678565679565680565681565682
Days
2020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020
No.
113114115116117118119120121122123124125126127128129130131132133134135136137138139140141142143144145146147148149150151152153154155156157158159160161162163164165166167168
Claim No.
565683565684565685565686565687565688565689565690565691565692565693565694565695565696565697565698565699565700565701565702565703565704565705565706565707565708565709565710565711565712565713578061578062578063578064578065578066578067578068578069578070578071578072578073578074578075578076578077578078578079578080578081578082.578083578084578085
Days
202020202020202020202020202020202020202020202020202020202020'
2020202020202020202020202020202020202020202020202020
Applied to the following Contiguous Claims (Conc'd)
No.
169170171172173174175176177178179180181182183184185186187188189190191192193194195196197198199200201202203204205206207208209210211212213214.2152162172182197.202212222215224
Claim No.
578086578087578088578089578091578092578093578094578095578096578097578098578099578100578101578102578103573104578105578106578107578108578109578110578111578112578113578114578115578116578117578118578119578121578122578123578124578125578126578127578128578129578130578131578132578133578134578135578136578137578138578139578140578141578142578151
Days
2020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020202020
No.
225226227228229230231232233234235236237238239240241.242243244245246247248249250251252253254255256
Claim Ne.
578152578153578J.54578155578156578157578158578159578160578161578162578163578164578165578166578167578168578169578170578171578172578173578174578175578176578177578178578179578180578181578182578183
Days
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