Aton Resources Announces New Regional Exploration Results From The Sir Bakis Prospect

VANCOUVER, Sept. 13, 2017 - Aton Resources Inc. (TSX-V:AAN) (“Aton” or the “Company") is pleased to provide investors with an update on their regional exploration activities, specifically at the Sir Bakis prospect, currently underway at the Company’s 100% owned Abu Marawat concession (“Abu Marawat” or the “Concession”), located in the Eastern Desert of Egypt.


Highlights:

- Field inspection of the Sir Bakis prospect (see Figure 1) has indicated the presence of widespread gold mineralization, over an area covering at least 1800m x 900m in size; indicating potential for the development of reduced intrusive related gold (RIRG) mineralization in the Sir Bakis area, associated with individual shear veins and sheeted vein systems;

- Initial grab and channel sampling from the Sir Bakis area has returned assays up to 150 g/t Au and 32.9 g/t Au from grab samples, and 29.5 g/t Au from channel samples;

- First pass surface trenching at the Sir Bakis prospect has returned a highly anomalous surface intersection of 109.1m @ 0.21 g/t Au;

- First pass regional reconnaissance has identified a new target area, the Black Gaharish prospect, and an initial sample returned an assay grade of 16.5 g/t Au.


Mark Campbell, President and CEO of Aton, commented “Most companies would be happy to have a single exploration district, whereas we have multiple districts at our Abu Marawat Concession area, each with unique geological characteristics. The recent exciting results from Sir Bakis prospect area, and at the old Sir Bakis mine demonstrate the huge exploration potential of the newly identified reduced intrusive related gold mineralization trend at Abu Marawat. We have returned similar results from Bohlog, and expect similar results from the old Semna mine, Massaghat and West Garida. Along with our recent new VMS discovery at Waayrah, which lies within the Waayrah-Miranda VMS trend, the potential overall scale of our Abu Marawat license area is impressive. The work that we are doing has created targets for our upcoming autumn drilling campaign. Now that we are moving towards developing our first mines at Hamama and Abu Marawat, which we hope to see producing by the middle of 2020, the focus now is to bring more of our projects on stream over time.”


Sir Bakis Prospect

The Sir Bakis prospect is located approximately 12km NE of the Company’s Hamama West mineral deposit, and has been extensively worked in both ancient and modern times. Review of remote sensing imagery indicates the widespread occurrence of ancient workings, as well as the remains of ancient mining settlements, and there is archaeological evidence suggesting that mining dates back to the New Kingdom period, over 3,000 years ago. During the modern era a British company, Eridia (Egypt) Exploration Company, mined at Sir Bakis between 1904 and 1906. The remains of the old processing plant, various other mine buildings, a tailings pile, and 2 open adits, which access the underground stopes are evident at Sir Bakis (see Figure 2), dating back to the modern phase of exploitation.

The Main Vein at Sir Bakis, which was the focus of the modern underground mining, can be traced at surface for a distance of some 1.6km in a N-S strike direction. The Main Vein is considered to be a shear vein and was mined at widths of up to 1.5m underground. Approximately 600m NW of the adits there is a zone of narrow sheeted veins which has been worked extensively at surface to shallow depths in ancient times, known as the NW Vein Swarm. The Vein Swarm is approximately 400m along its’ N-S strike length at surface, and in excess of 100m in width. There are also a number of other major veins in the area, to the NW of the modern mine workings, and numerous smaller veins and shears through the area which have been worked by the ancients. Limited previous sampling at Sir Bakis by the Company in 2014 has returned assays of 4.79 g/t Au from underground, and 2.38 g/t Au from surface channel sampling.

A Photo accompanying this announcement is available at http://www.globenewswire.com/NewsRoom/AttachmentNg/1d3d02b3-e232-47b2-be96-eb2b9f47bd04

The mineralization at Sir Bakis predominantly occurs in older basement granodiorites, and is spatially associated with a series of younger granite plutons, including the Ria al Jarrah pluton which outcrops to the north of Sir Bakis (see Figures 1 and 2). There is considerable hornfelsing and contact metamorphism of basement volcanic rocks by the younger intrusive plutons. The younger plutons are considered to represent evolved magmas, displaying aplitic textures in the immediate Sir Bakis area, and are associated with modern tungsten mining at Abu Garida (see Figure 1), and also fluorite mining at a site between Abu Garida and Hamama, to the SW of Sir Bakis. Mineralization at Sir Bakis is primarily located in basement granodiorites, and is typically low sulphide in nature, with only limited amounts of accessory arsenopyrite and pyrite. Previous sampling by the Company of a homogenized bulk sample of the modern tailings returned average assay values of 1.99 g/t Au, 1.71 g/t Ag, 26 ppm Cu, 91 ppm Pb and 82 ppm Zn.

A Photo accompanying this announcement is available at http://www.globenewswire.com/NewsRoom/AttachmentNg/d0b2c5f4-326e-4937-ac18-2f6742dbcc0d

During the first phase of recent sampling a total of 182 surface samples, predominantly channel samples, and some grab samples (see Figure 3) were collected from the general Sir Bakis area. Additionally 3 surface trenches were mechanically excavated, SBT-001 to SBT-003 for a total length of 704m, and were manually channel sampled, over nominal 2m intervals, with a total of 376 trench samples being collected. All samples were submitted to ALS Rosia Montana in Romania, and were analyzed for gold using fire assay with an atomic absorption finish, and for copper, lead, zinc and silver using an aqua regia digest with an atomic absorption finish.

The results from the initial sampling program are very encouraging, with 10% of the surface channel and grab samples returning assay grades greater than 1 g/t Au, with mineralized samples returned from all areas sampled. A single grab sample from an isolated ancient working approximately 2km NE of Sir Bakis between the modern mine and the Massaghat prospect returned an assay of 150 g/t Au. Channel samples from partially mined surface outcrops of the Main Vein returned assays of 29.5 g/t and 5.34 g/t Au; a channel sample from the westernmost vein returned an assay of 7.94 g/t Au, and a grab sample of vein quartz from the northern extension of the Main Vein workings returned an assay of 32.9 g/t Au. Results of the surface sampling are presented in Appendix A. Ag assays were typically low, as were Cu, Pb and Zn which typically had assay values less than 100ppm.

A Photo accompanying this announcement is available at http://www.globenewswire.com/NewsRoom/AttachmentNg/e4bb6623-72ec-44db-8a17-38a0015f2f7e

Results from the trenches are also encouraging with anomalous results being returned from all 3 trenches (see Table 1). The best results were obtained from the western end of trench SBT-001, (see Figure 3), which intersected a highly anomalous interval of 109.1m @ 0.21 g/t Au, over the NW Vein Swarm. The NW Vein Swarm was marked by many shallow, narrow ancient workings, typically less than a meter in width to a maximum of 3-4m depth, with the highest grade quartz veins having been removed by the ancient miners. It is therefore considered probable that the trench assays would therefore have considerably underestimated the true grade of the mineralized interval, prior to the ancient shallow mining activity.

         From   To  Interval   Au
Trench    (m)  (m)    (m)     (g/t)
SBT-001	3.5	112.6	109.1	0.21
SBT-001	203.9	225.4	21.5	0.09
SBT-001	234.4	240.9	6.5	0.22
SBT-002	57.4	59.4	2.0	0.26
SBT-002	132.2	136.8	4.6	0.50
SBT-002	162.2	162.8	0.6	0.97
SBT-002	169.7	190.2	20.5	0.09
SBT-003	34.0	36.0	2.0	0.58
SBT-003	70.0	74.0	4.0	0.42
SBT-003	84.0	86.0	2.0	0.48
SBT-003	173.8	175.8	2.0	0.64
SBT-003	203.8	205.8	2.0	1.24

Table 1 – Anomalous intersections from Sir Bakis trenches

The results of the initial phase of sampling at Sir Bakis are very encouraging and the Company believes that the mineralization identified at Sir Bakis displays strong affinities with reduced intrusion related gold (RIRG) systems, such as the proximity to evolved volatile-rich granite plutons, displaying evidence of tungsten and fluorite mineralization; gold mineralization associated with granodioritic host rocks; structural controls on mineralization in preferred orientations; the presence of narrow structurally controlled shear veins and vein swarms or sheeted vein systems; low levels of accessory sulphide minerals; and typically very low levels of silver, lead, zinc, and notably copper in the mineralization. Similar styles of mineralization have also been identified at the nearby Bohlog, Massaghat and Zeno prospects, and the Company believes that it has identified a significant belt of potential RIRG mineralization within the Concession, associated with the late granites (see Figure 1). Further follow-up field work and geochemical analysis of the mineralized samples is planned at Sir Bakis.

It is also noted that there are strong similarities between the Sir Bakis prospect and other significant gold mines and projects within the Egyptian Arabian-Nubian Shield, where mineralization is associated with high grade quartz veins and large lower grade zones of stockwork and sheeted vein mineralization, largely hosted in granitoid host rocks, such as Sukari, Fawakhir-El Sid, Hammash and possibly Anbat. AAN believes that the Arabian-Nubian Shield of Egypt has potential to emerge as a significant RIRG belt, with excellent potential within the Company’s Abu Marawat Concession, associated with the post-orogenic or younger granitoid suite of late intrusives.


Black Gaharish Prospect

The new Black Gaharish prospect was identified from investigation of remote sensing imagery, and the presence of ancient workings in the area was confirmed by local Bedouin who have extensive knowledge of many ancient workings in the whole region. A brief initial field visit to the prospect area revealed the presence of numerous ancient working sites, and ancient miners huts. The prospect is located approximately 3km south of the old British mine at Semna, and some 3.5km south-east of a large but remote ancient mining settlement at Zeno. The Company has previously reported high grade assays of up to 46.9 g/t Au from Zeno (see press release dated 15 August 2012).

Mineralisation at Black Gaharish is associated with flat lying structures within intrusive granodioritic host rocks. Limited iron staining and occasional minor copper staining was observed in the mineralised quartz veins, suggesting a generally low sulphide content of the mineralisation. Mineralisation is considered to be structurally controlled and orogenic in nature, and is similar in nature to that at the Semna mine. Further workings to the north were subsequently identified from imagery, and the mineralisation is considered to be an extension of the structurally controlled gold mineralisation system at Semna, and possibly also that at Zeno were many ancient workings have been identified from imagery. A single grab sample of vein quartz from one of the ancient workings returned an assay grade of 16.5 g/t Au. Further field follow up is planned at Black Gaharish, and also at Zeno when the cooler temperatures of autumn and winter will facilitate access to this rather remote site.


Activity update:

- Additional results from the preliminary field inspections and sampling conducted at the Semna and West Garida;

- Crone Geophysics has completed a ground and downhole electromagnetic survey of the 6 km long prospective horizon (or the hanging wall contact) at Hamama. Interpretation of the survey data has been delayed but is now complete, and the final geophysical synthesis of all geophysics including the 2008 IP and magnetics survey completed at Hamama is expected shortly;

- Phase 1 metallurgical test work conducted on Hamama West samples at ALS Metallurgy in Kamloops, BC, has been completed.


About Aton Resources Inc.

Aton Resources Inc. (TSX-V:AAN) is focused on its 100% owned Abu Marawat Concession (“Abu Marawat”), located in Egypt’s Arabian-Nubian Shield, approximately 200 km north of Centamin’s Sukari gold mine. Aton has identified a 40 km long gold mineralized trend at Abu Marawat, anchored by the Hamama deposit in the west and the Abu Marawat deposit in the east, containing numerous gold exploration targets, including three historic British mines. Aton has identified several distinct geological trends within Abu Marawat, which display potential for the development of RIRG and orogenic gold mineralization, VMS precious and base metal mineralization, and epithermal-IOCG precious and base metal mineralization. Abu Marawat is over 738km2 in size and is located in an area of excellent infrastructure, a four-lane highway, a 220kV power line, and a water pipeline are in close proximity.


Qualified Person

The technical information contained in this News Release was prepared by Roderick Cavaney BSc, MSc (hons), MSc (Mining & Exploration Geology), FAusIMM, SEG, GSA, SME, Vice President, Exploration, of Aton Resources Inc. Mr. Cavaney is a qualified person (QP) under National Instrument 43-101 Standards of Disclosure for Mineral Projects.

For further information regarding Aton Resources Inc., please visit us at www.atonresources.com or contact:

Mark Campbell, President and Chief Executive Officer
Tel: +1-936-689-2589
Email: mcampbell@atonresources.com



Note Regarding Forward-Looking Statements

Some of the statements contained in this release are forward-looking statements. Since forward- looking statements address future events and conditions; by their very nature they involve inherent risks and uncertainties. Actual results in each case could differ materially from those currently anticipated in such statements.

Neither TSX Venture Exchange nor its Regulation Services Provider (as that term is defined in policies of the TSX Venture Exchange) accepts responsibility for the adequacy or accuracy of this release.



Appendix A – Sir Bakis surface samples, assay data

Sample ID	Sample
Type	Easting	Northing	Au
(g/t)	Ag
(g/t)	Cu
(ppm)	Pb
(ppm)	Zn
(ppm)
AHA-14169	Channel	545118	2918999	0.09	<0.2	6	11	31
AHA-14170	Channel	545116	2918997	0.13	<0.2	6	5	25
AHA-14171	Channel	545139	2918977	0.02	<0.2	5	4	16
AHA-14172	Channel	545138	2918979	0.02	<0.2	22	31	73
AHA-14173	Channel	545135	2918979	0.02	<0.2	8	7	29
AHA-14174	Channel	545133	2918980	0.36	<0.2	15	43	40
AHA-14175	Channel	545131	2918981	0.30	<0.2	9	44	37
AHA-14176	Channel	545129	2918981	0.62	<0.2	5	37	27
AHA-14177	Grab	545130	2918979	32.90	3.8	11	120	20
AHA-14178	Channel	545195	2918957	0.29	0.2	274	2	15
AHA-14179	Channel	545193	2918956	0.24	<0.2	8	3	9
AHA-14180	Channel	545194	2918963	1.24	1.8	2230	4	26
AHA-14181	Channel	545200	2918946	0.07	<0.2	28	2	14
AHA-14182	Channel	545202	2918945	0.03	<0.2	18	2	17
AHA-14183	Channel	545152	2918886	0.02	<0.2	10	2	14
AHA-14184	Channel	545150	2918885	0.01	<0.2	15	2	22
AHA-14185	Channel	545148	2918886	0.03	<0.2	8	2	16
AHA-14186	Channel	545146	2918886	0.03	<0.2	31	4	11
AHA-14187	Channel	545144	2918885	0.01	<0.2	165	6	23
AHA-14188	Channel	545142	2918885	0.01	<0.2	19	8	22
AHA-14189	Channel	545140	2918884	0.02	0.4	34	9	20
AHA-14190	Channel	545138	2918883	0.01	<0.2	16	7	11
AHA-14191	Channel	545137	2918884	0.01	0.2	45	43	27
AHA-14192	Channel	545136	2918883	0.01	<0.2	55	18	14
AHA-14193	Channel	545134	2918882	0.01	<0.2	69	22	13
AHA-14194	Channel	545132	2918880	0.01	<0.2	29	15	9
AHA-14195	Channel	545131	2918879	0.05	<0.2	11	8	15
AHA-14196	Channel	545129	2918878	0.03	<0.2	9	7	16
AHA-14197	Channel	545127	2918876	0.02	0.2	12	20	52
AHA-14198	Channel	545125	2918875	0.03	3.0	8	72	67
AHA-14199	Channel	545123	2918874	0.01	3.0	9	107	39
AHA-14200	Channel	545122	2918871	0.01	0.2	7	21	12
AHA-14205	Channel	545140	2919196	0.06	0.2	11	4	8
AHA-14206	Channel	545142	2919195	0.05	<0.2	25	8	36
AHA-14207	Channel	545144	2919196	0.05	0.2	10	10	24
AHA-14208	Channel	545146	2919197	0.08	0.2	13	14	27
AHA-14209	Channel	545122	2919210	0.03	<0.2	7	2	112
AHA-14210	Channel	545125	2919209	0.01	<0.2	5	2	39
AHA-14211	Channel	545127	2919209	0.02	<0.2	10	3	87
AHA-14212	Channel	545129	2919209	0.02	<0.2	5	1	14
AHA-14213	Channel	545130	2919208	0.04	<0.2	12	3	65
AHA-14214	Channel	545132	2919209	0.10	<0.2	7	3	143
AHA-14215	Channel	545135	2919209	0.04	<0.2	15	3	133
AHA-14216	Channel	545136	2919210	0.02	<0.2	41	4	99
AHA-14217	Channel	545137	2919211	0.05	<0.2	34	3	123
AHA-14218	Channel	545139	2919211	0.06	<0.2	9	2	214
AHA-14219	Channel	545138	2919214	0.07	<0.2	16	2	62
AHA-14220	Channel	545140	2919216	0.11	<0.2	39	2	125
AHA-14221	Channel	545141	2919219	0.17	<0.2	4	2	130
AHA-14222	Channel	545143	2919219	0.02	<0.2	3	2	95
AHA-14223	Channel	545145	2919220	0.10	<0.2	4	2	121
AHA-14224	Channel	545147	2919222	0.08	<0.2	5	2	251
AHA-14225	Channel	545148	2919224	0.19	<0.2	5	4	196
AHA-14226	Channel	545151	2919225	0.08	<0.2	4	2	147
AHA-14227	Channel	545151	2919228	0.05	<0.2	6	2	247
AHA-14228	Channel	545153	2919227	0.03	<0.2	5	2	109


Sample ID	Sample
Type	Easting	Northing	Au
(g/t)	Ag
(g/t)	Cu
(ppm)	Pb
(ppm)	Zn
(ppm)
AHA-14229	Channel	545154	2919229	0.15	<0.2	5	3	86
AHA-14230	Channel	545156	2919232	0.03	<0.2	4	1	57
AHA-14231	Channel	545156	2919230	0.02	<0.2	5	3	35
AHA-14232	Channel	545159	2919231	0.02	<0.2	11	3	173
AHA-14233	Channel	545182	2919210	2.14	<0.2	8	2	89
AHA-14234	Channel	545182	2919208	0.14	<0.2	11	6	348
AHA-14235	Channel	545185	2919207	0.07	<0.2	8	3	260
AHA-14236	Channel	545186	2919206	0.02	<0.2	6	4	43
AHA-14237	Channel	545188	2919207	0.02	<0.2	5	3	32
AHA-14238	Channel	545189	2919204	0.01	<0.2	7	3	36
AHA-14239	Channel	545191	2919203	0.01	<0.2	8	5	29
AHA-14240	Channel	545193	2919201	0.01	<0.2	4	2	22
AHA-14241	Channel	545194	2919199	0.02	<0.2	6	4	41
AHA-14242	Channel	545195	2919198	0.03	<0.2	11	5	136
AHA-14243	Channel	545195	2919196	0.01	<0.2	10	5	295
AHA-14244	Channel	545194	2919192	0.00	<0.2	4	2	61
AHA-14245	Channel	545197	2919189	0.01	<0.2	3	3	35
AHA-14246	Channel	545201	2919191	0.01	<0.2	3	3	46
AHA-14247	Channel	544908	2919386	0.07	<0.2	6	3	21
AHA-14248	Channel	544909	2919386	0.33	<0.2	6	13	34
AHA-14249	Channel	544910	2919386	0.05	<0.2	7	3	23
AHA-14250	Channel	544911	2919389	0.02	<0.2	2	2	22
AHA-14251	Channel	544914	2919390	0.03	<0.2	12	4	18
AHA-14252	Channel	544916	2919391	1.12	3.0	16	7	78
AHA-14253	Channel	544918	2919393	0.00	<0.2	5	1	20
AHA-14254	Channel	544920	2919393	0.00	<0.2	5	1	18
AHA-14255	Channel	544948	2919407	0.15	<0.2	19	1	351
AHA-14256	Channel	544944	2919407	0.52	0.2	115	7	1495
AHA-14257	Channel	544944	2919407	0.08	0.2	31	2	883
AHA-14258	Channel	544853	2919302	0.01	<0.2	15	2	65
AHA-14259	Channel	544851	2919302	0.01	<0.2	26	5	90
AHA-14260	Channel	544849	2919302	0.02	<0.2	11	3	54
AHA-14261	Channel	544849	2919302	0.10	<0.2	27	5	209
AHA-14262	Channel	544857	2919372	0.01	<0.2	3	2	32
AHA-14263	Channel	544856	2919372	0.02	<0.2	5	2	45
AHA-14264	Channel	544854	2919371	0.08	<0.2	8	1	277
AHA-14265	Channel	544852	2919374	0.14	<0.2	11	2	625
AHA-14266	Channel	544849	2919373	0.05	<0.2	7	2	120
AHA-14267	Channel	544848	2919373	0.01	<0.2	6	3	62
AHA-14269	Channel	544847	2919372	0.01	<0.2	4	2	49
AHA-14270	Channel	544845	2919373	0.03	<0.2	9	2	94
AHA-14271	Channel	544843	2919370	0.28	<0.2	8	2	610
AHA-14272	Channel	544840	2919376	0.16	<0.2	11	4	417
AHA-14273	Channel	544837	2919372	0.09	<0.2	14	2	211
AHA-14274	Channel	544837	2919371	0.06	<0.2	33	4	63
AHA-14275	Channel	544835	2919369	1.26	<0.2	22	5	499
AHA-14276	Channel	544847	2919302	0.02	<0.2	21	5	124
AHA-14277	Channel	545229	2919579	0.03	<0.2	18	1	20
AHA-14279	Channel	545228	2919579	0.21	<0.2	393	4	15
AHA-14280	Channel	545227	2919579	0.01	<0.2	25	3	16
AHA-14281	Channel	545229	2919573	0.18	<0.2	139	3	20
AHA-14282	Grab	545227	2919587	1.85	1.2	253	15	25
AHA-14283	Channel	545234	2919553	0.01	<0.2	34	2	26
AHA-14284	Channel	545232	2919552	0.01	<0.2	60	4	25
AHA-14285	Channel	545230	2919550	0.01	<0.2	13	4	22
AHA-14286	Channel	545290	2919540	0.00	<0.2	5	3	10
AHA-14287	Channel	544335	2918677	6.94	3.0	5	44	24
AHA-14289	Channel	544328	2918697	0.31	<0.2	7	3	12


Sample ID	Sample
Type	Easting	Northing	Au
(g/t)	Ag
(g/t)	Cu
(ppm)	Pb
(ppm)	Zn
(ppm)
AHA-14290	Channel	544348	2918687	0.08	<0.2	20	3	11
AHA-14291	Channel	544723	2919339	0.04	<0.2	11	3	34
AHA-14292	Channel	544723	2919341	1.45	<0.2	26	10	33
AHA-14293	Channel	544725	2919343	0.17	<0.2	26	6	39
AHA-14294	Channel	544533	2919437	0.01	<0.2	6	3	7
AHA-14295	Channel	544520	2919472	3.78	4.0	52	5	25
AHA-14296	Channel	544522	2919368	0.01	0.2	21	5	37
AHA-14297	Channel	544521	2919365	0.03	<0.2	222	9	126
AHA-14298	Channel	544679	2919270	0.38	5.0	27	3	23
AHA-14300	Channel	544506	2919212	0.08	<0.2	8	6	31
AHA-14301	Channel	544505	2919212	0.40	<0.2	13	12	43
AHA-14302	Channel	544502	2919212	0.02	<0.2	7	5	24
AHA-14303	Channel	544571	2919129	0.03	<0.2	7	5	37
AHA-14304	Channel	544567	2919131	4.61	7.0	14	7	40
AHA-14305	Channel	544566	2919130	0.14	<0.2	6	3	42
AHA-14306	Channel	544565	2919104	0.43	<0.2	18	9	45
AHA-14307	Channel	544565	2919021	0.07	<0.2	20	8	34
AHA-14308	Channel	544564	2919020	0.04	3.0	7	10	22
AHA-14309	Channel	544564	2919020	0.04	<0.2	10	4	25
AHA-14311	Channel	544613	2918862	0.10	0.2	3	3	4
AHA-14312	Channel	544616	2918856	0.03	<0.2	24	3	21
AHA-14313	Channel	544585	2918920	0.03	<0.2	27	4	28
AHA-14314	Channel	544583	2918920	0.06	<0.2	9	4	24
AHA-14315	Channel	545211	2918471	0.03	<0.2	7	2	12
AHA-14316	Channel	545209	2918471	0.44	5.0	49	8	11
AHA-14317	Channel	545206	2918471	0.04	<0.2	13	4	13
AHA-14318	Channel	545191	2918519	0.03	<0.2	4	3	12
AHA-14319	Channel	545193	2918518	0.11	<0.2	8	3	20
AHA-14321	Channel	545195	2918520	0.29	<0.2	12	5	40
AHA-14322	Channel	545197	2918518	0.09	<0.2	7	3	10
AHA-14323	Channel	545200	2918518	0.28	0.2	9	14	13
AHA-14324	Channel	545190	2918556	0.11	3.0	13	14	18
AHA-14325	Channel	545183	2918580	0.28	4.0	16	11	60
AHA-14326	Channel	545186	2918580	0.54	3.0	14	5	57
AHA-14327	Channel	545180	2918621	0.22	<0.2	24	10	30
AHA-14328	Channel	545180	2918621	5.34	2.1	6	9	11
AHA-14329	Channel	545184	2918623	0.14	<0.2	23	3	17
AHA-14331	Channel	545176	2918637	0.40	0.2	21	14	22
AHA-14332	Channel	545179	2918637	0.77	5.0	19	26	26
AHA-14333	Channel	545180	2918637	0.06	<0.2	23	4	15
AHA-14334	Channel	545158	2918695	29.50	4.2	27	118	80
AHA-14335	Channel	545155	2918686	0.01	0.2	2	2	1
AHA-14336	Channel	545156	2918686	0.09	<0.2	6	5	8
AHA-14337	Channel	545161	2918688	1.45	7.0	29	8	36
AHA-14338	Channel	545161	2918687	0.58	<0.2	16	5	25
AHA-14339	Channel	545143	2918749	0.35	3.0	10	6	21
AHA-14341	Channel	545142	2918765	0.21	0.2	11	61	33
AHA-14342	Channel	545141	2918765	0.09	4.0	7	114	62
AHA-14343	Channel	545136	2918767	1.00	3.0	9	38	67
AHA-14344	Channel	545136	2918767	0.52	2.0	7	17	28
AHA-14345	Channel	545133	2918767	7.94	13.3	9	207	122
AHA-14346	Channel	545129	2918765	1.34	2.7	9	121	103
AHA-14347	Channel	545141	2918767	0.21	<0.2	3	5	26
AHA-14348	Grab	545137	2918772	0.12	1.6	17	601	257
AHA-14349	Grab	545137	2918811	0.13	5.0	32	22	204
AHA-14351	Grab	545132	2918809	4.09	4.3	3	179	179
AHA-14352	Channel	545135	2918821	0.76	5.0	13	64	138
AHA-14353	Channel	545133	2918815	0.28	2.0	5	7	21


Sample ID	Sample
Type	Easting	Northing	Au
(g/t)	Ag
(g/t)	Cu
(ppm)	Pb
(ppm)	Zn
(ppm)
AHA-14354	Channel	545368	2917923	0.04	<0.2	3	3	28
AHA-14355	Channel	545368	2917923	0.86	3.0	37	6	29
AHA-14356	Channel	545374	2917919	0.11	2.0	11	5	106
AHA-14357	Grab	545374	2917923	0.29	4.0	90	38	27
AHA-14358	Channel	545379	2917823	1.19	5.0	19	20	68
AHA-14359	Channel	545379	2917822	0.67	2.0	22	5	86
AHA-14361	Channel	545381	2917823	0.18	<0.2	17	5	51
AHA-14362	Grab	545197	2918415	0.06	2.0	11	4	30
AHA-14546	Grab	546560	2920852	0.50	2.3	51	468	88
AHA-14547	Grab	546560	2920852	150.50	47.0	108	1120	486