Phase 1 Results Confirm Highly Fractionated Pegmatites at Cisco West and Obamska; Phase 2 Assays Pending

Libra Energy Materials Inc. (CSE: LIBR) (OTCQB: LIBRF) (FSE: W0R0) ("Libra" or the "Company") is pleased to report results from the first field program ("Phase 1") completed at the Cisco West and Obamska lithium projects (collectively, the "Projects") in the Eeyou Istchee James Bay region of Québec. Phase 1 identified large, highly fractionated lithium-cesium-tantalum ("LCT") pegmatites at Obamska, where the lowest muscovite KRb ratios, the highest bulk-rock lithium values and several beryl occurrences coincide in the southern part of the property. The Company is releasing these results while it awaits assays from its larger follow-up program ("Phase 2"), completed in September 2026.

Highlights

  • Obamska – fractionation: Portable LIBS analyses of muscovite returned average K/Rb ratios as low as 10.9 and K/Cs ratios as low as 73, with nine of 44 samples returning K/Rb ratios below 15 (Figure 3);
  • Obamska – assays: Bulk-rock grab samples returned up to 739 ppm Li (0.16% Li₂O), 17,943 ppm Be (4.98% BeO), 221 ppm Cs, 2,561 ppm Rb, 39.9 ppm Ta and 135 ppm Nb, with four of ten samples exceeding 450 ppm Li (Figure 2);
  • Obamska – beryl: Beryl, including crystals up to 7-9 cm long, was identified in several pegmatites over a north-south distance of more than 2 km; all these occurrences were subsequently visited by the Company's Qualified Person during Phase 2 (Figure 4);
  • Priority target: Eight of the nine Obamska muscovite samples with K/Rb below 15 form a cluster measuring approximately 650 m by 400 m in the southern part of the property, which also hosts the two highest lithium assays and multiple beryl-bearing pegmatites;
  • Phase 2 completed, assays pending: An eight-person team of professional geologists and prospectors, supervised in the field by the Company's Vice President of Exploration, completed a follow-up program on the Projects from August 26 to September 12, 2026; assay results are expected in the coming months.

Phase 1 was carried out in June 2026, prior to the Company entering into the option agreement on the Projects announced on August 12, 2026 (the "Option Agreement"). The program was completed by two prospectors over five days, from June 8 to June 12, 2026, and consisted of a combination of helicopter-assisted and road-access prospecting. A total of 17 bulk-rock grab samples were collected on the Projects (eleven at Obamska and six at Cisco West) and submitted to SGS Canada Inc. ("SGS") for multi-element analysis, and 51 muscovite samples (44 at Obamska and seven at Cisco West) were analyzed with a portable laser-induced breakdown spectroscopy ("LIBS") analyzer to assess pegmatite fractionation. The LIBS results reported herein include, and supersede, the preliminary LIBS results referenced in the Company's news release dated August 12, 2026.

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FIGURE 1 – Regional map of the lower James Bay lithium district showing the locations of Libra's Cisco West and Obamska Projects relative to major lithium deposits including Galaxy, Whabouchi, Moblan, Rose, and Q2 Metals' Cisco Project, as well as the distribution of the region's greenstone belts. References for all cited mineral resource estimates are provided in the Sources section of this press release.

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"Phase 1 was a short, two-person program, but it gave us exactly the information we were looking for. It showed that Obamska hosts large, beryl-bearing pegmatites with muscovite K/Rb ratios down to about 11 and, importantly, that the most fractionated muscovite, the highest lithium values and the beryl occurrences all coincide in the same part of the property. I have since visited all of these outcrops myself during our Phase 2 program, and we look forward to receiving those assays by year-end," said Dr. Jérémie Pfister, Vice President of Exploration of Libra.

"These first results support our decision to make Cisco West and Obamska our flagship projects. Phase 1 defined a clear target area at Obamska after only five days in the field, and our much larger Phase 2 program was designed to follow up on these highly fractionated pegmatites, as well as to explore the Nottaway shear zone at Cisco West, the same structure that hosts Q2 Metals' Cisco pegmatite, and the northern part of Obamska. We look forward to sharing those results once received," said Koby Kushner, CEO of Libra.

Phase 1 Bulk-Rock Assay Results

Sixteen bulk-rock grab samples were analyzed for lithium and other rare elements (Annex 1). At Obamska, lithium values range from 44 to 739 ppm Li, and four of the ten samples returned more than 450 ppm Li: A00453711 (739 ppm Li; 0.16% Li₂O), A00453710 (568 ppm Li), A00453706 (481 ppm Li) and A00453508 (454 ppm Li). As shown on Figure 2, the highest lithium values (372-739 ppm Li) are located in the southern part of the property.

Obamska pegmatites are also enriched in other rare elements, with values of up to 17,943 ppm Be (4.98% BeO), 221 ppm Cs, 2,561 ppm Rb, 39.9 ppm Ta and 135 ppm Nb. The highest beryllium and cesium values were returned from sample A00453706, which included some of the large beryl crystals observed at this location, and three other samples returned more than 900 ppm Be (A00453506: 2,334 ppm; A00453507: 1,775 ppm; A00453504: 942 ppm), consistent with the beryl observed at these locations (Figure 4).

At Cisco West, the six bulk-rock samples returned between 24 and 69 ppm Li (Figure 2). Sample A00453503, collected from a very large beryl-bearing pegmatite, returned 260 ppm Be and 842 ppm Rb, and sample A00453701 returned 56.7 ppm Ta, 46 ppm Cs and 60 ppm Nb.

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FIGURE 2 – Phase 1 (June 2026) bulk-rock lithium results (ppm Li) at the Obamska and Cisco West Projects, shown with the claim boundaries, the Nottaway shear zone, the Billy Diamond Highway and Q2 Metals' Cisco project. Samples are classified as <138 ppm, 138-372 ppm and 372-739 ppm Li.

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Phase 1 LIBS Analyses of Muscovite

As a pegmatite-forming melt evolves, incompatible elements such as rubidium and cesium become progressively enriched relative to potassium, so muscovite from more highly evolved pegmatites, which are considered more prospective for lithium, has lower K/Rb and K/Cs ratios. A calibrated, portable SciAps Z-903 LIBS analyzer was used to measure rare element concentrations and fractionation ratios in muscovite. These LIBS data are semi-quantitative and are intended to support decision-making only: to establish general fractionation trends across the Projects and to rapidly vector toward areas hosting more highly evolved pegmatites. They are not a substitute for laboratory assays. Three measurements were made on each muscovite sample, and the average of the three measurements is reported herein (Annex 2).

At Obamska, 44 muscovite samples returned average K/Rb ratios between 10.9 and 61.7 and average K/Cs ratios between 73 and 4,180. Nine samples returned K/Rb ratios below 15 (Figure 3). Eight of these form a cluster measuring approximately 650 m by 400 m in the southern part of the property, which also hosts the two highest bulk-rock lithium values (A00453710 and A00453711) and several beryl-bearing pegmatites, and which returned the three lowest K/Cs ratios of the program (73, 135 and 150). The ninth sample (K/Rb of 14.5) was collected approximately 1 km to the northwest, at the location of sample A00453706, where large beryl crystals were observed.

At Cisco West, seven muscovite samples returned average K/Rb ratios between 23.1 and 40.0 and average K/Cs ratios between 156 and 3,598 (Figure 3). The lowest K/Cs ratio (156) was returned from the very large beryl-bearing pegmatite sampled by A00453503.

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FIGURE 3 – Phase 1 (June 2026) average K/Rb ratios in muscovite measured by portable LIBS at the Obamska and Cisco West Projects. Samples are classified as 10.9-15, 15-30 and 30-61.7. LIBS results are semi-quantitative.

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Beryl-Bearing Pegmatites at Obamska

Beryl was identified in several pegmatites at Obamska, over a north-south distance of more than 2 km (Figure 4). Notable occurrences include five to six large, slightly greenish beryl crystals measuring 7 to 9 cm at the location of sample A00453706, a large white beryl occurrence in an approximately 25 m-wide outcrop at sample A00453507, and beryl with garnet, muscovite and trace tourmaline in an approximately 15 m-wide outcrop along the contact with mafic volcanic rocks at sample A00453506. Beryl is a characteristic accessory mineral of LCT pegmatites, and its spatial association with the lowest K/Rb ratios and highest lithium values at Obamska supports the interpretation that the southern part of the property hosts an evolved, fertile pegmatite system. All of the beryl-bearing pegmatites shown on Figure 4 were visited by the Company's Qualified Person during Phase 2. Beryl was also observed at Cisco West, in the pegmatite represented by sample A00453503.

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FIGURE 4 – Beryl-bearing pegmatites identified during Phase 1 (June 2026) at the Obamska Project. All locations were subsequently visited by the Company's Qualified Person during Phase 2.

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Phase 2 Program and Next Steps

Following the signing of the Option Agreement, the Company completed a Phase 2 program on the Projects from August 26 to September 12, 2026. The program consisted of prospecting and sampling by an eight-person team of professional geologists (P.Geo.) and prospectors, and was supervised in the field by Dr. Jérémie Pfister, P.Geo., Vice President of Exploration of the Company. During Phase 2, Dr. Pfister visited the beryl-bearing pegmatites identified during Phase 1 as well as the other outcrops visited and sampled by the prospectors during Phase 1. Assay results from Phase 2 are expected by the end of 2026, and the combined Phase 1 and Phase 2 results will be used to plan the next stage of exploration on the Projects.

Sampling, Analytical Methods and QA/QC (Phase 1)

Bulk-rock grab samples weighing approximately 0.4 to 1.8 kg were collected from pegmatite outcrops and submitted to the SGS facility in Red Lake, Ontario. Samples were prepared at the SGS facility in Sudbury, Ontario, and analyzed at the SGS facility in Burnaby, British Columbia, by sodium peroxide fusion with an ICP-AES finish for Li and Be and an ICP-MS finish for Cs, Rb, Ta and Nb (SGS methods GE_ICP91A50 and GE_IMS91A50). Certified reference materials (OREAS 750 and OREAS 751) were inserted into the sample stream at regular intervals, in addition to the laboratory's internal quality control samples. SGS is independent of the Company, and the SGS Burnaby laboratory is accredited to ISO/IEC 17025 for the methods used.

Muscovite samples were analyzed with a calibrated, portable SciAps Z-903 LIBS analyzer. Three measurements were made on each sample, and the average of the three measurements is reported. LIBS data are semi-quantitative, have not been confirmed by laboratory analysis, and should not be relied upon as assay values; they are used by the Company to identify general fractionation trends and to prioritize areas for follow-up.

Qualified Person and Data Verification

The scientific and technical information contained in this news release has been reviewed and approved by Dr. Jérémie Pfister, P.Geo., Vice President of Exploration of the Company, who is a Qualified Person as defined by National Instrument 43-101 - Standards of Disclosure for Mineral Projects ("NI 43-101").

Phase 1 was carried out by two prospectors who are not registered professional geoscientists, prior to the Company entering into the Option Agreement, and was not conducted under the supervision of a Qualified Person. Dr. Pfister supervised the Phase 2 program in the field and, during Phase 2, personally visited the beryl-bearing pegmatites identified during Phase 1 as well as the other outcrops visited and sampled during Phase 1, confirming the sample locations and the main geological observations reported by the prospectors, including the presence of beryl. Dr. Pfister also reviewed the prospectors' field notes and sample descriptions; compared the assay values reported herein against the original SGS certificates of analysis; reviewed the results of the certified reference materials and the laboratory's internal quality control data; and reviewed the LIBS data files and the averaging of the three measurements per sample.

About Libra Energy Materials Inc.

Libra (CSE: LIBR) (OTCQB: LIBRF) (FSE: W0R0) is a Canadian mineral exploration company focused on the discovery and development of the critical minerals necessary for the green energy transition. Libra's flagship Canadian projects include the recently optioned Cisco West and Obamska lithium projects in Québec, located adjacent to Q2 Metals' Cisco deposit - the largest hard-rock lithium deposit in the Western Hemisphere. Libra's Flanders North, Flanders South, and SBC lithium projects in Ontario are being explored under a CAD $33 million earn-in deal with KoBold Metals Company. In addition, Libra holds a broader portfolio of battery metals projects across Canada and Brazil. The Libra team comprises a mix of seasoned executives, engineers, and geoscientists, with extensive experience in mining and mineral exploration, capital markets, asset management, energy, and First Nations engagement.

For more information, please contact Libra Energy Materials Inc.:

Koby Kushner, P.Eng., CFA
Chief Executive Officer and Director
Email: kkushner@libraenergymaterials.com
Telephone: 416-846-6164

Website: libraenergymaterials.com
LinkedIn: linkedin.com/company/libra-energy-materials
Instagram: @libraenergymaterials
X: @LibraEnergyMats

Sources
¹ NI 43-101 Technical Report – Mineral Resource Estimate for the Cisco Lithium Project, Eeyou Istchee James Bay region of Quebec, Canada, prepared for Q2 Metals Corporation by BBA Inc., effective date April 20, 2026, signature date June 3, 2026. Inferred Mineral Resource of 295 million tonnes grading 1.36% Li₂O referenced in Figure 1.
² Moblan Lithium Project – Mineral Resource Estimate Update (JORC 2012), Sayona Mining Ltd., May 2023. Indicated and Inferred Mineral Resource figures referenced in Figure 1.
³ Rose Lithium-Tantalum Project – Feasibility Study and Updated Mineral Resource Estimate (NI 43-101), Critical Elements Lithium Corp., August 2022. Indicated and Inferred Mineral Resource figures referenced in Figure 1.
⁴ Whabouchi Lithium Project – Updated Mineral Resource Estimate (NI 43-101), Nemaska Lithium Inc., October 2019. Measured + Indicated and Inferred Mineral Resource figures referenced in Figure 1.
⁵ Initial Lithium Mineral Resources and Ore Reserves Reporting (JORC 2012), Rio Tinto Group, December 4, 2025. Indicated and Inferred Mineral Resource figures for the Galaxy Deposit referenced in Figure 1.

Cautionary Note Regarding Adjacent Properties

This news release contains information about the Cisco project owned by Q2 Metals Corp. and other lithium deposits that are adjacent or proximal to the Company's Cisco West and Obamska projects. Mineralization on properties adjacent to or near the Company's projects is not necessarily indicative of mineralization on the Company's projects. Readers are cautioned that the Company has no interest in or right to acquire any interest in the Cisco project, and that the presence of mineral resources or mineralization on adjacent properties is not necessarily indicative of the presence of similar mineralization on the Projects. The Company's Qualified Person has not verified the mineral resource estimates or other information relating to the adjacent or nearby properties shown in Figure 1.

Forward-Looking Information

This news release contains forward-looking statements and forward-looking information within the meaning of applicable securities laws. Such statements relate to future events and include, without limitation, statements regarding the interpretation and significance of the exploration results reported herein, the prospectivity of the Projects for lithium and other rare elements, the timing of receipt of Phase 2 assay results, planned exploration programs on the Projects and their timing and scope, the Option Agreement and the Company's ability to satisfy the conditions thereunder, permitting and licensing, community engagement, reliance on third parties, and other risks associated with the natural resources industry. All statements other than historical facts are forward-looking statements.

These forward-looking statements are based on assumptions and expectations considered reasonable by management at the time they were made; however, no assurance can be given that such expectations will prove correct. Forward-looking statements involve known and unknown risks, uncertainties, and other factors that may cause actual results to differ materially from those anticipated. Accordingly, readers should not place undue reliance on such statements.

The forward-looking statements contained in this news release are made as of the date hereof, and the Company undertakes no obligation to update or revise them, except as required by applicable securities laws. Readers are cautioned that the foregoing list of factors is not exhaustive.

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

Annex 1 - Phase 1 Bulk-Rock Assay Results, Obamska and Cisco West (June 2026)

Sample ID Project UTM zone Easting
(m)
Northing
(m)
Li
(ppm)
Li₂O
(%)
Be
(ppm)
Cs
(ppm)
Rb
(ppm)
Ta
(ppm)
Nb
(ppm)
A00453504 Obamska 17N 676 904 5 635 472 241 0.052 942 24.5 424 4.6 68
A00453506 Obamska 17N 678 155 5 633 285 299 0.064 2,334 98 618 24.4 70
A00453507 Obamska 17N 678 284 5 633 042 138 0.030 1,775 48.7 609 16.7 53
A00453508 Obamska 17N 676 428 5 633 192 454 0.098 9 29.8 1,075 13.5 92
A00453704 Obamska 17N 676 803 5 635 247 210 0.045 <5 14.1 399 5.6 55
A00453705 Obamska 17N 677 317 5 633 998 95 0.020 109 19.3 499 39.9 101
A00453706 Obamska 17N 677 316 5 633 991 481 0.104 17,943 221 1,680 28.8 87
A00453707 Obamska 17N 682 094 5 637 948 44 0.009 8 12 983 11.6 60
A00453710 Obamska 17N 677 884 5 632 951 568 0.122 7 53 1,739 11.8 100
A00453711 Obamska 17N 678 167 5 632 933 739 0.159 11 74.8 2,561 17.4 135
A00453502 Cisco West 18N 303 625 5 626 590 69 0.015 <5 12.6 604 2.3 52
A00453503 Cisco West 18N 303 587 5 626 526 42 0.009 260 23.7 842 30.8 46
A00453701 Cisco West 18N 308 060 5 621 752 24 0.005 <5 46 622 56.7 60
A00453702 Cisco West 18N 307 706 5 622 303 25 0.005 7 11.6 214 13.7 34
A00453708 Cisco West 17N 708 274 5 634 518 25 0.005 15 2.2 214 0.5 3
A00453709 Cisco West 17N 694 907 5 644 290 43 0.009 32 7.9 138 1.2 8
All samples are bulk-rock grab samples of pegmatite, analyzed at SGS (Burnaby, BC) by sodium peroxide fusion with an ICP-AES finish (Li, Be) and an ICP-MS finish (Cs, Rb, Ta, Nb). Grab samples are selective by nature and are not necessarily representative of the mineralization on the Projects.
Coordinates are UTM NAD83, Zone 17N or 18N as indicated. Li₂O (%) = Li (ppm) × 2.153 / 10,000.

 

Annex 2 - Phase 1 Portable LIBS Results on Muscovite (K/Rb and K/Cs), Obamska and Cisco West (June 2026)

LIBS
sample
Project UTM
zone
Easting
(m)
Northing
(m)
K/Rb K/Cs
Reading
1
Reading
2
Reading
3
Average Reading
1
Reading
2
Reading
3
Average
1 Obamska 17N 682 094 5 637 947 31.9 43.2 29.0 34.7 2,807 3,790 3,080 3,226
2 Obamska 17N 677 356 5 634 853 29.2 28.0 32.3 29.8 2,002 762 519 1,094
3 Obamska 17N 676 791 5 635 215 22.7 40.4 41.9 35.0 3,076 2,465 2,531 2,691
4 Obamska 17N 676 803 5 635 245 61.8 55.7 67.5 61.7 4,043 2,891 1,715 2,883
5 Obamska 17N 676 650 5 635 333 44.4 41.6 36.3 40.8 1,500 1,242 1,004 1,248
6 Obamska 17N 676 659 5 635 412 36.0 36.8 33.9 35.6 4,029 3,820 1,556 3,135
7 Obamska 17N 676 788 5 635 240 38.7 42.3 43.7 41.6 2,525 4,639 2,744 3,303
8 Obamska 17N 677 316 5 633 989 14.9 15.2 13.4 14.5 652 467 353 491
9 Obamska 17N 677 315 5 633 999 12.3 25.4 19.2 19.0 1,293 1,163 871 1,109
10 Obamska 17N 674 728 5 634 996 17.0 18.2 16.3 17.2 1,070 1,509 745 1,108
11 Obamska 17N 676 854 5 635 358 35.3 43.6 29.5 36.2 2,394 3,025 2,237 2,552
12 Obamska 17N 676 847 5 635 347 35.4 28.4 36.3 33.4 907 1,413 1,492 1,271
13 Obamska 17N 676 878 5 635 372 53.6 56.1 63.1 57.6 3,628 2,891 3,220 3,246
14 Obamska 17N 677 335 5 634 926 36.4 34.0 39.7 36.7 1,587 1,556 2,155 1,766
15 Obamska 17N 676 905 5 635 473 35.9 48.6 32.6 39.0 1,635 2,878 2,941 2,485
16 Obamska 17N 677 815 5 634 011 35.2 25.3 24.6 28.4 3,300 2,911 6,328 4,180
17 Obamska 17N 676 959 5 635 547 22.6 25.0 22.3 23.3 322 287 317 309
18 Obamska 17N 676 877 5 635 402 39.2 42.8 46.1 42.7 2,600 3,189 3,935 3,241
19 Obamska 17N 676 900 5 635 469 48.1 53.7 70.8 57.5 2,894 3,639 2,596 3,043
20 Obamska 17N 674 780 5 635 319 27.8 24.4 25.9 26.1 4,535 1,814 1,566 2,638
21 Obamska 17N 676 882 5 635 391 34.2 31.4 36.4 34.0 3,021 1,548 3,504 2,691
22 Obamska 17N 677 671 5 633 997 20.2 24.3 28.7 24.4 709 833 2,094 1,212
23 Obamska 17N 676 894 5 635 423 40.9 48.2 46.0 45.0 3,232 2,941 3,361 3,178
24 Obamska 17N 677 641 5 633 996 39.7 28.5 40.9 36.4 2,076 2,230 2,578 2,294
25 Obamska 17N 677 612 5 633 992 26.6 21.8 21.8 23.4 2,443 1,116 2,141 1,900
26 Obamska 17N 676 874 5 635 379 32.2 26.9 33.5 30.9 503 356 999 619
27 Obamska 17N 674 757 5 635 394 21.2 22.0 17.9 20.4 1,972 946 985 1,301
28 Obamska 17N 677 725 5 634 028 37.3 45.9 33.7 39.0 3,455 3,106 2,273 2,945
29 Obamska 17N 678 221 5 632 977 20.7 16.6 15.7 17.7 2,398 3,224 2,477 2,700
30 Obamska 17N 678 166 5 632 935 13.9 17.9 17.1 16.3 1,578 1,288 1,187 1,351
31 Obamska 17N 677 894 5 632 956 12.7 15.0 13.6 13.8 542 224 227 331
32 Obamska 17N 678 284 5 633 042 9.2 11.5 12.1 10.9 419 799 873 697
33 Obamska 17N 677 675 5 633 101 14.2 11.7 13.3 13.1 84 69 68 73
34 Obamska 17N 677 868 5 632 946 12.2 12.1 13.1 12.5 109 183 112 135
35 Obamska 17N 677 807 5 632 874 14.5 13.7 15.7 14.6 2,865 2,174 3,894 2,978
36 Obamska 17N 678 155 5 633 285 23.0 20.4 21.2 21.5 3,548 3,187 1,715 2,817
37 Obamska 17N 678 210 5 633 289 13.7 13.9 13.3 13.6 164 175 113 150
38 Obamska 17N 678 141 5 633 290 22.8 28.0 22.0 24.3 2,267 3,628 2,402 2,766
39 Obamska 17N 678 296 5 633 063 9.3 10.8 13.3 11.2 161 217 316 231
40 Obamska 17N 678 326 5 633 083 15.1 10.8 11.8 12.6 272 143 499 305
41 Obamska 17N 678 345 5 633 094 15.1 17.1 16.6 16.3 785 667 1,326 926
42 Obamska 17N 678 249 5 633 024 18.9 14.8 13.5 15.7 970 865 2,637 1,491
43 Obamska 17N 676 376 5 633 191 20.5 16.7 18.7 18.6 613 186 644 481
44 Obamska 17N 678 164 5 633 286 24.3 30.2 22.4 25.6 2,362 2,454 3,386 2,734
72 Cisco West 18N 303 625 5 626 645 36.4 48.6 35.1 40.0 3,559 3,719 3,515 3,598
73 Cisco West 18N 303 625 5 626 593 18.7 24.9 25.8 23.1 4,471 2,005 2,571 3,016
74 Cisco West 18N 303 586 5 626 525 24.6 22.8 23.1 23.5 191 127 150 156
75 Cisco West 18N 303 607 5 626 562 22.8 26.4 26.5 25.3 1,217 496 549 754
76 Cisco West 18N 303 590 5 626 531 23.2 32.8 34.2 30.1 3,644 1,861 1,684 2,396
82 Cisco West 18N 304 573 5 625 068 24.9 22.2 25.8 24.3 600 568 963 710
83 Cisco West 18N 305 380 5 623 979 28.9 40.5 31.2 33.5 218 234 80 177
Three measurements were made on each muscovite sample with a calibrated, portable SciAps Z-903 LIBS analyzer; the average of the three measurements is shown in bold. LIBS results are semi-quantitative and are not equivalent to laboratory assays.
Coordinates are UTM NAD83, Zone 17N or 18N as indicated.

 

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