View Future GrowthSlave Lake Zinc 過去の業績過去 基準チェック /06Slave Lake Zinc は平均年間 25.1% の収益成長を遂げていますが、Metals and Mining 業界では年間 減少率 となっています。8.4% です。主要情報25.07%収益成長率36.25%EPS成長率Metals and Mining 業界の成長26.40%収益成長率n/a株主資本利益率-290.08%ネット・マージンn/a前回の決算情報31 Mar 2026最近の業績更新更新なしすべての更新を表示Recent updatesお知らせ • Jan 08Slave Lake Zinc Corp. Confirms High-Grade District Potential At O'connor Lake; Assays Return Up to 7.75% Lead and 6.62% ZincSlave Lake Zinc Corp. announced encouraging geochemical results from its late 2025 geologic review at the O'Connor Lake exploration property in the South Slave area, Northwest Territories. The program has successfully validated the Company's regional exploration model, identifying high-grade mineralization in multiple new structures several kilometres distant from the historic Shaft Zone. Highlights of the 2025 Program: High-Grade Mineralization Confirmed: Assays from recently identified vein systems returned grades of up to 7.75% Lead (Pb) and 6.62% Zinc (Zn). W widespread Mineralization: Results validate the presence of a district-scale hydrothermal system with multiple mineralized structures identified outside the known Shaft Zone deposit. Significant Byproduct Potential: Sampling revealed widespread copper values ranging from 0.17% to 0.92% Cu, along with elevated silver values (up to 19.5 g/t Ag), suggesting multi-element potential including precious metals. Geological Validation: Fieldwork confirms that the new vein systems share a similar orientation and appearance to the historic Shaft Zone, supporting the hypothesis of a large, deep-seated hydrothermal origin. Strategic Advancement: The program was successfully supported by the Northwest Territories Government's Mineral Incentive Program (MIP). Program Overview and Geological Context. During late September and early October 2025, Slave Lake Zinc contracted Aurora Geosciences Ltd. of Yellowknife to conduct a short 10-day geological reconnaissance program of the O'Connor Lake property. Operating from a float aircraft-supported tent camp, the field crew concentrated on evaluating historic showings along structural corridors located several kilometres from the historic "Shaft Zone." The results from this program help transform the Company's regional strategy into reality. The similarities in orientation and mineralogical character between these new discoveries and the original Shaft Zone vein strongly validate the hypothesis that the O'Connor Lake property hosts a regional-scale mineralizing system. The multi-element nature of the assays-highlighted by high-grade lead and zinc paired with significant copper and silver mineralization-points to a complex and fertile hydrothermal system capable of hosting substantial tonnage. Next steps. The Company is currently analyzing the findings of this successful program to define the next steps for the 2026 exploration program. This analysis involves integrating new geochemical data to optimize the locations of upcoming geological sampling, structural analysis and geophysical surveys and to delineate diamond drilling targets.お知らせ • Aug 21Slave Lake Zinc Corp. announced that it expects to receive CAD 0.5 million in fundingSlave Lake Zinc Corp announced a private placement financing of Flow-through units at issue price CAD 0.06 per share for gross proceeds CAD 350,000 on August 20, 2024. Each unit consists of One share and full warrant. Each warrant CAD 0.08 exercise price, expiring 2 years after closing.お知らせ • Feb 17Slave Lake Zinc Corp., Annual General Meeting, Apr 19, 2024Slave Lake Zinc Corp., Annual General Meeting, Apr 19, 2024.お知らせ • Jul 27Slave Lake Zinc Corp. Initiates Summer Lithium Exploration Program to Expand Critical Metals ProjectSlave Lake Zinc Corp. announced the commencement of its anticipated summer Lithium exploration program, as previously announced on July 17, 2022. This program marks a significant step towards enhancing the Company's "critical metals" project. The summer exploration program will begin with a focus on conducting reconnaissance prospecting and sampling within a 15 square kilometer area located west of the original headframe, where many pegmatite showings are mapped. The initial fieldwork will target a pegmatite dyke swarm within this region, where northwest trending pegmatites are found to intrude all other rock units. The Company's property is part of the regional-scale Yellowknife Lithium initiative, with the east arm of Great Slave Lake providing the only separation of SLZ from known lithium bearing pegmatites in this extensive lithium corridor. Slave Lake Zinc has engaged Aurora Geosciences of Yellowknife as their experienced geological consultants. CEO Ritch Wigham will accompany Aurora Geosciences during this phase of exploration. Aurora Geosciences, with over 30 years of experience in the North, is the sole exploration team based in the region, offering a comprehensive suite of exploration services required for discovery. Their involvement in this project enhances the potential for success. In preparation for the exploration program, Slave Lake Zinc has compiled and diligently studied historic (pre-1954) assessment reports, drill logs, government publications and university theses. The Company's reviews have identified numerous occurrences of pegmatites mapped and noted with no further exploration, which will be sampled as a matter of priority during this exploration program. The SLZ property lies on the projected southward extension of the Yellowknife Lithium corridor, which has been explored primarily on the North shore of Great Slave Lake. Desriptions of numerous pegmatites in the O'Connor Lake area have indicated showings of very coarse-grained material with large crystals of tourmaline, muscovite, and plagioclase. The net proceeds from the private placement will be used for general working capital. Three insiders of the Company purchased a total of 800,000 units for proceeds to the Company of $40,000, which comprises 40.0% of the total amount raised. The participation by such insiders is considered a "related-party transaction" within the meaning of Multilateral Instrument 61-101 - Protection of Minority Security Holders in Special Transactions ("MI 61-101"). The Company has relied on exemptions from the formal valuation and minority shareholder approval requirements of MI 61-101 contained in sections 5.5(a) and 5.7(1)(a) of MI 61-101 in respect of related party participation in the placement as neither the fair market value (as determined under MI 61-101) of the subject matter of the subject matter of, nor the fair market value of the consideration for, the transaction, whereby as it involved the related party, exceeded 25% of the Company's market capitalization (as determined underMI 61-101). The Company's board of directors and specifically the independent members of the board, as applicable, reviewed and approved the private placement subscriptions by the insiders. The Company did not file a material change report more than 21 days before the expected closing of the private placement as the date of closing was not previously known.お知らせ • Jul 26Slave Lake Zinc Corp. announced that it has received CAD 0.1 million in fundingSlave Lake Zinc Corp. announced a non-brokered private placement to issue 2,000,000 units at an issue price of CAD 0.05 per unit for the gross proceeds of CAD 100,000 on July 25, 2023. Each unit is comprised of one common share and one share purchase warrant, where each warrant entitles the holder to purchase one additional common share at a price of CAD 0.12 per share for two years. The securities issued pursuant to the private placement and any shares to be issued on the exercise of warrants are restricted from trading until November 26, 2023. The transaction included participation from three insiders who purchased a total of 800,000 units at an issue price of CAD 0.05 per unit for proceeds to the Company of CAD 40,000, which comprises 40.0% of the total amount raised.お知らせ • Feb 16Slave Lake Zinc Identifies Significant Lithium Potential At O'connor Lake ProjectSlave Lake Zinc Corp. has recognized that coarse-grained pegmatites occur on their O'Connor Lake property which is currently host to critical metals of zinc +/- copper. The pegmatites occur primarily as dykes but also occur as masses in complex multiple-phased intrusive granitic environments. Although no exploration has occurred on these pegmatites, there is potential to host spodumene mineralization, recognized to be the critical mineral for lithium potential. The Company knew of the pegmatite occurrences from the Prusti work (Ph.D. Thesis, 1954) and maintained confidentiality on the lithium potential until the land position was staked. Slave Lake Zinc continues to add recent geophysical and geological data to its historical database as they work to generate exploration targets. The design of a detailed exploration program is currently underway to evaluate the potential of the pegmatites for their lithium content as well as the well-documented coarse, base-metal (Zn-Pb+/- Cu) vein systems, considered to be of magmatic-hydrothermal origin. The structures/lineaments associated with the base-metal veins are well documented locally and are projected to continue to the north and northwest of the MWK # 1 Vein. The exploration program will include ground geophysics, geological mapping and sampling, and drilling to test selected targets. Although no lithium pegmatites have been identified within the Taltson Magmatic Zone, the pegmatites identified by Prusti and government geologists suggest the host rocks in the O'Connor Lake area are similar to the granitic intrusive complex in the Hearne Channel-Beaulieu River area on the north side of Great Slave Lake. The lithium pegmatites on the north side of Great Slave Lake are currently being aggressively evaluated by Li-FT and others.収支内訳Slave Lake Zinc の稼ぎ方とお金の使い方。LTMベースの直近の報告された収益に基づく。収益と収入の歴史OTCPK:SLZN.F 収益、費用、利益 ( )CAD Millions日付収益収益G+A経費研究開発費31 Mar 26000031 Dec 25000030 Sep 25000030 Jun 25000031 Mar 25000031 Dec 24000030 Sep 24000030 Jun 24000031 Mar 24000031 Dec 230-10030 Sep 230-10030 Jun 230-11031 Mar 230-11031 Dec 220-11030 Sep 220-11030 Jun 22001031 Mar 22000031 Dec 210-11030 Sep 210-11030 Jun 210-11031 Mar 210-11031 Dec 20000030 Sep 20000030 Jun 20000031 Mar 20000031 Dec 19000030 Sep 190-11030 Jun 190-11031 Mar 190-11031 Dec 180-11030 Sep 18000030 Jun 18000030 Sep 170000質の高い収益: SLZN.Fは現在利益が出ていません。利益率の向上: SLZN.Fは現在利益が出ていません。フリー・キャッシュフローと収益の比較過去の収益成長分析収益動向: SLZN.Fは利益を出していないが、過去 5 年間で年間25.1%の割合で損失を削減してきた。成長の加速: SLZN.Fの過去 1 年間の収益成長を 5 年間の平均と比較することはできません。現在は利益が出ていないためです。収益対業界: SLZN.Fは利益が出ていないため、過去 1 年間の収益成長をMetals and Mining業界 ( 82.4% ) と比較することは困難です。株主資本利益率高いROE: SLZN.Fは現在利益が出ていないため、自己資本利益率 ( -290.08% ) はマイナスです。総資産利益率使用総資本利益率過去の好業績企業の発掘7D1Y7D1Y7D1YMaterials 、過去の業績が好調な企業。View Financial Health企業分析と財務データの現状データ最終更新日（UTC時間）企業分析2026/06/22 02:03終値2026/06/09 00:00収益2026/03/31年間収益2025/09/30データソース企業分析に使用したデータはS&P Global Market Intelligence LLC のものです。本レポートを作成するための分析モデルでは、以下のデータを使用しています。データは正規化されているため、ソースが利用可能になるまでに時間がかかる場合があります。パッケージデータタイムフレーム米国ソース例会社財務10年損益計算書キャッシュ・フロー計算書貸借対照表SECフォーム10-KSECフォーム10-Qアナリストのコンセンサス予想+プラス3年予想財務アナリストの目標株価アナリストリサーチレポートBlue Matrix市場価格30年株価配当、分割、措置ICEマーケットデータSECフォームS-1所有権10年トップ株主インサイダー取引SECフォーム4SECフォーム13Dマネジメント10年リーダーシップ・チーム取締役会SECフォーム10-KSECフォームDEF 14A主な進展10年会社からのお知らせSECフォーム8-K* 米国証券を対象とした例であり、非米国証券については、同等の規制書式および情報源を使用。特に断りのない限り、すべての財務データは1年ごとの期間に基づいていますが、四半期ごとに更新されます。これは、TTM（Trailing Twelve Month）またはLTM（Last Twelve Month）データとして知られています。詳細はこちら。分析モデルとスノーフレークこのレポートを生成するために使用した分析モデルの詳細は、当社の Github ページ でご覧いただけます。また、レポートの使い方に関する ガイド や YouTube の チュートリアル もご用意しています。シンプリー・ウォールストリート分析モデルを設計・構築した世界トップクラスのチームについてご紹介します。業界およびセクターの指標私たちの業界とセクションの指標は、Simply Wall Stによって6時間ごとに計算されます。アナリスト筋Slave Lake Zinc Corp. 0 これらのアナリストのうち、弊社レポートのインプットとして使用した売上高または利益の予想を提出したのは、 。アナリストの投稿は一日中更新されます。0
お知らせ • Jan 08Slave Lake Zinc Corp. Confirms High-Grade District Potential At O'connor Lake; Assays Return Up to 7.75% Lead and 6.62% ZincSlave Lake Zinc Corp. announced encouraging geochemical results from its late 2025 geologic review at the O'Connor Lake exploration property in the South Slave area, Northwest Territories. The program has successfully validated the Company's regional exploration model, identifying high-grade mineralization in multiple new structures several kilometres distant from the historic Shaft Zone. Highlights of the 2025 Program: High-Grade Mineralization Confirmed: Assays from recently identified vein systems returned grades of up to 7.75% Lead (Pb) and 6.62% Zinc (Zn). W widespread Mineralization: Results validate the presence of a district-scale hydrothermal system with multiple mineralized structures identified outside the known Shaft Zone deposit. Significant Byproduct Potential: Sampling revealed widespread copper values ranging from 0.17% to 0.92% Cu, along with elevated silver values (up to 19.5 g/t Ag), suggesting multi-element potential including precious metals. Geological Validation: Fieldwork confirms that the new vein systems share a similar orientation and appearance to the historic Shaft Zone, supporting the hypothesis of a large, deep-seated hydrothermal origin. Strategic Advancement: The program was successfully supported by the Northwest Territories Government's Mineral Incentive Program (MIP). Program Overview and Geological Context. During late September and early October 2025, Slave Lake Zinc contracted Aurora Geosciences Ltd. of Yellowknife to conduct a short 10-day geological reconnaissance program of the O'Connor Lake property. Operating from a float aircraft-supported tent camp, the field crew concentrated on evaluating historic showings along structural corridors located several kilometres from the historic "Shaft Zone." The results from this program help transform the Company's regional strategy into reality. The similarities in orientation and mineralogical character between these new discoveries and the original Shaft Zone vein strongly validate the hypothesis that the O'Connor Lake property hosts a regional-scale mineralizing system. The multi-element nature of the assays-highlighted by high-grade lead and zinc paired with significant copper and silver mineralization-points to a complex and fertile hydrothermal system capable of hosting substantial tonnage. Next steps. The Company is currently analyzing the findings of this successful program to define the next steps for the 2026 exploration program. This analysis involves integrating new geochemical data to optimize the locations of upcoming geological sampling, structural analysis and geophysical surveys and to delineate diamond drilling targets.
お知らせ • Aug 21Slave Lake Zinc Corp. announced that it expects to receive CAD 0.5 million in fundingSlave Lake Zinc Corp announced a private placement financing of Flow-through units at issue price CAD 0.06 per share for gross proceeds CAD 350,000 on August 20, 2024. Each unit consists of One share and full warrant. Each warrant CAD 0.08 exercise price, expiring 2 years after closing.
お知らせ • Feb 17Slave Lake Zinc Corp., Annual General Meeting, Apr 19, 2024Slave Lake Zinc Corp., Annual General Meeting, Apr 19, 2024.
お知らせ • Jul 27Slave Lake Zinc Corp. Initiates Summer Lithium Exploration Program to Expand Critical Metals ProjectSlave Lake Zinc Corp. announced the commencement of its anticipated summer Lithium exploration program, as previously announced on July 17, 2022. This program marks a significant step towards enhancing the Company's "critical metals" project. The summer exploration program will begin with a focus on conducting reconnaissance prospecting and sampling within a 15 square kilometer area located west of the original headframe, where many pegmatite showings are mapped. The initial fieldwork will target a pegmatite dyke swarm within this region, where northwest trending pegmatites are found to intrude all other rock units. The Company's property is part of the regional-scale Yellowknife Lithium initiative, with the east arm of Great Slave Lake providing the only separation of SLZ from known lithium bearing pegmatites in this extensive lithium corridor. Slave Lake Zinc has engaged Aurora Geosciences of Yellowknife as their experienced geological consultants. CEO Ritch Wigham will accompany Aurora Geosciences during this phase of exploration. Aurora Geosciences, with over 30 years of experience in the North, is the sole exploration team based in the region, offering a comprehensive suite of exploration services required for discovery. Their involvement in this project enhances the potential for success. In preparation for the exploration program, Slave Lake Zinc has compiled and diligently studied historic (pre-1954) assessment reports, drill logs, government publications and university theses. The Company's reviews have identified numerous occurrences of pegmatites mapped and noted with no further exploration, which will be sampled as a matter of priority during this exploration program. The SLZ property lies on the projected southward extension of the Yellowknife Lithium corridor, which has been explored primarily on the North shore of Great Slave Lake. Desriptions of numerous pegmatites in the O'Connor Lake area have indicated showings of very coarse-grained material with large crystals of tourmaline, muscovite, and plagioclase. The net proceeds from the private placement will be used for general working capital. Three insiders of the Company purchased a total of 800,000 units for proceeds to the Company of $40,000, which comprises 40.0% of the total amount raised. The participation by such insiders is considered a "related-party transaction" within the meaning of Multilateral Instrument 61-101 - Protection of Minority Security Holders in Special Transactions ("MI 61-101"). The Company has relied on exemptions from the formal valuation and minority shareholder approval requirements of MI 61-101 contained in sections 5.5(a) and 5.7(1)(a) of MI 61-101 in respect of related party participation in the placement as neither the fair market value (as determined under MI 61-101) of the subject matter of the subject matter of, nor the fair market value of the consideration for, the transaction, whereby as it involved the related party, exceeded 25% of the Company's market capitalization (as determined underMI 61-101). The Company's board of directors and specifically the independent members of the board, as applicable, reviewed and approved the private placement subscriptions by the insiders. The Company did not file a material change report more than 21 days before the expected closing of the private placement as the date of closing was not previously known.
お知らせ • Jul 26Slave Lake Zinc Corp. announced that it has received CAD 0.1 million in fundingSlave Lake Zinc Corp. announced a non-brokered private placement to issue 2,000,000 units at an issue price of CAD 0.05 per unit for the gross proceeds of CAD 100,000 on July 25, 2023. Each unit is comprised of one common share and one share purchase warrant, where each warrant entitles the holder to purchase one additional common share at a price of CAD 0.12 per share for two years. The securities issued pursuant to the private placement and any shares to be issued on the exercise of warrants are restricted from trading until November 26, 2023. The transaction included participation from three insiders who purchased a total of 800,000 units at an issue price of CAD 0.05 per unit for proceeds to the Company of CAD 40,000, which comprises 40.0% of the total amount raised.
お知らせ • Feb 16Slave Lake Zinc Identifies Significant Lithium Potential At O'connor Lake ProjectSlave Lake Zinc Corp. has recognized that coarse-grained pegmatites occur on their O'Connor Lake property which is currently host to critical metals of zinc +/- copper. The pegmatites occur primarily as dykes but also occur as masses in complex multiple-phased intrusive granitic environments. Although no exploration has occurred on these pegmatites, there is potential to host spodumene mineralization, recognized to be the critical mineral for lithium potential. The Company knew of the pegmatite occurrences from the Prusti work (Ph.D. Thesis, 1954) and maintained confidentiality on the lithium potential until the land position was staked. Slave Lake Zinc continues to add recent geophysical and geological data to its historical database as they work to generate exploration targets. The design of a detailed exploration program is currently underway to evaluate the potential of the pegmatites for their lithium content as well as the well-documented coarse, base-metal (Zn-Pb+/- Cu) vein systems, considered to be of magmatic-hydrothermal origin. The structures/lineaments associated with the base-metal veins are well documented locally and are projected to continue to the north and northwest of the MWK # 1 Vein. The exploration program will include ground geophysics, geological mapping and sampling, and drilling to test selected targets. Although no lithium pegmatites have been identified within the Taltson Magmatic Zone, the pegmatites identified by Prusti and government geologists suggest the host rocks in the O'Connor Lake area are similar to the granitic intrusive complex in the Hearne Channel-Beaulieu River area on the north side of Great Slave Lake. The lithium pegmatites on the north side of Great Slave Lake are currently being aggressively evaluated by Li-FT and others.