View Past PerformanceGreat Atlantic Resources バランスシートの健全性財務の健全性 基準チェック /06Great Atlantic Resourcesの総株主資本はCA$-5.8M 、総負債はCA$671.0Kで、負債比率は-11.5%となります。総資産と総負債はそれぞれCA$314.4KとCA$6.1Mです。主要情報-11.51%負債資本比率CA$671.05k負債インタレスト・カバレッジ・レシオn/a現金CA$6.88kエクイティ-CA$5.83m負債合計CA$6.14m総資産CA$314.37k財務の健全性に関する最新情報更新なしすべての更新を表示Recent updatesお知らせ • 16hGreat Atlantic Resources Corp. Provides Update on Diamond Drilling At Pilley's Island ProjectGreat Atlantic Resources Corp. provided an update on diamond drilling by HM Exploration Corp. at Great Atlantic's Pilley's Island Project at Pilley's Island, north-central Newfoundland. HM Exploration holds an option to earn a 100% interest in the project. HM Exploration has provided an update for the ninth to twelfth drill holes (PI-26-009 to PI-26-012) completed this year at the project. The four holes were all drilled within the area of Great Atlantic's Pilley's Island Project. Drill holes PI-26-009 to PI-26-012 discussed in this news release represent an additional 1,115.60 metres for a total drilled meterage of 2,747.87 metres. Holes nine and ten have successfully intersected the new blind discovery of massive sulphide mineralization extending the strike length of the lower-zone to approximately 40m northwest. The upper-zone mineralized trend can be traced consistently over approximately 130m northwest. The mineralization observed in the lower-lens of holes nine and ten displays similar characteristics as PI-26-008. Multiple mineralized intervals were encountered displaying varying types of mineralization ranging from disseminated – semi-massive – massive sulphide, including: PI-26-009 from 17.00 – 22.45m down-hole; 5.45m drilled length. From 155.03 – 157.66m down-hole; 2.63m drilled length. PI-26-010 from 141.81 – 145.90m down-hole; 4.09m drilled length. Abundant angular copper-bearing clasts observed, potentially indicating limited transport from the source and proximity to a hydrothermal vent environment. Planning is underway for a downhole electromagnetic (EM) survey, followed by a Phase Two diamond drilling program designed to further test the expanding mineralized system. Assay results for the Phase One drilling program are expected to be released shortly. HM Exploration states the 2026 Phase One Drilling program was focused on evaluating the continuity of the mineralized system below known surface showings and along strike of the Clifford Jones Zone to improve their understanding of the geological controls on mineralization. Visual observations from drilled holes indicate that the upper targeted copper-bearing debris flow was successfully intersected, with zones of alteration and massive to semi-massive sulphide mineralization observed in the drill core. HM Exploration states that drill holes 9 and 10 have successfully intersected a lower mineralized sulphide lens that was previously undiscovered. Core samples have been submitted to the laboratory for analysis. Assay results will be released once they have been returned to HM Exploration. HM Exploration states the holes intersected a wide range of massive, semi-massive and disseminated sulphide mineralization over the following drill core lengths: PI-26-009 from 17.00 – 22.45m down-hole; 5.45m drilled length. From 155.03 – 157.66m down-hole; 2.63m drilled length. PI-26-010 from 141.81 – 145.90m down-hole; 4.09m drilled length. PI-26-011 from 143.57 – 144.94m down-hole; 1.37m drilled length. PI-26-012 from 22.32 – 23.15m down-hole; 0.83m drilled length. HM Exploration states observations from drill core continue to support the interpretation that the new lower mineralized sulphide lens may represent debris deposited closer to the original hydrothermal vent system. HM Exploration states that mineralization can be described as clast-dominated debris zones predominantly consisting of sub-angular to angular fragments of massive sulphide composed of Cpy + Py ± Sph ± Gn suspended in interstitial fine-grained disseminated sulphides (Py + Cpy ± Sph ± Gn) and milled felsic ± mafic rock. Matrix-dominated debris flow composed of fragments of sub-rounded to angular clasts of massive sulphide (Py + Cpy ± Sph ± Gn) and felsic ± mafic lithic fragments suspended in a matrix of fine-grained sulphide (Py + Cpy ± Sph ± Gn) and milled felsic ± mafic rock. More detailed classifications for individual intercepts are referenced in Table 2. HM Exploration and Great Atlantic caution that the presence of visible sulphides and visual estimates of mineral abundance are not indicative of grade and should not be considered a substitute for laboratory analysis. Assay results are pending. True widths of mineralized intersections are currently unknown. HM Exploration states the 2026 drill collar data; Coordinates reported in NAD83 - Zone 21N. HM Exploration states mineralized interval descriptions. HM Exploration states the Project is located within the Notre Dame Subzone of the Dunnage Tectonostratigraphic Zone. Most of the Project is underlain by Ordovician submarine volcanic rocks of the Roberts Arm Group which is regionally identified as part of a mature arc sequence referred to as the Buchans-Roberts Arm Belt that also hosts the historic Buchans mine. Mineralization occurs as lower grade (Spencer's Dock); medium grade (Old Mines); and high grade (3B-Zone/Clifford Jones) deposits that are of both sub-seafloor replacement and exhalative varieties. The deposits are often flanked by extensive chlorite, sericite, silica, K-feldspar and epidote alteration often observed in bimodal-felsic VMS systems. The Spencer's Dock area displays sericite/silica alteration that generally increases in intensity near mineralized zones, while the 3B/Old Mine areas display sericite/silica alteration that is abundant but less widespread and is more intense when proximal to mineralized zones. VMS deposits are a globally significant source of copper, zinc, lead, silver, and gold. The Project's geology shares key characteristics with known Volcanogenic Massive Sulphide districts in Newfoundland, including the past producing Buchans, Ming and Rambler Mines, supporting the exploration potential of the Project.お知らせ • Jun 03Great Atlantic Resources Reports Geophysical Results At Mount Raymond PropertyGreat Atlantic Resources Corp. provided an update regarding exploration progress at the Company's Mount Raymond Property, north-central New Brunswick, where Slam Exploration Ltd. holds an option to earn a 100% interest in the project through a combination of common share issuances and incurrence of exploration expenditures on the property. Slam Exploration Ltd. completed a VTEMTM-Plus airborne electromagnetic geophysical survey during early 2026 at its Goodwin copper-nickel-cobalt project. This survey covered much of Great Atlantic's Mount Raymond Property (mineral claim no. 8569). Slam Exploration is using the new VTEM survey over the Goodwin copper-nickel-cobalt project to generate targets and to plan the 2026 diamond drilling program. From a total of 432 anomalies, Slam Exploration has constructed plate models for 24 conductors that range in depth from 30 meters to 320 meters. Slam Exploration states that all of these models are potential extensions to the known zones of mineralization and could represent ovoid-type deposits with higher-grade mineralization at depth. Twenty-one VTEM electromagnetic conductors reported by Slam Exploration are within or along the boundaries of Great Atlantic's Mount Raymond Property. Most of these conductors are within two target areas identified by Slam Exploration (Target T07 and Target T08). The Mount Raymond Property was acquired by Great Atlantic during 2018 by staking. The property covers an area of approximately 175 hectares. The property covers a reported cobalt - copper - nickel mineral occurrence (New Brunswick Department of Natural Resources and Energy Development, Mineral Occurrence Database, Reference No. 1529). Drill core samples anomalous for vanadium are also reported (Gracia, 2012). A 2011 diamond drill hole (VM-11-16) reported within the area of the Mount Raymond Property was reported to intersect 1.65 meters of semi-massive sulfides (pyrrhotite) with chalcopyrite veinlets within gabbro (Gracia, 2012). This mineralized interval was reported to return 0.43% copper, 0.12% nickel and 0.11% cobalt over 1.65 meters (core length). Another one-meter core length sample from this hole was reported to return 0.18% cobalt while another one-meter core length sample from this hole was reported to return 0.12% vanadium (Gracia, 2012). These mineralized intervals are reported near surface (within 100 meters vertical depth). A qualified person has not verified this mineralization for Great Atlantic. David Martin, P.Geo. (New Brunswick and Newfoundland and Labrador), a Qualified Person as defined by NI 43-101 and VP Exploration for Great Atlantic, reviewed and approved the technical information contained in this News Release. Great Atlantic has not verified the VTEM electromagnetic anomalies stated in this news release.お知らせ • Feb 03Great Atlantic Resources Corp., Annual General Meeting, Mar 31, 2026Great Atlantic Resources Corp., Annual General Meeting, Mar 31, 2026.財務状況分析短期負債: GRAR.Fは マイナスの株主資本 を有しており、これは 短期資産 が 短期負債 をカバーしていないことよりも深刻な状況です。長期負債: GRAR.Fは株主資本がマイナスであり、これは短期資産が 長期負債 をカバーしていないことよりも深刻な状況です。デット・ツー・エクイティの歴史と分析負債レベル: GRAR.Fは 株主資本がマイナス となっており、これは高い負債レベルよりも深刻な状況です。負債の削減: GRAR.Fの株主資本はマイナスなので、時間の経過とともに負債が減少したかどうかを確認する必要はありません。貸借対照表キャッシュ・ランウェイ分析過去に平均して赤字であった企業については、少なくとも1年間のキャッシュ・ランウェイがあるかどうかを評価する。安定したキャッシュランウェイ: GRAR.Fは、現在の フリーキャッシュフロー に基づくと、キャッシュランウェイ が 1 年未満です。キャッシュランウェイの予測: フリーキャッシュフローが毎年11.4 % の歴史的率で成長し続ける場合、 GRAR.Fのキャッシュランウェイは 1 年未満になります。健全な企業の発掘7D1Y7D1Y7D1YMaterials 業界の健全な企業。View Dividend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2026/01/31 05:01終値2025/11/03 00:00収益2025/11/30年間収益2025/02/28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Great Atlantic Resources 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 • 16hGreat Atlantic Resources Corp. Provides Update on Diamond Drilling At Pilley's Island ProjectGreat Atlantic Resources Corp. provided an update on diamond drilling by HM Exploration Corp. at Great Atlantic's Pilley's Island Project at Pilley's Island, north-central Newfoundland. HM Exploration holds an option to earn a 100% interest in the project. HM Exploration has provided an update for the ninth to twelfth drill holes (PI-26-009 to PI-26-012) completed this year at the project. The four holes were all drilled within the area of Great Atlantic's Pilley's Island Project. Drill holes PI-26-009 to PI-26-012 discussed in this news release represent an additional 1,115.60 metres for a total drilled meterage of 2,747.87 metres. Holes nine and ten have successfully intersected the new blind discovery of massive sulphide mineralization extending the strike length of the lower-zone to approximately 40m northwest. The upper-zone mineralized trend can be traced consistently over approximately 130m northwest. The mineralization observed in the lower-lens of holes nine and ten displays similar characteristics as PI-26-008. Multiple mineralized intervals were encountered displaying varying types of mineralization ranging from disseminated – semi-massive – massive sulphide, including: PI-26-009 from 17.00 – 22.45m down-hole; 5.45m drilled length. From 155.03 – 157.66m down-hole; 2.63m drilled length. PI-26-010 from 141.81 – 145.90m down-hole; 4.09m drilled length. Abundant angular copper-bearing clasts observed, potentially indicating limited transport from the source and proximity to a hydrothermal vent environment. Planning is underway for a downhole electromagnetic (EM) survey, followed by a Phase Two diamond drilling program designed to further test the expanding mineralized system. Assay results for the Phase One drilling program are expected to be released shortly. HM Exploration states the 2026 Phase One Drilling program was focused on evaluating the continuity of the mineralized system below known surface showings and along strike of the Clifford Jones Zone to improve their understanding of the geological controls on mineralization. Visual observations from drilled holes indicate that the upper targeted copper-bearing debris flow was successfully intersected, with zones of alteration and massive to semi-massive sulphide mineralization observed in the drill core. HM Exploration states that drill holes 9 and 10 have successfully intersected a lower mineralized sulphide lens that was previously undiscovered. Core samples have been submitted to the laboratory for analysis. Assay results will be released once they have been returned to HM Exploration. HM Exploration states the holes intersected a wide range of massive, semi-massive and disseminated sulphide mineralization over the following drill core lengths: PI-26-009 from 17.00 – 22.45m down-hole; 5.45m drilled length. From 155.03 – 157.66m down-hole; 2.63m drilled length. PI-26-010 from 141.81 – 145.90m down-hole; 4.09m drilled length. PI-26-011 from 143.57 – 144.94m down-hole; 1.37m drilled length. PI-26-012 from 22.32 – 23.15m down-hole; 0.83m drilled length. HM Exploration states observations from drill core continue to support the interpretation that the new lower mineralized sulphide lens may represent debris deposited closer to the original hydrothermal vent system. HM Exploration states that mineralization can be described as clast-dominated debris zones predominantly consisting of sub-angular to angular fragments of massive sulphide composed of Cpy + Py ± Sph ± Gn suspended in interstitial fine-grained disseminated sulphides (Py + Cpy ± Sph ± Gn) and milled felsic ± mafic rock. Matrix-dominated debris flow composed of fragments of sub-rounded to angular clasts of massive sulphide (Py + Cpy ± Sph ± Gn) and felsic ± mafic lithic fragments suspended in a matrix of fine-grained sulphide (Py + Cpy ± Sph ± Gn) and milled felsic ± mafic rock. More detailed classifications for individual intercepts are referenced in Table 2. HM Exploration and Great Atlantic caution that the presence of visible sulphides and visual estimates of mineral abundance are not indicative of grade and should not be considered a substitute for laboratory analysis. Assay results are pending. True widths of mineralized intersections are currently unknown. HM Exploration states the 2026 drill collar data; Coordinates reported in NAD83 - Zone 21N. HM Exploration states mineralized interval descriptions. HM Exploration states the Project is located within the Notre Dame Subzone of the Dunnage Tectonostratigraphic Zone. Most of the Project is underlain by Ordovician submarine volcanic rocks of the Roberts Arm Group which is regionally identified as part of a mature arc sequence referred to as the Buchans-Roberts Arm Belt that also hosts the historic Buchans mine. Mineralization occurs as lower grade (Spencer's Dock); medium grade (Old Mines); and high grade (3B-Zone/Clifford Jones) deposits that are of both sub-seafloor replacement and exhalative varieties. The deposits are often flanked by extensive chlorite, sericite, silica, K-feldspar and epidote alteration often observed in bimodal-felsic VMS systems. The Spencer's Dock area displays sericite/silica alteration that generally increases in intensity near mineralized zones, while the 3B/Old Mine areas display sericite/silica alteration that is abundant but less widespread and is more intense when proximal to mineralized zones. VMS deposits are a globally significant source of copper, zinc, lead, silver, and gold. The Project's geology shares key characteristics with known Volcanogenic Massive Sulphide districts in Newfoundland, including the past producing Buchans, Ming and Rambler Mines, supporting the exploration potential of the Project.
お知らせ • Jun 03Great Atlantic Resources Reports Geophysical Results At Mount Raymond PropertyGreat Atlantic Resources Corp. provided an update regarding exploration progress at the Company's Mount Raymond Property, north-central New Brunswick, where Slam Exploration Ltd. holds an option to earn a 100% interest in the project through a combination of common share issuances and incurrence of exploration expenditures on the property. Slam Exploration Ltd. completed a VTEMTM-Plus airborne electromagnetic geophysical survey during early 2026 at its Goodwin copper-nickel-cobalt project. This survey covered much of Great Atlantic's Mount Raymond Property (mineral claim no. 8569). Slam Exploration is using the new VTEM survey over the Goodwin copper-nickel-cobalt project to generate targets and to plan the 2026 diamond drilling program. From a total of 432 anomalies, Slam Exploration has constructed plate models for 24 conductors that range in depth from 30 meters to 320 meters. Slam Exploration states that all of these models are potential extensions to the known zones of mineralization and could represent ovoid-type deposits with higher-grade mineralization at depth. Twenty-one VTEM electromagnetic conductors reported by Slam Exploration are within or along the boundaries of Great Atlantic's Mount Raymond Property. Most of these conductors are within two target areas identified by Slam Exploration (Target T07 and Target T08). The Mount Raymond Property was acquired by Great Atlantic during 2018 by staking. The property covers an area of approximately 175 hectares. The property covers a reported cobalt - copper - nickel mineral occurrence (New Brunswick Department of Natural Resources and Energy Development, Mineral Occurrence Database, Reference No. 1529). Drill core samples anomalous for vanadium are also reported (Gracia, 2012). A 2011 diamond drill hole (VM-11-16) reported within the area of the Mount Raymond Property was reported to intersect 1.65 meters of semi-massive sulfides (pyrrhotite) with chalcopyrite veinlets within gabbro (Gracia, 2012). This mineralized interval was reported to return 0.43% copper, 0.12% nickel and 0.11% cobalt over 1.65 meters (core length). Another one-meter core length sample from this hole was reported to return 0.18% cobalt while another one-meter core length sample from this hole was reported to return 0.12% vanadium (Gracia, 2012). These mineralized intervals are reported near surface (within 100 meters vertical depth). A qualified person has not verified this mineralization for Great Atlantic. David Martin, P.Geo. (New Brunswick and Newfoundland and Labrador), a Qualified Person as defined by NI 43-101 and VP Exploration for Great Atlantic, reviewed and approved the technical information contained in this News Release. Great Atlantic has not verified the VTEM electromagnetic anomalies stated in this news release.
お知らせ • Feb 03Great Atlantic Resources Corp., Annual General Meeting, Mar 31, 2026Great Atlantic Resources Corp., Annual General Meeting, Mar 31, 2026.