View Financial HealthBlast Resources 配当と自社株買い配当金 基準チェック /06Blast Resources配当金を支払った記録がありません。主要情報n/a配当利回り-8.7%バイバック利回り総株主利回り-8.7%将来の配当利回りn/a配当成長n/a次回配当支払日n/a配当落ち日n/a一株当たり配当金n/a配当性向n/a最近の配当と自社株買いの更新更新なしすべての更新を表示Recent updatesお知らせ • 9hBlast Resources Inc. Announces Structural Corridor At Wales Lake ProjectBlast Resources Inc. has announced a structural corridor found on the Blast mineral claims. The Company has 3 claim groups on the southwest side of the Athabasca Basin in northern Saskatchewan. Low magnetic susceptibility in regional surveys shows a NE-SW structural corridor that crosses the Blast claims for 9 km. The feature may be caused by alteration and destruction of magnetic minerals. The significance of a structural corridor zone is that it may host concentrations of uranium mineralization in individual or multiple shears or faults to hundreds of metre depths. This structural corridor is a zone of approximately parallel faults or shears in basement rock. The trend extends both NNW (330°) and SSE (150°) of the Blast claims continuous within the Blast claims for a length of 9 km. Width of the zone as indicated by basement conductors (Fission 3) may be 3 km. Info on this target are as a result of the December 2024 airborne magnetic survey done by the Company and historic F3 Uranium field work (public domain). In structural geology, a structural corridor refers to a long, relatively narrow area defined by specific geological structures, such as faults, shears or folds, which can influence the location of geological features and resources. The Athabasca Basin's structural corridors are critical for understanding the sites of uranium mineralization, particularly the relationship to unconformity-related deposits. These corridors, often major fault zones, act as pathways for uranium-bearing fluids and provide geometric traps for ore deposition. The Company is focussed on conductors in basement rock that acted as traps for uranium mineralization. Unconformity-related deposits, uranium mineralization is often associated with the unconformity surface, where older basement rocks are overlain by younger sedimentary rocks. Conductors in the basement rocks can guide fluids from deeper sources to the unconformity, where they can deposit uranium. The Wales Lake project is accessible along the all-weather gravel road provincial highway 955 from La Loche to the past-producing Cluff Lake uranium mine. Highway 955 crosses approximately 1.5km to the east of the project, and access to the west may be on ungazetted bush roads and tracks. The scientific and technical information contained in this news release was prepared and approved by Locke Goldsmith, M.Sc., P.Eng., P. Geo., Arctex Engineering Services and who is a Qualified Person as defined by National Instrument 43-101 - Standards of Disclosure for Mineral Projects. Situated south of Wales Lake and positioned just outside the southwest margin of the Athabasca Basin, the Project is strategically located within the Patterson Lake Corridor which hosts two significant uranium deposits (Triple R Deposit, 2,200,000 @ 1.58 U308 and 0.51 g/t Au & the Arrow Deposit which is the largest source of low-cost uranium globally, delivering up to 30,000,000 pounds of high-grade uranium per year). The deposits represent one of the largest high-grade uranium systems globally, comparable to world-class deposits such as McArthur River, Cigar Lake, and Key Lake.お知らせ • Jul 05Blast Resources Announces Exploration Results At Its Wales Lake Project In The Athabasca Basin RegionBlast Resources Inc. summarized results of exploration programs completed on 3 groups of claims in the southwestern Athabasca Basin region, northern Saskatchewan. In December 2024, a high resolution airborne magnetic survey was flown over the Britt Lake, the Brazier South and North Agar claims collectively referred to as the "Wales Lake Project". Five targets are selected for further investigation, based on magnetic lineaments and regional uranium/thorium anomalies. There are two structural trends, oriented NNW-SSE and NW-SE identified in the project area, likely representing the main tectonic fabric of the Taltson Domain locally. On a regional scale, folding in the Taltson is along a NE-SW axis, identified by magnetic stratigraphic markers. The Wales Lake project is apparently at the closure of a regional fold axis which trends NE-SW. The two major structural elements are noteworthy: a structural corridor, oriented NNW-SSE which disrupts the magnetic stratigraphy and is magnetite-destructive, possibly indicative of alteration; and a tectonic break, oriented NW-SE which appears to be a boundary between basement lithologies. The geological exploration model is designed to test conductors and primarily fault-controlled basement-hosted mineralization such as Rabbit Lake (Eldorado), and Arrow (NexGen Energy) and Triple R (Paladin) occurrences that are hosted in the Taltson Domain. The scientific and technical information contained in this news release was prepared and approved by Locke Goldsmith, M.Sc., P.Eng., P. Geo., and who is a Qualified Person as defined by National Instrument 43-101 – Standards of Disclosure for Mineral Projects. Situated south of Wales Lake and positioned just outside the southwest margin of the Athabasca Basin, the Project is strategically located within the Patterson Lake Corridor which hosts two significant uranium deposits (Triple R Deposit, 2.2 Mt @ 1.58 U308 and 0.51 g/t Au & the Arrow Deposit which is the largest source of low-cost uranium globally, potentially delivering up to 30 million pounds of high-grade uranium per year). The deposits represent the largest high-grade uranium systems globally, comparable to world-class deposits such as McArthur River, Cigar Lake, and Key Lake.お知らせ • Jun 02Blast Resources Inc Announces CFO ChangesBlast Resources Inc. announced the resignation of Derek Tam as Chief Financial Officer of the Company. Casey Forward assumed the role of interim CFO.決済の安定と成長配当データの取得安定した配当: BLSR.Fの 1 株当たり配当が過去に安定していたかどうかを判断するにはデータが不十分です。増加する配当: BLSR.Fの配当金が増加しているかどうかを判断するにはデータが不十分です。配当利回り対市場Blast Resources 配当利回り対市場BLSR.F 配当利回りは市場と比べてどうか？セグメント配当利回り会社 (BLSR.F)n/a市場下位25% (US)1.3%市場トップ25% (US)4.2%業界平均 (Oil and Gas)3.4%アナリスト予想 (BLSR.F) (最長3年)n/a注目すべき配当: BLSR.Fは最近配当金を報告していないため、配当金支払者の下位 25% に対して同社の配当利回りを評価することはできません。高配当: BLSR.Fは最近配当金を報告していないため、配当金支払者の上位 25% に対して同社の配当利回りを評価することはできません。株主への利益配当収益カバレッジ: BLSR.Fの 配当性向 を計算して配当金の支払いが利益で賄われているかどうかを判断するにはデータが不十分です。株主配当金キャッシュフローカバレッジ: BLSR.Fが配当金を報告していないため、配当金の持続可能性を計算できません。高配当企業の発掘7D1Y7D1Y7D1YUS 市場の強力な配当支払い企業。View Management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2026/07/07 09:21終値2026/07/07 00:00収益2026/04/30年間収益2026/01/31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Blast Resources Inc. 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 • 9hBlast Resources Inc. Announces Structural Corridor At Wales Lake ProjectBlast Resources Inc. has announced a structural corridor found on the Blast mineral claims. The Company has 3 claim groups on the southwest side of the Athabasca Basin in northern Saskatchewan. Low magnetic susceptibility in regional surveys shows a NE-SW structural corridor that crosses the Blast claims for 9 km. The feature may be caused by alteration and destruction of magnetic minerals. The significance of a structural corridor zone is that it may host concentrations of uranium mineralization in individual or multiple shears or faults to hundreds of metre depths. This structural corridor is a zone of approximately parallel faults or shears in basement rock. The trend extends both NNW (330°) and SSE (150°) of the Blast claims continuous within the Blast claims for a length of 9 km. Width of the zone as indicated by basement conductors (Fission 3) may be 3 km. Info on this target are as a result of the December 2024 airborne magnetic survey done by the Company and historic F3 Uranium field work (public domain). In structural geology, a structural corridor refers to a long, relatively narrow area defined by specific geological structures, such as faults, shears or folds, which can influence the location of geological features and resources. The Athabasca Basin's structural corridors are critical for understanding the sites of uranium mineralization, particularly the relationship to unconformity-related deposits. These corridors, often major fault zones, act as pathways for uranium-bearing fluids and provide geometric traps for ore deposition. The Company is focussed on conductors in basement rock that acted as traps for uranium mineralization. Unconformity-related deposits, uranium mineralization is often associated with the unconformity surface, where older basement rocks are overlain by younger sedimentary rocks. Conductors in the basement rocks can guide fluids from deeper sources to the unconformity, where they can deposit uranium. The Wales Lake project is accessible along the all-weather gravel road provincial highway 955 from La Loche to the past-producing Cluff Lake uranium mine. Highway 955 crosses approximately 1.5km to the east of the project, and access to the west may be on ungazetted bush roads and tracks. The scientific and technical information contained in this news release was prepared and approved by Locke Goldsmith, M.Sc., P.Eng., P. Geo., Arctex Engineering Services and who is a Qualified Person as defined by National Instrument 43-101 - Standards of Disclosure for Mineral Projects. Situated south of Wales Lake and positioned just outside the southwest margin of the Athabasca Basin, the Project is strategically located within the Patterson Lake Corridor which hosts two significant uranium deposits (Triple R Deposit, 2,200,000 @ 1.58 U308 and 0.51 g/t Au & the Arrow Deposit which is the largest source of low-cost uranium globally, delivering up to 30,000,000 pounds of high-grade uranium per year). The deposits represent one of the largest high-grade uranium systems globally, comparable to world-class deposits such as McArthur River, Cigar Lake, and Key Lake.
お知らせ • Jul 05Blast Resources Announces Exploration Results At Its Wales Lake Project In The Athabasca Basin RegionBlast Resources Inc. summarized results of exploration programs completed on 3 groups of claims in the southwestern Athabasca Basin region, northern Saskatchewan. In December 2024, a high resolution airborne magnetic survey was flown over the Britt Lake, the Brazier South and North Agar claims collectively referred to as the "Wales Lake Project". Five targets are selected for further investigation, based on magnetic lineaments and regional uranium/thorium anomalies. There are two structural trends, oriented NNW-SSE and NW-SE identified in the project area, likely representing the main tectonic fabric of the Taltson Domain locally. On a regional scale, folding in the Taltson is along a NE-SW axis, identified by magnetic stratigraphic markers. The Wales Lake project is apparently at the closure of a regional fold axis which trends NE-SW. The two major structural elements are noteworthy: a structural corridor, oriented NNW-SSE which disrupts the magnetic stratigraphy and is magnetite-destructive, possibly indicative of alteration; and a tectonic break, oriented NW-SE which appears to be a boundary between basement lithologies. The geological exploration model is designed to test conductors and primarily fault-controlled basement-hosted mineralization such as Rabbit Lake (Eldorado), and Arrow (NexGen Energy) and Triple R (Paladin) occurrences that are hosted in the Taltson Domain. The scientific and technical information contained in this news release was prepared and approved by Locke Goldsmith, M.Sc., P.Eng., P. Geo., and who is a Qualified Person as defined by National Instrument 43-101 – Standards of Disclosure for Mineral Projects. Situated south of Wales Lake and positioned just outside the southwest margin of the Athabasca Basin, the Project is strategically located within the Patterson Lake Corridor which hosts two significant uranium deposits (Triple R Deposit, 2.2 Mt @ 1.58 U308 and 0.51 g/t Au & the Arrow Deposit which is the largest source of low-cost uranium globally, potentially delivering up to 30 million pounds of high-grade uranium per year). The deposits represent the largest high-grade uranium systems globally, comparable to world-class deposits such as McArthur River, Cigar Lake, and Key Lake.
お知らせ • Jun 02Blast Resources Inc Announces CFO ChangesBlast Resources Inc. announced the resignation of Derek Tam as Chief Financial Officer of the Company. Casey Forward assumed the role of interim CFO.