View Financial HealthBlast Resources 배당 및 자사주 매입배당 기준 점검 0/6Blast Resources 배당금을 지급한 기록이 없습니다.핵심 정보n/a배당 수익률-8.7%자사주 매입 수익률총 주주 수익률-8.7%미래 배당 수익률n/a배당 성장률n/a다음 배당 지급일n/a배당락일n/a주당 배당금n/a배당 성향n/a최근 배당 및 자사주 매입 업데이트업데이트 없음모든 업데이트 보기Recent updates공시 • 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.공시 • 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.공시 • 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.지급의 안정성과 성장배당 데이터 가져오는 중안정적인 배당: 과거에 BLSR.F 의 주당 배당금이 안정적이었는지 판단하기에는 데이터가 부족합니다.배당금 증가: BLSR.F 의 배당금 지급이 증가했는지 판단하기에는 데이터가 부족합니다.배당 수익률 vs 시장Blast Resources 배당 수익률 vs 시장BLSR.F의 배당 수익률은 시장과 어떻게 비교되나요?구분배당 수익률회사 (BLSR.F)n/a시장 하위 25% (US)1.3%시장 상위 25% (US)4.2%업계 평균 (Oil and Gas)3.4%분석가 예측 (BLSR.F) (최대 3년)n/a주목할만한 배당금: 회사가 최근 지급을 보고하지 않았기 때문에 하위 25%의 배당금 지급자에 대해 BLSR.F 의 배당 수익률을 평가할 수 없습니다.고배당: 회사가 최근 지급을 보고하지 않았기 때문에 배당금 지급자의 상위 25%에 대해 BLSR.F 의 배당 수익률을 평가할 수 없습니다.주주 대상 이익 배당수익 보장: 배당금 지급이 수익으로 충당되는지 확인하기 위해 BLSR.F 의 지급 비율을 계산하기에는 데이터가 부족합니다.주주 현금 배당현금 흐름 범위: BLSR.F 에서 지급을 보고하지 않았기 때문에 배당 지속 가능성을 계산할 수 없습니다.높은 배당을 제공하는 우량 기업 찾기7D1Y7D1Y7D1YUS 시장에서 배당이 강한 기업.View Management기업 분석 및 재무 데이터 상태데이터최종 업데이트 (UTC 시간)기업 분석2026/07/07 09:21종가2026/07/07 00:00수익2026/04/30연간 수익2026/01/31데이터 소스당사의 기업 분석에 사용되는 데이터는 S&P Global Market Intelligence LLC에서 제공됩니다. 아래 데이터는 이 보고서를 생성하기 위해 분석 모델에서 사용됩니다. 데이터는 정규화되므로 소스가 제공된 후 지연이 발생할 수 있습니다.패키지데이터기간미국 소스 예시 *기업 재무제표10년손익계산서현금흐름표대차대조표SEC 양식 10-KSEC 양식 10-Q분석가 컨센서스 추정치+3년재무 예측분석가 목표주가분석가 리서치 보고서Blue Matrix시장 가격30년주가배당, 분할 및 기타 조치ICE 시장 데이터SEC 양식 S-1지분 구조10년주요 주주내부자 거래SEC 양식 4SEC 양식 13D경영진10년리더십 팀이사회SEC 양식 10-KSEC 양식 DEF 14A주요 개발10년회사 공시SEC 양식 8-K* 미국 증권에 대한 예시이며, 비(非)미국 증권에는 해당 국가의 규제 서식 및 자료원을 사용합니다.별도로 명시되지 않는 한 모든 재무 데이터는 연간 기간을 기준으로 하지만 분기별로 업데이트됩니다. 이를 TTM(최근 12개월) 또는 LTM(지난 12개월) 데이터라고 합니다. 자세히 알아보기.분석 모델 및 스노우플레이크이 보고서를 생성하는 데 사용된 분석 모델에 대한 세부 정보는 당사의 Github 페이지에서 확인하실 수 있으며, 보고서 활용 방법에 대한 가이드와 YouTube 튜토리얼도 제공하고 있습니다.Simply Wall St 분석 모델을 설계하고 구축한 세계적 수준의 팀에 대해 알아보세요.산업 및 섹터 지표산업 및 섹터 지표는 Simply Wall St가 6시간마다 계산하며, 프로세스에 대한 자세한 내용은 Github에서 확인할 수 있습니다.분석가 소스Blast Resources Inc.는 0명의 분석가가 다루고 있습니다. 이 중 0명의 분석가가 우리 보고서에 입력 데이터로 사용되는 매출 또는 수익 추정치를 제출했습니다. 분석가의 제출 자료는 하루 종일 업데이트됩니다.
공시 • 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.
공시 • 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.
공시 • 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.