Aankondiging • Feb 19

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Asian Battery Metals plc Provides an Update on the Upcoming 2025 Phase 3 Exploration Program At the Oval Cu-Ni Prospect in the Southwestern Part of Mongolia

Asian Battery Metals PLC provided an update on the upcoming 2025 Phase 3 exploration program at the Oval Cu-Ni prospect in the southwestern part of Mongolia. The goal of the exploration program is to extend from last year's intercepts of high-grade massive sulphide in drill holes OVD021, OVD025, OVD0263and OVD027, and to scout drill any extension of mineralisation discovered. Extensive regional geophysical surveys from 2022 to 2024 have delineated compelling exploration areas for drilling within the Yambat tenement area. These areas exhibit a strong spatial correlation, with elevated copper (Cu), nickel (Ni) and platinum group element (PGE) values coincident with high magnetic, gravity anomalies corresponding to IP resistivity lows. The target area selection process integrated these geophysical data with results from soil samples collected between 2022 and 2024 and analysed by ABM geologists. Physical property data from the samples has been integrated to improve the existing 3D geophysical models. Priority DHEM conductive plates for testing during the Phase 3 drilling program will be those that extend the high-grade mineralisation further within the Oval gabbroic intrusion and also some outside the geologically known gabbro boundary. Based on the current geological interpretation and geophysical data plates OVD021_Late_F (depth), OVD009_170-F (SE part of Oval), OVD026_L2_A (extension to north), OVD011_EOH_A (depth extension, combined with gravity anomaly testing) and OVD025_L6_B (North Oval) will be the priority plates for testing along with other target areas in the detailed exploration area from the following list of all initial and modified DHEM plates. A gravity high anomaly identified in a revised inversion model of current gravity data will be tested during the Phase 3 drilling program. Drillhole OVD010, designed to test the gravity high anomaly during the 2024 Phase 1 program, encountered no significant mineralisation or gabbroic intrusive. The revised gravity model, incorporating detailed topographic and drillhole data, indicates OVD010 missed the core of the gravity anomaly without fully testing it. The technical team is studying an optimal drill hole design to test this gravity high anomaly in combination with drilling of the OVD011_EOH-A plate. The geophysical signatures in the regional geological context may be spatially associated with the Oval intrusive, either along structural trends or parallel features. It is important to note that all of these areas are concealed beneath cover or sedimentary rocks, remain untested by drilling or other subsurface exploration methods, and their geological explanation is yet to be determined. Six exploration areas have been prioritised in the 2025 Phase 3 Program for follow-up exploration drilling out of the approximately 30 areas initially defined by the geophysical surveys within the detailed exploration area in prior works. These prioritised areas display particularly robust geophysical signatures, characterised by coincident high magnetic and gravity responses, coupled with low resistivity or low magnetic and high gravity responses with low resistivity. In addition, two highly prospective soil anomalies have been identified through analysis of samples previously collected and processed by ABM geologists. Their underlying geological explanation is yet to be determined and is being investigated. Current geological modeling and targeting work of cluster analysis by self-organising mapping (SOM) focus on anomalies using data obtained during the 2024 Phase 2 program. This includes measurements of density and magnetic susceptibility on cores and identification of exploration areas with features similar to those at depth below the Oval gabbroic intrusion. As disclosed in the ASX announcement dated 13 January 2025 "High Grade Massive Sulphide Interprets Confirmed At Oval", the gravity data and inversion model indicates vertical high anomalies directly underneath Oval and North Oval. In the detailed exploration area, GRIP (gradient-induced polarisation) and PDIP (pole-dipole) surveys delineated the Central and South (will be referred to as Quartz Hill) areas based on chargeability highs at 200-250 metres depth from the surface. Other studies, such as the CSAMT/AMT pilot program and 3D inversion of gravity, support these areas with indications of sub-vertical/vertical features. The AMT and CSAMT surveys delineated deeper targets with moderate to low resistivity zones (500-1000 ·m). These zones exhibit a spatial correlation with surface PDIP chargeability anomalies (<18 mV/V). This coincident geophysical response is further corroborated at depth by corresponding high gravity values (0.043 g/cc <), suggesting a coherent geological feature. The convergence of these independent geophysical datasets (resistivity, chargeability, and gravity) strengthens the interpretation of a significant subsurface region that warrants further investigation. A grab sample collected from the gabbroic outcrop near Quartz Hill returned anomalous copper and nickel values such as Cu 2150ppm, and Ni 408ppm in 2024, as disclosed in the ASX announcement "Regional Exploration Identifies New Copper & Nickel Targets" dated 6 August 2024. This result, together with the southeast-trending, high-chargeability corridor, suggests the potential for nickel and copper mineralised gabbroic intrusion(s) at depth in this area. Depending on the results of planned geophysical surveys and further ground reconnaissance work, additional scout drilling may be needed in the resistivity low anomaly defined by gradient and resistivity IP (GRIP) and the Magnetic High (Magnetic Area, North of Oval). Ground magnetics data-based structural interpretation is ongoing to increase understanding of geology and regional context. The modelling also covers the analysis of potential areas below the Oval intrusion in correlation with other identified geophysical anomalies, including the parallel geophysical feature of the magnetic high area (north of Oval) and the resistivity low area (south of Oval). Parallel geophysical features are important from a geological and structural perspective.

Percentage CEO-salaris	50.27%
Dienstverband CEO	2yrs
Eigendom CEO	8.5%
Management gemiddelde ambtstermijn	geen gegevens
Gemiddelde ambtstermijn bestuur	2yrs

Datum	Totale vergoeding	Salaris	Bedrijfswinsten
Dec 31 2025	AU$278k	AU$140k	-AU$2m
Sep 30 2025	n/a	n/a	-AU$2m
Jun 30 2025	n/a	n/a	-AU$1m
Mar 31 2025	n/a	n/a	-AU$4m
Dec 31 2024	AU$144k	AU$69k	-AU$6m

Naam	Positie	Tenure	Compensatie	Eigendom
Gan-Ochir Zunduisuren	MD & Director	2yrs	AU$277.89k	8.51% € 853.2k
David Paull	Independent Non-Executive Chairman	2yrs	AU$101.94k	2.04% € 204.8k
Kirsten Livermore	Independent Non-Executive Director	2yrs	AU$83.09k	0.28% € 27.6k
Neil Young	Independent Non-Executive Director	2yrs	AU$83.09k	geen gegevens

Gegevens	Laatst bijgewerkt (UTC-tijd)
Bedrijfsanalyse	2026/06/08 05:30
Aandelenkoers aan het einde van de dag	2026/06/08 00:00
Inkomsten	2025/12/31
Jaarlijkse inkomsten	2025/12/31

Pakket	Gegevens	Tijdframe	Voorbeeld Amerikaanse bron ^*
Financiële gegevens bedrijf	10 jaar	Resultatenrekening Kasstroomoverzicht Balans	SEC-formulier 10-K SEC-formulier 10-Q
Consensus schattingen analisten	+3 jaar	Financiële prognoses Koersdoelen analisten	Onderzoeksrapporten van analisten Blue Matrix
Marktprijzen	30 jaar	Aandelenprijzen Dividenden, splitsingen en acties	ICE Marktgegevens SEC-formulier S-1
Eigendom	10 jaar	Top aandeelhouders Handel met voorkennis	SEC-formulier 4 SEC-formulier 13D
Beheer	10 jaar	Leiderschapsteam Raad van bestuur	SEC-formulier 10-K SEC-formulier DEF 14A
Belangrijkste ontwikkelingen	10 jaar	Bedrijfsaankondigingen	SEC-formulier 8-K

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