Kingsland Minerals : Successful ASX Listing

onlyKingsland Minerals completes IPO and lists on ASX with high grade Uranium projects in the Northern Territory

of Australia

• Kingsland Minerals (ASX:KNG) successfully lists on ASX and raises $4.7m

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Assumes 100% ownership of exciting Uranium, Copper and Gold Projects in the Pine Creek region of the Northern Territory (NT)

Appointment of highly experienced uranium exploration and resource geologist, David Princep (ex Paladin Energy Ltd) in advisory role

Drilling to commence shortly targeting Uranium in the NT

Significant historical Uranium drill results at the Allamber Project include:

personal	- 42m at 611 ppm U₃O₈ from 97m (TAL062RC) incl:
▪	8m at	1,579 ppm U₃O₈ from 99m
	▪ 3m at	1,347 ppm U₃O₈ from 124m

- 23m at 1,318 ppm U₃O₈ from 86m (TAL079RC) incl:

▪ 5m at 3,169 ppm U₃O₈ from 102m

- 49m at 787 ppm U₃O₈ from 58m (TAL0107RC) incl: ▪ 17m at 1,286 ppm U₃O₈ from 78m

- 18m at 932 ppm U₃O₈ from 70m (TAL108RC) incl: ▪ 4m at 2,600 ppm U₃O₈ from 82m

▪ 13m at 251 ppm U₃O₈ from 123m

• Significant historical Uranium drill results at the Bella Rose Project include: - 6m at 1,199 ppm U₃O₈ from 79m (TPCRC106) incl:

▪ 1m at 5,230 ppm U₃O₈ from 80m ▪ 2m at 636 ppm U₃O₈ from 113m ▪ 1m at 210 ppm U₃O₈ from 161m

ForKingsland Minerals Ltd (ASX:KNG) (Kingsland or Company) is pleased to announce that it has successfully raised $4.7m and has been accepted for admission to the official list of the Australian Stock Exchange (ASX). Shares in Kingsland will begin trading on 14 June 2022 at 11:00 AM (WST). The Initial Public Offering (IPO) has raised $4.7m through the issue of 23.5m shares at an issue price of $0.20. The total undiluted shares on issue at the date of listing in 37.4m with KNG having a Market Capitalisation of $7.5m and an Enterprise Value (EV) of $2.7m.

Kingsland has accumulated an exciting package of tenements in the Northern Territory and Western Australia that are highly prospective for Uranium, Copper, Gold and Nickel. Exploration will commence shortly in the Northern Territory and Western Australia. Approvals to drill have been obtained for the Lake Johnston Project in Western Australia and are in the application process for projects in the Northern Territory.

ALLAMBER URANIUM PROJECT

onlyThe Allamber Uranium Project contains historical drilling targeting Uranium dating from the early 1980's when uranium mineralisation was first discovered. Exploration has been focussed on an embayment in the Cullen Granites (Figures 1 and 2). Reverse circulation (RC) and Diamond core drilling by previous explorers has delineated broad, high grade drill intersections of U₃O₈ at the Twin, Dam and Cliff South prospects.

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Figure 1: Kingsland Minerals Allamber Project
Kingsland Minerals has designed drilling programs to firstly confirm the historical drill results and
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secondly to extend the known mineralisation. The focus will be to collect data and information and to delineate additional uranium mineralisation to ultimately enable the estimation of a Mineral Resource Estimate.

Uranium mineralisation has been found to be associated with thin felsic/granitic dykes intruded into the hosting carbonaceous sediments of the Masson Formation. Figure 2 shows a more detailed map of the geology in the embayment within the Cullen granites. Several radiometric anomalies are shown with a majority of drilling to date focussed on Twin, Dam and Cliff South. The area is under explored and Kingsland will prioritise the exploration of this prospective area.

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personal	Figure 2: Allamber Uranium Prospects
Twin Uranium Prospect

The Twin deposit is located in a strongly folded syncline of Lower Protoerzoic metasediments enclosed and intruded by dykes of Cullen granite. The lithologies forming the syncline include a basal psammite, quartzites and sericite-chlorite schists. The unit is overlain by a thick sequence of Forcarbonaceous shales which, when affected by faulting, become graphitic and chlorite schists. The carbonaceous shale sequence contains interbedded dolomite lenses. The uppermost unit exposed at

the Twin deposit is a coarse-grained quartzite which occupies the core of the syncline.

The Twin syncline has been strongly faulted, with faults trending parallel to the axial plane of the syncline. These faults have become the loci of subsequent intrusion by late phases of the Cullen granite. The uranium mineralisation is also concentrated within these faults. A secondary, later, fault system, oblique to the axial plane of the syncline, has displaced both the stratigraphy and the earlier fault system. The later faults do not appear to be mineralised. Mineralisation at Twin is both primary and secondary, with remobilisation and redeposition of the uranium minerals having taken place at or near the water table.

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Figure 3: Schematic cross section through Twin

		Table 1: Significant Drill Intersections Twin Prospect
							Width
only		Hole	From (m)		To (m)		(m)		U₃O₈ ppm
	TRC707	52		55		3		252
	and	52		56		4		342
		TRC708	32		60		28		709
		inc	32		42		10		1,489
		TRC713	32		36		4		285
		and	47		50		5		487
		TRC716	0		10		10		237
		and	28		32		4		432
use		TRC718	0		19		19		269
	TRC721	22		26		4		231
	TRC722	40		60		20		627
		inc	51		57		6		1,336
		TRC730	42		47		5		1,220
		inc	45		47		2		2,595
		TRC734	47		54		7		793
personal		inc	47		50		3		1,431
	TRC735	44		47		3		858
	and	54		57		3		370
		TRC736	16		31		15		242
		TRC737	23		31		8		680
		inc	23		25		2		1,012
		and	45		48		3		851
		TRC738	30		53		23		749
		inc	37		43		6		1,618
		TRC739	33		38		5		773
		and	43		48		5		488
		TRC740	17		29		12		201
		and	39		48		9		243
		TRC741	39		47		8		412
		and	51		58		7		301
		TRC744	30		33		3		282
		and	50		51		1		1,100
		TRC748	0		14		14		321
For		TRC754	21		28		7		418
Dam Uranium Prospect

Mineralisation at the Dam deposit occurs higher in the stratigraphic sequence than at Twin. A large proportion of the lower units of the syncline have been adsorbed into the Cullen granite, particularly to the west. At the Dam deposit, mineralisation is more widely spread through the stratigraphy. There is also less evidence for secondary concentration of mineralisation at or near the water table. The syncline at Dam is much broader and the dip of the sediments not as steep as Twin. The later, oblique faulting is better defined and both groups of faults host uranium mineralisation.