# Savannah Resources Plc Maiden Lithium Resource of 3.2Mt for the Mina do Barroso Lithium Project

- Link: https://www.directorstalkinterviews.com/savannah-resources-plc-maiden-lithium-resource-3-2mt-mina-barroso-lithium-project/412742354
- Published: 2017-12-18T07:31:44+00:00
- Author: Giles Arbor

**Savannah Resources plc** (LON:SAV), the AIM quoted resource development company,
has today announced a maiden Mineral Resource Estimate of 3.2 million tonnes for
the Reservatorio Deposit, which is one of three targets currently being advanced
as part of the ongoing exploration and development programme for the Mina do Barroso
Lithium Project (‘Mina do Barroso’ or the ‘Project’) in northern Portugal (Figure
1). Crucially further upside remains as the drill programme is ongoing, with the
aim of further expanding the Reservatorio Mineral Resource and defining new JORC–
2012 compliant Mineral Resource Estimates at other deposits. To view the press release
with the illustrative maps and diagrams please use the following link: [Savannah PDF](https://www.directorstalkinterviews.com/wp-content/uploads/2017/12/5746Z_-2017-12-17.pdf)

**HIGHLIGHTS:**

· Initial Inferred Mineral Resource of 3.2Mt at 1.0% Li₂O containing 32,000t of 
Li₂O for Reservatorio Deposit

· Reservatorio is one of at least eight pegmatite deposits on the Mina do Barroso
Mining Lease and one of three deposits currently being drilled

· Further drilling is now planned both down dip and targeting the potential eastern
extension of the deposit where higher lithium grades occur

· Mineral Resource updates are likely for Reservatorio during 2018 as the drilling
programme continues

· A maiden Mineral Resource Estimate for the Grandao deposit is expected during 
Q1 2018

· Drilling is ongoing and will take a short break over Christmas before commencing
again in early January at which time a second rig will be introduced to accelerate
the drilling programme

> **Savannah Resources Plc CEO, David Archer said:** “That we have an estimated 
> 3.2 million tonne Resource from just one of at least eight pegmatite deposits 
> at our Mina do Barroso Lithium Project gives an indication of the potential scale
> of this project. We are now focused on defining a significant aggregate Mineral
> Resource from the multiple pegmatites that sit within the major lithium mineralised
> corridor that runs through our Mining Lease. The first to add to this aggregate
> Mineral Resource will be the high-grade (up to 2.1% Li₂O) Grandao deposit where
> we have completed extensive drilling and expect to deliver a Resource Estimate
> in the first quarter of 2018.
> “The drilling results announced to date continue to underscore the potential of
> the Mina do Barroso Lithium Project to be a strategic upstream feature in the 
> European lithium value chain. We believe Mina do Barroso is the closest European
> analogue to the very successful Australian hard-rock, open cut mine developments,
> which produce highly sought-after lithium spodumene concentrates for international
> markets. Our focus is therefore on rapidly advancing the project so that we can
> look to provide a European source of battery-grade lithium to supply the growing
> number of European battery manufacturers. With this in mind, we look forward to
> continuing to advance at pace our drilling and metallurgical test work programmes,
> which will be used to support an early scoping study around a potential mine development.”

Figure 1. Mina do Barroso Project Summary Map showing prospects and 2017 drilling

**Mineral Resource Estimate**

A Mineral Resource Estimate for the Reservatorio lithium deposit (Table 1-2 and 
Figures 2-4) has been completed by Payne Geological Services Pty. Ltd, an external
and independent mining consultancy. The Reservatorio deposit forms part of Savannah’s
Mina do Barroso project in northern Portugal. The deposit largely comprises a single,
tabular pegmatite dyke with minor splays and the estimate is based entirely on results
from 20 reverse circulation holes drilled by Savannah in 2017. The deposit outcrops
over a strike length of approximately 500m and remains open, particularly at depth.

The Mineral Resource has been classified as Inferred Mineral Resource in accordance
with the JORC Code, 2012 Edition.

**Table 1. Reservatorio Deposit Inferred Mineral Resource Summary (above 0.5% Li2O
cut-off grade)**

  |

Reservatorio Deposit

  |

Tonnes

  |

Li_(2)O

  |

Fe_(2)O_(3)

  |

Li_(2)O

  |  
 |

Mt

  |

%

  |

%

  |

Tonnes

  |  
 |

3.2

  |

1.00

  |

1.4

  |

32,000

  |

 

Figure 2. Reservatorio Deposit – Geology and Drill Plan

Figure 3. Reservatorio Deposit – Mineral Estimate Model looking South

Figure 4. Reservatorio Deposit – Cross Section through the resource model

**Table 2**.

Reservatorio December 2017 Inferred Mineral Resource Estimate

0.5% Li2O Cut-off

  |

 |

 |

 |

 |

 |

 |

 |

 |

 |

 |

 |

 |

 |

 |  
 |

Bench

  |

Weathered

  |

Fresh

  |

Total

  |  
 |

Top

  |

Tonnes

  |

Li_(2)O

  |

Ta_(2)O_(5)

  |

Fe_(2)O_(3)

  |

Tonnes

  |

Li_(2)O

  |

Ta_(2)O_(5)

  |

Fe_(2)O_(3)

  |

Tonnes

  |

Li_(2)O

  |

Ta_(2)O_(5)

  |

Fe_(2)O_(3)

  |

Li_(2)O

  |  
 |

RL

  |

t

  |

%

  |

ppm

  |

%

  |

t

  |

%

  |

ppm

  |

%

  |

t

  |

%

  |

ppm

  |

%

  |

Tonnes

  |  
 |

610

  |

1,000

  |

1.20

  |

21

  |

1.4

  |

 |

 |

 |

 |

1,000

  |

1.20

  |

21

  |

1.4

  |

 |  
 |

600

  |

87,000

  |

1.06

  |

19

  |

1.3

  |

7,000

  |

1.38

  |

15

  |

1.5

  |

94,000

  |

1.09

  |

18

  |

1.3

  |

1,000

  |  
 |

590

  |

97,000

  |

1.03

  |

20

  |

1.3

  |

124,000

  |

1.19

  |

21

  |

1.4

  |

221,000

  |

1.12

  |

20

  |

1.3

  |

2,500

  |  
 |

580

  |

19,000

  |

0.88

  |

17

  |

1.2

  |

284,000

  |

1.12

  |

20

  |

1.4

  |

303,000

  |

1.11

  |

20

  |

1.4

  |

3,400

  |  
 |

570

  |

5,000

  |

0.96

  |

20

  |

1.5

  |

381,000

  |

1.04

  |

18

  |

1.4

  |

387,000

  |

1.04

  |

18

  |

1.4

  |

4,000

  |  
 |

560

  |

24,000

  |

0.95

  |

18

  |

1.4

  |

485,000

  |

1.01

  |

16

  |

1.4

  |

509,000

  |

1.00

  |

16

  |

1.4

  |

5,100

  |  
 |

550

  |

15,000

  |

0.80

  |

14

  |

1.3

  |

495,000

  |

1.00

  |

17

  |

1.4

  |

510,000

  |

0.99

  |

17

  |

1.4

  |

5,100

  |  
 |

540

  |

1,000

  |

0.83

  |

14

  |

1.5

  |

415,000

  |

0.97

  |

16

  |

1.4

  |

417,000

  |

0.97

  |

16

  |

1.4

  |

4,100

  |  
 |

530

  |

 |

 |

 |

 |

361,000

  |

0.96

  |

15

  |

1.4

  |

361,000

  |

0.96

  |

15

  |

1.4

  |

3,500

  |  
 |

520

  |

 |

 |

 |

 |

208,000

  |

0.91

  |

15

  |

1.3

  |

208,000

  |

0.91

  |

15

  |

1.3

  |

1,900

  |  
 |

510

  |

 |

 |

 |

 |

119,000

  |

0.85

  |

14

  |

1.3

  |

119,000

  |

0.85

  |

14

  |

1.3

  |

1,000

  |  
 |

500

  |

 |

 |

 |

 |

54,000

  |

0.88

  |

14

  |

1.3

  |

54,000

  |

0.88

  |

14

  |

1.3

  |

500

  |  
 |

490

  |

 |

 |

 |

 |

7,000

  |

0.93

  |

14

  |

1.3

  |

7,000

  |

0.93

  |

14

  |

1.3

  |

100

  |  
 |

Total

  |

250,000

  |

1.01

  |

19

  |

1.3

  |

2,940,000

  |

1.00

  |

17

  |

1.4

  |

3,190,000

  |

1.00

  |

17

  |

1.4

  |

32,000

  |

        

**Resource Summary – Reservatorio Lithium Deposit**

**Geology**

At the Mina do Barroso Project, lithium mineralisation occurs predominantly in the
form of spodumene-bearing pegmatites which are hosted in metapelitic and mica schists,
and occasionally carbonate schists of upper Ordovician to lower Devonian age. The
Reservatorio pegmatite is quite tabular and continuous and varies in thickness from
10m-30m. It strikes broadly NE-SW and dips to the NW at 25o to 40o.

Lithium is present in pegmatite bodies which are typically of aplite compositions
and laboratory test work confirms that the lithium is almost exclusively within 
spodumene. Distinct lithium grade zonation occurs within the pegmatite, with weakly
mineralised zones often evident at the margins of the dyke. Minor xenoliths and 
inliers of schist are observed on occasions.

The weathering profile comprises a shallow, surficial zone of weak to moderate oxidation,
particularly of the schistose country rock. A zone of deeper weathering exists in
the vicinity of an interpreted fault.

**Drilling**

A total of 20 reverse circulation (RC) holes define the Reservatorio Mineral Resource.
The holes were drilled on an approximate grid spacing of 40m spaced holes on 80m
spaced cross sections. All holes were drilled by Savannah in 2017 and all drill 
hole information and results have been previously reported to the market.

Drill collar locations are recorded in UTM coordinates using hand-held GPS, with
elevations adjusted to a regional topographic DTM. All Savannah drilling has been
down-hole surveyed using a gyroscopic tool.

**Sampling and Sub-Sampling Techniques**

For the Savannah drilling, a face-sampling hammer was used with samples collected
at 1m intervals from pegmatite zones with composite sampling of typically 4m in 
the surrounding schists. The 1m samples were collected through a rig-mounted rotary
splitter and were 4-6kg in weight. The 4m composites were collected by spear sampling
of the 1m intervals. Samples were weighed to assess the sample recovery which was
determined to be satisfactory.

**Sample Analysis Method**

For all Savannah drilling, whole samples were crushed then riffle split to produce
a 250g split for pulverizing and analysis at the ALS Laboratories facility in Seville,
Spain.

The samples were analysed using ALS laboratories ME-MS89L Super Trace method, which
combines a sodium peroxide fusion with ICP-MS analysis. A multi-element suite is
analysed.

QAQC protocols were in place for the drilling programs and included the used of 
standards, blanks and field duplicates. The data has confirmed the quality of the
sampling and assaying for use in Mineral Resource estimation.

**Estimation Methodology**

For the Reservatorio Mineral Resource, a Surpac block model was constructed with
block sizes of 40m (EW) by 10m (NS) by 5m (elevation) with sub-celling to 10m by
2.5m by 1.25m. The typical drill hole spacing is 80m (EW) by 40m (NS).

Interpretation of the pegmatite dykes was completed using detailed geological logging.
Wireframes of the pegmatites were prepared and within those the sample data was 
extracted and analysed. A clear break in the grade distribution occurs at 0.5% Li2O
and this grade threshold was used to prepare the internal grade domains for estimation.

Pegmatite and mineralisation domains were extrapolated up to 80m down-dip of the
drill hole intersections and 40m along strike.

Sample data was composited into 1m intervals then block model grades estimated using
inverse distance squared (ID2) grade interpolation. A first pass search range of
120m was used and oriented to match the dip and strike of the mineralisation. A 
minimum of 10 samples and a maximum of 24 samples were used to estimate each block.
The majority of the resource (98%) was estimated in the first pass with an expanded
search radius of 240m used for the few blocks not estimated in the first pass. No
high-grade cuts were applied to the estimate.

Iron within the pegmatite is uniformly low, with a mean Fe2O3 grade of 1.4%. Other
similar deposits have reported that a large proportion of the assayed iron is due
to contamination from the abrasion of steel drilling and sample preparation equipment
and this will be investigated as part of ongoing studies at the project.

No bulk density data is available for the deposit, so values were derived from similar
deposits, which have been recently estimated. Bulk density values applied to the
Reservatorio estimate were 2.2t/m3 for oxide lithologies, 2.6t/m3 for unoxidized
pegmatite and 2.8t/m3 for unoxidized schist.

**Mineral Resource Classification**

The Mineral Resources was classified in accordance with the Australasian Code for
the Reporting of Exploration Results, Mineral Resources and Ore Reserves (JORC, 
2012).

The main pegmatite dyke at Reservatorio has been defined by 40m spaced drill holes
on 80m spaced sections. The two easternmost sections are defined by single drill
holes. Within the main pegmatite, the continuity of lithium mineralisation is good,
however due to the broad drill hole spacing, the entire deposit has been classified
as Inferred Mineral Resource.

The Mineral Resource has been reported to a depth of 130m vertical.

**Cut-off Grades**

The shallow, outcropping nature of the deposit and moderate to gentle dip suggests
good potential for open pit mining if sufficient resources can be delineated to 
consider a mining operation. As such, the Mineral Resource has been reported at 
a 0.5% Li2O lower cut-off grade to reflect assumed exploitation by open pit mining.

**Metallurgy**

Metallurgical test work has been conducted by Savannah on representative mineralisation
at the Mina Do Barroso project. The work was completed by Nagrom Metallurgical in
Australia and confirmed that high grade lithium, low grade iron concentrate can 
be generated from the mineralisation using conventional processing technology. Microscopy
confirmed that the concentrate was almost entirely spodumene.

**Modifying Factors**

No modifying factors were applied to the reported Mineral Resource estimate. Parameters
reflecting mining dilution, ore loss and metallurgical recoveries will be considered
during the any future mining evaluation of the project.

**Preliminary Metallurgical Test Work (previously reported 26/06/17)**

· Results from the preliminary ore characterisation metallurgical test work on a
composite sample from Mina do Barroso to determine if the lithium bearing minerals
can be recovered from the rock using commercially available technology and a saleable
product produced have been received.

· Work confirms that a high grade very pure low iron spodumene concentrate can be
produced from the Mina do Barroso lithium mineralisation.

· Single analysis of the combined sample confirmed a high Li2O head grade (~1.95%
Li2O) and low Fe2O3 head grade (~0.9%)

· Heavy Liquid Separation (“HLS”) shows a very pure (~8%) Li2O product can be produced

· Flotation results utilising a simple one stage float without any optimisation 
achieved ~83.7% Li2O recovery at ~5.9% Li2O, this is very positive and can be improved
through optimisation

· Microscopy confirmed that the concentrate was almost entirely spodumene with only
very minor amounts of petalite

· Test work confirms that a high quality spodumene concentrate can be produced using
conventional commercially available processing technologies.

**Competent Person and Regulatory Information**

The information in this report that relates to exploration results is based on, 
and fairly represents information and supporting documentation prepared by Mr Dale
Ferguson, a Competent Person who is a member of The Australasian Institute of Mining
and Metallurgy. Mr Ferguson is a director of Savannah Resource plc and has sufficient
experience that is relevant to the style of mineralisation and type of deposit under
consideration and to the activity being undertaken to qualify as a Competent Person
as defined in the 2012 Edition of the “Australasian Code for Reporting of Exploration
Results, Mineral Resource and Ore Reserves”. Mr Ferguson consents to the inclusion
in this report of the matters based on his information in the form and context in
which it appears.

The Information in this report that relates to Mineral Resources is based on information
compiled by Mr Paul Payne, a Competent Person who is a Fellow of the Australasian
Institute of Mining and Metallurgy. Mr Payne is a full-time employee of Payne Geological
Services. Mr Payne has sufficient experience that is relevant to the style of mineralisation
and type of deposit under consideration and to the activity being undertaken to 
qualify as a Competent Person as defined in the 2012 Edition of the “Australasian
Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves”. 
Mr Payne consents to the inclusion in the report of the matters based on his information
in the form and context in which it appears.

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