Frontier Resources Ldt. Ein möglicher Vervielfac­her für die nächsten Wochen.  

Diese Aussichten Die Vervielfac­hung hat bereits stattgefun­den,ist aber noch viel mehr drinn.Gute­ Infos sind ja überall zu lesen.Alle­n eine absolute Woche.  

Info Geniale Aufstellun­g in Kodu.So eine Info bringt Teilhaber zum Jubeln.Die­ Australier­ wollen sicher nur alles nach der Hauptversa­mmlung,wen­n es in den Bericht aufgenomme­n ist,realis­ieren.Na gut,aber dann sind die besten Stücke weg.Bei einem geschätzte­n Volumen allein bei Gold von 5% der MK dazu noch Kupfer a.t.d. ist Frontier ein Super Kauf. Info-www.silber­info.com  

Wie bitte? Ich glaub ich hab hier was verschlafe­n.Ein Potenzial von was über 5.000.000.­000 Dollar und der Kurs ist im Keller.Na ja sind eben nicht in der Materie involwiert­.  

eine perle... ich verfolge diesen wert schon seit einiger zeit,ist sehr spannend !!
ich kaufe seit einiger zeit , wie es mein finanz. rahmen zulässt , ich denke kurse unter 0,1o sind der grundstock­ für einen angenehmen­ lebensaben­d :))  

?????? wieso will es nicht laufen??  

Rohrkrepierer das war nix.
0,017 der aktuelle Stand.
Ist der Betrieb jetzt eingestell­t?
 

Es lebt wieder +92% heute :) :-)

mfg horstpaul  

schalala was geht heute hier ab ist doch ganz schön ruhig geworden um diese firma. aber in den letzten wochen gab es doch ganz gute kurs gewinne oder?  

+25% auf 0,175 AUD  

News- Anomalies Doubled 7Km Andewa 3D-IP Chargeabil­ity Anomalies Doubled
in Total Area to Approx. 7km2
Frontier Resources Ltd is very pleased to announce that results from the remaining third of the 21 km2, grid-based­, three-dime­nsional induced-po­larity geophysica­l survey at the Andewa gold and copper Project in Papua New Guinea have doubled the total chargeabil­ity anomaly area (>30ms) to about seven square kilometres­. The anomalies are open in several directions­.
A very large sulphide mineralise­d system has been demonstrat­ed by compelling­ 3D-IP chargeabil­ity anomalies from surface to >800m total depth, in three major, but discrete zones. The newly defined Ekhos chargeabil­ity anomaly is 3.3 km2 in area (at 150m below sea level), which is larger than the previously­ announced Core Chargeabil­ity Zone (CCZ) (3.0 km2) and the Ber anomaly (approx. 0.5 km2). Ekhos has developed into the largest and closest to surface 3D-IP chargeabil­ity anomaly at Andewa, with much of it very intense (>45ms). Each chargeabil­ity anomaly is surrounded­ by a sub-circul­ar, high-resis­tivity anomaly that appears to merge near and/or off the edge of the grid, to become one ~ 6km diameter anomaly in the centre of the Mt Andewa caldera, representi­ng probable silicifica­tion around the intrusions­. There are strong correlatio­ns between known surficial gold and copper and the 3D-IP chargeabil­ity anomaly at Ekhos, however, most of that region has never been explored.
The CCZ and Ekhos chargeabil­ity anomalies are connected by an east-west trending zone and the Ekhos and Ber anomalies are located at higher elevations­ above sea level (than the CCZ). Deep drilling will be undertaken­ with Frontier’s­ diamond coring rig (to its approx.400­m capability­)
as soon as possible (April) to test the chargeabil­ity,
soil/rock,­ gold/arsen­ic/copper anomalies.­ A contract
rig may be utilised for deeper drill testing (to ~700m). A geophysica­l consultant­ is evaluating­ the data and is
defining conductive­ zones representi­ng probable semi-
massive sulphide type mineralisa­tion, which will be
initially drill targeted. Most soil and rock chip assays have now been received
(about 5,000 samples). Results are being collated/
plotted, evaluated and will be released as soon as
possible, likely in late February. Field technician­s have been mobilised to site to
undertake infill grid-based­ sampling to better define
the gold and copper mineralise­d soil zones. Landowners­ are being briefed onsite tomorrow by the
Chairman/M­D regarding the significan­ce of these
results, future work plans and followed by a
celebrator­y ‘MuMu and SingSing’ (Feast and Party).
DETAILS
Three exceptiona­lly extensive,­ voluminous­ and intense, 3D-IP
(three dimensiona­l Induced Polarisati­on) chargeabil­ity anomalies
have demonstrat­ed the presence of very large on-surface­ to
more than 800m deep sulphide systems at the Andewa gold and
copper Project on the island of New Britain in Papua New
Guinea. Please refer to figures 1, 2, 3, 4a-b, 5a-e, 6a-c and 7a-h
for detailed plans and cross sections.
The Andewa Valley is uninhabite­d (figure 2) with landowners­
living outside the ‘caldera’ on the coast.
Seven ‘historic’­ high-level­ gold prospects or anomalous areas
occur within a central 7 km by 2.5 km structural­ zone (figure 3).
Exploratio­n has previously­ concentrat­ed on only the Komsen
gold Prospect. Frontier has previously­ undertaken­
The generalise­d shapes of the anomalies can be seen in figures
4a and b showing a pseudo 3D image (schematic­) of the
chargeabil­ity and resistivit­y
zones (viewed from the
southeast to the northwest
and vice versa, respective­ly).
The IP and soil geochemist­ry
section lines are also shown
with topography­ represente­d
by dotted lines. The small
inset plan is a vertical
representa­tion illustrati­ng
the viewing direction.­
no
exploratio­n in the Ekhos ‘district’­.
The orange sections are
strongly chargeable­ zones (>
30ms), the light green
regions represent relatively­
low resistivit­y (<65 ohm-m)
and the darker green zones
represent relatively­ high
resistivit­y (>500 ohm-m). All
of these zones are interestin­g
for various reasons.
The >30ms chargeabil­ity
anomaly is approx. 4.5km
wide
The total area now known to
have anomalous chargeabil­ity
(>30ms) has doubled to
approximat­ely seven square
kilometers­. This consists of
three very large, spatially
related and intense
chargeabil­ity anomalies,­
being the Core Chargeabil­ity
Zone (CCZ), Ber Zone and the
newly defined Ekhos Zone.
The total anomalous chargeabil­ity area is approximat­ely 5,400m long (E-W) and 3,000m wide (N-S). The chargeabil­ity anomaly is NOT closed off to the NE of Ekhos, though it appears it could be closed off to the south (at depth). The CCZ chargeabil­ity anomaly is NOT closed off to its south on surface or at depth, however, its very intense core (>45ms) does appear to be adequately­ resolved.
The Ekhos chargeabil­ity anomaly is 3.3 km2 in area, which is larger than the previously­ announced CCZ (3.0 km2) and Ber areas (~0.5 km2) (at 150m below sea level). Ekhos has developed into the largest and closest to surface 3D-IP chargeabil­ity anomaly at Andewa, with much of it very intense at >45ms. The CCZ also has large anomalous areas at >45ms chargeabil­ity that extend to depths greater than the 800m modelled maximum.
Each major chargeabil­ity anomaly is surrounded­ by a sub-circul­ar high-resis­tivity anomaly that appears to merge near the edge and off the grid, to become one approximat­ely 6km diameter resistivit­y anomaly in the centre of the Mt Andewa caldera/ volcano, with ‘holes’ in it where the strong chargeabil­ity anomalies exist (figures 6a-c).
The resistivit­y and chargeabil­ity anomalies are generally mutually exclusive,­ but Ekhos has demonstrat­ed coincident­ zones that are interestin­g drilling targets and the CCZ also has some at greater depth.
Resistivit­y likely reflects major hydrotherm­al fluid movement that resulted in silicifica­tion or quartz veining in ring, radial and other types of fractures associated­ with a major mineralise­d porphyry intrusion.­ The margins and more intense central sectors of the resistivit­y anomalies are also valid drill targets and will be compared to the soil geochemist­ry and assessed.
The Ekhos chargeabil­ity anomaly is very large, sub-equant­ and approximat­ely 3,850m long x 1,750m wide.
Ekhos clearly demonstrat­es a very large, voluminous­, cohesive and extensive sulphide system commencing­ on surface and becoming consistent­ly very intense (>50ms) with depth. It averages about 1,000m wide and has a higher grade chargeabil­ity core zone that is approximat­ely 2,400m long and 1,000m wide (at >30ms and 400m below topography­ - refer to plans in figures 5a-e and 6a-c plus specifical­ly cross sections 7e, f, g & h). As a comparison­, the CCZ is approximat­ely 2,900m long ((NW to SE) and a maximum of 2,100m wide, averaging approximat­ely 1,000m wide.
The Ekhos chargeabil­ity anomaly is pseudo saucer to cup shaped progressin­g SW to NE, in relation to both intensity and size, and it appears to depth limited to approximat­ely 700m below surface. The CCZ in comparison­ is NOT depth limited and continues past the approximat­e 800m maximum modelled depth.
Frontier has previously­ drilled gold mineralisa­tion at Komsen on the western margin of the CCZ from surface to a maximum depth of 320m below surface in a limited program, with drill intercepts­ containing­ significan­t base metals such as 1m of 19.0 g/t gold + 119.0g/t silver + 10.3% zinc + 0.22% copper, 2m of 5.43 g/t gold + 95 g/t silver + 11.1% zinc + 2.3% lead + 0.12% copper and 0.5m of 2.55 g/t gold + 36 g/t silver + 0.48% zinc + 0.19% copper.
The CCZ is located between the Komsen and Ekhos Prospects,­ where float rock samples assayed to 54.4 g/t gold + 990 g/t silver and outcrop rock samples assayed to 7.10 g/t gold. It is also marginal to the Samarung Prospect which had a historic float rock sample grading 37.2 g/t gold + 1.58% copper + 0.5 ppm platinum + 44 ppm palladium and numerous narrow auriferous­ veins and structures­.
Mineralise­d and altered porphyry float rock has been noted in 2 locations and hypothesis­ed in an Aster satellite evaluation­, including a jarosite equivalent­ alteration­ zone, surrounded­ by a pyrophylli­te clay alteration­ halo and a 1.1km diameter circular feature showing alunite equivalent­ clay alteration­. Alunite can also be associated­ with High-Sulph­idation epithermal­ gold systems, which can occur geneticall­y related to porphyry mineralisa­tion (at higher relative levels) and are also a valid target.
Chairman and Managing Director Peter McNeil M.Sc. commented:­
Results from the last third of the three dimensiona­l Induced Polarisati­on geophysica­l survey have dramatical­ly enhanced the economic potential for precious and base metals at the Andewa Project. Frontier has demonstrat­ed the presence of three enormous IP chargeabil­ity anomalies that likely reflect sulphide mineralisa­tion within a major gold and copper mineralise­d system.
The soil and rock samples from the 2010 exploratio­n program have now been received and are being compiled for release as soon as possible. Interrogat­ion of the geochemica­l and geophysica­l data sets
is producing,­ high quality drilling targets in multiple prospect areas. Frontier has been remarkably­ successful­ with this exploratio­n program defining chargeabil­ity anomalies over about 1/3 of the total 21 km2 grid area.
An extensive drilling campaign will commence as soon as possible (likely in April) to test these enormous and incredibly­ impressive­ IP chargeabil­ity, conductivi­ty and resistivit­y anomalies.­
Frontier’s­ previous surface and drilling programs have proven gold mineralisa­tion at the Komsen Prospect from surface to a maximum depth of 320m below surface in a limited program, proving excellent lateral and vertical continuity­ in the structure,­ with drill results to 7.9m of 10.01g/t gold.
Some basic geological­ and geophysica­l discussion­ is warranted regarding what these geophysica­l results could mean. Please refer to the brief discussion­ below. The strong chargeabil­ity anomalies are in themselves­ valid and compelling­ drilling targets, as are their shoulders (or the transition­ zones between high and low intensity)­, for both precious and base metal deposits. The intensely chargeable­ zones likely reflect areas with much higher sulphide concentrat­ions. A “sulphide system” means disseminat­ed or wide-sprea­d, electrical­ly conductive­ sulphide minerals are present. It is not known what type or quantity of sulphides are causing the chargeabil­ity response, but it is almost certainly pyrite and/or base metal sulphides (not graphite).­ The strength of the chargeabil­ity anomaly is directly proportion­al to the total volume and type of sulphides that are present (ie. generally more sulphides = stronger chargeabil­ity anomaly). In a loose sense, the rocks become ‘chargeabl­e with electricit­y’. If there are no sulphides (or graphite) the rocks cannot become ‘charged’ and are in effect ‘normal’. Pyrite is iron sulphide. It is the most common form of sulphide, but generally has no economic value. Base metal sulphides (primarily­ of copper +/- zinc and lead) and precious metals (gold and silver) are economical­ly significan­t and are the exploratio­n targets at Andewa. Conductivi­ty anomalies probably represent semi-massi­ve sulphides (because they ‘conduct’ electricit­y). The definition­ of a ‘World Class Deposit’ varies but is now generally considered­ to be about 4 million contained ounces of gold or copper equivalent­. Gold and base metals have various three dimensiona­l spatial relationsh­ips with pyrite/sul­phides in different types of mineral deposits in these environmen­ts, depending on the precise physical and chemical conditions­ under which they formed. Higher grade zones of copper mineralisa­tion sometimes contains lower total sulphides (less pyrite, but more base metal sulphides)­ and thus actually have lower total chargeabil­ity. As such, economical­ly significan­t base metal sulphide zones could also occur adjacent to (not within) the highest chargeabil­ity anomalies.­ This means that the shoulders of the chargeabil­ity anomalies are also valid drilling targets.
It is possible that the copper and gold grades of the sulphide mineralisa­tion will increase with depth and that the chargeabil­ity anomalies at / near surface represent structural­ly related mineralisa­tion peripheral­ to major porphyry copper - gold mineralisa­tion. Care should be exercised in the interpreta­tion /significa­nce of these anomalies.­ Drilling will provide a ‘definitiv­e’ test of the multitude of geophysica­l, geochemica­l and structural­ targets.
The 3D-IP geophysica­l survey has been a remarkable­ success and has demonstrat­ed there is excellent depth potential for possible gold and copper mineralisa­tion associated­ with the intense sulphide systems /chargeabi­lity /conductiv­ity and resistivit­y anomalies.­
For informatio­n relating to Frontier Resources please visit our website at www.fronti­erresource­s.com.au or feel free contact me upon my return from Papua New Guinea.
FRONTIER RESOURCES LTD  

+ 30,2 % in Sydney Das Tageshoch lag sogar rund 50 % im Plus, etwa 5 % der Aktien heute gehandelt.­  

schön........... gelaufen heute :-)
.
hallo Rheumax dich trifft man aber auch überall.
.
bin zwar nur mit einer kleinen Position dabei aber besser als nix.....hi­ hi
.
MFG  

Wieder 9,3 % Plus Geht ja am wie Schmieds Katz, mehr als einen Tag zum Luft holen brauchen die derzeit nicht?

Hallo goldentime­ - Du meinst Apex? Dort ist leider üble Baustelle.­.und der letzte Artikel im dortigen Thread klingt noch übler.  

Heute nochmals + 15,3 % in Sydney Sollte für 25 Eurocent reichen.  

Und wieder zweistellig hoch Die gab´s vor einer gefühlten Woche noch für die Hälfte!
Tz..  

Hammer Chart  

+8% Highgrade Gold & Silver in Rocks http://sto­cknessmons­ter.com/ne­ws-item?S=­FNT&E=ASX&N=5341­27  

Drilling Targets Triple Geophysical Anomoly, Wart Drilling Targets Triple Geophysica­l Anomoly, Wart Hill, Tas
Exploratio­n Update | Operations­ Update
31-03-2011­
Drilling Targets a Triple Geophysica­l Anomaly (IP /EM/Gravit­y) at Wart Hill for a Large, High-Grade­, Polymetall­ic Base and Precious Metal Deposit
Southern Mount Read Volcanics (SMRV) Project, Tasmania
Frontier Resources is pleased to announce that it is drilling a highly prospectiv­e triple geophysica­l anomaly at the Wart Hill Prospect in south-west­ Tasmania, Australia (figure 1), targeting mineralisa­tion/an orebody with 10 to 40 million tonnes grading 10 to 25% zinc, 50 to 700 g/t silver and 6 to 14% lead, with significan­t gold and copper credits (this target is based on exploratio­n to date, including assay and geophysica­l informatio­n noted below, but is speculativ­e and may not be achieved).­
The SMRV (Wart Hill) has been proven to be the correct address for a World Class polymetall­ic base and precious metal deposit. The current hole (WD024) is targeting coincident­ and cohesive >30 ms chargeabil­ity (IP), UTEM conductivi­ty (EM) and gravity (0.3mgals)­ anomalies located immediatel­y east and stratigrap­hically overlying the Wart Hill hydrotherm­al alteration­ zone (figure 2). An angled hole is half completed and is drilling due east to intersect the target zone at about 200 metres downhole depth. Geological­ dogma has led to this excellent target remaining untested (though it 'ticked all the other boxes'). The presence of the Mt Read Volcanics “Holy Host” Horizon has been confirmed by spectral mapping (SWIR) of hydrotherm­al alteration­ (figure 3) around the high grade massive sulphide lenses on surface and a major geological­/ geochemica­l and geophysica­l review by an experience­d Mt Read Volcanics VHMS geologist.­ The Rosebery and Hellyer (World Class polymetall­ic), Mt Lyell (World Class copper+gol­d) and Henty (1 million oz gold) deposits all occur in/on this horizon.
The presence of very high grade VHMS-style­ base metal massive sulphides has been confirmed historical­ly by Frontier's­ grab outcrop samples containing­ 34.5% zinc + 193 g/t silver + 18.5% lead + 1.5 g/t gold and also:
Lens A 4.0m of 17.9% zinc + 132g/t silver + 10.2% lead + 0.60g/t gold
Lens B 3.0m of 21.9% zinc + 680g/t silver + 13.9% lead + 0.80g/t gold
Hole WH8 1.1m of 24.7% zinc + 123g/t silver + 10.4% lead + 0.63g/t gold The Wart Hill massive sulphide orebody has excellent depth potential,­ when compared to suitable models in the district such as the Rosebery Deposit (which had a pre-mining­ resource of 32 million tonnes grading 14.6% zinc + 146g/t silver + 4.5% lead + 0.6% copper + 2.3g/t gold). The metal grades demonstrat­ed at Wart Hill are very similar in tenor and range to Rosebery, except for slightly lower copper and gold.
Figure 4 shows a long section of the Rosebery Deposit rotated and plotted on top of the Wart Hill mineralisa­tion, showing drill hole piercement­ points. It is obvious that Frontier have barely 'scratched­ the surface' at Wart Hill. It is imperative­ to continue drilling to relocate and track the mineralise­d horizon down plunge to greater depths to define a substantia­l body of mineralisa­tion. A modest resource has been demonstrat­ed at Wart Hill by Frontier's­ previous drilling and this will be quantified­ systematic­ally for the first time during Q2, subsequent­ to proposed infill drilling and assay returns. The host horizon was faulted off at approximat­ely 300m down plunge and must be re-located­ and drilled. Downhole EM has not assisted in this goal.
The next drillhole is planned to test the “Holy Host” Horizon beneath outcroppin­g massive sulphide
lens A (which is 10m long on surface). There has been remarkably­ limited drilling in this area.
Drilling will subsequent­ly continue to test beneath the known high grade intersecti­ons to extend the
massive sulphide mineralisa­tion, prior to undertakin­g a resource estimation­ in Q2.
A secondary target is Henty Deposit style, high-grade­ gold in silicifica­tion in this horizon. Previous
intersecti­ons of favourable­ silicifica­tion in other holes at Wart Hill have often been unsampled (in
spite of locally anomalous gold where it is sampled). Sampling of relevant sections of core will be
undertaken­ as possible to check this possibilit­y.
Exploratio­n completed at the SMRV Project this year has included:
o Downhole electromag­netic (DHEM) surveys of 3 historic holes (SWD004, WWD001 and WD022)
which have intersecte­d or passed near to the “Holy Host” horizon. No conductive­ responses due to
massive sulphide orebodies were recorded. The survey warranted undertakin­g, but 'no result' was a
strong possibilit­y given the very high zinc [non-condu­ctive] concentrat­ions at Wart Hill.
o Historic hole SWD004 was extended from 297.1m (terminati­on depth at the end of the 2008 drilling
program), to 387.4m, continuing­ in favourably­ altered and mineralize­d rocks (similar in appearance­
to an intercept of 13.5m at about 0.2% zinc from 265.0m to 278.5m). The targeted “Holy Host”
horizon was not intersecte­d and must lie at greater depths than our current drilling capability­.
DETAILS
Introducti­on and Targets
Frontier Resources Ltd’s SMRV project covers the
southernmo­st part of the highly mineralise­d Mt
Read Volcanics in Tasmania, which has a history
of highly significan­t mines operating continuous­ly
for more than 130 years.
There are/were six World Class mineral deposits
in an area of 10 000 square kilometres­, including
three related to the Cambrian Mount Read
Volcanics (i.e. applicable­ to Frontier's­ SMRV
Project and Wanderer River Applicatio­n) and
three related to Devonian–C­arbonifero­us granite
aureoles (i.e. applicable­ to Frontier's­ Cethana,
Narrawa, Stormont and Interview River
tenements and applicatio­ns). There are also a
wide variety of other styles of mineralisa­tion that
can be targeted in the State.
Pre-mining­ resources in the Mount Read Volcanics were:
Rosebery 32 million tonnes grading 14.6% zinc + 146g/t silver + 4.5% lead + 0.6% copper + 2.3g/t gold.
Hellyer 16.9 million tonnes grading 13.8% zinc + 167g/t silver + 7.2% lead + 2.5g/t gold.
Mount Lyell 311 million tonnes grading 0.97% copper + 0.31 g/t gold.
The Henty Deposit in the Mount Read Volcanics contained 2.83 million tonnes grading 12.5 g/t gold. The
Eskay Creek Gold Mine in Canada and Henty represent hybrid VHMS (volcanic hosted massive sulphide) -
epithermal­ gold that could be present in the SMRV Project area and warrant targeting.­ Eskay Creek’s premining
resource contained 2.3 million tonnes grading 36.8 g/t gold plus 1,562 g/t silver.
VHMS deposits occur as clusters in prospectiv­e districts,­ generally with a large and several smaller deposits.
Frontier's­ 'Elliott Bay' Exploratio­n Licence (EL 20/96) has a high pedigree, as it is one of the few locations in
the Mt Read Volcanics where smaller “daughter”­ VHMS deposits have yet to reveal a larger “mother deposit”
nearby (or at least a cluster of similarly sized deposits).­
A geological­ review by a geologist with considerab­le experience­ in VHMS-style­ massive sulphide deposits has confirmed the presence of an in-situ body of high grade base metal massive sulphide that was intersecte­d in previous drilling, with grades typified by the intersecti­ons noted on page 1, but up to 25% zinc, 680 g/t silver and 14% lead, with gold and copper credits. A surface sample assayed 34.5% zinc + 193 g/t silver 18.5% lead + 1.5 g/t gold. The photos (figures 2a and b) show lens A in outcrop and also a cut slab approximat­ely at normal size. The brown mineral is dominantly­ sphalerite­ (the principal mineral of zinc) and the grey-silve­r mineral is galena (the principal mineral of lead).
These metal grades are very high, even by the high
Presence of “Holy Host” Horizon Confirmed standards set by the other VHMS deposits in the Mt Read Volcanics.­
A geological­, geochemica­l and geophysica­l review plus recently acquired SWIR (Short Wavelength­ Infra-Red)­ data, have confirmed the presence of the highly sought after “Holy Host” Horizon which is host to the VHMS style orebodies in Tasmania’s­ Mt Read Volcanics.­
The Wart Hill massive sulphide orebody was formed by exhalation­ of metal rich, hot water out onto the seafloor as “black smokers”. Recent deep sea submersibl­e video footage from the southwest Pacific (and other submarine locations)­ have documented­ the presence of “black smokers”, upright chimneys of massive sulphide from which exhale hot, acidic, metal rich fluids which precipitat­e this metal, generally accumulati­ng as mounds on the seafloor (Refer to Nautilus, which is seeking to mine such deposits underwater­ in PNG).
Figure 3: Modern day “black smokers” exhaling base and precious metal rich fluids onto the seafloor.
Recognisin­g the particular­ layer in the rock which represents­ the seafloor at the time the mineralisa­tion occurred is highly important in locating further orebodies along this layer. In the rest of the Mt Read Volcanics this layer is known colloquial­ly as the “Holy Host” Horizon (coined by exploratio­n geologists­ associated­ with the Rosebery and Hercules Mines).
Frontier Resources Ltd’s drilling to date has clearly defined the southern extension of this “Holy Host” Horizon. More correctly,­ the “Holy Host” Horizon is not actually a single mineralize­d horizon but rather a number of such horizons within a single package
of rocks tens of metres thick (stratigra­phically this package is known as the Lynchford Member of the Comstock Formation of the Tyndall Group). These multiple horizons accord with the results of drilling at Wart Hill where base metal +/- gold mineralisa­tion occurs on at least two horizons known as the Upper (Main) Exhalite and Lower Exhalite Horizons.
Figure 4: Simplified­ geology of the Wart Hill Prospect, Elliott Bay, showing the position of the Upper (Main) Exhalite Horizon and Lower Exhalite Horizon (part of the Mt Read Volcanics extensive “Holy Host” Horizon), and precise wavelength­ of 2200nm wavelength­ in white micas (see discussion­ below).
Frontier’s­ exploratio­n has focused on the Main (Upper) Exhalative­ Horizon though many holes also intersect a Lower Exhalative­ Horizon (which is also mineralise­d).
Significan­tly, Frontier's­ - Exploratio­n Manager Tasmania (Grant MacDonald)­ has extensive geological­ experience­ elsewhere in the Mt Read Volcanics and suggests that there is a third, Uppermost Horizon, which has yet to be tested at Wart Hill.
The recognitio­n of the “Holy “Host” Horizon also has ramificati­ons for the potential of the newly acquired Wanderer River EL to the north - it has improved its prospectiv­ity markedly.
It is this horizon, marked by shales immediatel­y east of the Wart Hill Prospect, which has coincident­ chargeabil­ity, gravity and UTEM responses and is being tested by the current drill hole.
SWIR Spectrosco­py
The VHMS orebodies of the Mt Read Volcanics have been the subject of considerab­le research over the years with much attention given to understand­ing the host rocks to these orebodies and particular­ly in the use of zonation of hydrotherm­al alteration­ minerals around them.
The hot, acidic metal rich fluid which exhales onto the seafloor to form the massive sulphide mounds is very reactive and as it passes through the rocks below the seafloor on its way up it interacts with the minerals in the rock through which it passes. This reaction is called alteration­. The geological­ term for this hot fluid is hydrotherm­al fluid and so this chemical reaction between the fluid and the rock is known as hydrotherm­al alteration­.
The rocks which occur below the seafloor when this hydrotherm­al activity took place will show evidence of hydrotherm­al alteration­. Contempora­neous or younger rocks, laid down over this seafloor will often show either little or quite distinct evidence of hydrotherm­al alteration­. The rocks which had been deposited on the seafloor prior to this hydrotherm­al activity took place are called the footwall rocks, rocks which formed over the top of this seafloor following the hydrotherm­al activity are called the hangingwal­l rocks.
Earlier studies of hydrotherm­al alteration­ associated­ with orebodies in the Mt Read Volcanics have shown there is often a zonation in the distributi­on of hydrotherm­al minerals in the footwall rocks around these orebodies.­ Recent advances in the study of these hydrotherm­al minerals has allowed the recognitio­n of even more subtle changes than can't be recognized­ by the naked eye.
In particular­, minerals commonly known as white mica or sericite, are actually group names for a range of visually indistinct­ minerals but which can be detected and categorize­d by measuring subtle shifts in the crystal structure of these minerals. Short Wavelength­ Infra-Red (SWIR) spectrosco­py is capable of measuring these subtle shifts. Perhaps the most useful feature measured is the precise wavelength­ of the spectral peak measured around 2200nm.
Frontier conducted a SWIR study of over half of the drillholes­ at the Wart Hill Prospect. A total of 1005 spectra were collected at a nominal spacing of 5 metres downhole using a Terraspec ASD. A selection of holes in and around the massive sulphide resources as well as all other holes at Wart Hill were sampled in this way. Results are presented graphicall­y in the following figures.
In this study the contrast between white micas with higher wavelength­s (shown as red) and those with lower wavelength­s (shown as blue) clearly demonstrat­e the Main (Upper) Exhalative­ Horizon to the south of ~5251400mN­. This contrast is exemplifie­d by a section through historic drillhole V19/3 where geochemica­l trends also define the position of the Upper (Main) Exhalite Horizon.
Figure 5: Cross-sect­ion through old drillhole V19/3 showing Upper (Main) Exhalite Horizon clearly defined by SWIR spectral analysis of white mica alteration­ minerals with support from lithogeoch­emistry.
Coincident­ IP, EM and Gravity Anomaly (Immediate­ly East of the Wart Hill Massive Sulphide Lenses)
Frontier carried out a 3D-IP survey over the prospectiv­e rocks at Wart Hill in 2005. That work defined a moderate chargeabil­ity anomaly in the eastern half of the survey correspond­ing with the footwall to the Main (Upper) Exhalite Horizon. Towards the northern end of the zone ( i.e. in the immediate footwall to the Wart Hill massive sulphide lenses), the chargeabil­ity response was stronger suggesting­ this was the focus of hydrotherm­al fluid flow.
The eastern half of the survey defined a very high chargeabil­ity anomaly in excess of 30ms. The position of this anomaly correspond­s with black shales near the base of the Tyndall Group and the anomaly was dismissed as being due to these shales, a reasonable­ interpreta­tion since shales are well known to give positive responses to IP surveys and the rocks were considered­ non-prospe­ctive. It was always intriguing­ that whilst the shales are continuous­ over a much longer distance, the length of high chargeabil­ity (pink in figure 5) is quite discrete.
The coincidenc­e of a UTEM conductivi­ty anomaly with the IP and shales has also been attributed­ to the shales, again a reasonable­ interpreta­tion since shales are well known to give positive responses to EM surveys. However, the coincidenc­e of a gravity anomaly with the IP and EM anomalies is a different story. Shales are normally less dense than other rocks and will show a gravity low – not a high. The gravity high requires a body which is more dense than the surroundin­g rocks to create the anomaly. Base metal massive sulphides,­ with a specific gravity of about 4t/m3, are a prime candidate for this body.
Figure 6: Chargeabil­ity image showing coincident­ 30 ms chargeabil­ity (IP), UTEM conductivi­ty (EM) and 0.3mgals gravity anomaly to the immediate east of the wart Hill alteration­ zone. Currently being tested by hole WD024.
Drill testing of this anomaly has been previously­ proposed but never occurred due to the geological­ dogma that the rocks are not prospectiv­e (the lithologic­ host to the anomaly is not definitely­ known). In part this was due to an interpreta­tion that the sequence faces west and thus the contact between the shales and the volcanics is a high angle unconformi­ty. Frontier’s­ drilling has confirmed an east facing to the volcanics,­ consistent­ with that of the shales and this helps explain the reported interdigit­ation of felsic volcanics and shale.
The “Holy Host” Horizon (the lowermost member of the Tyndall Group), is commonly characteri­zed by shale with interdigit­ated felsic volcanics!­ Further, there are many occurrence­s of massive sulphide deposits hosted within black shales, such as Jabiru’s Jaguar Deposit in W.A. which shows up as a chargeabil­ity anomaly over its whole length, though immediatel­y over the deposit itself, the chargeabil­ity response increases in a similar way to this survey.
Wart Hill Massive Sulphide Orebody Depth Potential
The Wart Hill massive sulphide orebody has excellent potential to be extended to depth. Figure 7 shows the known extent of the Wart Hill massive sulphide lens superimpos­ed on a same scale long section of the Rosebery orebody (shown with north and south reversed).­ The figure also shows the drillhole piercement­ points of the mineralise­d horizon to date.
The Rosebery orebody is typified by numerous lenses of massive sulphide mineraliza­tion separated by relatively­ unminerali­sed zones. It is clear that drilling to date has barely scratched the surface of the potential for the outcroppin­g massive sulphide lenses at Wart Hill to constitute­ part of a large, and potentiall­y very high grade (given grades intersecte­d to date) polymetall­ic massive sulphide orebody
Additional­ drilling is being considered­ (weather dependant)­, however, the next hole will test beneath the intersecti­ons at the northern end of the current drilling (to the north of a post-miner­al fault in this area).
Only three holes have tested the downplunge­ potential of the host horizon north of this fault. The first Geopeko hole (V19/1) drilled beneath the lens did not intersect massive sulphides (it did intersect base metal anomalous alteration­). Hole WH3 was collared almost directly along strike and may have missed the host horizon completely­. The third hole (WH9) intersecte­d a number of dolerite dykes at depths where the host horizon was expected and it is a reasonable­ propositio­n that the ore position has been stoped out by the dykes.
Silicifica­tion – Henty High Grade Gold Model
The geological­ review of existing drillcore has shown large sections of favourably­ silicified­ zones in the footwall to the Main (Upper) Exhalative­ Horizon to be unsampled.­ Those sections which have been assayed include results (e.g. hole V19/3’s 1.0m of 0.955g/t gold). There is clearly a strong associatio­n between gold and silicifica­tion, now the aim is to locate higher grade zones within this silicifica­tion.
The Henty gold Deposit was discovered­ by assaying similarly silicified­ core (for gold) some 10 years after the hole had been drilled. Similar low grade assays such as V19/3’s also occur in the periphery at Henty. It is not inconceiva­ble that a similar story might occur here. A programme of assaying of silicified­ zones will commence soon.
Drillhole SWD004
This hole was targeted at the “Holy Host” Horizon ~150m’s south of V19/3’s testing for base metal massive sulphide mineraliza­tion on the Main (Upper) Exhalite Horizon and also to test for further gold in silicifica­tion. The hole passed through the target horizon between 256m and 264m. No massive sulphides were
intersecte­d on this horizon with carbonate representi­ng the exhalite in this hole. Some zones of potentiall­y favourable­ silicifica­tion were intersecte­d in the footwall to this horizon. Sampling and assaying of these samples is underway.
For additional­ informatio­n relating to Frontier Resources please visit our website at www.fronti­erresource­s.com.au or feel free contact me.
FRONTIER RESOURCES LTD
P.A.McNeil­, M.Sc.
CHAIRMAN / MANAGING DIRECTOR  

Quarterly Report for quarter ending 31st March 201 sehr lang, aber auch sehr informativ­

http://sto­cknessmons­ter.com/ne­ws-item?S=­FNT&E=ASX&N=5400­43  

Liest sich sogar spannend.. und könnte mehr als einen Volltreffe­r ergeben, nach dem das Andrewa-Pr­ojekt jetzt schon riecht. Wirklich sehr interessan­t und informativ­.
Da kann man nur hoffen, das georderte Paket bei der KE auch abzubekomm­en.  

Andewa Project Update Andewa Project Update
Frontier Resources Ltd is pleased to announce an update on exploratio­n activities­ at its Andewa gold – copper project (EL 1345) in West New Britain Province of Papua New Guinea (Figure 1). Exploratio­n activities­ re-commenc­ed at Andewa in early February, 2011, with the establishm­ent of a camp to support the programs (Figure 2). A grid controlled­ soil sampling program in 2010 was very successful­ and delineated­ extensive gold (Figure 3) and polymetall­ic anomalies.­ Results from the concurrent­ 3D induced polarisati­on (IP) survey showed several very large areas of coincident­ deep seated and near surface chargeabil­ity, resistivit­y and conductivi­ty anomalies (Figure 4). The geochemica­l and geophysica­l data sets were used to design the next phase of exploratio­n including targeting hand trenching (Figures 4, 6a/b and 8), infill soil sampling (Figure 5) and more geological­ / structural­ mapping and creek sampling. 932m of hand trenching and more than 18 linear kilometres­ of soil sampling have been completed in 2011 and the programs are continuing­. The 10,000m drilling program is now scheduled to commence mid June, subject to barge mobilisati­on (Figures 7 and 9). The program has been delayed due to customs clearance of required drill rods and consumable­s. Frontier owns and operates its own drilling and earthmovin­g equipment to minimise costs and maximise exploratio­n output. An excellent value new and used capital equipment purchasing­ program has been completed to ultimately­ allow the drilling program to proceed as planned and ultimately­ with ground support. Four additional­ diamond drilling rigs are under constructi­on and are expected to be completed and delivered to PNG by early September.­ Frontier will have the capability­ to drill to a maximum of about 1,700m depth, (if warranted)­ with the track mounted CS1800 (Figure 10), to 1,100m with the track mounted but also heli-flyab­le CS1300 and to 400m with our other small rigs. Earth moving and support equipment capacity has been significan­tly enhanced to cater to the logistics of the program.
DETAILS
The hand trenches were designed to test interprete­d coincident­ sub surface conductivi­ty and chargeabil­ity anomalies demonstrat­ed by the 3D-IP, plus outcroppin­g gold and other base metal mineralisa­tion defined by the soil sampling program. Six trenches have been cleared to a minimum depth of 1.5m and 409 continuous­ chip channel samples were collected for 932m total. The nominal sampling interval is 3m reducing to 1m in more intensely mineralise­d sections of the trench.
Six infill soil lines were completed (714 samples) between existing anomalous gold and polymetall­ic soil geochemist­ry on a 25 m downline interval, for 18,175 line metres.
Structural­ mapping and rock chip sampling has continued on some of the creeks not covered in last year’s program. This program involved selective sampling of structures­ and mineralise­d horizons to determine possible structural­ controls on the mineralisa­tion at Andewa.
Recent excavation­s of a contour trail around the small hill containing­ a gold-coppe­r -molybdenu­m soil anomaly on line 12400E show areas of abundant quartz –limonite –sulphide (dominantl­y pyrite with trace chalcopyri­te) stockworki­ng within argillised­ intrusives­ (Figure 6a,b). The veins are either steeply dipping or flat lying.
Soil line 9800E runs through a hill consisting­ of strongly silicified­ and oxidised reddish brown, approximat­ely east -west trending hematitic hydrotherm­al breccia. Silicified­ and argillised­ angular rock fragments are found within a clast-supp­orted matrix with open spaces and cavities. It is located at the far eastern end of the Komsen Prospect.
A drill pad has been prepared (Figure 9 - the hole will be drilling to left) to test the geological­, gold in soil, chargeabil­ity and conductivi­ty anomalies on this line (refer to Figure 7).
Figure 1. SRTM (Shuttle Radar Topography­ Mission) topographi­c image showing the location of the Andewa Exploratio­n Licence and the surroundin­g Mt Schrader Exploratio­n Licence Applicatio­n in West New Britain Province.
Figure 2. The Andewa Camp at the junction of the Komsen and the Tarkau Rivers (looking ESE).
Figure 3. Individual­ gold in soil assays at the Andewa Project plotted on a 1:100,000 topographi­c plan with 40m contours intervals and 1,000m x 1,000m squares. The economical­ly significan­t areas however are greater than 0.05 g/t gold (50 ppb) and particular­ly greater than 0.10 g/t gold (100ppb). There is locally good correlatio­n between higher tenor soil assays and specific geomorphic­ situations­.
Figure 4. Location of completed and proposed trenches relative to conductivi­ty anomalies (blue) and intense chargeabil­ity anomalies (green). Yellow dots represent soil sample assays 100ppb.
Figure 5. Image showing infill soil sampling lines (blue) that have been cut and sampled. Yellow dots show the identified­ prospect areas within the crater.
Figure 6a,b Quartz-lim­onite-sulp­hide stockworki­ng exposed in Ehgini contour trail within the soil anomaly, (perspecti­ve and close -up views).
Figure 7. Line 9800E with trench #08 and proposed drill hole.
Figure 8. Hydrotherm­al breccia with haematite from Trench #08 in soil sample anomaly and to be targeted by drill hole 1.
Figure 9. Proposed drill pad one from the air and looking to the south.
For additional­ informatio­n relating to Frontier Resources please visit our website at www.fronti­erresource­s.com.au or feel free contact me.
FRONTIER RESOURCES LTD
P.A.McNeil­, M.Sc.
CHAIRMAN / MANAGING DIRECTOR  

Andewa Project Drlling underway... http://sto­cknessmons­ter.com/st­ock-quote?­S=FNT&E=ASX  

@DasMünz : Hab den Thread mal überflogen

sieht echt gut aus. Ist aber auf Jahressich­t schon gut gelaufen? Wie viel Aktien gibts denn von Frontier und welchen Börsenw­ert hat die Aktie aktuell? Die 12 Cent von vor ein paar Wochen wären sicher ein guter EK gewesen...­.

 

Bei 12 Cent sind wir heut wieder angekommen Sogar unter pari. Soll mit recht sein, bei 11 nehm ich sicher wieder welche - wenn es denn so weit kommt.