RL got its drill permits for the Blue Lake Cu-Ni-Pt-Pd property, Labrador Trough, Quebec. The Company
has mobilized fuel and supplies to its base camp in preparation for
drilling commencing in early July.
The Blue Lake sulfide deposits are nickeliferous pyrrhotite
ores, with a copper content twice that of nickel, containing significant
platinum and palladium. The historical tonnage, established in 1989,
was 4.03 Mt at 0.85% Cu, 0.52% Ni and 0.84 g/t platinum and palladium.
The Blue Lake historical deposits are located within a Québec Special
Mining lease BEP-93, one of five Special Mining leases optioned to
Rockland from La Fosse Platinum Group. In addition to the Blue Lake
property, Rockland controls, the Retty Lake, Jimmick, Chance Lake,
Glance Lake, Fredrickson and Lac Aulneau properties, all in the southern
Labrador Trough. The Blue Lake area is ideally located as a positive
mining destination, approximately 60 km from the town of Schefferville,
Quebec which has its own airport and railhead. Rockland is
systematically exploring this region and its goal is to discover
mineralization, confirm and expand tonnage on its property holdings.
A blog about mineral exploration current events with a focus on Gold, Base Metals and the companies that search for them all over the world. My particular focus is on exploration in Quebec's Labrador Trough and following the New Yukon Gold Rush.
Showing posts with label copper. Show all posts
Showing posts with label copper. Show all posts
Thursday, June 07, 2012
Tuesday, August 23, 2011
Rockland News: Retty Lake Cu-Ni-PGM Core Sampling Completed, Quebec
Rockland Minerals Corp. (TSX VENTURE:RL) (the "Company") is pleased to announce that core samples from the 1,500 meter Retty Lake Cu-Ni-PGE drilling program have been submitted to a commercial laboratory for precious metals fire assay and multi-element geochemical analysis. The core was carefully saw-cut, and a half-split was retained at the IOS Services Géoscientifiques facility in Chicoutimi, QC for detailed logging and petrographic studies. The precious metals fire assay procedure to be used for palladium and platinum will be a more robust one assay-ton (50g charge) to insure the most reliable and repeatable results.
Gold fire assay results and multi-element geochemical results are also awaited from Rockland's Schefferville Gold Project, where 367 surface rock chip samples were collected from the new Rusty Acres area during an early summer 2011 field program guided by a detailed 50 meter-spaced heli-mag survey flown in May 2011.
George Sanders, P.Geo, a director of the Company, and qualified Person under NI 43-101 responsible for the technical content of this News Release states: "We all share the anticipation of the Retty Lake drilling results. The drill core was flown from Retty Lake to the nearby town of Schefferville when the drill was de-mobed, but remained in the queue to be transported via rail to the port of Sept-Îles for quite awhile. The intense iron ore development in the Schefferville area is exciting, and better infrastructure favours advancement of Rockland's two exploration projects located very close to Schefferville. There will be bottlenecks here and there as the service sector matures, but the first look at the rock samples from both projects is very encouraging."
Gold fire assay results and multi-element geochemical results are also awaited from Rockland's Schefferville Gold Project, where 367 surface rock chip samples were collected from the new Rusty Acres area during an early summer 2011 field program guided by a detailed 50 meter-spaced heli-mag survey flown in May 2011.
George Sanders, P.Geo, a director of the Company, and qualified Person under NI 43-101 responsible for the technical content of this News Release states: "We all share the anticipation of the Retty Lake drilling results. The drill core was flown from Retty Lake to the nearby town of Schefferville when the drill was de-mobed, but remained in the queue to be transported via rail to the port of Sept-Îles for quite awhile. The intense iron ore development in the Schefferville area is exciting, and better infrastructure favours advancement of Rockland's two exploration projects located very close to Schefferville. There will be bottlenecks here and there as the service sector matures, but the first look at the rock samples from both projects is very encouraging."
Wednesday, July 20, 2011
Rockland Gold and Cu-Ni-PGM Exploration Update Labrador Trough Area
News release, July 19, 2011, Rockland Minerals Corp. (RL-TSX Venture) has provided an update with regard to its exploration activities in Labrador Trough area of northeastern Quebec. So far during the current field season Rockland has drilled the Retty Lake Cu-Ni-PGE (platinum group elements) property, and has flown a detailed heli-mag survey over the most promising portion of the Schefferville gold property to guide follow-up field mapping and sampling.
A total of 1,500 metres was drilled in the Northwest Retty Lake area with 10 holes that targeted known copper-nickel-platinum-palladium mineralization along a significant trend that is largely covered by Rockland claims. The target middle sill peridotite unit was intersected in all the holes, and significant disseminated chalcopyrite (copper mineral) was observed in broad zones of the host rock peridotite with highly favourable net texture of disseminated sulphides. The drill core was shipped via rail from Schefferville, Que., and has arrived at the core processing facility in Chicoutimi, Que. It is now being logged, saw cut and sampled, and assay results will be released as soon as possible after each batch of samples passes strict quality assurance/quality control protocols.
Follow-up fieldwork is now well under way on the northern block of Rockland Minerals Corp.'s Schefferville gold property, using recently flown data from a low-altitude draped heli-borne magnetometer survey on a 50-metre-spaced grid. The focus of Rockland's 2011 geological fieldwork is on the Rusty Acres area, which has never been drilled. Here, several clusters of plus-one-gram-per-tonne Au historic surface samples in outcropping rusty, iron-formations are seen on the compilation map. A total of 367 surface samples have been taken so far, and have been shipped for assay.
George Sanders, PGeo, a director of the company, is the qualified person under National Instrument 43-101 responsible for the technical content of this news release.
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Thursday, June 23, 2011
Pictures: Retty Lake Cu-Ni-PGE Drill Core and Write up
Must see new pictures of Rockland's Retty Lake Cu-Ni-PGE drill core and a technical write-up comparing the rocks to the Ungava southern mineral belt. See pictures at http://bit.ly/mjfwQr . Assay results are in process.
Wednesday, June 22, 2011
Rockland Completes Drilling at Retty Lake Cu-Ni-PGE, Quebec
For Immediate Release. Vancouver, British Columbia, June 22, 2011: Rockland Minerals Corp. (TSX Venture: RL) (the “Company”) has completed its 1,500 meter diamond drilling program on the Retty Lake Cu-Ni-Pt-Pd Property located near Schefferville, Quebec. A total of 10 holes were drilled to explore for zones of disseminated and massive sulfide within the targeted middle peridotite sill in the NW Retty Lake area. The core is being shipped off site to a core processing facility to be saw cut and sampled.
Photographs of Retty Lake drill core textures and a brief geological write-up have been posted on Rockland's website at www.rocklandminerals.ca.
Initial logging of the core has revealed widespread disseminated sulfide mineralization with visible chalcopyrite (copper mineral) within the lower portion of the middle peridotite sill. In several instances, favourable "net-texture" sulfides were observed to be crystallized within cumulate-texture peridotite. Two drill holes found an unexpected rock type in place of the middle peridotite horizon. Instead of the ultramafic peridotite, there was a melanocratic gabbro, which indicates assimilation of the wall rock by the peridotite intrusion. This typically happens adjacent to feeder dykes, and suggests they may be nearby, although they have never been described at Retty Lake. Mineralization was also drilled in the upper sill, in addition to the widespread disseminated mineralization found in the middle sill. This confirms the presence of "stacked" mineralization at Retty Lake.
George F. Sanders, P.Geo, a director of the Company, and Qualified Person under National Instrument 43-101 responsible for the technical content of this news release, states: “We see highly encouraging disseminated sulfide textures in hand samples of the drill core from the Retty Lake Project, and we're only in the beginning stages of unlocking the copper-nickel-platinum-palladium potential of this district. Because this is the first drill core to come from this area since the 1950's, we plan on doing a careful, thorough job of sawing, splitting and sampling the core."
Photographs of Retty Lake drill core textures and a brief geological write-up have been posted on Rockland's website at www.rocklandminerals.ca.
The Retty Lake property is on-trend with four adjacent copper-nickel-platinum group metal (PGM) lenses known as the “Blue Lake Deposits” -- originally outlined by Hollinger North Shore Exploration (Iron Ore Company of Canada) in the 1950's. Evidently, the Blue Lake Cu-Ni-Pt-Pd deposits were formed at or near the basal zone of the ("Middle") ultramafic peridotite, where the sill intrudes sulfur-rich metasediments. This favourable stratabound horizon runs for some ten kilometers or more, throughout the Rockland property, in a northwest-southeast trajectory. Rockland is looking forward to discovery of additional base metal - precious deposits within its Retty Lake property. Rockland is earning a 100% interest in the property from E.D. Black, Geologist.
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Thursday, June 09, 2011
What are net-texture sulphides?
Rockland Minerals (TSX Venture: RL) recently provided an update on its drilling program at the Retty Lake copper-nickel-platinum-palladium property, in Quebec. In particular, Rockland mentioned observing very encouraging "net-textured" sulphides in this news release.
To provide a bit more insight into "net-textured" sulphides I have posted some info from Wiki-pedia.
"The morphology of Kambalda-type Ni-Cu-PGE deposits is distinctive because the nickel sulfide can be shown to be associated with the floor of a komatiite lava flow, concentrated within a zone of highest flow in the lava channel facies.
The lava channel is typically recognised within a komatiite sequence by;
Wiki goes on to say ....
"The massive sulfide is in some cases overlain by a zone of matrix sulfide. The ideal Kambalda type-section lacks matrix sulfides, which is interpreted to be because of either physical remobilisation, or because matrix ore will only form in quiescent magma conditions, and thus does not form in active channel zones except, perhaps, late in the eruption. However, most other komatiitic nickel ore sections contain matrix to net-textured ore.
Matrix sulfide ore, in high-grade metamorphic areas, is characterised by jackstraw texture, composed of bladed to acicular metamorphic olivine which resembles spinifex textured olivines, within a matrix of nickel sulfide. This texture is formed by metamorphism of the ore, which is interpreted to have been composed of olivine crystals floating in massive sulfide.
Net-textured ore is rarely observed, being the ideal condition of sulfide-silicate immiscibility. This texture is difficult to prove from the majority of komatiite mineralisation profiles, but is known from the Jinchuan intrusive, China, where nickel sulfide forms a network textured groundmass liquid in which olivine floats. Most net-textured ores in komatiites are considered metamorphic overprints.
Disseminated sulfide zones occasionally overly the matrix sulfide zone, grading upwards into barren ultramafic olivine adcumulate. These zones are rarely economic to mine in the majority of komatiites, except when close to surface."
To provide a bit more insight into "net-textured" sulphides I have posted some info from Wiki-pedia.
"The morphology of Kambalda-type Ni-Cu-PGE deposits is distinctive because the nickel sulfide can be shown to be associated with the floor of a komatiite lava flow, concentrated within a zone of highest flow in the lava channel facies.
The lava channel is typically recognised within a komatiite sequence by;
- Thickening of the basal flow of the komatiite sequence
- Increased MgO, Ni, Cu, and concomitant decrease in Zn, Cr, Fe, Ti as compared to 'flanking flows'
- A 'sediment free window' where sediment has been scoured or melted from the basal or footwall contact of the komatiite with the underlying substrate
- A trough morphology, which is recognisable by a reentrant flat and steep-sided embayment in the footwall underlying thickest cumulate piles
Wiki goes on to say ....
"The massive sulfide is in some cases overlain by a zone of matrix sulfide. The ideal Kambalda type-section lacks matrix sulfides, which is interpreted to be because of either physical remobilisation, or because matrix ore will only form in quiescent magma conditions, and thus does not form in active channel zones except, perhaps, late in the eruption. However, most other komatiitic nickel ore sections contain matrix to net-textured ore.
Matrix sulfide ore, in high-grade metamorphic areas, is characterised by jackstraw texture, composed of bladed to acicular metamorphic olivine which resembles spinifex textured olivines, within a matrix of nickel sulfide. This texture is formed by metamorphism of the ore, which is interpreted to have been composed of olivine crystals floating in massive sulfide.
Net-textured ore is rarely observed, being the ideal condition of sulfide-silicate immiscibility. This texture is difficult to prove from the majority of komatiite mineralisation profiles, but is known from the Jinchuan intrusive, China, where nickel sulfide forms a network textured groundmass liquid in which olivine floats. Most net-textured ores in komatiites are considered metamorphic overprints.
Disseminated sulfide zones occasionally overly the matrix sulfide zone, grading upwards into barren ultramafic olivine adcumulate. These zones are rarely economic to mine in the majority of komatiites, except when close to surface."
Monday, June 06, 2011
Raglan to Labrador Trough Presentation
Presentation by Rockland Minerals comparing the southern Raglan mineral belt and the rocks in the Labrador Trough, where Rockland has its Retty Lake Cu-Ni-PGM project (presentation here.) The Raglan Mine is a large nickel mining complex in the Nunavik region of northern Quebec, Canada. It is owned and operated by Toronto, Ontario based Xstrata Nickel (formerly Falconbridge Ltd.), a division of Swiss-based Xstrata plc.
Friday, June 03, 2011
Rockland Drills "Net-Texture" Sulfides in Ultramafic Rocks at Retty Lake Cu-Ni-PGE, Québec
For Immediate Release. Vancouver, British Columbia, May 31, 2011: Rockland Minerals Corp. (TSX Venture: RL) (the “Company”) has intersected several zones of disseminated sulfides within the targeted middle peridotite sill being drilled on the Retty Lake Cu-Ni-Pt-Pd Property. In diamond drill hole number 849-05, drilled near the "Lac Retty Ouest" showing, Rockland geologists have observed very encouraging "net-textured" disseminated pyrrhotite and visible chalcopyrite (copper mineral) within a 14-meter basal zone of cumulate-texture ultramafic peridotite. Rockland is currently half way through a planned 1,500 meter program, which commenced on May 15th, 2011. After all drilling is complete, assaying of the mineralized core will begin.
Hole 849-03 encountered 60 meters of disseminated pyrrhotite with visible chalcopyrite -- in coarse cumulate- textured peridotite -- at the Lost Lake showing. All of the drilling so far has intersected zones of layered massive sulfide and cross-cutting sulfide, within black shales. These metamorphosed sediments at Retty Lake are intruded by mafic gabbros and ultramafic peridotites, in a setting very similar to the southern Raglan Cu-Ni-PGE mineralized belt in Québec's Ungava region to the north.
Upon completion of the drill program Rockland plans to transport the Retty core to the IOS Services Geoscientifiques Inc. processing facility where Rockland's geotechs will split and select mineralized segments for assaying. Assay results will be made available as completed.
George F. Sanders, P.Geo, a director of the Company, and Qualified Person under National Instrument 43-101 responsible for the technical content of this news release, states: "Our Retty Lake drilling program is progressing very well. The 'net textured' disseminated sulfides within the lower portion of the middle peridotite sill are guides to discovery of more massive sulfide lenses, similar to the adjacent Blue Lake Cu-Ni-PGE cluster. We have chosen to transport the drill core offsite for more precise logging, sawing and sampling. This is the first drilling in this area since the 1960's, and Rockland intends to process it thoroughly, to unlock the Cu-Ni-PGE potential of these deposits. Sample shipments and assaying will be expedited, and results will be released a soon as possible."
The Retty Lake property is on-trend with four adjacent copper-nickel-platinum group metal (PGM) lenses known as the “Blue Lake Deposits” -- originally outlined by Hollinger North Shore Exploration (Iron Ore Company of Canada) in the 1950's. Evidently, the Blue Lake Cu-Ni-Pt-Pd deposits were formed at or near the basal zone of the ("Middle") ultramafic peridotite, where the sill intrudes sulfur-rich metasediments. This favourable stratabound horizon runs for some ten kilometers or more, throughout the Rockland property, in a northwest-southeast trajectory. Rockland is looking forward to discovery of additional base metal - precious deposits within its Retty Lake property. Rockland is earning a 100% interest in the property from E.D. Black, Geologist.
Hole 849-03 encountered 60 meters of disseminated pyrrhotite with visible chalcopyrite -- in coarse cumulate- textured peridotite -- at the Lost Lake showing. All of the drilling so far has intersected zones of layered massive sulfide and cross-cutting sulfide, within black shales. These metamorphosed sediments at Retty Lake are intruded by mafic gabbros and ultramafic peridotites, in a setting very similar to the southern Raglan Cu-Ni-PGE mineralized belt in Québec's Ungava region to the north.
Upon completion of the drill program Rockland plans to transport the Retty core to the IOS Services Geoscientifiques Inc. processing facility where Rockland's geotechs will split and select mineralized segments for assaying. Assay results will be made available as completed.
George F. Sanders, P.Geo, a director of the Company, and Qualified Person under National Instrument 43-101 responsible for the technical content of this news release, states: "Our Retty Lake drilling program is progressing very well. The 'net textured' disseminated sulfides within the lower portion of the middle peridotite sill are guides to discovery of more massive sulfide lenses, similar to the adjacent Blue Lake Cu-Ni-PGE cluster. We have chosen to transport the drill core offsite for more precise logging, sawing and sampling. This is the first drilling in this area since the 1960's, and Rockland intends to process it thoroughly, to unlock the Cu-Ni-PGE potential of these deposits. Sample shipments and assaying will be expedited, and results will be released a soon as possible."
The Retty Lake property is on-trend with four adjacent copper-nickel-platinum group metal (PGM) lenses known as the “Blue Lake Deposits” -- originally outlined by Hollinger North Shore Exploration (Iron Ore Company of Canada) in the 1950's. Evidently, the Blue Lake Cu-Ni-Pt-Pd deposits were formed at or near the basal zone of the ("Middle") ultramafic peridotite, where the sill intrudes sulfur-rich metasediments. This favourable stratabound horizon runs for some ten kilometers or more, throughout the Rockland property, in a northwest-southeast trajectory. Rockland is looking forward to discovery of additional base metal - precious deposits within its Retty Lake property. Rockland is earning a 100% interest in the property from E.D. Black, Geologist.
Rockland Minerals Provides Retty Lake Cu-Ni-PGM Project Update
April 19, 2011, Vancouver, BC, Canada – Rockland Minerals Corp. (The “Company” or “Rockland”), (TSX.V: RL) is pleased to provide an update on its ongoing preparation for drilling at its Retty Lake Cu-Ni-Pt-Pd Property, northwest of Schefferville, Québec. Rockland has completed its fuel purchase order of Diesel and Jet-A for the 2011 program. Rockland recently announced that it had signed a drill contract with Cartwright Drilling of Goose Bay, Labrador to drill a minimum of 1,500 meters, of core holes at the Retty Lake for late May. The fuel barrels will now be flown to the Retty Lake area from Schefferville. Rockland has selected Air Saguenay of Jonquière, QC , for its fixed wing air capability and sourcing of the fuel. Rockland is working with its turn-key service provider, IOS Services Geoscientifiques Inc. (“IOS”) of Chicoutimi, Québec, to finalize the Retty Lake project logistics.
The Retty Lake property is on-trend with four known adjacent copper-nickel-platinum group metals (PGM) lenses known as the “Blue Lake Deposits” originally outlined by Hollinger North Shore Exploration in the 1950's. The Blue Lake Cu-Ni-Pt-Pd deposits were formed at or near the basal zone of a ultramafic peridotite sill, where it was intruded sulfur-rich metasediments. This favourable horizon runs through the Rockland property in a northwest trajectory and Rockland is looking to discover additional lenses on the Retty Lake property.
George F. Sanders, P.Geo, a director of the Company, and the Qualified Person under National Instrument 43-101 responsible for the technical content of this news release.
The Retty Lake property is on-trend with four known adjacent copper-nickel-platinum group metals (PGM) lenses known as the “Blue Lake Deposits” originally outlined by Hollinger North Shore Exploration in the 1950's. The Blue Lake Cu-Ni-Pt-Pd deposits were formed at or near the basal zone of a ultramafic peridotite sill, where it was intruded sulfur-rich metasediments. This favourable horizon runs through the Rockland property in a northwest trajectory and Rockland is looking to discover additional lenses on the Retty Lake property.
George F. Sanders, P.Geo, a director of the Company, and the Qualified Person under National Instrument 43-101 responsible for the technical content of this news release.
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