Rapier Gold provides exploration update on the Pen Gold Project, 37.6 g/t sample taken in new target area

Transcription

1 Suite W. Georgia Street P.O. Box 11144, Royal Centre Vancouver, BC V6E 3P3 Telephone: rapiergold.com October 4, 2013 TSX-V: RPR Rapier Gold provides exploration update on the Pen Gold Project, 37.6 g/t sample taken in new target area Vancouver, BC Rapier Gold Inc. (TSX-V: RPR) (the Company ) is pleased to provide an exploration program update for its Pen Gold Project, approximately 75 km southwest of Timmins, Ontario. The summer mapping and prospecting program was completed last week. The majority of the field work has focused on the northern portion of the Pen Gold Project to expand on previous prospecting by Rio Tinto and to meet the expenditure obligations under our share purchase agreement. Highlights of the work to date include: 37.6 g/t sample taken at the Area, 2 km southwest of the Talc Mine Area, confirms the potential for a new target location. The anomalous trend has been extended to a distance of 3.5 km. The Porphyry Hill Area anomalous trend appears to be 1.5 km long. Geochemist Dr. Tim Barrett has completed an initial review of data. We have commenced further work to test for possible Volcanogenic Massive Sulphide (VMS) mineralization, initially identified in drill hole PG Links to Appendices: Appendix 1 - Maps of 2013 sample locations and 2013 an 2010 geochemical anomalies: Appendix 2 - Sampling results, see Appendix 1 for map of anomalies: Appendix 3 - Area: Appendix 4 - New Hydro Line Area: Mapping/Prospecting: See Appendix 1 for sample location map and Appendix 2 for sample results table Approximately 4,100 hectares, or approximately 25%, of the Pen Gold Project s 16,000 hectare property has now been covered by mapping and prospecting crews. More than 90% of the assays have been returned. 43 samples reported grades greater than 50 ppb gold. Highest values are 37.6 g/t from the Area and 4.89 g/t from a sub-outcrop west of the Area. The Area, 2 km southwest of the Talc Mine Area, was identified initially in our data compilation work. Eighteen anomalous values were returned from the stripped area reconfirming the anomalous values found by Steetley Industries Limited (Steetley) in the 1980s. This includes a 37.6 g/t sample taken close to the location of a grab sample taken by Steetley that returned 1.3 oz/t from a narrow east-west structure. (See Appendix 3 for more details on the Area.)

2 Three new anomalous gold values were returned from east of the Area ( Eastgate ), where a grab sample assayed 1.2 g/t, potentially extending the zone another 1,000 m to the east. Anomalous gold values from grab sampling have now been returned over a distance of 2.5 km along this ridge of altered mafic volcanics with quartz veining and sulphides. Another grab sample from sub-outcrop, taken earlier this summer, returned a value of 4.89 g/t gold from a similar style of mineralization another 1 km west along this trend, possibly extending the mineralization for a total length of 3.5 km. The area where this sub-crop sample was taken was re-examined without finding the source of the anomalous assay, although similar veining is located nearby. The Porphyry Hill Area, which returned a grab assay value of 4.41 g/t gold in 2010 and four anomalous assays earlier in the summer, was followed up by further prospecting and sampling. This sampling returned three additional anomalous values from sheared and altered porphyry. The trend appears to be 1.5 km long. In the process of preparing ground for a new hydro line for Imerys, north of the Talc Mine Area, outcrops of sediment and porphyry with quartz veining were uncovered. Grab samples were taken at a few locations with some anomalous values returned. The area will be washed and channel sampled within the next few weeks. See Appendix 4 for an example of the veining at the new hydro line area. Geochemistry: Dr. Tim Barrett has completed a site visit and preliminary analysis of the data from the holes around PG and has recommended that a few more samples to be analyzed for geochemical signatures to determine rock types. He has also recommended petrography of the core from drill hole PG to determine if the sulphides present are depositional or replacement in nature. The results of his findings will be used to determine the next steps in exploring this zone as a potential VMS target. Planned Work Programs for Remainder of 2013: Data compilation and interpretation of the work from previous work and this field program will be used to generate new maps and prospective targets for further exploration along the known trends as well as new areas. Weather permitting, the hydro line area will be washed and channel sampled, and a number of other targeted areas will be chosen for overburden stripping and channel sampling. An airborne magnetic and EM survey is being considered for late fall/early winter to cover the Pen Gold North area to bring geophysical coverage up to the same standard as Pen Gold South. This data will be used to interpolate geology where other geological/geochemical methods cannot be used due to lack of rock exposure. About Rapier Gold Inc. Rapier was listed on the TSX.V on March 8, 2013 and currently has 23,917,838 shares issued. Rapier s activities are solely focused on exploring the Pen Gold Project which comprises 16,448 hectares (approximately 160 sq km), 75 km southwest of Timmins, Ontario, in close proximity to the western extension of the Porcupine-Destor Deformation (Fault) Zone, one of the most productive gold structures in the world. AuRico Gold Inc. owns 19.9% of Rapier Gold. Quality Assurance Quality Control ( QA/QC ) Industry best practices are followed on the project including the routine insertion of blank and standard samples in all grab samples. The samples are submitted directly to Actlabs in Timmins for preparation and analysis. Gold analyses are conducted on 1 assay-ton aliquots, using fire assay methods with an atomic absorption finish for samples grading up to 5 g/t Au and with a gravimetric finish for samples above that level. Gary Wong, P.Eng., Vice-President Exploration of the Company, and a Qualified Person under the definition in National Instrument , has reviewed and approved the technical content of this release. ON BEHALF OF THE BOARD OF DIRECTORS Roger Walsh, President & CEO Contact: Roger Walsh Phone: info@rapiergold.com Website:

3 Neither the TSX Venture Exchange nor its Regulation Services Provider (as that term is defined in the policies of the TSX Venture Exchange) accepts responsibility for the adequacy or accuracy of this news release. Cautionary Note Regarding Forward Looking Statements: Certain disclosure in this release constitutes forward-looking statements. In making the forward-looking statements in this release, the Company has applied certain factors and assumptions that are based on the Company's current beliefs as well as assumptions made by and information currently available to the Company, including that the Company is able to obtain any government or other regulatory approvals required to complete the Company's planned exploration activities, that the Company is able to procure personnel, equipment and supplies required for its exploration activities in sufficient quantities and on a timely basis and that actual results of exploration activities are consistent with management's expectations. Although the Company considers these assumptions to be reasonable based on information currently available to it, they may prove to be incorrect, and the forward-looking statements in this release are subject to numerous risks, uncertainties and other factors that may cause future results to differ materially from those expressed or implied in such forward-looking statements. Such risk factors include, among others, that actual results of the Company's exploration activities will be different than those expected by management and that the Company will be unable to obtain or will experience delays in obtaining any required government approvals or be unable to procure required equipment and supplies in sufficient quantities and on a timely basis. Readers are cautioned not to place undue reliance on forward-looking statements. The Company does not intend, and expressly disclaims any intention or obligation to, update or revise any forward-looking statements whether as a result of new information, future events or otherwise, except as required by law.

4 Appendix 1 Maps of 2013 sample locations and 2013 and 2010 geochemical anomalies

5 Appendix 1 (Continued)

6 Appendix 2 Sampling results (see Appendix 1 for map of anomalies): 2013 Grab Sampling Sample Easting Northing Au (g/t) Au (ppb) Description Occurrence Area altered mafic volcanic; 70% quartz-ankerite veining; % py sheared mafic volcanic; 30% carbonate stringers; 64 minor py mafic volcanic; strong ankerite alteration; 70% 540 quartz veining > intermediate volcanic; trace py mafic volcanic; moderate carbonate alteration; 4% 74 quartz veining; 1% py sheared quartz feldspar porphyry; weak ankerite 289 alteration ; 5% quartz veining; trace py Porphyry Hill fractured feldspar porphyry near diabase dike; 10% 132 quartz veining Porphyry Hill chlorite-silica schist; sheared and altered sediment; 125 1% py massive feldspar porphyry with minor quartz 253 fracture filling; 7% quartz Porphyry Hill contact between feldspar porphyry and mafic dike; 60 8% quartz sweats; local chlorite (1) 5% py sub-outcrop-rubble; rusty quartz-ankerite vein with sheared mafic volcanic; sericite-ankerite-chlorite schist; light grey and white mottled quartz stringers diorite; 60-70% quartz-chlorite veining cm white quartz vein altered diorite; 5-10% white to grey quartz stringers 359 and flooding; 10-20% asp and po altered diorite; 60-70% mottled grey quartz veining 81 and flooding; 5-10% asp and po altered diorite; strong quartz flooding; 5-10% asp 290 and po altered diorite; abundant quartz; 3-5% asp and po altered diorite; 50-60% suggary grey quartz veining; 946 abundant chlorite; 10-20% asp, py and po altered diorite; 50-60% grey to white quartz veining; % asp and po quartz gabbro; 3-5% po cm white quartz vein; rusty margins; 0.5-1% py cm rusty zone in quartz diorite; 3-5% po cm smokey grey quartz vein with 3-5% asp in quartz 357 diorite along margins of vein mineralized boulder; 5cm smokey grey quartz vein with >5% asp in quartz diorite along margins of vein altered diorite; 5-10% asp and po sheet of rusty grey quartz veining in diorite; 1% py and asp; 95% quartz

7 Appendix 2 (Continued) Sample Easting Northing Au g/t Au (ppb) Description Occurrence Area sheared diorite; 30-40% rusty quartz veining; 1-3% asp cm zone of strongly sheared diorite; 5-10% quartzankerite veining; 1% asp strongly altered diorite; 30-40% quartz veining and 365 flooding; 5% asp cm wide mottled grey quartz vein; 1% aspy; 95% 206 quartz resample of ; feldspar porphyry; moderate 228 ankerite and sericite; 25% quartz fracture fill Porphyry Hill resample of ; feldspar porphyry; weak 53 ankerite and sericite; 5-10% quartz fracture fill Porphyry Hill resample of ; fractured and weakly altered 615 feldspar porphyry; 5% quartz stringers; trace py Porphyry Hill mafic volcanic; weak carbonate and chlorite 146 alteration; quartz veinlets; 2-3% py cm dark grey quartz stringer in altered mafic volcanic; cutting foliation for >1m; minor py in 1240 quartz Eastgate 5-30cm white quartz vein in altered mafic volcanic; % py Eastgate cm white quartz vein in altered mafic volcanic; % py; 20% quartz Eastgate 5-10cm grey fractured rusty and yellow quartz vein in fg sediments; similar to "contact" vein at mine; % quartz New hydro line grey to white sugary quartz veins in fg sediments; % quartz New hydro line cm greenish white quartz stringer in altered diorite; > % asp; Steetley Talc vein sugary white quartz vein in mafic volcanic; local 51 chlorite; minor py and po; 0.5% cpy; 75% quartz sheared mafic volcanic; 2% cpy and py Notes: 1.This grab sample occurred in sub-outcrop and will be further explored to identify outcrop.

8 Appendix 2 (Continued) 2010 (Rio Tinto) Grab Samples Sample Easting Northing Au g/t Au (ppb) Description Occurrence Area quartz veins with black tourmaline and trace fuchsite; in quartz feldspar > 3000 porphyry Porphyry Hill > 3000 quartz stringer zone in mafic volcanic; strong ankerite and sericite alteration; 2% py mafic volcanic; strong ankerite and sericite alteration; 3-5% py quartz-black tourmaline vein; bleached ankerite alteration halo in mafic volcanic; 5% py sericite-ankerite schist; quartz porphyry or altered sediment; 2% sulphides quartz-ankerite-tourmaline vein stockwork in mafic volcanic quartz-tourmaline stringers in mafic volcanic; strong ankerite alteration; 1-2% py felsic sill or volcanic; 2-3% py mafic volcanic; moderate ankerite and sericite alteration; quartz-ankerite stringer; 2% py in wallrock mafic volcanic; moderate to strong ankerite and sericite alteration; 20-30% quartz veining; 2-3% py quartz-tourmaline vein; trace py in wallrock mafic volcanic; strong ankerite and sericite alteration; quartz-ankerite stringers; 2-3% py mafic volcanic; weak to moderate ankerite and sericite; minor quartz stringers; 1% py mafic volcanic; strong ankerite alteration; 20-30% white quartzankerite vein stockwork; trace py mafic volcanic; strong ankerite alteration; 20-30% white quartzankerite vein stockwork; minor py quartz-ankerite vein in mafic volcanic; strong ankerite and sericite alteration rusty mafic volcanic or chloritic sediment; 2 cm quartz vein; trace py

9 Appendix 3 Area Prospecting on the stripped area found large areas of alteration, quartz veining, shearing, and sulphides (pyrite, arsnopyrite, and pyrrhotite). It also established that it was under-sampled, historically. The Steetley mapping of the stripped area indicates that some large veins have not been sampled. Others have been sampled only partially, mainly across the contact between host rock and quartz vein leaving large widths of the veins unsampled. While most of the channel samples appear to be adequately taken, a few examples were found of very shallow and uneven samples. Drill logs from the five holes drilled by Steetley also indicate under-sampling. Veins and sulphides noted in the logs were not always sampled. The highest assay returned from the Steetley drilling, 6,200 ppb from m in drillhole S-88-1, had no additional samples (bracket samples) taken around this assay. The mineralization remains open in all directions and to depth. The surrounding area is highly prospective, especially the contacts between the diorite, host to the Nib Yellowknife and possibly a part of the Reeves Ultramafic Complex, and other rock units including komatiitic volcanics (and possibly carb rock), porphyry, sediments, and possible mafic volcanics. Un-sampled veins at the stripped area

10 Appendix 3 (Continued) Poorly sampled channel at the stripped area Most of vein unsampled at the stripped area

11 Appendix 4 New Hydro Line Area Imerys has logged and stripped an area north of the Talc Mine Area to construct a new hydro line. During this process they uncovered outcrops of sediment and porphyry with quartz veining. Grab samples were taken at a few locations with some anomalous values returned. The area will be washed and channel sampled within the next few weeks. This is time sensitive work since the hydro line is being filled with waste rock. Grey quartz vein in sediments at New Hydro Line Area