DLP Resources Expands Copper and Molybdenum Zone on the 100 % Owned Esperanza Project With an Additional 53 Rock Samples Returning up to 3.46 % Cu, 130.5ppm Mo, 7930ppm Zn and 245ppm Co
DLP Resources Expands Copper and Molybdenum Zone on the 100 % Owned Esperanza Project With an Additional 53 Rock Samples Returning up to 3.46 % Cu, 130.5ppm Mo, 7930ppm Zn and 245ppm Co
Cranbrook, British Columbia--(Newsfile Corp. - April 25, 2024) - DLP Resources Inc. (TSXV: DLP) (OTCQB: DLPRF) ("DLP" or the "Company") announces receipt of the second phase of rock sampling results from the Esperanza porphyry copper-molybdenum project immediately south of the Chapi Mine in Southern Peru (Figure 1).
不列颠哥伦比亚省克兰布鲁克--(Newsfile Corp.-2024 年 4 月 25 日)- DLP Resources Inc.(多伦多证券交易所股票代码:DLP)(场外交易代码:DLPRF) (”DLP“或者”公司“)宣布收到了位于秘鲁南部查皮矿以南的埃斯佩兰萨斑岩铜钼项目的第二阶段岩石采样结果(图1)。
Results for the additional 53 rock samples taken in the initial reconnaissance sampling and mapping of the northwestern part of the project have returned highly anomalous copper, molybdenum, cobalt and zinc in mapped intrusive stocks and polymictic breccias within the overlying volcanics (Figures 2, 3, 4, 5 and 6).
在项目西北部的初步侦察采样和测绘中采集的另外53个岩石样本的结果显示,在上覆火山岩中测绘的侵入性储量和多晶角砾岩中发现了高度异常的铜、钼、钴和锌(图2、3、4、5和6)。
Highlights
亮点
- Fifteen of the fifty-three rock chip samples returned values between 0.3% Cu and 3.46% Cu (Table 1 and Figure 2). These samples were taken from outcropping quartz diorite and polymictic breccias with visible copper-oxides, iron oxides and tourmaline in fractures.
- Rock chip samples with high copper grades included:
- Sample 1208 - 0.69% Cu, 130.50ppm Mo, 7930ppm Zn and 42.30ppm Co.
- Sample 1226 - 1.84% Cu, 1.38ppm Mo, 1115ppm Zn and 42.50ppm Co.
- Sample 1227 - 1.71% Cu, 5.56ppm Mo, 2490ppm Zn and 176.50ppm Co.
- Sample 1229 - 3.46% Cu, 16.15ppm Mo, 1480ppm Zn and 185ppm Co.
- Sample 1231 - 1.26% Cu, 2.43ppm Mo, 1050ppm Zn and 39.60ppm Co.
- Sample 1232 - 0.70% Cu, 3.75ppm Mo, 487ppm Zn and 22.50ppm Co.
- Sample 1237 - 1.54% Cu, 6.34ppm Mo, 774ppm Zn and 57.20ppm Co.
- Sample 1240 - 0.82%Cu, 4.10ppm Mo, 410ppm Zn and 17.10ppm Co.
- 五十三个岩屑样品中有十五个返回的值介于 0.3% 铜和 3.46% 铜之间(表 1 和图 2)。这些样本取自露出的石英闪长岩和多晶角砾岩,裂缝中有可见的氧化铜、氧化铁和电气石。
- 铜等级高的岩屑样品包括:
- 样品 1208-0.69% 铜、130.50ppm Mo、7930ppm 锌和 42.30ppm Co.
- 样品 1226-1.84% 铜、1.38ppm Mo、1115ppm 锌和 42.50ppm Co.
- 样品 1227-1.71% 铜、5.56ppm Mo、2490ppm 锌和 176.50ppm Co.
- 样品 1229-3.46% 铜、16.15ppm Mo、1480ppm 锌和 185ppm Co.
- 样品 1231-1.26% 铜、2.43ppm Mo、1050ppm 锌和 39.60ppm Co.
- 样品 1232-0.70% 铜、3.75ppm Mo、487ppm 锌和 22.50ppm Co.
- 样品 1237-1.54% 铜、6.34ppm Mo、774ppm 锌和 57.20ppm Co.
- 样品 1240-0.82% 铜、4.10ppm Mo、410ppm 锌和 17.10ppm Co.
See Table 1 for the anomalous set of results for the second phase of rock chip samples and Table 2 for the first phase of anomalous results reported on March 13, 2024 (see DLP Resources Inc., news release of March 13, 2024).
有关第二阶段岩屑样本的一组异常结果,见表1;2024年3月13日报告的第一阶段异常结果见表2(参见DLP资源公司,2024年3月13日新闻稿)。
Mr. Gendall, President and CEO commented: "With two phases of rock sampling and mapping completed on the Esperanza project, an area of 3.5km x 1.5km has now been identified with anomalous copper and molybdenum in rock samples. These anomalous copper-molybdenum values coupled with other porphyry copper indicators are very encouraging for locating a mineralized system at depth in this porphyry copper belt immediately south of the Chapi copper mine."
总裁兼首席执行官根德尔先生评论说:“随着Esperanza项目的两个阶段的岩石采样和测绘工作已经完成,现在已经确定了3.5km x 1.5km的区域在岩石样本中含有异常的铜和钼。这些异常的铜钼值加上其他斑岩铜指标,对于在恰皮铜矿以南的斑岩铜带深处定位矿化系统非常令人鼓舞。”
Table 1. Summary of Select Rock Chip Results for the Esperanza Porphyry Cu-Mo Project - Phase 2.
表 1。 Esperanza Porphyry Cu-Mo 项目(第 2 阶段)的精选岩屑结果摘要。
SAMPLE | Northing | Easting | Elev. | Cu | Mo | Zn | Co | Description |
No | m | m | m | % | ppm | ppm | ppm | Rock Chip Samples 2x2m Sampling Area |
1201 | 8134576 | 243185 | 1711 | <0.01 | 15.3 | 33 | 0.7 | Qtz-Tourmaline breccia |
1202 | 8134575 | 243085 | 1721 | <0.01 | 22.5 | 67 | 0.8 | Intensely fractured diorite with FeOx boxworks |
1203 | 8134566 | 243075 | 1707 | <0.01 | 23.2 | 69 | 0.9 | Diorite with SS clasts and Fe-oxides + Tourmaline |
1204 | 8134585 | 243094 | 1710 | <0.01 | 41.2 | 98 | 5.1 | Sandstone with Fe-oxides + Quartz-sericite |
1205 | 8134584 | 243102 | 1721 | <0.01 | 20.5 | 63 | 9.9 | Diorite with argillic alteration + intense veining of Fe oxides |
1206 | 8134570 | 243107 | 1712 | 0.01 | 35.3 | 20 | 1.7 | Diorite + Veining with FeOx + Mn + Neo + Tm |
1207 | 8134507 | 243151 | 1714 | 0.02 | 37.8 | 107 | 58.5 | Diorite + Veining with FeOx + Tm |
1208 | 8134485 | 243190 | 1729 | 0.69 | 130.5 | 7930 | 42.3 | Diorite, Arg, with SS and Qtz vlts and FeOx boxworks +Tm |
1209 | 8134293 | 243141 | 1716 | 0.01 | 11.05 | 146 | 13.8 | Diorite, Arg with SS and Qtz vlts and FeOx boxworks +Tm |
1210 | 8134454 | 243330 | 1729 | 0.04 | 37.3 | 45 | 4.8 | Diorite, Arg altered, qtz-FeOx + Tm + fine alunite? in matrix. |
1211 | 8134676 | 242844 | 1728 | 0.02 | 34 | 138 | 10.9 | Diorite Sil, Qtz vlts, Mn-Tm, intense angular fractures. |
1214 | 8134817 | 242754 | 1729 | 0.01 | 17.35 | 23 | 9.3 | Diorite, Arg Alteration, Vlts of Qz, FeOx, Mn +Tm |
1215 | 8134846 | 242718 | 1728 | 0.01 | 20.2 | 33 | 33.7 | Polymictic Bx frag of SS with FeOx veins + Mn |
1217 | 8134918 | 242865 | 1718 | 0.01 | 7.48 | 22 | 11.7 | Diorite QSP with Qtz vlts and FeOx-Mn |
1218 | 8134971 | 242872 | 1711 | 0.01 | 7.37 | 23 | 11.6 | Diorite QS with FeOx, Mn veins + intense fractures. |
1226 | 8136321 | 244504 | 1886 | 1.84 | 1.38 | 1115 | 42.5 | Polymictic Bx, pseudostratified with presence of malachite |
1227 | 8136164 | 244682 | 1852 | 1.71 | 5.56 | 2490 | 176.5 | Polymictic Bx, pseudostratification + malachite and Mn |
1229 | 8136181 | 244817 | 1852 | 3.46 | 16.15 | 1480 | 185 | Polymictic Bx?, with malachite and Mn in matrix |
1230 | 8136224 | 244609 | 1887 | 0.46 | 5.73 | 373 | 11.8 | Polymictic Bx?, with malachite and Mn in matrix |
1231 | 8136198 | 244557 | 1589 | 1.26 | 2.43 | 1050 | 39.6 | Polymictic Bx?, with malachite and Mn in matrix |
1232 | 8136152 | 244500 | 1884 | 0.7 | 3.75 | 487 | 22.5 | Subhorizontal polymictic Bx with malachite and Mn in matrix |
1234 | 8136108 | 244494 | 1876 | 0.41 | 4.77 | 553 | 54 | Polymictic Bx with malachite and Mn in subhorizontal horizons |
1235 | 8136033 | 244518 | 1878 | 0.44 | 5.02 | 547 | 24.1 | Polymictic Bx with malachite and Mn in subhorizontal horizons |
1236 | 8136080 | 244564 | 1853 | 0.76 | 7.91 | 1270 | 245 | Polymictic Bx with malachite and Mn in subhorizontal horizons |
1237 | 8135958 | 244587 | 1856 | 1.54 | 6.34 | 774 | 57.2 | Polymictic Bx with malachite, atacamite and Mn |
1239 | 8135880 | 244513 | 1863 | 0.25 | 4.36 | 379 | 20.6 | Polymictic Bx with malachite in a subhorizontal horizon |
1240 | 8135792 | 244510 | 1861 | 0.82 | 4.1 | 410 | 17.1 | Polymictic Bx with malachite in a subhorizontal horizon |
1241 | 8135679 | 244568 | 1852 | 0.38 | 6.14 | 506 | 26.5 | Polymictic Bx with malachite in a subhorizontal horizon |
1242 | 8135353 | 244010 | 1789 | 0.12 | 3.2 | 2100 | 146 | Polymictic Bx with malachite in a subhorizontal horizon |
1244 | 8135443 | 244065 | 1792 | 0.32 | 4.38 | 1500 | 115 | Polymictic Bx with malachite in a subhorizontal horizon |
1245 | 8134403 | 242718 | 1674 | 0.01 | 14 | 31 | 8.9 | Diorite, Arg., with Mn in irregular veins |
1246 | 8134540 | 242985 | 1691 | 0.01 | 51 | 241 | 34.4 | Diorite, Arg., with Mn in irregular veins |
1247 | 8134364 | 242830 | 1667 | <0.01 | 23 | 55 | 3.5 | Diorite, Qtz, Tm, FeOx in boxworks + intense fracturing + veins |
1249 | 8134200 | 242674 | 1645 | <0.01 | 5.79 | 49 | 6.3 | Quartzite/SS with FeOx in veinlets/fractures and presence of Tm |
1250 | 8134158 | 242640 | 1637 | <0.01 | 17.05 | 11 | 1.6 | Quartzite/SS with FeOx in veinlets/fractures and presence of Ser |
1751 | 8134093 | 242562 | 1628 | <0.01 | 26.9 | 48 | 19.7 | Bx of quartzite/SS with FeOx boxworks + FeOx in fractures |
1752 | 8134627 | 242082 | 1626 | <0.01 | 12.2 | 84 | 18.1 | Diorite, Arg, FeOx + quartzite/SS with FeOx boxworks |
1754 | 8134434 | 242254 | 1645 | 0.02 | 59.5 | 89 | 1.7 | Vein?, QSP, malachite and OxFe in fractures and boxworks |
1755 | 8134249 | 242291 | 1634 | <0.01 | 12.3 | 7 | 1.1 | Bx, QSP +FeOx boxworks +quartz |
1756 | 8134244 | 242276 | 1643 | <0.01 | 4.87 | 27 | 3.6 | Bx, QSP, presence of FeOx boxworks + quartz |
1757 | 8134220 | 242248 | 1651 | <0.01 | 10.25 | 139 | 29.4 | Bx, subangular fragments, Qtz-Tm? |
1759 | 8134070 | 242351 | 1607 | <0.01 | 10.05 | 29 | 2.8 | Diorite, QSP, FeMo in fractures, FeOx +intense fracturing |
1760 | 8134168 | 242265 | 1644 | <0.01 | 13.8 | 121 | 18.7 | Bx, quartz veins with FeOx, Mn and Tm in fractures |
Notes: Bx-Breccia, Qtz-Quartz, Tm-Tourmaline, Vlts-veinlets, FeOx-Iron Oxides, FeMo-ferrimolybdenite, Mt-magnetite, SS-sandstone, Py-Pyrite, Ep-Epidote, Chl-Chlorite, Arg-Argillic, QSP-Quartz-sericite-pyrite, Ser-Sericite, Sil-Silicified, Lim-Limonite, Neo-Neotocite, Mn-Manganese, Qtz-Quartz, V-Very, Frac-Fractured |
样本 | 北方 | 向东 | Elev。 | 铜 | Mo | 锌 | 有限公司 | 描述 |
没有 | m | m | m | % | ppm | ppm | ppm | Rock Chip 样品 2x2M 采样区域 |
1201 | 8134576 | 243185 | 1711 | 15.3 | 33 | 0.7 | Qtz-Tourmaline 角砾岩 | |
1202 | 8134575 | 243085 | 1721 | 22.5 | 67 | 0.8 | 使用 FeOx boxworks 严重断裂的闪长岩 | |
1203 | 8134566 | 243075 | 1707 | 23.2 | 69 | 0.9 | 含有 SS 碎片和氧化铁的闪长岩 + 电气石 | |
1204 | 8134585 | 243094 | 1710 | 41.2 | 98 | 5.1 | 含铁氧化物的砂岩 + 石英-蚕丝岩 | |
1205 | 8134584 | 243102 | 1721 | 20.5 | 63 | 9.9 | 具有泥质蚀变的闪长岩 + 铁氧化物的强烈脉纹 | |
1206 | 8134570 | 243107 | 1712 | 0.01 | 35.3 | 20 | 1.7 | 闪长岩 + 使用 FeOx + Mn + Neo + Tm 进行脉纹处理 |
1207 | 8134507 | 243151 | 1714 | 0.02 | 37.8 | 107 | 58.5 | 使用 FeOx + Tm 进行闪长岩 + 脉纹处理 |
1208 | 8134485 | 243190 | 1729 | 0.69 | 130.5 | 7930 | 42.3 | 闪长岩、Arg、带有 SS 和 Qtz volts 以及 FeOx boxworks +Tm |
1209 | 8134293 | 243141 | 1716 | 0.01 | 11.05 | 146 | 13.8 | 闪长岩、带有 SS 和 Qtz volts 的 Arg 以及 FeOx boxworks +Tm |
1210 | 8134454 | 243330 | 1729 | 0.04 | 37.3 | 45 | 4.8 | 闪长岩、Arg 改性、Qtz-Feox + Tm + 精细校友呢?在矩阵中。 |
1211 | 8134676 | 242844 | 1728 | 0.02 | 34 | 138 | 10.9 | 闪长岩 Sil、Qtz vlts、Mn-Tm、强烈的角裂缝。 |
1214 | 8134817 | 242754 | 1729 | 0.01 | 17.35 | 23 | 9.3 | 闪长岩、Arg 变化、Qz Volts、FeOx、Mn +Tm |
1215 | 8134846 | 242718 | 1728 | 0.01 | 20.2 | 33 | 33.7 | 带有 FeOx 静脉的 SS 的 Polymictic Bx 片段 + Mn |
1217 | 8134918 | 242865 | 1718 | 0.01 | 7.48 | 22 | 11.7 | 带 Qtz volts 和 Feox-Mn 的闪长岩 QSP |
1218 | 8134971 | 242872 | 1711 | 0.01 | 7.37 | 23 | 11.6 | 含有 FeOx、Mn 静脉 + 剧烈骨折的闪长岩 QS。 |
1226 | 8136321 | 244504 | 1886 | 1.84 | 1.38 | 1115 | 42.5 | Polymictic Bx,假分层,存在孔雀石 |
1227 | 8136164 | 244682 | 1852 | 1.71 | 5.56 | 2490 | 176.5 | Polymictic Bx,伪分层 + 孔雀石和 Mn |
1229 | 8136181 | 244817 | 1852 | 3.46 | 16.15 | 1480 | 185 | Polymictic Bx?,以孔雀石和锰为基体 |
1230 | 8136224 | 244609 | 1887 | 0.46 | 5.73 | 373 | 11.8 | Polymictic Bx?,以孔雀石和锰为基体 |
1231 | 8136198 | 244557 | 1589 | 1.26 | 2.43 | 1050 | 39.6 | Polymictic Bx?,以孔雀石和锰为基体 |
1232 | 8136152 | 244500 | 1884 | 0.7 | 3.75 | 487 | 22.5 | 基质中含有孔雀石和锰的亚水平多聚体 Bx |
1234 | 8136108 | 244494 | 1876 | 0.41 | 4.77 | 553 | 54 | Polymictic Bx 含孔雀石和 Mn 位于次水平视野中 |
1235 | 8136033 | 244518 | 1878 | 0.44 | 5.02 | 547 | 24.1 | Polymictic Bx 含孔雀石和 Mn 位于次水平视野中 |
1236 | 8136080 | 244564 | 1853 | 0.76 | 7.91 | 1270 | 245 | Polymictic Bx 含孔雀石和 Mn 位于次水平视野中 |
1237 | 8135958 | 244587 | 1856 | 1.54 | 6.34 | 774 | 57.2 | 含有孔雀石、阿塔卡米特和锰的 Polymictic Bx |
1239 | 8135880 | 244513 | 1863 | 0.25 | 4.36 | 379 | 20.6 | Polymictic Bx,孔雀石位于水平以下的地平线上 |
1240 | 8135792 | 244510 | 1861 | 0.82 | 4.1 | 410 | 17.1 | Polymictic Bx,孔雀石位于水平以下的地平线上 |
1241 | 8135679 | 244568 | 1852 | 0.38 | 6.14 | 506 | 26.5 | Polymictic Bx,孔雀石位于水平以下的地平线上 |
1242 | 8135353 | 244010 | 1789 | 0.12 | 3.2 | 2100 | 146 | Polymictic Bx,孔雀石位于水平以下的地平线上 |
1244 | 8135443 | 244065 | 1792 | 0.32 | 4.38 | 1500 | 115 | Polymictic Bx,孔雀石位于水平以下的地平线上 |
1245 | 8134403 | 242718 | 1674 | 0.01 | 14 | 31 | 8.9 | 闪长岩,Arg.,不规则静脉中含锰 |
1246 | 8134540 | 242985 | 1691 | 0.01 | 51 | 241 | 34.4 | 闪长岩,Arg.,不规则静脉中含锰 |
1247 | 8134364 | 242830 | 1667 | 23 | 55 | 3.5 | 箱体中的闪长岩、Qtz、Tm、FeOx + 剧烈压裂 + 静脉 | |
1249 | 8134200 | 242674 | 1645 | 5.79 | 49 | 6.3 | 静脉/裂缝中含有 FeOx 的石英岩/SS 以及 Tm 的存在 | |
1250 | 8134158 | 242640 | 1637 | 17.05 | 11 | 1.6 | 静脉/裂缝中含有 FeOx 的石英岩/Ss 以及Ser的存在 | |
1751 | 8134093 | 242562 | 1628 | 26.9 | 48 | 19.7 | 装有 FeOx boxworks 的石英岩/SS + 裂缝中的 FeOx | |
1752 | 8134627 | 242082 | 1626 | 12.2 | 84 | 18.1 | 含有 FeOx boxworks 的闪长岩、Arg、FeOx + 石英岩/SS | |
1754 | 8134434 | 242254 | 1645 | 0.02 | 59.5 | 89 | 1.7 | 静脉?、裂缝和箱体工程中的 QSP、孔雀石和 OxFe |
1755 | 8134249 | 242291 | 1634 | 12.3 | 7 | 1.1 | Bx、QSP +FeoX boxworks +石英 | |
1756 | 8134244 | 242276 | 1643 | 4.87 | 27 | 3.6 | Bx、QSP、FeoX boxworks + 石英的存在 | |
1757 | 8134220 | 242248 | 1651 | 10.25 | 139 | 29.4 | Bx,亚角碎片,Qtz-Tm? | |
1759 | 8134070 | 242351 | 1607 | 10.05 | 29 | 2.8 | 裂缝中的闪长岩、QSP、FeMo、FeOx +强度压裂 | |
1760 | 8134168 | 242265 | 1644 | 13.8 | 121 | 18.7 | Bx,骨折中含有 FeOx、Mn 和 Tm 的石英静脉 | |
备注:Bx-Breccia、Qtz-Quartz、Tm-Tourmaline、VLTS-Veinlet、Feox-氧化铁、钼铁矿、MT-磁铁矿、SS-砂岩、Py-Pyrite、Ep-Epidote、Chl-Chrite、Argillic、Qsp-Quartz-sericite-Pyrite、Sil-Sericite、Sil-Pyrite、Epidote、Chl-Argillic、Qsp-Quartz-sericite-Pyrite、Sil-Sericite、Sil-Pyrite、硅化、Lim-Limonite、新新石英、锰锰、Qtz-Quartz、V-Very、裂缝断裂 |
Table 2. Summary of Select Rock Chip Results for the Esperanza Porphyry Cu-Mo Project - Phase 1.
表 2。Esperanza Porphyry Cu-Mo 项目(第 1 阶段)的精选岩屑结果摘要。
SAMPLE | Northing | Easting | Elev. | Cu | Mo | Zn | Co | Description |
No | m | m | m | % | ppm | ppm | ppm | Rock Chip Samples 2x2m Sampling Area |
1153 | 8136819 | 244380 | 1953 | 0.44 | 0.77 | 2010 | 79.9 | Quartz Diorite, FeOx + Malachite + Mn + Tm? |
1159 | 8136708 | 244451 | 1940 | 0.01 | 6.31 | 59 | 7.6 | Quartz Diorite, Qtz Veinlets + FeOx + Calcite |
1160 | 8136536 | 244530 | 1929 | 0.01 | 6.84 | 71 | 4.2 | Aplite Dyke, FeOx + Neotocite |
1161 | 8136324 | 244719 | 1959 | 3.88 | 1.47 | 3540 | 281 | Polymictic Bx, Qtz + Tm + Ox Cu + Mn |
1162 | 8136329 | 244714 | 1959 | 2.84 | 1.75 | 2510 | 237 | Polymictic Bx, Qtz + Tm + Ox Cu + Mn |
1163 | 8136311 | 244723 | 1955 | 3.34 | 1.39 | 1905 | 238 | Polymictic Bx, Qtz + Tm + Ox Cu + Mn |
1164 | 8136313 | 244674 | 1853 | 3.85 | 1.46 | 1885 | 323 | Polymictic Bx, Qtz + Tm + Ox Cu + Mn |
1165 | 8136818 | 244384 | 1954 | 3.17 | 1.26 | 1600 | 210 | Quartz Diorite, FeOx, CuOx, Malachite + Mn + Tm? |
1166 | 8136818 | 244384 | 1954 | 0.22 | 0.54 | 1490 | 68.3 | Quartz Diorite, FeOx, CuOx, Malachite + Mn + Tm? |
1167 | 8136818 | 244384 | 1953 | 1.10 | 1.49 | 2030 | 155.0 | Quartz Diorite, FeOx, CuOx, Malachite + Mn + Tm? |
1168 | 8136818 | 244384 | 1953 | 0.07 | 0.34 | 361 | 23.20 | Quartz Diorite, FeOx, CuOx, Malachite + Mn + Tm? |
1169 | 8136818 | 244384 | 1953 | 0.42 | 0.89 | 3270 | 136.5 | Quartz Diorite, FeOx, CuOx, Malachite + Mn + Tm? |
1171 | 8136739 | 244409 | 1930 | 4.67 | 1.76 | 3060 | 209 | Quartz Diorite, Arg Alteration, Qtz Vlts, FeOx, + Vlts Calc |
1172 | 8136324 | 244719 | 1932 | 4.71 | 1.63 | 2030 | 383 | Polymictic Bx, Qtz + Tm + Ox Cu + Mn |
1173 | 8136329 | 244714 | 1853 | 1.15 | 1.32 | 2730 | 286 | Polymictic Bx, Qtz + Tm + Ox Cu + Mn |
1174 | 8136311 | 244723 | 1853 | 1.45 | 1.28 | 1155 | 26.4 | Polymictic Bx, Qtz + Tm + Ox Cu + Mn |
1188 | 8134456 | 241824 | 1917 | 0.01 | 14.8 | 65 | 30.9 | Breccia, FeOx, Lim boxworks |
1189 | 8134615 | 241913 | 1922 | 0.01 | 28.8 | 24 | 4.70 | Polymictic Bx, FeOx in fractures |
1191 | 8135447 | 242573 | 1930 | 0.02 | 10.2 | 82 | 17.20 | Quartz vein, Strong Fracturing with FeOx + Mn |
1192 | 8134631 | 243258 | 1926 | 0.02 | 6.54 | 98 | 5.80 | Andesite fragment, FeOX, Intense Fracturing |
1193 | 8134646 | 243282 | 1929 | 0.01 | 2.46 | 27 | 2.20 | Quartz Diorite, QS Alteration, Very Fractured |
1194 | 8134745 | 243125 | 1929 | 0.01 | 2.95 | 48 | 2.60 | Quartz Diorite, FeOx, Turgite, |
1195 | 8134797 | 243341 | 1925 | <0.01 | 3.08 | 77 | 0.80 | Quartz Diorite, FeOx, Turgite, Intense Fractures |
1196 | 8134471 | 243472 | 1924 | <0.01 | 14.8 | 42 | 4.00 | Quartz Diorite, Quartz Vlts, FeOx boxworks, Intense Frac. |
1197 | 8134164 | 243266 | 1917 | <0.01 | 3.76 | 95 | 3.60 | Diorite with Qtz Vlts, Leached - FeOx + Qtz Tm vlts |
Notes: Bx-Breccia, Qtz-Quartz, Tm-Tourmaline, Vlts-veinlets, FeOx-Iron Oxides, Mt-magnetite, Py-Pyrite, Ep-Epidote, Chl-Chlorite, Lim-Limonite, Neo-Neotocite, Mn-Manganese, Calc-Calcite, V-Very, Frac-Fractured |
样本 | 北方 | 向东 | Elev。 | 铜 | Mo | 锌 | 有限公司 | 描述 |
没有 | m | m | m | % | ppm | ppm | ppm | Rock Chip 样品 2x2M 采样区域 |
1153 | 8136819 | 244380 | 1953 | 0.44 | 0.77 | 2010 | 79.9 | 石英闪长岩、FeOx + 孔雀石 + Mn + Tm? |
1159 | 8136708 | 244451 | 1940 | 0.01 | 6.31 | 59 | 7.6 | 石英闪长岩、Qtz Veinlets + FeoX + 方解石 |
1160 | 8136536 | 244530 | 1929 | 0.01 | 6.84 | 71 | 4.2 | Aplite Dyke、FeOx + Neotocite |
1161 | 8136324 | 244719 | 1959 | 3.88 | 1.47 | 3540 | 281 | Polymictic Bx,Qtz + Tm + Ox Cu + Mn |
1162 | 8136329 | 244714 | 1959 | 2.84 | 1.75 | 2510 | 237 | Polymictic Bx,Qtz + Tm + Ox Cu + Mn |
1163 | 8136311 | 244723 | 1955 | 3.34 | 1.39 | 1905 | 238 | Polymictic Bx,Qtz + Tm + Ox Cu + Mn |
1164 | 8136313 | 244674 | 1853 | 3.85 | 1.46 | 1885 | 323 | Polymictic Bx,Qtz + Tm + Ox Cu + Mn |
1165 | 8136818 | 244384 | 1954 | 3.17 | 1.26 | 1600 | 210 | 石英闪长岩、FeOx、CuOx、孔雀石 + Mn + Tm? |
1166 | 8136818 | 244384 | 1954 | 0.22 | 0.54 | 1490 | 68.3 | 石英闪长岩、FeOx、CuOx、孔雀石 + Mn + Tm? |
1167 | 8136818 | 244384 | 1953 | 1.10 | 1.49 | 2030 | 155.0 | 石英闪长岩、FeOx、CuOx、孔雀石 + Mn + Tm? |
1168 | 8136818 | 244384 | 1953 | 0.07 | 0.34 | 361 | 23.20 | 石英闪长岩、FeOx、CuOx、孔雀石 + Mn + Tm? |
1169 | 8136818 | 244384 | 1953 | 0.42 | 0.89 | 3270 | 136.5 | 石英闪长岩、FeOx、CuOx、孔雀石 + Mn + Tm? |
1171 | 8136739 | 244409 | 1930 | 4.67 | 1.76 | 3060 | 209 | 石英闪长岩、Arg Alts、Qtz Volts、FeOx、+ Vlts Calc |
1172 | 8136324 | 244719 | 1932 | 4.71 | 1.63 | 2030 | 383 | Polymictic Bx,Qtz + Tm + Ox Cu + Mn |
1173 | 8136329 | 244714 | 1853 | 1.15 | 1.32 | 2730 | 286 | Polymictic Bx,Qtz + Tm + Ox Cu + Mn |
1174 | 8136311 | 244723 | 1853 | 1.45 | 1.28 | 1155 | 26.4 | Polymictic Bx,Qtz + Tm + Ox Cu + Mn |
1188 | 8134456 | 241824 | 1917 | 0.01 | 14.8 | 65 | 30.9 | 角砾岩、FeOx、Lim boxworks |
1189 | 8134615 | 241913 | 1922 | 0.01 | 28.8 | 24 | 4.70 | 骨折中的 Polymictic Bx、FeOx |
1191 | 8135447 | 242573 | 1930 | 0.02 | 10.2 | 82 | 17.20 | 石英脉,使用 FeOx + Mn 进行强力压裂 |
1192 | 8134631 | 243258 | 1926 | 0.02 | 6.54 | 98 | 5.80 | 安山岩碎片、FeOx、强度压裂 |
1193 | 8134646 | 243282 | 1929 | 0.01 | 2.46 | 27 | 2.20 | 石英闪长岩,QS 蚀变,极度断裂 |
1194 | 8134745 | 243125 | 1929 | 0.01 | 2.95 | 48 | 2.60 | 石英闪长岩、FeOx、Turgite |
1195 | 8134797 | 243341 | 1925 | 3.08 | 77 | 0.80 | 石英闪长岩、FeOx、Turgite、强烈断裂 | |
1196 | 8134471 | 243472 | 1924 | 14.8 | 42 | 4.00 | 石英闪长岩、石英熔体、FeOx boxworks、Intense Frac。 | |
1197 | 8134164 | 243266 | 1917 | 3.76 | 95 | 3.60 | 带 Qtz Vlts 的闪长岩,浸出-FeOx + Qtz Tm vlts | |
备注:Bx-Breccia、Qtz-Quartz、Tm-Tourmaline、VLTS-Veinlet、Feox-氧化铁、MT-磁铁矿、Py-Pyrite、Ep-Epidote、Chl-Chrite、Lim-Limonite、新新月石、锰锰、方解石、V-Very、断裂断裂 |
Quality Control and Quality Assurance
质量控制和质量保证
DLP Resources Peru S.A.C, a subsidiary of DLP Resources Inc., supervises sampling and carries out surface sampling and mapping of outcrop at the Esperanza project. Rock chip sampling was done within a maximum area of 2m x 2m and descriptions were carried out by a geologist. Samples are bagged and sealed on site before transportation to the ALS Peru S.A.C. sample preparation facility in Arequipa by Company vehicles and staff. Rocks are crushed with 70% passing <2mm. Sample is split with riffle splitter and 250g pulverized to 85% less than 75um. Prepared samples are sent to Lima by ALS Peru S.A.C. for analysis. ALS Peru S.A.C. is an independent laboratory. Samples are analyzed for 48 elements using a four-acid digestion and ICP-MS analysis (ME-MS61). Overlimit samples for copper and silver were re-analysed by four-acid digestion and ICP-AES (ME-OG62). In addition, sequential copper analyses are done and reports, soluble copper using sulphuric acid leach, soluble copper in cyanide leach, residual copper and total copper. ALS meets all requirements of International Standards ISO/IEC 17025:2005 and ISO 9001:2015 for analytical procedures.
DLP Resources Peru S.A.C是DLP资源公司的子公司,负责监督埃斯佩兰萨项目的采样并对露头进行地表采样和测绘。岩屑采样是在2m x 2m的最大区域内进行的,并由地质学家进行了描述。样品在现场装袋并密封,然后由公司车辆和工作人员运送到位于阿雷基帕的ALS Peru S.A.C. 样本制备设施。岩石以 70% 的速度被压碎
DLP Resources independently monitors quality control and quality assurance ("QA/QC") through a program that includes the insertion of certified reference materials.
DLP Resources 通过包括插入认证参考材料在内的计划独立监控质量控制和质量保证(“QA/QC”)。
Esperanza Project
埃斯佩兰萨项目
The Esperanza Cu-Mo Project is an early-stage exploration project in Southern Peru consisting of 4,600 Ha of claims which are 100% owned by DLP. Esperanza is located ~35 km SW of the Cerro Verde Mine in Arequipa and immediately south of the Chapi Copper Mine.
埃斯佩兰萨铜钼项目是秘鲁南部的一个早期勘探项目,由4,600公顷的土地组成,100%归DLP所有。埃斯佩兰萨位于阿雷基帕塞罗佛得矿西南约35公里处,紧邻查皮铜矿以南。
Copper-molybdenum mineralization was initially observed in an early reconnaissance program undertaken in 2022. Subsequently we have completed a satellite alteration mapping program over the project and identified alteration consistent with porphyry copper-molybdenum systems. Follow-up of alteration and subsequent sampling and mapping commenced in early 2024.
铜钼矿化最初是在2022年进行的一项早期侦察计划中观察到的。随后,我们完成了该项目的卫星改动测绘计划,并确定了与斑岩铜钼系统一致的变化。变更的后续行动以及随后的采样和测绘于2024年初开始。
Figure 1: Esperanza Project Location
图 1:Esperanza 项目位置
Figure 2: Esperanza Project -Anomalous copper, molybdenum, zinc and cobalt in rock samples.
图 2:Esperanza 项目-岩石样品中的异常铜、钼、锌和钴。
Figure 3: Esperanza Project - Simplified geology with anomalous copper in rock samples.
图 3:Esperanza 项目-简化的地质结构,岩石样品中含有异常铜。
Figure 4: Esperanza Project - Simplified geology with anomalous molybdenum in rock samples.
图 4:Esperanza 项目-岩石样品中含有异常钼的简化地质学。
Figure 5: Esperanza Project - Simplified geology with anomalous zinc in rock samples.
图 5:Esperanza 项目-简化的地质结构,岩石样品中含有异常锌。
Figure 6: Esperanza Project - Simplified geology with anomalous cobalt in rock samples.
图 6:Esperanza 项目-简化的地质结构,岩石样品中含有异常钴。
Qualified Person
合格人员
David L. Pighin, consulting geologist and co-founder of DLP Resources, is the qualified person of the Company as defined by National Instrument 43-101. Mr. Pighin has reviewed and approved the technical contents of this news release.
根据国家仪器43-101的定义,咨询地质学家兼DLP Resources联合创始人大卫·皮金是该公司的合格人员。皮金先生已经审查并批准了本新闻稿的技术内容。
About DLP Resources Inc.
关于 DLP Resources Inc.
DLP Resources Inc. is a mineral exploration company operating in Southeastern British Columbia and Peru, exploring for Base Metals and Cobalt. DLP is listed on the TSX-V, trading symbol DLP and on the OTCQB, trading symbol DLPRF. Please refer to our web site for additional information.
DLP Resources Inc. 是一家矿产勘探公司,在不列颠哥伦比亚省东南部和秘鲁开展业务,勘探基本金属和钴。DLP在TSX-V上市,交易代码为DLP,在OTCQB上市,交易代码为DLPRF。请参阅我们的网站以获取更多信息。
FOR FURTHER INFORMATION PLEASE CONTACT:
欲了解更多信息,请联系:
DLP RESOURCES INC.
Ian Gendall, CEO & President
Jim Stypula, Executive Chairman
Robin Sudo, Office & Land Manager/Corporate Secretary
Maxwell Reinhart, Investor Relations
Telephone: 250-426-7808
Email: iangendall@dlpresourcesinc.com
Email: jimstypula@dlpresourcesinc.com
Email: robinsudo@dlpresourcesinc.com
Email: maxreinhart@dlpresourcesinc.com
DLP 资源公司
伊恩·根德尔,首席执行官兼总裁
吉姆·斯蒂普拉,执行主席
Robin Sudo,办公室和土地经理/公司秘书
麦克斯韦尔·莱因哈特,投资者关系
电话:250-426-7808
电子邮件:iangendall@dlpresourcesinc.com
电子邮件:jimstypula@dlpresourcesinc.com
电子邮件:robinsudo@dlpresourcesinc.com
电子邮件: maxreinhart@dlpresourcesinc.com
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 release.
多伦多证券交易所风险投资交易所及其监管服务提供商(该术语在多伦多证券交易所风险投资交易所的政策中定义)均不对本新闻稿的充分性或准确性承担责任。
Cautionary Note Regarding Forward-Looking Information
关于前瞻性信息的警示说明
This release includes certain statements and information that may constitute forward-looking information within the meaning of applicable Canadian securities laws. Forward-looking statements relate to future events or future performance and reflect the expectations or beliefs of management of the Company regarding future events. Generally, forward-looking statements and information can be identified by the use of forward-looking terminology such as "intends" or "anticipates", or variations of such words and phrases or statements that certain actions, events or results "may", "could", "should", "would" or "occur". This information and these statements, referred to herein as "forward‐looking statements", are not historical facts, are made as of the date of this news release and include without limitation, statements regarding discussions of future plans, estimates and forecasts and statements as to management's expectations and intentions with respect to further sampling, mapping and advancement of the Esperanza Project in Peru.
本新闻稿包括某些陈述和信息,这些陈述和信息可能构成适用的加拿大证券法所指的前瞻性信息。前瞻性陈述与未来事件或未来业绩有关,反映了公司管理层对未来事件的期望或信念。通常,前瞻性陈述和信息可以通过使用诸如 “打算” 或 “预期” 之类的前瞻性术语来识别,或者某些行为、事件或结果 “可能”、“应该”、“将” 或 “发生” 的此类词语和短语的变体或陈述。这些信息和这些陈述(此处称为 “前瞻性陈述”)不是历史事实,是截至本新闻稿发布之日发布的,包括但不限于有关未来计划、估计和预测讨论的声明,以及关于管理层对秘鲁埃斯佩兰萨项目进一步抽样、测绘和推进的预期和意图的陈述。
These forward‐looking statements involve numerous risks and uncertainties and actual results might differ materially from results suggested in any forward-looking statements. These risks and uncertainties include, among other things rock chip results expected from the Esperanza Project in Peru.
这些前瞻性陈述涉及许多风险和不确定性,实际结果可能与任何前瞻性陈述中建议的结果存在重大差异。除其他外,这些风险和不确定性包括秘鲁Esperanza项目预期的岩石芯片结果。
Although management of the Company has attempted to identify important factors that could cause actual results to differ materially from those contained in forward-looking statements or forward-looking information, there may be other factors that cause results not to be as anticipated, estimated or intended. There can be no assurance that such statements will prove to be accurate, as actual results and future events could differ materially from those anticipated in such statements. Accordingly, readers should not place undue reliance on forward-looking statements and forward-looking information. Readers are cautioned that reliance on such information may not be appropriate for other purposes. The Company does not undertake to update any forward-looking statement, forward-looking information or financial out-look that are incorporated by reference herein, except in accordance with applicable securities laws. We seek safe harbor.
尽管公司管理层试图确定可能导致实际业绩与前瞻性陈述或前瞻性信息中包含的业绩存在重大差异的重要因素,但可能还有其他因素导致业绩与预期、估计或预期不符。无法保证此类陈述会被证明是准确的,因为实际结果和未来事件可能与此类陈述中的预期存在重大差异。因此,读者不应过分依赖前瞻性陈述和前瞻性信息。提醒读者,依赖此类信息可能不适合用于其他目的。除非根据适用的证券法,否则公司不承诺更新此处以引用方式纳入的任何前瞻性陈述、前瞻性信息或财务展望。我们寻求安全港。