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Marimaca Copper Corp T.MARI

Alternate Symbol(s):  MARIF

Marimaca Copper Corp. is a Canada-based exploration and development company focused on base metal projects in Chile. The Company’s principal asset is the Marimaca Copper Project, located in the Antofagasta Region of northern Chile. The Marimaca Copper Project is situated at a low altitude in Chile’s Coastal Copper Belt, 25 kilometers (km) east of the port of Mejillones and 45 km north of Antofagasta, Marimaca has access to water and power, road and rail networks supplying sulphuric acid and other consumables, as well as deepwater ports. The Marimaca Copper Project comprises a set of concessions (the 1-23 Claims), properties 100% owned and optioned by the Company, combined with the adjacent La Atomica and Atahualpa claims, over which Marimaca Copper has the right to explore and exploit resources. The Company also has an option agreement to acquire the Pampa Medina project (Pampa Medina), which consists of four mining concessions totaling 144 hectares.


TSX:MARI - Post by User

Post by fundinvestoron Dec 09, 2020 8:18am
147 Views
Post# 32065687

News: Marimaca Copper Identifies Large Surface Geochemical A

News: Marimaca Copper Identifies Large Surface Geochemical A

Marimaca Copper Identifies Large Surface Geochemical Anomaly at Mercedes Target

 


VANCOUVER, British Columbia, Dec. 09, 2020 (GLOBE NEWSWIRE) -- Marimaca Copper Corp. (“Marimaca Copper” or the “Company”) (TSX: MARI) is pleased to announce the results of a recently completed surface geochemical sampling and reconnaissance mapping program at the Mercedes Target, which is located 3km to the north of the Company’s flagship Marimaca Oxide Deposit (“MOD”).

Highlights

  • Geochemical sampling has identified a large copper anomaly with grades as high as 0.6% in surface sampling
    • Central geochemical high is approximately 300 metres by 300 metres and is coincident with historical mine workings with grades ranging from 0.2% up to 0.6% copper
    • A large plus 200ppm Cu anomaly extends over an area of approximately 600 metres by 500 metres, which compares favorably to the MOD
    • Approximately half of the Mercedes Target is concealed by post mineral gravels
      • The geochemical anomaly is potentially larger than the footprint indicates
    • Very little of the mineralized zone is exposed at surface and there is a superficial leached zone 
      • Indicates the current anomaly is strong relative to typical background copper levels in this area and compares favorably to the MOD
  • The geochemical anomaly has the same host rocks and controlling structures as observed at the MOD
    • Intensely fractured monzodiorite host rock
    • North-south striking, east dipping, parallel sheeted fractures hosting mineralization
    • North-west trending late or post mineral fractures that control the supergene oxidation at MOD
  • Naguayn Fault System, the key controlling fault at the MOD, crosses the Mercedes Target
  • 1:1000 geological mapping and reconnaissance and geochemical sampling has commenced at the Cindy Target, approximately 1.5km to the north of the Mercedes Target
  • Exploration work is underway to further refine targets for the upcoming drilling campaigns which are expected to commence in early Q1 2021.

Sergio RiveraVP Exploration of Marimaca Copper, commented:

We have identified a large surface copper anomaly coincident with the previously identified magnetic anomaly at Mercedes, which is very encouraging.We continue to note the many similarities with the MOD including the intensely fractured intrusive host rock, the presence of key copper oxides, the flat sheeted structural controls of mineralization as well as dyke swarms and faulting which cross the anomalous area.

We believe this anomaly compares favourably with the surface anomaly encountered at the MOD and, while the anomalous area is already large, a significant proportion of it is covered by gravels.Unlike the MOD, very little of the mineralization isexposed. To have grades as high as 0.6% Cu in surface geochemical sampling – which is well above the economic cut-off grade at the MOD – is a very encouraging indication of the potential mineralization. As a result, it presents an exciting target for a shallow scout drilling program early in the New Year.

“We are in the process of building our surface facilities and mobilizing our drilling contractors to start the next phase of exploration drilling which,based on our current timelines, we expect to commence in early 2021.”

Surface Geochemical Sampling and Reconnaissance Geology

The Mercedes Target is located approximately 3km to the north of the MOD and was identified as a large-scale magnetic anomaly, which has many characteristics in common with the MOD (refer to release 23 September 2020) including its structural orientation and size.

The magnetic anomaly is within close proximity to the important, regionally extensive, Naguayn Fault System, dips in a similar orientation to the magnetic anomaly at Marimaca and is also coincident with historical artisanal, open pit, oxide copper workings. 

The Company has completed a sampling program on a 50 metre by 50 metre grid in the area immediately coincident with the magnetic anomaly, extending to the west over the area believed to be prospective for oxide mineralization, as well as completing geological mapping and reconnaissance work over the same area. This defined a large copper anomaly extending approximately 600 metres by 500 metres with values above 200ppm copper.

Key features noted were similar host rocks (a strongly fractured monzodiorite) and structures to those observed at Marimaca. In particular, north-south striking, east dipping, parallel sheeted fracturing intruded by various dykes and crosscut by late stage faulting on a west north west orientation. The copper mineralization includes brochantite, chrysocolla and atacamite, which are the key oxide minerals at the MOD.

Figure 1Map Showing the Area of Interest and Geochemical Anomaly Relative to the Magnetic Anomaly - https://www.globenewswire.com/NewsRoom/AttachmentNg/9cb09514-ae90-48ba-a11e-f26c0d8addc8

The core of the geochemical anomaly is also coincident with an area which has several small scale historical artisanal workings. Grades in this area were as high as 0.6% Cu, with numerous samples of between 0.2% and 0.5% Cu. These workings have exposed mineralization and structural controls and allowed Marimaca Copper’s geological team to observe numerous similarities with the MOD. One key feature is the presence of easterly dipping, north-south oriented, sheeted fracture zones which were prevalent at the MOD. As at Marimaca, the sheeted fractures host and control the copper mineralization at Mercedes.

Figure 2 shows a small artisanal pit which has exposed oxide mineralization. Importantly, it very clearly shows a similar style of easterly dipping, sheeted, fracturing which controls the oxide mineralization at Mercedes, and which is so prevalent at the MOD.

Figure 2: Photo of Small-Scale Artisanal Workings, looking South, Exposing Mineralization and Structure - https://www.globenewswire.com/NewsRoom/AttachmentNg/6c185bef-a393-4cdb-b09b-0d9715152429

As part of the mobilization process for the upcoming drilling campaigns, the Company will build new roads and drill pads, which should expose the mineralization horizon and allow for more detailed mapping and sampling to be completed prior to drilling these exciting targets.

The area coincident with the large magnetic anomaly at Mercedes is overlain by an extensive cover of post mineralization gravels. These gravels tend to get thicker towards the west of the magnetic anomaly, which is the area believed to be most prospective for Marimaca Style oxide mineralization. Surface geological mapping has identified several areas where oxide mineralization has been exposed below gravel cover which provides additional evidence for the potential for oxide mineralization at Mercedes.

Figure 3Oxide Mineralization Exposure below Gravel Cover and Extensive Gravel Cover at the Mercedes Target - https://www.globenewswire.com/NewsRoom/AttachmentNg/2fb28a0a-e2ff-455d-b891-f3ad4b0008bc

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