The Lost Cities Project, Ecuador
Geology & Exploration Potential
The Lost City Project is found in the SE part of the Republic of Ecuador, in the Province of Morona-Santiago. It consists of circa 208,000 hectares in 42 concessions occupying the central part of the Cordillera de Cutucu. The concessions extend approximately 95 km along the Cordillera.
Regional Geological Setting
The Cordillera de Cutucu is contiguous with the Cordillera del Condor to the south, together forming foothills on the Amazon-side of the Andes mountain chain. The cordilleras Cutucu and Condor are separated by the valley of the Santiago River, which is the only river which breaches the divide and flows to the east, into the Amazon River system. The two cordilleras are essentially one geological and geomorphic feature. They represent an uplifted “back-arc” rift basin of Jurassic age, into which numerous porphyry bodies and their volcanic counterparts have been emplaced. This rift basin extends from Peru right to the Colombian border and beyond. In the southern part of Ecuador, the original rift basin consists of three steps that have been uplifted to different extents:
- The northern block has undergone the least uplift and it contains the Pastaza oil field, north of the Cutucu;
- The reservoir rocks have been uplifted by faulting in the Cutucu to circa 2,000 metre elevations which suggests that the Cordillera has been faulted upwards as much as 7 kilometres;
- The Cordillera del Condor, which lies to the south of the Cutucu, has been uplifted the most of the three blocks.
This is a key observation when it comes to exploration for epithermal gold and porphyry copper deposits since erosion of uplifts would strip off the barren cover rocks, exposing the volcanic roots and underlying porphyries. In geology this is referred to as the “epizone” and is the shallowest depth where porphyries can intrude. Most of the volcanic cover in the Cordillera del Condor has been eroded, exposing numerous porphyry copper deposits and streams contain at least some alluvial gold which is presumably all that is left of extensive epithermal vein systems. The Fruta del Norte gold-silver epithermal deposit was preserved from erosion in a down-faulted block adjacent to originally deeper-level porphyries.
In the Cutucu, where there has been less erosion, epithermal gold vein systems should be better preserved; the best area to prospect would be the central spine of the cordillera where erosion should have removed most of the cover rocks, but not be so deep as to expose copper porphyries. The Santiago and Chapiza Formations, which host the down-dropped Fruta del Norte and other deposits in the Cordillera del Condor, are present throughout the Project Area.
Oil companies have reconnaissance mapped the Cutucu since the 1920’s, because its stratigraphy is the same as the Pastaza Basin to the north, and inferences can therefore be made about the geology of the buried basin, 4,000 metres below surface. The Cutucu itself contains some oil seeps and has been drilled in a few places, but the rocks are outside of the “oil window” because of uplift, and offer little to no potential for oil and gas. The mapping by the oil companies right up to the 1980’s however has been key for this project, because Aurelian geologists recognized the nature of the host volcanics to Fruta del Norte in 2006 through 2008. Aurania has used this knowledge for advantage and acquired all the similar and most likely areas of identical volcanic rock.
The Cordillera de Cutucu forms part of the Northern Andean Jurassic Metallogenic Belt (“NAJMB”) that extends from 3° north in Colombia to 5° south in Ecuador and northern Peru. The Belt contains clusters of porphyry copper, gold-copper skarn and epithermal gold deposits.
Modern exploration only started in the Ecuadorian segment of the NAJMB in the mid-1990s, focused on the Cordillera del Condor, and resulted in the delineation of 19 million ounces (“Moz”) of gold, 61Moz of silver and 9 million pounds (“Mlbs”) of copper in measured and indicated resources, with an additional 7Moz, 30Moz and 22Blbs, respectively, in inferred resources
Deposits in the Cordillera del Condor are hosted by Upper Triassic to Late Jurassic – Early Cretaceous rocks (Figure 2). The lower part of the Triassic Santiago Formation contains tholeiitic basalts that formed during a period of extensive continental rifting, while the upper sequence of volcanic rocks are subduction-related, calc-alkaline lavas that were linked to development of a Mesozoic volcanic arc – an early analogy to the present Andean mountain chain. The gold-copper skarns of the Nambija deposit and the Fruta del Norte gold-silver deposit formed within the Piuntza Member that constitutes the lower part of the Santiago Formation.
Exploration program Phase 1
A grassroots exploration program consisting of the following Phase 1 program is planned for 2017 and 2018:
- A Landsat imagery study designed to determine the tectonic framework of the Cordillera de Cutucu through the identification of the interplay between faults and folds, sedimentary facies changes and potential growth sequences, as well as the location of intrusive stocks (due Q1, 2017);
- An airborne magnetic and radiometric survey by helicopter in order to identify porphyry systems through the detection of the magnetic core and coincident potassic alteration (through radiometric data) that is typical of these deposits in the correlative Cordillera del Condor immediately to the south (due Q3, 2017);
- A regional stream sediment sampling campaign to cover the main river basins within the permit area. However, it is highly likely that the stream sediment sampling program will identify targets that will warrant follow-up exploration, including soil sampling, systematic rock sampling where possible, and drilling, while regional stream sediment sampling continues in other areas (due to start Q2, 2017 – continue to end of 2018).
Table 1. Summary of NI43-101 resources in the Cordillera del Condor.