NI 43-101 Technical Report for the Escandalosa Project in Caribbean, Santo Domingo dated November 2010 (Q30957): Difference between revisions
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Revision as of 19:37, 11 March 2024
an NI 43-101 Technical Report pulled from the GeoArchive collection
| Language | Label | Description | Also known as |
|---|---|---|---|
| English | NI 43-101 Technical Report for the Escandalosa Project in Caribbean, Santo Domingo dated November 2010 |
an NI 43-101 Technical Report pulled from the GeoArchive collection |
Statements
Central Cordillera of Hispaniola and is hosted by Cretaceous age Tireo Formation volcanic rocks and
strike slip fault zones, and is part of the Early Cretaceous to Paleogene Greater Antilles island
2008). Primitive island arc volcanic rocks of the Early Cretaceous Los Ranchos and Maimón Formations in
Perfit, 1994). Cessation of subduction in the mid Cretaceous was marked by accretion of the Loma del
Central Cordilleras (Draper et al., 1996), and by Early Cretaceous greenstones and intrusions of the Duarte
sedimentary rocks of the Tireo Formation of Late Cretaceous to Eocene age in the Central Cordillera
American plate boundary. La Escandalosa is hosted by Cretaceous age Tireo Formation volcanic rocks and
Valle, dated at 85 to 92 million years old (Ma) (Late Cretaceous) (Bernárdez & Soler, 2004; Joubert, 2004). GoldQuest
mineralization at La Escandalosa are as follows: • Hosted by Cretaceous age Tireo Formation island arc sequence. •
Hispaniola peridotite belt: orogenic expression of the mid-Cretaceous Caribbean arc polarity reversal? Geology,
rifting and back-arc basin development in the Late Cretaceous: Geochemical, isotopic and geochronological
1994, Petrochemistry and tectonic significance of Cretaceous island-arc rocks, Cordillera Oriental,
Dominguez, H.D., 1991, Lithology and stratigraphy of upper Cretaceous volcanic and volcaniclastic rocks of
fault zones, and is part of the Early Cretaceous to Paleogene Greater Antilles island arc (Figure 8.1).
Rivieres or Peralta Formation of Upper Campanian to Paleogene age. The contact with the Tireo Formation
Juan graben with a thick sequence of Oligocene to Quaternary molasse sediments deposited in a marine
deposited in a marine to lagoon environment, with Quaternary alkaline basalts related to graben extension. The
relatively little time for oxidation. Unconsolidated Quaternary overburden deposits mapped are active
77,043
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