NI 43-101 Technical Report for the Escandalosa Project in Caribbean, Santo Domingo dated November 2010 (Q30957): Difference between revisions

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Property / addresses subject
 
Property / addresses subject: Cretaceous Period / rank
 
Normal rank
Property / addresses subject: Cretaceous Period / qualifier
 
concept highlight: Central Cordillera of Hispaniola and is hosted by Cretaceous age Tireo Formation volcanic rocks and
Property / addresses subject: Cretaceous Period / qualifier
 
concept highlight: strike slip fault zones, and is part of the Early Cretaceous to Paleogene Greater Antilles island
Property / addresses subject: Cretaceous Period / qualifier
 
concept highlight: 2008). Primitive island arc volcanic rocks of the Early Cretaceous Los Ranchos and Maimón Formations in
Property / addresses subject: Cretaceous Period / qualifier
 
concept highlight: Perfit, 1994). Cessation of subduction in the mid Cretaceous was marked by accretion of the Loma del
Property / addresses subject: Cretaceous Period / qualifier
 
concept highlight: Central Cordilleras (Draper et al., 1996), and by Early Cretaceous greenstones and intrusions of the Duarte
Property / addresses subject: Cretaceous Period / qualifier
 
concept highlight: sedimentary rocks of the Tireo Formation of Late Cretaceous to Eocene age in the Central Cordillera
Property / addresses subject: Cretaceous Period / qualifier
 
concept highlight: American plate boundary. La Escandalosa is hosted by Cretaceous age Tireo Formation volcanic rocks and
Property / addresses subject: Cretaceous Period / qualifier
 
concept highlight: Valle, dated at 85 to 92 million years old (Ma) (Late Cretaceous) (Bernárdez & Soler, 2004; Joubert, 2004). GoldQuest
Property / addresses subject: Cretaceous Period / qualifier
 
concept highlight: mineralization at La Escandalosa are as follows: • Hosted by Cretaceous age Tireo Formation island arc sequence. •
Property / addresses subject: Cretaceous Period / qualifier
 
concept highlight: Hispaniola peridotite belt: orogenic expression of the mid-Cretaceous Caribbean arc polarity reversal? Geology,
Property / addresses subject: Cretaceous Period / qualifier
 
concept highlight: rifting and back-arc basin development in the Late Cretaceous: Geochemical, isotopic and geochronological
Property / addresses subject: Cretaceous Period / qualifier
 
concept highlight: 1994, Petrochemistry and tectonic significance of Cretaceous island-arc rocks, Cordillera Oriental,
Property / addresses subject: Cretaceous Period / qualifier
 
concept highlight: Dominguez, H.D., 1991, Lithology and stratigraphy of upper Cretaceous volcanic and volcaniclastic rocks of
Property / addresses subject: Cretaceous Period / reference
 
Property / addresses subject: Cretaceous Period / reference
 
Property / addresses subject
 
Property / addresses subject: Paleogene Period / rank
 
Normal rank
Property / addresses subject: Paleogene Period / qualifier
 
concept highlight: fault zones, and is part of the Early Cretaceous to Paleogene Greater Antilles island arc (Figure 8.1).
Property / addresses subject: Paleogene Period / qualifier
 
concept highlight: Rivieres or Peralta Formation of Upper Campanian to Paleogene age. The contact with the Tireo Formation
Property / addresses subject: Paleogene Period / reference
 
Property / addresses subject: Paleogene Period / reference
 
Property / addresses subject
 
Property / addresses subject: Quaternary Period / rank
 
Normal rank
Property / addresses subject: Quaternary Period / qualifier
 
concept highlight: Juan graben with a thick sequence of Oligocene to Quaternary molasse sediments deposited in a marine
Property / addresses subject: Quaternary Period / qualifier
 
concept highlight: deposited in a marine to lagoon environment, with Quaternary alkaline basalts related to graben extension. The
Property / addresses subject: Quaternary Period / qualifier
 
concept highlight: relatively little time for oxidation. Unconsolidated Quaternary overburden deposits mapped are active
Property / addresses subject: Quaternary Period / reference
 
Property / addresses subject: Quaternary Period / reference
 

Revision as of 20:52, 19 April 2023

an NI 43-101 Technical Report pulled from the GeoArchive collection
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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
    P97 (Deleted Property)
    4530692:JU4TXU37 Property P97 not found, cannot determine the data type to use.
    0 references