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 23:09, 29 August 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

    addresses subject
    Cretaceous Period
    concept highlight
    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
    2 references
    knowledge source
    xDD Cyberinfrastructure
    reference URL
    https://geodeepdive.org/api/snippets?docid=620d1074ad0e9c819b058f26&term=Cretaceous%20Period,Cretaceous&dictid_filter=71&full_results&clean
    Paleogene Period
    concept highlight
    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
    2 references
    knowledge source
    xDD Cyberinfrastructure
    reference URL
    https://geodeepdive.org/api/snippets?docid=620d1074ad0e9c819b058f26&term=Paleogene%20Period,Paleogene&dictid_filter=71&full_results&clean
    Quaternary Period
    concept highlight
    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
    2 references
    knowledge source
    xDD Cyberinfrastructure
    reference URL
    https://geodeepdive.org/api/snippets?docid=620d1074ad0e9c819b058f26&term=Quaternary%20Period,Quaternary&dictid_filter=71&full_results&clean
    metadata URL
    https://w3id.org/usgs/z/4530692/JU4TXU37
    MIME type
    text/html
    application/json
    0 references
    Zotero Version Number
    77,043
    0 references
    Zotero Attachment Key
    PM39TPG8
    data size
    4,270,241
    0 references
     
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