NI 43-101 Technical Report for the Ptarmagin Project in North America dated March 2012 (Q28988): Difference between revisions

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Property / GDDID
 
Property / GDDID: 620cf223ad0e9c819b050d89 / rank
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Property / addresses subject
 
Property / addresses subject: Cambrian Period / rank
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Property / addresses subject: Cambrian Period / qualifier
concept highlight: of the Moyie-Dibble Creek Fault between the Early Cambrian and Late Devonian. Subsequent uplift of
 
Property / addresses subject: Cambrian Period / qualifier
concept highlight: site, mineralization is hosted in marble of the Lower Cambrian Badshot Formation. There are three ore
 
Property / addresses subject: Cambrian Period / reference
 
Property / addresses subject: Cambrian Period / reference
 
Property / addresses subject
 
Property / addresses subject: Devonian Period / rank
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Property / addresses subject: Devonian Period / qualifier
concept highlight: parautochthonous terrane comprised of Helikian to Middle Devonian age strata. The stratigraphy of the area
 
Property / addresses subject: Devonian Period / qualifier
concept highlight: Moyie-Dibble Creek Fault between the Early Cambrian and Late Devonian. Subsequent uplift of the area to the south
 
Property / addresses subject: Devonian Period / qualifier
concept highlight: igneous rocks in the area. Andesitic volcanic rocks are Devonian in age, and hosted in the Mount Forster
 
Property / addresses subject: Devonian Period / qualifier
concept highlight: (Laramide Orogeny), and Eocene trans-tension. Helikian to Devonian extension and passive margin development
 
Property / addresses subject: Devonian Period / reference
 
Property / addresses subject: Devonian Period / reference
 
Property / addresses subject
 
Property / addresses subject: Cretaceous Period / rank
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Property / addresses subject: Cretaceous Period / qualifier
concept highlight: Cordilleran Orogeny, from the Middle Jurassic to Late Cretaceous, these strata were thrust eastwards and
 
Property / addresses subject: Cretaceous Period / qualifier
concept highlight: with the Laramide Orogeny, spanning the Jurassic to Cretaceous, 160-60 Ma (Lydon, 2007). The East Kootenay
 
Property / addresses subject: Cretaceous Period / qualifier
concept highlight: this period is related to a Late Jurassic to Early Cretaceous event of sinistral transpression and
 
Property / addresses subject: Cretaceous Period / qualifier
concept highlight: Cretaceous event of sinistral transpression and Late Cretaceous to Palaeocene dextral transpression;
 
Property / addresses subject: Cretaceous Period / qualifier
concept highlight: events, granitic plutonism occurred during the Mid-Cretaceous, 115-90 Ma (Cook and Van der Velden,
 
Property / addresses subject: Cretaceous Period / qualifier
concept highlight: cratonic North America during the Late Jurassic to Early Cretaceous (Cook and Van der Velden, 1995; Paiement
 
Property / addresses subject: Cretaceous Period / qualifier
concept highlight: propagated eastward during a period of Jurassic to Cretaceous contraction. This contraction resulted
 
Property / addresses subject: Cretaceous Period / qualifier
concept highlight: the Proterozoic sedimentary pile. During the Late Cretaceous and Early Tertiary, deformation further
 
Property / addresses subject: Cretaceous Period / qualifier
concept highlight: ultramafic dykes. The Horsethief Creek Batholith is Middle Cretaceous in age; with intrusive ages that range
 
Property / addresses subject: Cretaceous Period / qualifier
concept highlight: This structure was subsequently plugged by the Late Cretaceous Horsethief Creek Batholith. The root
 
Property / addresses subject: Cretaceous Period / qualifier
concept highlight: compressional structures are transtensional late Cretaceous to Tertiary structures. Pope (1990) notes
 
Property / addresses subject: Cretaceous Period / qualifier
concept highlight: associated with felsic intrusions, correlated to the Cretaceous Bayonne Magmatic Suite, that intrude
 
Property / addresses subject: Cretaceous Period / qualifier
concept highlight: lead and zinc veins that are interpreted to be Late Cretaceous to Early Tertiary in age. Proterozoic
 
Property / addresses subject: Cretaceous Period / qualifier
concept highlight: Supergroup. In contrast, mineralization associated with Cretaceous to Tertiary veins are interpreted to
 
Property / addresses subject: Cretaceous Period / qualifier
concept highlight: the host rocks along the Kootenay Arc during the Cretaceous and are correlated to the Bayonne Magmatic
 
Property / addresses subject: Cretaceous Period / qualifier
concept highlight: from the Delphine Panel, subsequently plugged by the Cretaceous Horsethief Creek Batholith to the north
 
Property / addresses subject: Cretaceous Period / qualifier
concept highlight: share a similar tectonic history during the late Cretaceous to Tertiary when mineralization in these
 
Property / addresses subject: Cretaceous Period / qualifier
concept highlight: These faults are likely Tertiary in age as they cut Cretaceous age folds and thrust faults and appear
 
Property / addresses subject: Cretaceous Period / reference
 
Property / addresses subject: Cretaceous Period / reference
 
Property / addresses subject
 
Property / addresses subject: Jurassic Period / rank
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Property / addresses subject: Jurassic Period / qualifier
concept highlight: sequences. During the Cordilleran Orogeny, from the Middle Jurassic to Late Cretaceous, these strata were thrust
 
Property / addresses subject: Jurassic Period / qualifier
concept highlight: associated with the Laramide Orogeny, spanning the Jurassic to Cretaceous, 160-60 Ma (Lydon, 2007). The
 
Property / addresses subject: Jurassic Period / qualifier
concept highlight: 2007). Deformation during the Laramide Orogeny (Late Jurassic to Tertiary) was dominated by compressional
 
Property / addresses subject: Jurassic Period / qualifier
concept highlight: features found within the Purcell Anticlinorium are Jurassic to Tertiary in age, and formed in association
 
Property / addresses subject: Jurassic Period / qualifier
concept highlight: Deformation during this period is related to a Late Jurassic to Early Cretaceous event of sinistral
 
Property / addresses subject: Jurassic Period / qualifier
concept highlight: terrane with cratonic North America during the Late Jurassic to Early Cretaceous (Cook and Van der Velden,
 
Property / addresses subject: Jurassic Period / qualifier
concept highlight: faults were propagated eastward during a period of Jurassic to Cretaceous contraction. This contraction
 
Property / addresses subject: Jurassic Period / qualifier
concept highlight: convection. The second event occurred during the Late Jurassic to Tertiary Laramide Orogeny. Porphyry-style
 
Property / addresses subject: Jurassic Period / qualifier
concept highlight: HelikianDevonian extension and development of a passive margin, Jurassic-Paleocene contraction (Laramide Orogeny),
 
Property / addresses subject: Jurassic Period / qualifier
concept highlight: stratigraphic thickness of units across fault systems. Jurassic-Paleocene contraction is characterized
 
Property / addresses subject: Jurassic Period / reference
 
Property / addresses subject: Jurassic Period / reference
 
Property / addresses subject
 
Property / addresses subject: Triassic Period / rank
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Property / addresses subject: Triassic Period / qualifier
concept highlight: kimberlitic to lamprophyric affinities, and are Permo-Triassic (245 Ma) in age. These small intrusive
 
Property / addresses subject: Triassic Period / reference
 
Property / addresses subject: Triassic Period / reference
 
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Latest revision as of 16:26, 6 July 2024

an NI 43-101 Technical Report pulled from the GeoArchive collection
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NI 43-101 Technical Report for the Ptarmagin Project in North America dated March 2012
an NI 43-101 Technical Report pulled from the GeoArchive collection

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