NI 43-101 Technical Report for the San Jose Project in North America dated November 2013 (Q29011): Difference between revisions
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Property / addresses subject | |||
Property / addresses subject: Carboniferous Period / rank | |||
Normal rank | |||
Property / addresses subject: Carboniferous Period / qualifier | |||
concept highlight: G.Corbett, 92p. Dickinson, W.R., and Lawton, T.F., 2001. Carboniferous to Cretaceous assembly and fragmentation | |||
Property / addresses subject: Carboniferous Period / reference | |||
Property / addresses subject: Carboniferous Period / reference | |||
Property / addresses subject | |||
Property / addresses subject: Cretaceous Period / rank | |||
Normal rank | |||
Property / addresses subject: Cretaceous Period / qualifier | |||
concept highlight: fault-bounded prism of strongly deformed Jurassic and Cretaceous oceanic and arc volcanic rocks that structurally | |||
Property / addresses subject: Cretaceous Period / qualifier | |||
concept highlight: age, limestones and calcareous sedimentary rocks of Cretaceous age and continental conglomerates of | |||
Property / addresses subject: Cretaceous Period / qualifier | |||
concept highlight: Dickinson, W.R., and Lawton, T.F., 2001. Carboniferous to Cretaceous assembly and fragmentation of Mexico. | |||
Property / addresses subject: Cretaceous Period / reference | |||
Property / addresses subject: Cretaceous Period / reference | |||
Property / addresses subject | |||
Property / addresses subject: Jurassic Period / rank | |||
Normal rank | |||
Property / addresses subject: Jurassic Period / qualifier | |||
concept highlight: west-dipping fault-bounded prism of strongly deformed Jurassic and Cretaceous oceanic and arc volcanic | |||
Property / addresses subject: Jurassic Period / reference | |||
Property / addresses subject: Jurassic Period / reference | |||
Property / addresses subject | |||
Property / addresses subject: Neogene Period / rank | |||
Normal rank | |||
Property / addresses subject: Neogene Period / qualifier | |||
concept highlight: intruded by granodiorite to diorite stocks of possible Neogene age. Figure 7.2 Local geology of the San | |||
Property / addresses subject: Neogene Period / reference | |||
Property / addresses subject: Neogene Period / reference | |||
Property / addresses subject | |||
Property / addresses subject: Paleogene Period / rank | |||
Normal rank | |||
Property / addresses subject: Paleogene Period / qualifier | |||
concept highlight: dacitic volcanic and volcaniclastic rocks of presumed Paleogene age. These units have been significantly | |||
Property / addresses subject: Paleogene Period / qualifier | |||
concept highlight: to dacitic effusive volcanic sequence of presumed Paleogene age. Further to the east, these andesites | |||
Property / addresses subject: Paleogene Period / qualifier | |||
concept highlight: area is underlain by a thick sequence of presumed Paleogene-age andesitic to dacitic volcanic and | |||
Property / addresses subject: Paleogene Period / qualifier | |||
concept highlight: Martinez-Serrano, et al, 2008). In the Taviche area, the Paleogene-age volcanics are intruded by granodiorite | |||
Property / addresses subject: Paleogene Period / qualifier | |||
concept highlight: dacitic volcanic and volcaniclastic rocks of presumed Paleogene age (Figure 7.3). These units have been | |||
Property / addresses subject: Paleogene Period / qualifier | |||
concept highlight: displacement Andesitic to dacitic subaerial to subaqueous lava flows Paleogene (?) Quartz-carbonate veins, hydrothermal | |||
Property / addresses subject: Paleogene Period / qualifier | |||
concept highlight: dacitic subaerial and subaqueous lava flows of presumed Paleogene age. Major vein systems recognized in | |||
Property / addresses subject: Paleogene Period / reference | |||
Property / addresses subject: Paleogene Period / reference | |||
Revision as of 20:56, 19 April 2023
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 San Jose Project in North America dated November 2013 |
an NI 43-101 Technical Report pulled from the GeoArchive collection |
Statements
G.Corbett, 92p. Dickinson, W.R., and Lawton, T.F., 2001. Carboniferous to Cretaceous assembly and fragmentation
fault-bounded prism of strongly deformed Jurassic and Cretaceous oceanic and arc volcanic rocks that structurally
age, limestones and calcareous sedimentary rocks of Cretaceous age and continental conglomerates of
Dickinson, W.R., and Lawton, T.F., 2001. Carboniferous to Cretaceous assembly and fragmentation of Mexico.
west-dipping fault-bounded prism of strongly deformed Jurassic and Cretaceous oceanic and arc volcanic
intruded by granodiorite to diorite stocks of possible Neogene age. Figure 7.2 Local geology of the San
dacitic volcanic and volcaniclastic rocks of presumed Paleogene age. These units have been significantly
to dacitic effusive volcanic sequence of presumed Paleogene age. Further to the east, these andesites
area is underlain by a thick sequence of presumed Paleogene-age andesitic to dacitic volcanic and
Martinez-Serrano, et al, 2008). In the Taviche area, the Paleogene-age volcanics are intruded by granodiorite
dacitic volcanic and volcaniclastic rocks of presumed Paleogene age (Figure 7.3). These units have been
displacement Andesitic to dacitic subaerial to subaqueous lava flows Paleogene (?) Quartz-carbonate veins, hydrothermal
dacitic subaerial and subaqueous lava flows of presumed Paleogene age. Major vein systems recognized in
P97 (Deleted Property)
4530692:5PU2ZIPQ Property P97 not found, cannot determine the data type to use.
0 references