NI 43-101 Technical Report for the Rodeo Project in North America dated February 2010 (Q29331): 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: province is dominantly comprised of a Jurassic- to Cretaceous-age, shelf-margin, carbonate sequence | |||
Property / addresses subject: Cretaceous Period / qualifier | |||
concept highlight: ii _________________________________________________________________________________ Cretaceous-age marine siltstone-sandstone flysch | |||
Property / addresses subject: Cretaceous Period / qualifier | |||
concept highlight: rocks in regional fault contact with the older late Cretaceous-age carbonate flysch rocks of the Indidura | |||
Property / addresses subject: Cretaceous Period / qualifier | |||
concept highlight: unmineralized quartz veining related to the Late Cretaceous Laramide-related tectonics. Precious | |||
Property / addresses subject: Cretaceous Period / qualifier | |||
concept highlight: conformably overlain by a back-arc successor basin of Cretaceous-age marine siltstone-sandstone flysch | |||
Property / addresses subject: Cretaceous Period / qualifier | |||
concept highlight: Cura’ Formations which range from early to middle Cretaceous in age. A late Cretaceous | |||
Property / addresses subject: Cretaceous Period / qualifier | |||
concept highlight: middle Cretaceous in age. A late Cretaceous carbonaceous and calcareous turbiditic | |||
Property / addresses subject: Cretaceous Period / qualifier | |||
concept highlight: the margins of the Coahuila Platform at the end of Cretaceous time. The Sierra Madre Occidental mountain | |||
Property / addresses subject: Cretaceous Period / qualifier | |||
concept highlight: continental and marine clastic rocks overlain by Cretaceous-age platform and basinal carbonate rocks. Northcentral | |||
Property / addresses subject: Cretaceous Period / qualifier | |||
concept highlight: subjected to the compressional Laramide orogeny in Late Cretaceous to Early Tertiary time related to the | |||
Property / addresses subject: Cretaceous Period / qualifier | |||
concept highlight: North American Plate (de Cserna, 1989). The late Cretaceous geosynclinal limestone-flysch sequence | |||
Property / addresses subject: Cretaceous Period / qualifier | |||
concept highlight: rhyolite flow domes in fault contact with older late Cretaceous-age carbonate flysch rocks of the Indidura | |||
Property / addresses subject: Cretaceous Period / qualifier | |||
concept highlight: platform limestone and siltstone belonging to the Late Cretaceous-age Indidura Formation. The northnorthwesterly | |||
Property / addresses subject: Cretaceous Period / qualifier | |||
concept highlight: Oligocene Paleocene to Early Oligocene Paleocene Late Cretaceous Unit Alluvium ‘Rodeo’ Volcanics Intrusion Regional | |||
Property / addresses subject: Cretaceous Period / qualifier | |||
concept highlight: angular unconformable contract between the Upper Cretaceous Indidura Formation carbonate flysch units | |||
Property / addresses subject: Cretaceous Period / qualifier | |||
concept highlight: volcaniclastics ‘Heroes de Mexico’ or 'Rodeo' Fault Zone Late Cretaceous Indidura Formation Fracturing Tensional Normal Compressional Description Not | |||
Property / addresses subject: Cretaceous Period / qualifier | |||
concept highlight: Tertiary-age rhyolitic tuffs and breccias and Upper Cretaceous silty limestones (Durning and Hillemeyer, | |||
Property / addresses subject: Cretaceous Period / qualifier | |||
concept highlight: unmineralized quartz veining related to the Late Cretaceous Laramide-related tectonics (Blackwell | |||
Property / addresses subject: Cretaceous Period / qualifier | |||
concept highlight: and quartz-carbonate veining commonly occurs Late Cretaceous Indidura Formation near the Rodeo Fault. | |||
Property / addresses subject: Cretaceous Period / qualifier | |||
concept highlight: forming a local angular unconformity between the Upper Cretaceous Indidura Formation carbonate flysch units | |||
Property / addresses subject: Cretaceous Period / qualifier | |||
concept highlight: on the southwestern, hangingwall side. The Upper Cretaceous Indidura Formation is locally comprised | |||
Property / addresses subject: Cretaceous Period / qualifier | |||
concept highlight: Andesite - dacitic to basaltic, pyritic MESOZOIC Late Cretaceous Indidura Formation KIF Limestone, sandstone, | |||
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: Mesa Central province is dominantly comprised of a Jurassic- to Cretaceous-age, shelf-margin, carbonate | |||
Property / addresses subject: Jurassic Period / qualifier | |||
concept highlight: Central tectonic province is dominantly comprised of a Jurassic- to Cretaceous-age, shelf-margin, carbonate | |||
Property / addresses subject: Jurassic Period / qualifier | |||
concept highlight: to youngest, the limestone formations are the late Jurassic ‘Zualoga’ and ‘Caja’ Formations that are | |||
Property / addresses subject: Jurassic Period / reference | |||
Property / addresses subject: Jurassic Period / reference | |||
Property / addresses subject | |||
Property / addresses subject: Triassic Period / rank | |||
Normal rank | |||
Property / addresses subject: Triassic Period / qualifier | |||
concept highlight: unconformably deposited on the metamorphic basement rocks in Triassic time representing possible erosion prior | |||
Property / addresses subject: Triassic Period / reference | |||
Property / addresses subject: Triassic Period / reference | |||
Revision as of 20:55, 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 Rodeo Project in North America dated February 2010 |
an NI 43-101 Technical Report pulled from the GeoArchive collection |
Statements
province is dominantly comprised of a Jurassic- to Cretaceous-age, shelf-margin, carbonate sequence
ii _________________________________________________________________________________ Cretaceous-age marine siltstone-sandstone flysch
rocks in regional fault contact with the older late Cretaceous-age carbonate flysch rocks of the Indidura
unmineralized quartz veining related to the Late Cretaceous Laramide-related tectonics. Precious
conformably overlain by a back-arc successor basin of Cretaceous-age marine siltstone-sandstone flysch
Cura’ Formations which range from early to middle Cretaceous in age. A late Cretaceous
middle Cretaceous in age. A late Cretaceous carbonaceous and calcareous turbiditic
the margins of the Coahuila Platform at the end of Cretaceous time. The Sierra Madre Occidental mountain
continental and marine clastic rocks overlain by Cretaceous-age platform and basinal carbonate rocks. Northcentral
subjected to the compressional Laramide orogeny in Late Cretaceous to Early Tertiary time related to the
North American Plate (de Cserna, 1989). The late Cretaceous geosynclinal limestone-flysch sequence
rhyolite flow domes in fault contact with older late Cretaceous-age carbonate flysch rocks of the Indidura
platform limestone and siltstone belonging to the Late Cretaceous-age Indidura Formation. The northnorthwesterly
Oligocene Paleocene to Early Oligocene Paleocene Late Cretaceous Unit Alluvium ‘Rodeo’ Volcanics Intrusion Regional
angular unconformable contract between the Upper Cretaceous Indidura Formation carbonate flysch units
volcaniclastics ‘Heroes de Mexico’ or 'Rodeo' Fault Zone Late Cretaceous Indidura Formation Fracturing Tensional Normal Compressional Description Not
Tertiary-age rhyolitic tuffs and breccias and Upper Cretaceous silty limestones (Durning and Hillemeyer,
unmineralized quartz veining related to the Late Cretaceous Laramide-related tectonics (Blackwell
and quartz-carbonate veining commonly occurs Late Cretaceous Indidura Formation near the Rodeo Fault.
forming a local angular unconformity between the Upper Cretaceous Indidura Formation carbonate flysch units
on the southwestern, hangingwall side. The Upper Cretaceous Indidura Formation is locally comprised
Andesite - dacitic to basaltic, pyritic MESOZOIC Late Cretaceous Indidura Formation KIF Limestone, sandstone,
Mesa Central province is dominantly comprised of a Jurassic- to Cretaceous-age, shelf-margin, carbonate
Central tectonic province is dominantly comprised of a Jurassic- to Cretaceous-age, shelf-margin, carbonate
to youngest, the limestone formations are the late Jurassic ‘Zualoga’ and ‘Caja’ Formations that are
unconformably deposited on the metamorphic basement rocks in Triassic time representing possible erosion prior
P97 (Deleted Property)
4530692:PERE8KRX Property P97 not found, cannot determine the data type to use.
0 references