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Statements

Subject Item
dbr:Cathedral_Peak_Granodiorite
rdfs:label
Cathedral-Peak-Granodiorit Cathedral Peak Granodiorite
rdfs:comment
The Cathedral Peak Granodiorite (CPG) was named after its type locality, Cathedral Peak in Yosemite National Park, California. The granodiorite forms part of the Tuolumne Intrusive Suite (Tuolumne Batholith), one of the four major intrusive suites within the Sierra Nevada. It has been assigned radiometric ages between 88 and 87 million years and therefore reached its cooling stage in the Coniacian (Upper Cretaceous). Der Cathedral-Peak-Granodiorit wurde nach seiner Typlokalität, dem im US-amerikanischen Yosemite-Nationalpark gelegenen Cathedral Peak benannt. Das Granodioritmassiv ist ein Bestandteil der (auch Tuolumne Batholith) – einer der vier großen Intrusivkomplexe innerhalb der Sierra Nevada. Altersangaben für das Massiv fallen in die Oberkreide (Coniacium) und schwanken zwischen 88 und 87 Millionen Jahren.
foaf:depiction
n6:MatterhornPeakCA.jpg n6:Plagioclase_Replacement.jpg n6:Map_of_Cathedral_Peak_Granodiorite.svg n6:Cathedral_Range.jpg
dcterms:subject
dbc:Geology_of_Yosemite_National_Park dbc:Igneous_petrology_of_California dbc:Cretaceous_magmatism
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dbr:Displacement_(vector) dbr:Crystal_twinning dbr:Perthite dbr:Potassium dbr:Apatite dbr:Turonian dbr:Coniacian dbr:John_Muir_Intrusive_Suite dbr:Biotite dbr:Yosemite_National_Park dbr:Magma_chamber dbr:Mantle_(geology) dbr:Titanite dbr:Cataclastic_rock dbr:Aplite dbr:Sonora_Plutonic_Complex dbr:Clay_mineral dbr:Trace_element dbr:Pleochroic_halo dbr:Paleozoic dbr:K-feldspar dbr:Pleochroism dbr:Geology_of_the_Yosemite_area dbr:Plagioclase dbr:Barium dbr:Cathedral_Range dbr:Matterhorn_Peak dbr:California dbr:Subduction dbr:Half_Dome_Granodiorite dbr:Madera_County dbr:Mono_County dbr:Interstitial_defect dbr:Quartz dbr:Sentinel_granodiorite dbr:Crystallization dbr:Ostwald_ripening dbr:Megacryst dbr:Petrographic dbr:Tower_Peak_(California) dbr:Metasomatism dbr:Radiometric_dating dbc:Geology_of_Yosemite_National_Park dbr:Isotope_ratio dbr:Alkali_feldspar dbr:Santonian dbr:Magnetite dbr:Hornblende dbr:Country_rock_(geology) dbr:Phenocryst dbr:Magma n16:MatterhornPeakCA.jpg dbr:Granodiorite n16:Map_of_Cathedral_Peak_Granodiorite.svg dbr:Thermobarometry dbr:Rubidium dbr:Ladder_dike dbr:Metamorphism dbr:Felsic dbr:Metasediment dbr:Ilmenite dbr:Kuna_Crest_Granodiorite dbr:Mariposa_County dbr:Neodymium dbr:Silica dbr:Matrix_(geology) dbr:Tuolumne_Meadows dbr:Allanite dbr:Tuolumne_Intrusive_Suite dbr:Shoshonite dbr:Calc-alkaline dbc:Igneous_petrology_of_California dbr:Zircon dbr:Metaluminous dbr:Jurassic dbr:Tectonics dbr:Cathedral_Peak_(California) dbr:Europium dbr:Mount_Whitney_Intrusive_Suite dbr:California_State_Route_120 dbr:El_Capitan_Granite dbr:Porphyritic dbr:Strontium dbr:Calcium dbr:Myrmekite dbr:Nickel dbc:Cretaceous_magmatism dbr:Inclusion_(mineral) n16:Plagioclase_Replacement.jpg dbr:Scandium dbr:Intrusive_suites dbr:Sierra_Nevada dbr:Fractional_crystallization_(geology) dbr:Mafic dbr:Microcline dbr:Magmatic_foliations dbr:Schlieren dbr:Volcanic_arc dbr:Oligoclase dbr:Metavolcanic dbr:LREE dbr:Sodium dbr:CIPW_Norm dbr:Quartz_diorite dbr:Orthoclase dbr:Shear_zone n16:Cathedral_Range.jpg dbr:Poikilitic dbr:Chromium dbr:Johnson_Granite_Porphyry dbr:Tuolumne_County
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dbo:thumbnail
n6:MatterhornPeakCA.jpg?width=300
dbo:abstract
Der Cathedral-Peak-Granodiorit wurde nach seiner Typlokalität, dem im US-amerikanischen Yosemite-Nationalpark gelegenen Cathedral Peak benannt. Das Granodioritmassiv ist ein Bestandteil der (auch Tuolumne Batholith) – einer der vier großen Intrusivkomplexe innerhalb der Sierra Nevada. Altersangaben für das Massiv fallen in die Oberkreide (Coniacium) und schwanken zwischen 88 und 87 Millionen Jahren. The Cathedral Peak Granodiorite (CPG) was named after its type locality, Cathedral Peak in Yosemite National Park, California. The granodiorite forms part of the Tuolumne Intrusive Suite (Tuolumne Batholith), one of the four major intrusive suites within the Sierra Nevada. It has been assigned radiometric ages between 88 and 87 million years and therefore reached its cooling stage in the Coniacian (Upper Cretaceous).
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wikipedia-en:Cathedral_Peak_Granodiorite?oldid=1079814710&ns=0
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wikipedia-en:Cathedral_Peak_Granodiorite