Metamorphic and stratigraphic constraints on the evolution of the Santa Catalina Mountains metamorphic core complex, Arizona
Journal Article
·
· Journal of Geophysical Research; (United States)
- Arizona State Univ., Tempe (United States)
Contact metamorphic mineral assemblages in the Santa Catalina Mountains metamorphic core complex constrain the emplacement depth of the metaluminous Late Cretaceous Leatherwood quartz diorite to between 7.5 and 14 km (2-3.8 kbar). The peraluminous Eocene Wilderness granite is constrained to have been emplaced at depths of less than 14 km. Stratigraphic and tectonic considerations are consistent with emplacement of both the Leatherwood quartz diorite and Wilderness granite at upper crustal levels. Published igneous thermobarometry (Anderson et al., 1988), although in approximate agreement with the metamorphic and tectonostratigraphic estimates for the depth of emplacement of the Wilderness granite, suggests that the Leatherwood quartz diorite was emplaced at depths of {approximately} 21 km (5.6 kbar) or greater. The discrepancy between the different emplacement estimates may reflect ambiguities associated with interpretations of the results from each technique. Igneous barometric assemblages may reflect conditions experienced during a period of crystallization during ascent of the magma through the crust (i.e., ponding of the magma). Alternatively, emplacement of the voluminous Wilderness granite and associated plutons may have entirely overprinted earlier Leatherwood-related contact metamorphism. The proposed upper crustal emplacement of the Leatherwood quartz diorite is consistent with the observation that Laramide-age crustal thickening in southeast Arizona probably did not exceed 8 km.
- OSTI ID:
- 5073962
- Journal Information:
- Journal of Geophysical Research; (United States), Journal Name: Journal of Geophysical Research; (United States) Vol. 95:B1; ISSN 0148-0227; ISSN JGREA
- Country of Publication:
- United States
- Language:
- English
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Petrology and geobarometry of Admiralty-Revillagigedo belt granitoids near Petersburg, southeastern Alaska
Journal Article
·
Thu Jan 02 19:00:00 EST 2025
· Tectonics
·
OSTI ID:2511364
Structural reconstruction and zonation of a tilted mid-crustal magma chamber: the felsic Chemehuevi Mountains plutonic suite
Journal Article
·
Fri Jul 01 00:00:00 EDT 1988
· Geology; (United States)
·
OSTI ID:7183336
Petrology and geobarometry of Admiralty-Revillagigedo belt granitoids near Petersburg, southeastern Alaska
Conference
·
Wed Mar 31 23:00:00 EST 1993
· Geological Society of America, Abstracts with Programs; (United States)
·
OSTI ID:5099237
Related Subjects
58 GEOSCIENCES
580000* -- Geosciences
ARIZONA
CONSTRAINTS
CONTINENTAL CRUST
CRETACEOUS PERIOD
CRYSTALLIZATION
DEPTH
DEVELOPED COUNTRIES
DIMENSIONS
EARTH CRUST
FEDERAL REGION IX
GEOLOGIC AGES
GEOLOGIC HISTORY
GEOLOGIC MODELS
GEOLOGY
GRANITES
IGNEOUS ROCKS
MAGMA
MESOZOIC ERA
METAMORPHIC ROCKS
METAMORPHISM
MINERALOGY
MINERALS
MOUNTAINS
NORTH AMERICA
OROGENESIS
OXIDE MINERALS
PHASE TRANSFORMATIONS
PLUTONIC ROCKS
QUARTZ
ROCKS
STRATIGRAPHY
TECTONICS
THICKNESS
USA
580000* -- Geosciences
ARIZONA
CONSTRAINTS
CONTINENTAL CRUST
CRETACEOUS PERIOD
CRYSTALLIZATION
DEPTH
DEVELOPED COUNTRIES
DIMENSIONS
EARTH CRUST
FEDERAL REGION IX
GEOLOGIC AGES
GEOLOGIC HISTORY
GEOLOGIC MODELS
GEOLOGY
GRANITES
IGNEOUS ROCKS
MAGMA
MESOZOIC ERA
METAMORPHIC ROCKS
METAMORPHISM
MINERALOGY
MINERALS
MOUNTAINS
NORTH AMERICA
OROGENESIS
OXIDE MINERALS
PHASE TRANSFORMATIONS
PLUTONIC ROCKS
QUARTZ
ROCKS
STRATIGRAPHY
TECTONICS
THICKNESS
USA