Log InRegister
Quick Links : The Mindat ManualThe Rock H. Currier Digital LibraryMindat Newsletter [Free Download]
Home PageAbout MindatThe Mindat ManualHistory of MindatCopyright StatusWho We AreContact UsAdvertise on Mindat
Donate to MindatCorporate SponsorshipSponsor a PageSponsored PagesMindat AdvertisersAdvertise on Mindat
Learning CenterWhat is a mineral?The most common minerals on earthInformation for EducatorsMindat ArticlesThe ElementsThe Rock H. Currier Digital LibraryGeologic Time
Minerals by PropertiesMinerals by ChemistryAdvanced Locality SearchRandom MineralRandom LocalitySearch by minIDLocalities Near MeSearch ArticlesSearch GlossaryMore Search Options
Search For:
Mineral Name:
Locality Name:
Keyword(s):
 
The Mindat ManualAdd a New PhotoRate PhotosLocality Edit ReportCoordinate Completion ReportAdd Glossary Item
Mining CompaniesStatisticsUsersMineral MuseumsClubs & OrganizationsMineral Shows & EventsThe Mindat DirectoryDevice SettingsThe Mineral Quiz
Photo SearchPhoto GalleriesSearch by ColorNew Photos TodayNew Photos YesterdayMembers' Photo GalleriesPast Photo of the Day GalleryPhotography

Bornite from
Mammoth Breccia Pipe, Copper Creek (Copper Creek Canyon), Bunker Hill District (Copper Creek District), Pinal County, Arizona, USA


Locality type:Pipe
Classification
Species:Bornite
Formula:Cu5FeS4
Confirmation
Validity:Believed Valid
Data
Mineral Data:Click here to view Bornite data
Locality Data:Click here to view Mammoth Breccia Pipe, Copper Creek (Copper Creek Canyon), Bunker Hill District (Copper Creek District), Pinal County, Arizona, USA
Data Identifiers
Mindat Occurrence Record ID:608145
Long-form Identifier:1:3:608145:4
GUID (UUID V4):632802ea-95d9-4506-8cc7-da7ebabcd9ba
References
Reference Search (possible matching items)
Journal (article/letter/editorial)
geochemistry of the Mammoth breccia pipe, Copper Creek mining district, southeastern Arizona: evidence for...The Copper Creek mining district, southeastern Arizona, contains more than 500 mineralized breccia pipes...porphyry-style, copper-bearing stockworks, and distal lead–silver veins. The breccia pipes are hosted...hosted by the Copper Creek Granodiorite and the Glory Hole volcanic rocks. The unexposed Mammoth breccia pipe... The pipe consists of angular clasts of granodiorite cemented by quartz, chalcopyrite, bornite, anhydrite
Book
Publication Number 16 Geology and Genesis of Major Copper Deposits and Districts of the World: A Tribute...Publication Number 16 Geology and Genesis of Major Copper Deposits and Districts of the World: A Tribute...label: Aerial view of the Bingham Canyon copper mine, Kennecott Utah Copper, September 2003. Photo courtesy...contribution to the understanding of the world’s major copper deposits SOCIETY OF ECONOMIC GEOLOGISTS, INC...Geologic Setting and Evolution of the Porphyry Copper-Molybdenum and CopperGold Deposits at Los Pelambres
Journal (article/letter/editorial)
and heated axes. Cupolas may form initially as breccia pipes by volatile phase (rather than magma) reaming-out...the formation of magmatic–hydrothermal porphyry copper deposits upon emplacement in the upper crust. Mungall...and metals in the Laramide porphyry systems of Arizona. Moreover, Titley (1987, 2001) has specifically...ore deposits including porphyries in southwestern USA, because the ratios of these elements correlate closely...unlikely that this argument can be extended to copper, except perhaps on the margins. 2.4.2. Sources
 
Mineral and/or Locality  
Mindat Discussions Facebook Logo Instagram Logo Discord Logo
Mindat.org is an outreach project of the Hudson Institute of Mineralogy, a 501(c)(3) not-for-profit organization.
Copyright © mindat.org and the Hudson Institute of Mineralogy 1993-2024, except where stated. Most political location boundaries are Š OpenStreetMap contributors. Mindat.org relies on the contributions of thousands of members and supporters. Founded in 2000 by Jolyon Ralph.
Privacy Policy - Terms & Conditions - Contact Us / DMCA issues - Report a bug/vulnerability Current server date and time: May 2, 2024 11:10:27
Go to top of page