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

Schlegel, Tobias U., Wagner, Thomas, Fusswinkel, Tobias (2020) Fluorite as indicator mineral in iron oxide-copper-gold systems: explaining the IOCG deposit diversity. Chemical Geology, 548. 119674pp. doi:10.1016/j.chemgeo.2020.119674

Advanced
   -   Only viewable:
Reference TypeJournal (article/letter/editorial)
TitleFluorite as indicator mineral in iron oxide-copper-gold systems: explaining the IOCG deposit diversity
JournalChemical Geology
AuthorsSchlegel, Tobias U.Author
Wagner, ThomasAuthor
Fusswinkel, TobiasAuthor
Year2020 (August)Volume548
Page(s)119674
PublisherElsevier BV
DOIdoi:10.1016/j.chemgeo.2020.119674Search in ResearchGate
Mindat Ref. ID4572192Long-form Identifiermindat:1:5:4572192:2
GUID6e10e4d6-4e61-478f-a9f8-93e30b3352cb
Full ReferenceSchlegel, Tobias U., Wagner, Thomas, Fusswinkel, Tobias (2020) Fluorite as indicator mineral in iron oxide-copper-gold systems: explaining the IOCG deposit diversity. Chemical Geology, 548. 119674pp. doi:10.1016/j.chemgeo.2020.119674
Plain TextSchlegel, Tobias U., Wagner, Thomas, Fusswinkel, Tobias (2020) Fluorite as indicator mineral in iron oxide-copper-gold systems: explaining the IOCG deposit diversity. Chemical Geology, 548. 119674pp. doi:10.1016/j.chemgeo.2020.119674
In(2020) Chemical Geology Vol. 548. Elsevier BV

References Listed

These are the references the publisher has listed as being connected to the article. Please check the article itself for the full list of references which may differ. Not all references are currently linkable within the Digital Library.

Barton (2014) 13.20 - Iron Oxide(–Cu–Au–REE–P–Ag–U–Co) Systems , 515
Ehrig (2012) Soc. Econ. Geol. Spec. Publ. Geology and mineralogical zonation of the Olympic Dam iron oxide Cu-U-Au-Ag deposit, South Australia 16, 237
Fleischer (1969) Indian Mineralogist The lanthanide elements in fluorite 10, 36
Freeman (2010) Geological setting of iron oxide related mineralisation in the southern Mount Woods domain, South Australia 3, 171
Goldstein (1994) Systematics of fluid inclusions in diagenetic minerals
Guillong (2008) SILLS; a MATLAB-based program for the reduction of laser ablation ICP-MS data of homogeneous materials and inclusions 40, 328
Jacob (1974) , 99
Mark (2000) The evolution of the Ernest Henry Fe-Oxide-(Cu-Au) hydrothermal system 1, 123
Pollard (2000) Evidence of a magmatic fluid and metal source for Fe-oxide Cu-Au mineralization 1, 27
Reeve (1990) Australasian Institute of Mining and Metallurgy Monograph Series Olympic Dam copper-uranium-gold-silver deposit 14, 1009
Ridley (2000) Rev. Econ. Geol. Fluid chemistry of orogenic lode gold deposits and implications for genetic models 13, 141
Roedder (1984) Rev. Mineral. Geochem. Fluid inclusions 12
Rusk (2010) Physical and chemical characteristics of the Ernest Henry iron oxide copper gold deposit, Australia; implications for IOCG genesis 3, 201
Simon (2018) Soc. Econ. Geol. Spec. Publ. Kiruna-type iron oxide-apatite (IOA) and iron oxide-copper-gold (IOCG) deposits form by a combination of igneous and magmatic-hydrothermal processes: evidence from the Chilean iron belt 21, 89
Williams (2005) Iron oxide copper-gold deposits: geology, space-time distribution, and possible modes of origin , 371
Williams (2017) Metallogenic significance of altered volcanic rocks near the Prominent Hill IOCG deposit, South Australia 3, 895
Williams (2017) Prominent Hill copper-gold deposit 32, 611


See Also

These are possibly similar items as determined by title/reference text matching only.

 
and/or  
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 © 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 3, 2024 13:33:23
Go to top of page