Vote for your favorite mineral in #MinCup25! - Calcite vs. Perovskite
This match of heavy hitters is bound to end in heartbreak as classic calcite faces off against futuristic perovskite.
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

Smith, W. W. (1959) Pseudomorphs after olivine in Markle basalt. Mineralogical Magazine and Journal of the Mineralogical Society, 32 (247) 324-331 doi:10.1180/minmag.1959.032.247.05

Advanced
   -   Only viewable:
Reference TypeJournal (article/letter/editorial)
TitlePseudomorphs after olivine in Markle basalt
JournalMineralogical Magazine and Journal of the Mineralogical Society
AuthorsSmith, W. W.Author
Year1959 (December)Volume32
Issue247
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_32/32-247-324.pdf+
DOIdoi:10.1180/minmag.1959.032.247.05
Generate Citation Formats
Mindat Ref. ID5537Long-form Identifiermindat:1:5:5537:0
GUID0
Full ReferenceSmith, W. W. (1959) Pseudomorphs after olivine in Markle basalt. Mineralogical Magazine and Journal of the Mineralogical Society, 32 (247) 324-331 doi:10.1180/minmag.1959.032.247.05
Plain TextSmith, W. W. (1959) Pseudomorphs after olivine in Markle basalt. Mineralogical Magazine and Journal of the Mineralogical Society, 32 (247) 324-331 doi:10.1180/minmag.1959.032.247.05
In(1959) Mineralogical Magazine Vol. 32 (247) Mineralogical Society
Abstract/NotesSummaryPseudomorphs after olivine in Markle basalt from Holyrood Park, Edinburgh, consist of an intimate mixture of hematite and chlorite, along with a small percentage of quartz. A definite relationship exists between the orientations of the two main constituents and is dependent upon their structures.


See Also

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

 
and/or  
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 1993-2025, except where stated. Most political location boundaries are Β© OpenStreetMap contributors. Mindat.org relies on the contributions of thousands of members and supporters. Founded in 2000 by Jolyon Ralph.
To cite: Ralph, J., Von Bargen, D., Martynov, P., Zhang, J., Que, X., Prabhu, A., Morrison, S. M., Li, W., Chen, W., & Ma, X. (2025). Mindat.org: The open access mineralogy database to accelerate data-intensive geoscience research. American Mineralogist, 110(6), 833–844. doi:10.2138/am-2024-9486.
Privacy Policy - Terms & Conditions - Contact Us / DMCA issues - Report a bug/vulnerability Current server date and time: September 4, 2025 10:34:05
Go to top of page