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

Springfield basin, Cradock, South Flinders Ranges, Flinders Ranges, South Australia, Australiai
Regional Level Types
Springfield basinBasin
Cradock- not defined -
South Flinders Ranges- not defined -
Flinders RangesMining Region
South AustraliaState
AustraliaCountry

This page is currently not sponsored. Click here to sponsor this page.
PhotosMapsSearch
Latitude & Longitude (WGS84):
32° 7' 47'' South , 138° 23' 25'' East
Latitude & Longitude (decimal):
Area:
9 km2
Type:
Mindat Locality ID:
269868
Long-form identifier:
mindat:1:2:269868:0
GUID (UUID V4):
8c4fead8-00d8-4057-b1de-2da34b76a0fd


Conglomerates

128 diamonds and fragments were recovered in the mid-1980s from Permian basal conglomerate. In 1998, an additional 56 diamonds were recovered from renewed exploration trenching, the largest being 3.5 mm and weighing 0.34 ct. Fresh indicator minerals, particularly garnet with a kelyphytic rind, suggested that the kimberlite source was relatively close to the basin. Site is that of exposed conglomerate of the basal conglomerate, Conglomerate unit A located at the SE-extent of the basin , and from which diamonds were recovered from a ~1m thick cobble unit as exposed in costeans. Surface mapping of the basal conglomerate or Conglomerate Unit A suggested the unit represents material deposited in river channels. Flow direction as estimated from studies of clast orientation indicate flow for the very basal member was into the area from a south-westerly direction. Subsequent drilling of 6 diamond holes confirmed continuity and thickening of conglomeritic beds within this basal sequence including the persistence of basal conglomerates, including a possible correlative of the diamondiferous cobble unit with a thickness of 2.05m. A study of indicator minerals from the core indicated a freshness that suggests a primary source in close proximity, possibly within 2km of the basin edge. Suggested volume of basal unit from mapping and drilling was 1.82 million cubic metres (for thickness 1.66m), and for overlying conglomerate unit with thickness 6.3m = 6.95 million cubic metres.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Mineral List


5 valid minerals.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
β“˜Diamond1.CB.10aC
Group 4 - Oxides and Hydroxides
β“˜Magnesiochromite4.BB.05MgCr2O4
β“˜Ilmenite4.CB.05Fe2+TiO3
β“˜var. Picroilmenite4.CB.05(Fe2+,Mg)TiO3
Group 9 - Silicates
β“˜Pyrope9.AD.25Mg3Al2(SiO4)3
β“˜Diopside
var. Chromium-bearing Diopside
9.DA.15Ca(Mg,Cr)Si2O6
β“˜9.DA.15CaMgSi2O6

List of minerals for each chemical element

CCarbon
Cβ“˜ DiamondC
OOxygen
Oβ“˜ Diopside var. Chromium-bearing DiopsideCa(Mg,Cr)Si2O6
Oβ“˜ DiopsideCaMgSi2O6
Oβ“˜ IlmeniteFe2+TiO3
Oβ“˜ MagnesiochromiteMgCr2O4
Oβ“˜ PyropeMg3Al2(SiO4)3
Oβ“˜ Ilmenite var. Picroilmenite(Fe2+,Mg)TiO3
MgMagnesium
Mgβ“˜ Diopside var. Chromium-bearing DiopsideCa(Mg,Cr)Si2O6
Mgβ“˜ DiopsideCaMgSi2O6
Mgβ“˜ MagnesiochromiteMgCr2O4
Mgβ“˜ PyropeMg3Al2(SiO4)3
Mgβ“˜ Ilmenite var. Picroilmenite(Fe2+,Mg)TiO3
AlAluminium
Alβ“˜ PyropeMg3Al2(SiO4)3
SiSilicon
Siβ“˜ Diopside var. Chromium-bearing DiopsideCa(Mg,Cr)Si2O6
Siβ“˜ DiopsideCaMgSi2O6
Siβ“˜ PyropeMg3Al2(SiO4)3
CaCalcium
Caβ“˜ Diopside var. Chromium-bearing DiopsideCa(Mg,Cr)Si2O6
Caβ“˜ DiopsideCaMgSi2O6
TiTitanium
Tiβ“˜ IlmeniteFe2+TiO3
Tiβ“˜ Ilmenite var. Picroilmenite(Fe2+,Mg)TiO3
CrChromium
Crβ“˜ Diopside var. Chromium-bearing DiopsideCa(Mg,Cr)Si2O6
Crβ“˜ MagnesiochromiteMgCr2O4
FeIron
Feβ“˜ IlmeniteFe2+TiO3
Feβ“˜ Ilmenite var. Picroilmenite(Fe2+,Mg)TiO3

Other Regions, Features and Areas containing this locality

Australia
Australian PlateTectonic Plate

This page contains all mineral locality references listed on mindat.org. This does not claim to be a complete list. If you know of more minerals from this site, please register so you can add to our database. This locality information is for reference purposes only. You should never attempt to visit any sites listed in mindat.org without first ensuring that you have the permission of the land and/or mineral rights holders for access and that you are aware of all safety precautions necessary.

References

 
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 Β© 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 1, 2024 21:33:27 Page updated: March 25, 2024 15:37:49
Go to top of page