SUPPORT US. If mindat.org is important to you, click here to donate to our Fall 2019 fundraiser!
Log InRegister
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 ElementsBooks & Magazines
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 MuseumsMineral Shows & EventsThe Mindat DirectoryDevice Settings
Photo SearchPhoto GalleriesNew Photos TodayNew Photos YesterdayMembers' Photo GalleriesPast Photo of the Day GalleryMineral Photography

Bungalow prospect, Cowell, Eyre Peninsula, South Australia, Australia

This page is currently not sponsored. Click here to sponsor this page.
 
Latitude & Longitude (WGS84): 33° 35' 42'' South , 136° 53' 17'' East
Latitude & Longitude (decimal): -33.59500,136.88806
Köppen climate type:BSk : Cold semi-arid (steppe) climate


This is one of several localities on the Eyre Peninsula Centrex Metals propose as being a 'possible mine' in the future. At this time (April 2011) it is still only part of their pospectus. M.Willoughby.

BIF deposit.
Located 9 km NNW of Cowell.

Bungalow prospect,recognised by its prominent aeromagnetic anomaly, and investigated in the late 1950's by ground geophysical surveys and drilling by SADME. The magnetic anomaly was a double peak of 5-14 000 nT, 9 km strike length, and over 600 m wide. Cover thickness of younger sediment was 15-35 m, thickening to the south. It was drill tested in cross-section by five drill holes (Bungalow BD1-3, 4 & 6). BD2 intersected banded iron formation (BIF), grading from dominantly quartz-cummingtonite-magnetite to magnetite-talc to quartz-magnetite. The volume percent of magnetite was similar to that found in the Middleback Range. Best assays BD2, 15 m @ 29.4% Fe, 9 m @ 39.6% Fe. More recent exploration included low-level aeromagnetics, gravity, diamond drilling with geochemistry and Davis Tube test work. The magnetics were resolved into a number of narrow, elongate, high amplitude anomalies. Drilling carried out on 2 sections confirmed a folded BIF band of true width ~36 m. Cover depth varied from 20-75 m, lateritic weathering 30-90 m below ground level. Best magnetite-bearing BIF occurred in a micro- to mesobanded magnetite-bearing BIF, typically as magnetite-rich bands alternating with quartz, iron-rich silicates and carbonate. Generally the magnetite was quite fine grained with a significant proportion <75 microns. A global weighted average grade was 38.02% DTR (Davis Tube Recovery) at 67.66% Fe and 5.37% SiO2. Total resource May 2012 at 239Mt at 30.7%Fe head grade, 35.2DTR% at 38 micron grind for product at 69.8%Fe. Revised exploration target in the order of 500-750Mt, based on results to 2010, and new aeromagnetics. Age dating of interbanded, biotite-garnet-sillimanite schist (metasediment) appears to indicate that the iron formation was deposited some time after ca. 2555 Ma and may therefore be correlative of the iron formations in the Middleback Range itself, with recent maximum depositional ages for schist in the Middleback Range being ca. 2565 Ma. Granites, including garnet-bearing S-type leucosomes were emplaced into the Bungalow iron formation-bearing sedimentary sequence at ca. 1730 Ma, likely during the early phase of the Kimban Orogeny. One of these granites has inherited zircons as old as ca. 3445 Ma.


Mineral List


4 valid minerals.

Regional Geology

This geological map and associated information on rock units at or nearby to the coordinates given for this locality is based on relatively small scale geological maps provided by various national Geological Surveys. This does not necessarily represent the complete geology at this locality but it gives a background for the region in which it is found.

Click on geological units on the map for more information. Click here to view full-screen map on Macrostrat.org

Cenozoic
0 - 66 Ma



ID: 697918
sand plain 38499

Age: Cenozoic (0 - 66 Ma)

Description: Sand or gravel plains; may include some residual alluvium; quartz sand sheets commonly with ferruginous pisoliths or pebbles; local clay, calcrete, laterite, silcrete, silt, colluvium

Comments: regolith; synthesis of multiple published descriptions

Lithology: Regolith

Reference: Raymond, O.L., Liu, S., Gallagher, R., Zhang, W., Highet, L.M. Surface Geology of Australia 1:1 million scale dataset 2012 edition. Commonwealth of Australia (Geoscience Australia). [5]

Paleoproterozoic
1600 - 2500 Ma



ID: 3192844
Paleoproterozoic intrusive rocks

Age: Proterozoic (1600 - 2500 Ma)

Comments: Gawler Craton

Lithology: Intrusive igneous rocks

Reference: Chorlton, L.B. Generalized geology of the world: bedrock domains and major faults in GIS format: a small-scale world geology map with an extended geological attribute database. doi: 10.4095/223767. Geological Survey of Canada, Open File 5529. [154]

Data and map coding provided by Macrostrat.org, used under Creative Commons Attribution 4.0 License



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

Sort by Year (asc) | by Year (desc) | by Author (A-Z) | by Author (Z-A)
SA Geodata Database, Deposit Number: 8294

External Links


 
Mineral and/or Locality  
Mindat.org is an outreach project of the Hudson Institute of Mineralogy, a 501(c)(3) not-for-profit organization. Public Relations by Blytheweigh.
Copyright © mindat.org and the Hudson Institute of Mineralogy 1993-2019, except where stated. Most political location boundaries are © OpenStreetMap contributors. Mindat.org relies on the contributions of thousands of members and supporters.
Privacy Policy - Terms & Conditions - Contact Us Current server date and time: November 13, 2019 20:22:31 Page generated: March 1, 2018 07:21:20
Go to top of page