IMPORTANT MESSAGE. We need your support now to keep mindat.org running. Click here to find out why.
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 Educators
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 CompaniesStatisticsThe ElementsUsersBooks & MagazinesMineral MuseumsMineral Shows & EventsThe Mindat DirectoryDevice Settings
Photo SearchPhoto GalleriesNew Photos TodayNew Photos YesterdayMembers' Photo GalleriesPast Photo of the Day Gallery

Jinyinzhai Mine (Chenxian Mine; Sanerlin Mine; U deposit No. 320), Suxian District, Chenzhou Prefecture, Hunan Province, China

This page is currently not sponsored. Click here to sponsor this page.
 
Location is approximate, estimate based on other nearby localities.
 
Latitude & Longitude (WGS84): 25° North , 113° East (est.)
Margin of Error:~35km
Köppen climate type:Cfa : Humid subtropical climate


Lower Tertiary hydrothermal-reworked uranium deposit of so-called C-Si-pelite type, hosted in black siliceous and carbonaceous shales of the Upper Permian Dangchong formation that are interstratified with quartz sandstone and thin coal beds. The irregular breccia-vein ore bodies are separately hosted in the cores of three secondary anticlines. They consist of uraniferous quartz veins and fragments of black silicified shale and sandstone that are cemented by quartz and minor calcite.

Located in the Xiang river (Xiang Jiang) valley near Chenzhou. Jinyinzhai was the first Chinese uranium mine. It was started in 1962.


Note:
In Chinese, "Sanerlin" means "320".


Mineral List


31 valid minerals. 1 (TL) - type locality of valid minerals.

Rock Types Recorded

Note: this is a very new system on mindat.org and data is currently VERY limited. Please bear with us while we work towards adding this information!

Select Rock List Type

Alphabetical List Tree Diagram


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)
Damao Wu and Yansong Tan (1981): New data on hawleyite. Geology and Prospecting 17(9), 34-36.
Jianwei Li, Meifou Zhou, Xianfu Li, Zijin Li, and Zhaoren Fu (2002): Origin of a large breccia-vein system in the Sanerlin uranium deposit, southern China: a reinterpretation. Mineralium Deposita 37, 213-225.
Jianwei Li, Meifu Zhou, Xianfu Li, Zhaoren Fu, and Zijin Li (2002): Structural control on uranium mineralization in South China: Implications for fluid flow in continental strike-slip faults. Science in China, Series D (Earth Sciences), 45(9), 851-864.
Dahlkamp, F.J., Ed. (2009): Uranium Deposits of the World. Springer (Berlin, Heidelberg), pp. 31-156.

Mineral and/or Locality  
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 1993-2018, except where stated. Mindat.org relies on the contributions of thousands of members and supporters.
Privacy Policy - Terms & Conditions - Contact Us Current server date and time: November 16, 2018 11:57:40 Page generated: January 13, 2018 22:43:29
Go to top of page