Help|Log In|Register|
Home PageMindat NewsThe Mindat ManualHistory of MindatCopyright StatusManagement TeamContact UsAdvertise on Mindat
Donate to MindatSponsor a PageSponsored PagesTop Available PagesMindat AdvertisersAdvertise on MindatThe Mindat Store
Minerals by PropertiesMinerals by ChemistryRandom MineralSearch by minIDLocalities Near MeSearch GlossaryMore Search Options
Search For:
Mineral Name:
Locality Name:
The Mindat ManualAdd a New PhotoRate PhotosLocality Edit ReportAdd Glossary Item
StatisticsMember ListBooks & MagazinesMineral Shows & EventsThe Mindat DirectoryHow to Link to MindatDevice Settings
Photo SearchPhoto GalleriesNew Photos TodayNew Photos YesterdayMembers' Photo GalleriesPast Photo of the Day Gallery

Maoantan pegmatite field, Quanzhou Co., Guilin Prefecture, Guangxi Zhuang Autonomous Region, China

This page is currently not sponsored. Click here to sponsor this page.
Granite pegmatite dykes with polymetallic rare-metal mineralizations (Ta-Nb-Zr-Hf-Be-Sn-W and minor U), hosted in volcaniclastic rocks of the Proterozoic Danzhou group along NE-trending second-order fractures within a narrow stretch of land between two NNE-trending shear zones along the eastern margin of a composite batholith, which is composed mainly of Caledonian medium-grained porphyritic biotite granite. The pegmatites are poorly differentiated and do not exhibit zoning phenomenons, but there is zoning observed within the field in that the tantalum, niobium and tin grades increase from the north to the south.

The pegmatite field forms part of a U-W-Mo-Sn mineralization belt that extends for more than 100 km between Luzhai County of Liuzhou Prefecture and Quanzhou County of Guilin Prefecture. Within this belt, more than 50 deposits were discovered that cover a wide range of genetic types, including magmatic, pegmatite and skarn mineralizations, tin-bearing placers, and hydrothermal deposits formed at high to low temperatures.

NOTE: Li and Zhang (1995) refer to this locality as an undisclosed pegmatite deposit "in some area of Guangxi", but they provide geological details that are very obviously the same as those provided by other authors for the Quanzhou ore field and the tin-tungsten deposits in Guanyang County, which all form part of the same metallogenic zone. The name of the pegmatite field and the grid reference are taken from the report by Kamitani et al. (2007).

Mineral List

32 entries listed. 23 valid minerals.

The above list contains all mineral locality references listed on 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 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.


- Renke Li and Xuming Zhang (1995): Characteristics of Ta-Nb-Be granite pegmatite deposit in some area of Guangxi. Geology and Prospecting 31(6), 15-22.
- Kamitani, M., Okumura, K., Teraoka, Y., Miyano, S., and Watanabe, Y. (2007): Mineral Resources Map of East Asia. Geological Survey of Japan.

Mineral and/or Locality is an outreach project of the Hudson Institute of Mineralogy, a 501(c)(3) not-for-profit organization.
Copyright © and the Hudson Institute of Mineralogy 1993-2015, except where stated. relies on the contributions of thousands of members and supporters.
Privacy Policy - Terms & Conditions - Contact Us Current server date and time: October 7, 2015 09:05:45 Page generated: June 10, 2015 02:38:45