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Guangzitian U deposit, Quanzhou Uranium ore field, Quanzhou Co., Guilin, Guangxi, Chinai
Regional Level Types
Guangzitian U depositDeposit
Quanzhou Uranium ore fieldOre Field
Quanzhou Co.County
GuilinPrefecture-level City
GuangxiAutonomous Region
ChinaCountry

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Latitude & Longitude (WGS84):
26° North , 110° East (est.)
Estimate based on other nearby localities or region boundaries.
Margin of Error:
~1km
Type:
Köppen climate type:
Mindat Locality ID:
225832
Long-form identifier:
mindat:1:2:225832:7
GUID (UUID V4):
ad11d189-fc3d-41cd-9ad2-87c1b91541f9
Name(s) in local language(s):
广子田铀矿床, 兴安铀矿田, 兴安县, 桂林市, 广西壮族自治区, 中国


Hydrothermal-reworked C-Si-pelite-type uranium deposit, hosted in Devonian dolomitic pelite, pelitic dolomite and pelitic limestone to the east of the Yuechengling granitic massif.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Mineral List


2 valid minerals.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 4 - Oxides and Hydroxides
Uraninite4.DL.05UO2
var. Pitchblende4.DL.05UO2
Group 5 - Nitrates and Carbonates
Dolomite5.AB.10CaMg(CO3)2

List of minerals for each chemical element

CCarbon
C DolomiteCaMg(CO3)2
OOxygen
O DolomiteCaMg(CO3)2
O Uraninite var. PitchblendeUO2
O UraniniteUO2
MgMagnesium
Mg DolomiteCaMg(CO3)2
CaCalcium
Ca DolomiteCaMg(CO3)2
UUranium
U Uraninite var. PitchblendeUO2
U UraniniteUO2

Other Regions, Features and Areas containing this locality

AsiaContinent
China
Yangtze 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  
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