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โ‡ฑ Shangyou granitic complex, Shangyou Co., Ganzhou, Jiangxi, China


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Shangyou granitic complex, Shangyou Co., Ganzhou, Jiangxi, Chinai
Regional Level Types
Shangyou granitic complexComplex
Shangyou Co.County
GanzhouPrefecture
JiangxiProvince
ChinaCountry

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Latitude & Longitude (WGS84):
25ยฐ 49' 34'' North , 114ยฐ 28' 52'' East
Latitude & Longitude (decimal):
Type:
Kรถppen climate type:
Mindat Locality ID:
447088
Long-form identifier:
mindat:1:2:447088:8
GUID (UUID V4):
0


The generation of ion-adsorbing REE deposits in these different types is suggested to be associated with the REE patterns for the parent granites, as the weathering profile usually inherits the REE patterns of the parent granite. The granites related to the ion-adsorbing REE deposits are mainly generated in the Jurassic to Cretaceous extensional setting, which is induced by the slab foundering and roll-back and subsequent steep subduction of the Paleo-Pacific Ocean slab. In addition, the Early Paleozoic granites also play an important role in generating the ion-adsorbing REE deposits in South China, as the parent granites for ion-adsorbing REE deposits in Shangyou, Yangbu, Ninghua, Weipu, Gutian, and Sanbiao areas are all generated in the Early Paleozoic. The Shangyou granitic complex is in the west of Shangyou City and intruded in the Cambrian metamorphic rocks. The main bodies of the Shangyou granitic complex are biotite granite, while locally occurred muscovite granite around by the biotite granite.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Mineral List


3 valid minerals.

Rock Types Recorded

Note: data is currently VERY limited. Please bear with us while we work towards adding this information!

Select Rock List Type

Alphabetical List Tree Diagram

Detailed Mineral List:

โ“˜ 'Apatite'
Formula: Ca5(PO4)3(Cl/F/OH)
โ“˜ 'Biotite'
Formula: K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
โ“˜ 'Feldspar Group'
โ“˜ 'K Feldspar'
โ“˜ Muscovite
Formula: KAl2(AlSi3O10)(OH)2
โ“˜ 'Plagioclase'
Formula: (Na,Ca)[(Si,Al)AlSi2]O8
โ“˜ Quartz
Formula: SiO2
โ“˜ Zircon
Formula: Zr(SiO4)

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 4 - Oxides and Hydroxides
โ“˜Quartz4.DA.05SiO2
Group 9 - Silicates
โ“˜Zircon9.AD.30Zr(SiO4)
โ“˜Muscovite9.EC.15KAl2(AlSi3O10)(OH)2
Unclassified
โ“˜'Biotite'-K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
โ“˜'Feldspar Group'-
โ“˜'Plagioclase'-(Na,Ca)[(Si,Al)AlSi2]O8
โ“˜'K Feldspar'-
โ“˜'Apatite'-Ca5(PO4)3(Cl/F/OH)

List of minerals for each chemical element

HHydrogen
Hโ“˜ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Hโ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Hโ“˜ ApatiteCa5(PO4)3(Cl/F/OH)
OOxygen
Oโ“˜ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Oโ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Oโ“˜ QuartzSiO2
Oโ“˜ ZirconZr(SiO4)
Oโ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
Oโ“˜ ApatiteCa5(PO4)3(Cl/F/OH)
FFluorine
Fโ“˜ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Fโ“˜ ApatiteCa5(PO4)3(Cl/F/OH)
NaSodium
Naโ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
MgMagnesium
Mgโ“˜ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
AlAluminium
Alโ“˜ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Alโ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Alโ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
SiSilicon
Siโ“˜ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Siโ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Siโ“˜ QuartzSiO2
Siโ“˜ ZirconZr(SiO4)
Siโ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
PPhosphorus
Pโ“˜ ApatiteCa5(PO4)3(Cl/F/OH)
ClChlorine
Clโ“˜ ApatiteCa5(PO4)3(Cl/F/OH)
KPotassium
Kโ“˜ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Kโ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
CaCalcium
Caโ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
Caโ“˜ ApatiteCa5(PO4)3(Cl/F/OH)
TiTitanium
Tiโ“˜ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
FeIron
Feโ“˜ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
ZrZirconium
Zrโ“˜ ZirconZr(SiO4)

Other Regions, Features and Areas containing this locality

AsiaContinent
China
Eurasian Plate
Yangtze PlateTectonic Plate

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References

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