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Dangba deposit, Ke'eryin pegmatite field, Jinchuan Co., Ngawa Autonomous Prefecture (Aba Autonomous Prefecture), Sichuan, China i
Regional Level Types
Dangba deposit Deposit
Ke'eryin pegmatite field Group of Pegmatite Fields
Jinchuan Co. County
Ngawa Autonomous Prefecture (Aba Autonomous Prefecture) Prefecture
Sichuan Province
China Country

Regional Level Types
Dangba deposit	Deposit
Ke'eryin pegmatite field	Group of Pegmatite Fields
Jinchuan Co.	County
Ngawa Autonomous Prefecture (Aba Autonomous Prefecture)	Prefecture
Sichuan	Province
China	Country

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Predictive Mineralogy

Latitude & Longitude (WGS84):

31° 46' North , 102° 1' East

Latitude & Longitude (decimal):

Type:

Köppen climate type:

Cwb : Subtropical highland climate or temperate oceanic climate with dry winters

Mindat Locality ID:

427406

Long-form identifier:

mindat:1:2:427406:6

GUID (UUID V4):

Granitic pegmatite type Cassiterite U-Pb age: 208.1‒199.3 Ma Li2O resources: 660.87×103 t; Li2O grade: 1.34%.

The Dangba LCT pegmatite-type lithium deposit is situated in the southeastern part of the Ke'eryin composite pluton. The exposed stratigraphic units in the mining area include the Zagunao Formation (T3z), Zhuwo Formation (T3zw), and Quaternary deposits (Q). The Zhuwo Formation (T3zw), the most widely distributed unit in the region, accounts for over 95 % of the area and serves as the primary host horizon for mineralized pegmatites. Its protoliths consist of gray, medium- to thin-bedded metamorphic feldspathic quartz sandstone, feldspathic lithic sandstone, and rhythmic interbeds of silty slate and slate. Locally, thick-bedded sandstone intercalated with slate and slate-dominated intervals are observed, with the rhythmic alternation of sandstone and slate representing a distinctive feature of this formation. A total of 11 confirmed ore bodies (Ⅰ,V -VIII, XIV-XVI, XX, XXIV, and XXVI) have been identified in the Dangba mining area. These ore bodies are all hosted within granitic pegmatite dikes. Medium- to small-scale ore bodies within Li-bearing pegmatite dikes generally exhibit full-vein lithium mineralization, resulting in simple morphologies that align closely with the pegmatite dikes. Ore bodies exceeding 500 m in length include VIII, XV, XIV, VI, Ⅶ, and XVI, while those with Li2O resources surpassing 10,000 tonnes comprise V, VI, Ⅶ, VIII, XIV, XV, XVI, and XXIV.

Its status as the largest albite-spodumene pegmatite deposit in Asia, with identified Li resources of 1.12 Mt Li2O at an average grade of 1.33%.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Commodity List

This is a list of exploitable or exploited mineral commodities recorded at this locality.

ⓘ Lithium

Mineral List

21 valid minerals.

Rock Types Recorded

Select Rock List Type

Alphabetical List Tree Diagram

ⓘ Granite

ⓘ Lithic-arenite

ⓘ 'Pegmatite'

ⓘ 'Pegmatitic granite'

ⓘ Sandstone

ⓘ Slate

Detailed Mineral List:

ⓘ Albite

Formula: Na(AlSi₃O₈)

References:

Feng, Dabo; Ran, Fengqin; Peng, Bo; Chen, Hao; Xiong, Changli; Zhao, Yuan; Han, Jingrui (2025) Source of ore-forming materials for the Redamen deposit: Constraints from geochronology and mica geochemistry. Ore Geology Reviews, 186. 106897 doi:10.1016/j.oregeorev.2025.106897

Zhao, Yuan; Ran, Fengqin; Peng, Bo; Feng, Dabo; Yang, Yang; Han, Jingrui; Dai, Yongkun (2026) The contribution of two-stage immiscibility for the formation of lithium-rich pegmatite: Insights from tourmaline in the Ke’eryin region. Ore Geology Reviews, 188. 107051 doi:10.1016/j.oregeorev.2025.107051

Chen, Xiao-Dong; Chen, Bin; Li, Wen-Jing; Tan, Xi-Juan; Zou, Hao; Cao, Hua-Wen; Zhang, Yan; Wang, Qiang; Fei, Guang-Chun; Lai, Xiang; et al. (2026) Li hyper-enrichment in granitic pegmatites driven by preferential partitioning into transitional melt-fluids: Example from the Dangba Li deposit, NW China. Ore Geology Reviews, 196. p.107467. doi:10.1016/j.oregeorev.2026.107467

ⓘ 'Apatite'

Formula: Ca₅(PO₄)₃A

References:

ⓘ Beryl

Formula: Be₃Al₂(Si₆O₁₈)

References:

ⓘ Beusite

Formula: Mn²⁺Mn²⁺₂ (PO₄)₂

References:

ⓘ 'Biotite'

Formula: K(Fe²⁺/Mg)₂(Al/Fe³⁺/Mg/Ti)([Si/Al/Fe]₂Si₂O₁₀)(OH/F)₂

References:

ⓘ Cassiterite

Formula: SnO₂

References:

Zhang, Bo, Qi, Fan-yu, Gao, Xue-zheng, Li, Xiao-lei, Shang, Yun-tao, Kong, Zhao-yu, Jia, Li-qiong, Meng, Jie, Guo, Hui, Fang, Fu-kang, et al. (2022) Geological characteristics, metallogenic regularity, and research progress of lithium deposits in China. China Geology, 5 (4). 734-767

ⓘ 'Columbite-(Fe)-Columbite-(Mn) Series'

References:

ⓘ 'Columbite-Tantalite'

References:

ⓘ Cookeite

Formula: (LiAl₄◻)[AlSi₃O₁₀](OH)₈

References:

ⓘ Cristobalite

Formula: SiO₂

References:

ⓘ Elbaite

Formula: Na(Li_1.5Al_1.5)Al₆(Si₆O₁₈)(BO₃)₃(OH)₃(OH)

References:

ⓘ Fairfieldite

Formula: Ca₂Mn²⁺(PO₄)₂ · 2H₂O

References:

ⓘ 'Feldspar Group'

References:

ⓘ 'Ferberite-Hübnerite Series'

References:

ⓘ 'Lepidolite'

References:

ⓘ Magnetite

Formula: Fe²⁺Fe³⁺₂O₄

References:

ⓘ 'Mica Group'

References:

ⓘ Microcline

Formula: K(AlSi₃O₈)

References:

ⓘ Muscovite

Formula: KAl₂(AlSi₃O₁₀)(OH)₂

References:

ⓘ Nahcolite

Formula: NaHCO₃

References:

ⓘ Orthoclase

Formula: K(AlSi₃O₈)

References:

ⓘ 'Plagioclase'

Formula: (Na,Ca)[(Si,Al)AlSi₂]O₈

References:

ⓘ Polylithionite

Formula: KLi₂Al(Si₄O₁₀)(F,OH)₂

References:

ⓘ Quartz

Formula: SiO₂

References:

ⓘ Rutile

Formula: TiO₂

References:

ⓘ Schorl

Formula: NaFe²⁺₃Al₆(Si₆O₁₈)(BO₃)₃(OH)₃(OH)

References:

ⓘ Spodumene

Formula: LiAlSi₂O₆

References:

ⓘ 'Tantalite'

Formula: (Mn,Fe)(Ta,Nb)₂O₆

References:

ⓘ Titanite

Formula: CaTiO(SiO₄)

References:

ⓘ 'Tourmaline'

Formula: AD₃G₆(T₆O₁₈)(BO₃)₃X₃Z

References:

ⓘ Zabuyelite

Formula: Li₂CO₃

References:

ⓘ Zircon

Formula: Zr(SiO₄)

References:

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 4 - Oxides and Hydroxides
ⓘ	Magnetite	4.BB.05	Fe²⁺Fe³⁺₂O₄
ⓘ	Quartz	4.DA.05	SiO₂
ⓘ	Cristobalite	4.DA.15	SiO₂
ⓘ	Cassiterite	4.DB.05	SnO₂
ⓘ	Rutile	4.DB.05	TiO₂
Group 5 - Nitrates and Carbonates
ⓘ	Zabuyelite	5.AA.05	Li₂CO₃
ⓘ	Nahcolite	5.AA.15	NaHCO₃
Group 8 - Phosphates, Arsenates and Vanadates
ⓘ	Beusite	8.AB.20	Mn²⁺Mn²⁺₂ (PO₄)₂
ⓘ	Fairfieldite	8.CG.05	Ca₂Mn²⁺(PO₄)₂ · 2H₂O
Group 9 - Silicates
ⓘ	Zircon	9.AD.30	Zr(SiO₄)
ⓘ	Titanite	9.AG.15	CaTiO(SiO₄)
ⓘ	Beryl	9.CJ.05	Be₃Al₂(Si₆O₁₈)
ⓘ	Elbaite	9.CK.05	Na(Li_1.5Al_1.5)Al₆(Si₆O₁₈)(BO₃)₃(OH)₃(OH)
ⓘ	Schorl	9.CK.05	NaFe²⁺₃Al₆(Si₆O₁₈)(BO₃)₃(OH)₃(OH)
ⓘ	Spodumene	9.DA.30	LiAlSi₂O₆
ⓘ	Muscovite	9.EC.15	KAl₂(AlSi₃O₁₀)(OH)₂
ⓘ	Polylithionite	9.EC.20	KLi₂Al(Si₄O₁₀)(F,OH)₂
ⓘ	Cookeite	9.EC.55	(LiAl₄◻)[AlSi₃O₁₀](OH)₈
ⓘ	Microcline	9.FA.30	K(AlSi₃O₈)
ⓘ	Orthoclase	9.FA.30	K(AlSi₃O₈)
ⓘ	Albite	9.FA.35	Na(AlSi₃O₈)
Unclassified
ⓘ	'Biotite'	-	K(Fe²⁺/Mg)₂(Al/Fe³⁺/Mg/Ti)([Si/Al/Fe]₂Si₂O₁₀)(OH/F)₂
ⓘ	'Feldspar Group'	-
ⓘ	'Lepidolite'	-
ⓘ	'Tantalite'	-	(Mn,Fe)(Ta,Nb)₂O₆
ⓘ	'Tourmaline'	-	AD₃G₆(T₆O₁₈)(BO₃)₃X₃Z
ⓘ	'Mica Group'	-
ⓘ	'Columbite-(Fe)-Columbite-(Mn) Series'	-
ⓘ	'Plagioclase'	-	(Na,Ca)[(Si,Al)AlSi₂]O₈
ⓘ	'Ferberite-Hübnerite Series'	-
ⓘ	'Columbite-Tantalite'	-
ⓘ	'Apatite'	-	Ca₅(PO₄)₃A

List of minerals for each chemical element

H	Hydrogen
H	ⓘ Biotite	K(Fe²⁺/Mg)₂(Al/Fe³⁺/Mg/Ti)([Si/Al/Fe]₂Si₂O₁₀)(OH/F)₂
H	ⓘ Cookeite	(LiAl₄◻)[AlSi₃O₁₀](OH)₈
H	ⓘ Elbaite	Na(Li_1.5Al_1.5)Al₆(Si₆O₁₈)(BO₃)₃(OH)₃(OH)
H	ⓘ Fairfieldite	Ca₂Mn²⁺(PO₄)₂ · 2H₂O
H	ⓘ Muscovite	KAl₂(AlSi₃O₁₀)(OH)₂
H	ⓘ Nahcolite	NaHCO₃
H	ⓘ Polylithionite	KLi₂Al(Si₄O₁₀)(F,OH)₂
H	ⓘ Schorl	NaFe₃²⁺Al₆(Si₆O₁₈)(BO₃)₃(OH)₃(OH)
Li	Lithium
Li	ⓘ Cookeite	(LiAl₄◻)[AlSi₃O₁₀](OH)₈
Li	ⓘ Elbaite	Na(Li_1.5Al_1.5)Al₆(Si₆O₁₈)(BO₃)₃(OH)₃(OH)
Li	ⓘ Polylithionite	KLi₂Al(Si₄O₁₀)(F,OH)₂
Li	ⓘ Spodumene	LiAlSi₂O₆
Li	ⓘ Zabuyelite	Li₂CO₃
Be	Beryllium
Be	ⓘ Beryl	Be₃Al₂(Si₆O₁₈)
B	Boron
B	ⓘ Elbaite	Na(Li_1.5Al_1.5)Al₆(Si₆O₁₈)(BO₃)₃(OH)₃(OH)
B	ⓘ Schorl	NaFe₃²⁺Al₆(Si₆O₁₈)(BO₃)₃(OH)₃(OH)
B	ⓘ Tourmaline	AD₃G₆(T₆O₁₈)(BO₃)₃X₃Z
C	Carbon
C	ⓘ Nahcolite	NaHCO₃
C	ⓘ Zabuyelite	Li₂CO₃
O	Oxygen
O	ⓘ Albite	Na(AlSi₃O₈)
O	ⓘ Beusite	Mn²⁺Mn₂²⁺ (PO₄)₂
O	ⓘ Biotite	K(Fe²⁺/Mg)₂(Al/Fe³⁺/Mg/Ti)([Si/Al/Fe]₂Si₂O₁₀)(OH/F)₂
O	ⓘ Beryl	Be₃Al₂(Si₆O₁₈)
O	ⓘ Cassiterite	SnO₂
O	ⓘ Cookeite	(LiAl₄◻)[AlSi₃O₁₀](OH)₈
O	ⓘ Cristobalite	SiO₂
O	ⓘ Elbaite	Na(Li_1.5Al_1.5)Al₆(Si₆O₁₈)(BO₃)₃(OH)₃(OH)
O	ⓘ Fairfieldite	Ca₂Mn²⁺(PO₄)₂ · 2H₂O
O	ⓘ Magnetite	Fe²⁺Fe₂³⁺O₄
O	ⓘ Microcline	K(AlSi₃O₈)
O	ⓘ Muscovite	KAl₂(AlSi₃O₁₀)(OH)₂
O	ⓘ Nahcolite	NaHCO₃
O	ⓘ Orthoclase	K(AlSi₃O₈)
O	ⓘ Polylithionite	KLi₂Al(Si₄O₁₀)(F,OH)₂
O	ⓘ Quartz	SiO₂
O	ⓘ Rutile	TiO₂
O	ⓘ Schorl	NaFe₃²⁺Al₆(Si₆O₁₈)(BO₃)₃(OH)₃(OH)
O	ⓘ Spodumene	LiAlSi₂O₆
O	ⓘ Tantalite	(Mn,Fe)(Ta,Nb)₂O₆
O	ⓘ Titanite	CaTiO(SiO₄)
O	ⓘ Tourmaline	AD₃G₆(T₆O₁₈)(BO₃)₃X₃Z
O	ⓘ Zabuyelite	Li₂CO₃
O	ⓘ Zircon	Zr(SiO₄)
O	ⓘ Columbite-(Fe)-Columbite-(Mn) Series
O	ⓘ Plagioclase	(Na,Ca)[(Si,Al)AlSi₂]O₈
O	ⓘ Ferberite-Hübnerite Series
O	ⓘ Apatite	Ca₅(PO₄)₃A
F	Fluorine
F	ⓘ Biotite	K(Fe²⁺/Mg)₂(Al/Fe³⁺/Mg/Ti)([Si/Al/Fe]₂Si₂O₁₀)(OH/F)₂
F	ⓘ Polylithionite	KLi₂Al(Si₄O₁₀)(F,OH)₂
Na	Sodium
Na	ⓘ Albite	Na(AlSi₃O₈)
Na	ⓘ Elbaite	Na(Li_1.5Al_1.5)Al₆(Si₆O₁₈)(BO₃)₃(OH)₃(OH)
Na	ⓘ Nahcolite	NaHCO₃
Na	ⓘ Schorl	NaFe₃²⁺Al₆(Si₆O₁₈)(BO₃)₃(OH)₃(OH)
Na	ⓘ Plagioclase	(Na,Ca)[(Si,Al)AlSi₂]O₈
Mg	Magnesium
Mg	ⓘ Biotite	K(Fe²⁺/Mg)₂(Al/Fe³⁺/Mg/Ti)([Si/Al/Fe]₂Si₂O₁₀)(OH/F)₂
Al	Aluminium
Al	ⓘ Albite	Na(AlSi₃O₈)
Al	ⓘ Biotite	K(Fe²⁺/Mg)₂(Al/Fe³⁺/Mg/Ti)([Si/Al/Fe]₂Si₂O₁₀)(OH/F)₂
Al	ⓘ Beryl	Be₃Al₂(Si₆O₁₈)
Al	ⓘ Cookeite	(LiAl₄◻)[AlSi₃O₁₀](OH)₈
Al	ⓘ Elbaite	Na(Li_1.5Al_1.5)Al₆(Si₆O₁₈)(BO₃)₃(OH)₃(OH)
Al	ⓘ Microcline	K(AlSi₃O₈)
Al	ⓘ Muscovite	KAl₂(AlSi₃O₁₀)(OH)₂
Al	ⓘ Orthoclase	K(AlSi₃O₈)
Al	ⓘ Polylithionite	KLi₂Al(Si₄O₁₀)(F,OH)₂
Al	ⓘ Schorl	NaFe₃²⁺Al₆(Si₆O₁₈)(BO₃)₃(OH)₃(OH)
Al	ⓘ Spodumene	LiAlSi₂O₆
Al	ⓘ Plagioclase	(Na,Ca)[(Si,Al)AlSi₂]O₈
Si	Silicon
Si	ⓘ Albite	Na(AlSi₃O₈)
Si	ⓘ Biotite	K(Fe²⁺/Mg)₂(Al/Fe³⁺/Mg/Ti)([Si/Al/Fe]₂Si₂O₁₀)(OH/F)₂
Si	ⓘ Beryl	Be₃Al₂(Si₆O₁₈)
Si	ⓘ Cookeite	(LiAl₄◻)[AlSi₃O₁₀](OH)₈
Si	ⓘ Cristobalite	SiO₂
Si	ⓘ Elbaite	Na(Li_1.5Al_1.5)Al₆(Si₆O₁₈)(BO₃)₃(OH)₃(OH)
Si	ⓘ Microcline	K(AlSi₃O₈)
Si	ⓘ Muscovite	KAl₂(AlSi₃O₁₀)(OH)₂
Si	ⓘ Orthoclase	K(AlSi₃O₈)
Si	ⓘ Polylithionite	KLi₂Al(Si₄O₁₀)(F,OH)₂
Si	ⓘ Quartz	SiO₂
Si	ⓘ Schorl	NaFe₃²⁺Al₆(Si₆O₁₈)(BO₃)₃(OH)₃(OH)
Si	ⓘ Spodumene	LiAlSi₂O₆
Si	ⓘ Titanite	CaTiO(SiO₄)
Si	ⓘ Zircon	Zr(SiO₄)
Si	ⓘ Plagioclase	(Na,Ca)[(Si,Al)AlSi₂]O₈
P	Phosphorus
P	ⓘ Beusite	Mn²⁺Mn₂²⁺ (PO₄)₂
P	ⓘ Fairfieldite	Ca₂Mn²⁺(PO₄)₂ · 2H₂O
P	ⓘ Apatite	Ca₅(PO₄)₃A
K	Potassium
K	ⓘ Biotite	K(Fe²⁺/Mg)₂(Al/Fe³⁺/Mg/Ti)([Si/Al/Fe]₂Si₂O₁₀)(OH/F)₂
K	ⓘ Microcline	K(AlSi₃O₈)
K	ⓘ Muscovite	KAl₂(AlSi₃O₁₀)(OH)₂
K	ⓘ Orthoclase	K(AlSi₃O₈)
K	ⓘ Polylithionite	KLi₂Al(Si₄O₁₀)(F,OH)₂
Ca	Calcium
Ca	ⓘ Fairfieldite	Ca₂Mn²⁺(PO₄)₂ · 2H₂O
Ca	ⓘ Titanite	CaTiO(SiO₄)
Ca	ⓘ Plagioclase	(Na,Ca)[(Si,Al)AlSi₂]O₈
Ca	ⓘ Apatite	Ca₅(PO₄)₃A
Ti	Titanium
Ti	ⓘ Biotite	K(Fe²⁺/Mg)₂(Al/Fe³⁺/Mg/Ti)([Si/Al/Fe]₂Si₂O₁₀)(OH/F)₂
Ti	ⓘ Rutile	TiO₂
Ti	ⓘ Titanite	CaTiO(SiO₄)
Mn	Manganese
Mn	ⓘ Beusite	Mn²⁺Mn₂²⁺ (PO₄)₂
Mn	ⓘ Fairfieldite	Ca₂Mn²⁺(PO₄)₂ · 2H₂O
Mn	ⓘ Tantalite	(Mn,Fe)(Ta,Nb)₂O₆
Mn	ⓘ Columbite-(Fe)-Columbite-(Mn) Series
Mn	ⓘ Ferberite-Hübnerite Series
Fe	Iron
Fe	ⓘ Biotite	K(Fe²⁺/Mg)₂(Al/Fe³⁺/Mg/Ti)([Si/Al/Fe]₂Si₂O₁₀)(OH/F)₂
Fe	ⓘ Magnetite	Fe²⁺Fe₂³⁺O₄
Fe	ⓘ Schorl	NaFe₃²⁺Al₆(Si₆O₁₈)(BO₃)₃(OH)₃(OH)
Fe	ⓘ Tantalite	(Mn,Fe)(Ta,Nb)₂O₆
Fe	ⓘ Columbite-(Fe)-Columbite-(Mn) Series
Fe	ⓘ Ferberite-Hübnerite Series
Zr	Zirconium
Zr	ⓘ Zircon	Zr(SiO₄)
Nb	Niobium
Nb	ⓘ Tantalite	(Mn,Fe)(Ta,Nb)₂O₆
Nb	ⓘ Columbite-(Fe)-Columbite-(Mn) Series
Sn	Tin
Sn	ⓘ Cassiterite	SnO₂
Ta	Tantalum
Ta	ⓘ Tantalite	(Mn,Fe)(Ta,Nb)₂O₆
W	Tungsten
W	ⓘ Ferberite-Hübnerite Series

Other Regions, Features and Areas containing this locality

AsiaContinent

Hindukush Himalayan RegionGroup of Mountain Ranges

China

Songpan-Ganzi Li Mineral BeltMineral Belt
⭔Southwest ChinaRegion

Eurasian PlateTectonic Plate

Songpan-Ganzi Hoh-Xil TerraneOrogenic Belt

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

Li, Xin, Dai, Hongzhang, Wang, Denghong, Liu, Shanbao, Wang, Genhou, Wang, Chenghui, Huang, Fan, Zhu, Haiyang (2022) Geochronological and geochemical constraints on magmatic evolution and mineralization of the northeast Ke’eryin pluton and the newly discovered Jiada pegmatite-type lithium deposit, Western China. Ore Geology Reviews, 105164

[1]Zhao, Yuan; Ran, Fengqin; Peng, Bo; Feng, Dabo; Yang, Yang; Han, Jingrui; Dai, Yongkun (2026) The contribution of two-stage immiscibility for the formation of lithium-rich pegmatite: Insights from tourmaline in the Ke’eryin region. Ore Geology Reviews, 188. 107051 doi:10.1016/j.oregeorev.2025.107051

[2]Chen, Xiao-Dong; Chen, Bin; Li, Wen-Jing; Tan, Xi-Juan; Zou, Hao; Cao, Hua-Wen; Zhang, Yan; Wang, Qiang; Fei, Guang-Chun; Lai, Xiang; et al. (2026) Li hyper-enrichment in granitic pegmatites driven by preferential partitioning into transitional melt-fluids: Example from the Dangba Li deposit, NW China. Ore Geology Reviews, 196. p.107467. doi:10.1016/j.oregeorev.2026.107467

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