The Qiuguobi gold deposit is a recently identified gold deposit of silicified fractured altered rock-type within the Yalujiang metallogenic belt, with proven gold resources of ∼9.6 t at an average grade of 3.2 g/t. Exposed lithological units in the mining area exhibit a banded distribution and are dominated by the Paleoproterozoic Li’eryu (Pt1lr), Gaojiayu (Pt1ghyp), and Gaixian formations (Pt1gx) of the Liaohe Group, together with Cenozoic Quaternary deposits (Q). The Gaixian Formation outcrops in the northern and central mining area and consists predominantly of low-grade metamorphic clastic rocks, in which biotite schist is the dominant lithology. This unit constitutes the principal wall rock hosting the gold orebodies. The orebodies of the Qiuguobi gold deposit occur exclusively within biotite schist of the Paleoproterozoic Gaixian Formation of the Liaohe Group. They are predominantly vein-like and lenticular in morphology, with some exhibiting branching and merging characteristics. Their distribution is closely controlled by ore-bearing fracture zones and lamprophyre dikes and is characterized by discontinuous extension. The ore-bearing fracture zones are 2–8 m wide and display well-developed silicification and pyritization. Orebody thickness and gold grade increase significantly at the intersections between fracture zones and lamprophyre dikes.
The first stage is the quartz–pyrite stage (Stage 1), representing the earliest mineralization event. The second stage is the quartz–polymetallic sulfide stage (Stage 2). Smoky-gray polymetallic sulfide veinlets approximately 1-cm-wide crosscut the earlier milky-white quartz veins, and oxidation of chalcopyrite to malachite is observed in field outcrops. The third stage is the quartz–ankerite–polymetallic sulfide stage (Stage 3), which mainly occurs as hydrothermal breccia within fracture zones and represents the principal ore-bearing style of the Qiuguobi gold deposit. It is characterized by breccias formed through tectonic fragmentation of earlier quartz–sulfide veins and wall rocks, subsequently filled and cemented by quartz–ankerite–polymetallic sulfide assemblages. The fourth stage is the calcite–quartz stage (Stage 4). Calcite–quartz veinlets crosscut the hydrothermal breccias formed during Stage 3.

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Standard Detailed Gallery Strunz Chemical Elements

Commodity List

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

ⓘ Gold

Mineral List

19 valid minerals.

Rock Types Recorded

Select Rock List Type

Alphabetical List Tree Diagram

ⓘ 'Hydrothermal breccia'

Detailed Mineral List:

ⓘ Acanthite

Formula: Ag₂S

References:

Sun, Nantian; Chen, Peiwen; Chen, Hui; Shi, Chuang; Wu, Songsong; Zeng, Qingdong; Sun, Guotao; Fu, Yong; Yu, Bing (2026) Geological characteristics and genesis of the Qiuguobi gold deposit in the Liaodong Peninsula, NE China: Constraints from in situ sulfide geochemistry and monazite U–Pb geochronology. Ore Geology Reviews, 197. p.107531. doi:10.1016/j.oregeorev.2026.107531

ⓘ Ankerite

Formula: Ca(Fe²⁺,Mg)(CO₃)₂

References:

ⓘ 'Apatite'

Formula: Ca₅(PO₄)₃A

References:

ⓘ Arsenopyrite

Formula: FeAsS

References:

ⓘ Azurite

Formula: Cu₃(CO₃)₂(OH)₂

References:

ⓘ Baryte

Formula: BaSO₄

References:

ⓘ 'Biotite'

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

References:

ⓘ Calcite

Formula: CaCO₃

References:

ⓘ 'Calcium Amphibole Subgroup'

Formula: A_nCa₂(C²⁺_5-mC³⁺_m)(Si_8-(n+m)Al_(n+m))W₂

References:

ⓘ 'Calcium Amphibole Subgroup var. Hornblende'

Formula: A_nCa₂(Z²⁺_5-mZ³⁺_m)(Si_8-(n+m)Al_(n+m))(OH,F,Cl)₂

References:

ⓘ Chalcocite

Formula: Cu₂S

References:

ⓘ Chalcopyrite

Formula: CuFeS₂

References:

ⓘ Galena

Formula: PbS

References:

ⓘ Gersdorffite

Formula: NiAsS

References:

ⓘ Malachite

Formula: Cu₂(CO₃)(OH)₂

References:

ⓘ Millerite

Formula: NiS

References:

ⓘ 'Monazite Group'

Formula: REE(PO₄)

References:

ⓘ Native Gold

Formula: Au

References:

ⓘ Native Silver

Formula: Ag

References:

ⓘ 'Plagioclase'

Formula: (Na,Ca)[(Si,Al)AlSi₂]O₈

References:

ⓘ Pyrite

Formula: FeS₂

References:

ⓘ Quartz

Formula: SiO₂

References:

ⓘ Rutile

Formula: TiO₂

References:

ⓘ Siderite

Formula: FeCO₃

References:

ⓘ Sphalerite

Formula: ZnS

References:

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
ⓘ	Native Gold	1.AA.05	Au
ⓘ	Native Silver	1.AA.05	Ag
Group 2 - Sulphides and Sulfosalts
ⓘ	Chalcocite	2.BA.05	Cu₂S
ⓘ	Acanthite	2.BA.35	Ag₂S
ⓘ	Sphalerite	2.CB.05a	ZnS
ⓘ	Chalcopyrite	2.CB.10a	CuFeS₂
ⓘ	Millerite	2.CC.20	NiS
ⓘ	Galena	2.CD.10	PbS
ⓘ	Pyrite	2.EB.05a	FeS₂
ⓘ	Arsenopyrite	2.EB.20	FeAsS
ⓘ	Gersdorffite	2.EB.25	NiAsS
Group 4 - Oxides and Hydroxides
ⓘ	Quartz	4.DA.05	SiO₂
ⓘ	Rutile	4.DB.05	TiO₂
Group 5 - Nitrates and Carbonates
ⓘ	Calcite	5.AB.05	CaCO₃
ⓘ	Siderite	5.AB.05	FeCO₃
ⓘ	Ankerite	5.AB.10	Ca(Fe²⁺,Mg)(CO₃)₂
ⓘ	Azurite	5.BA.05	Cu₃(CO₃)₂(OH)₂
ⓘ	Malachite	5.BA.10	Cu₂(CO₃)(OH)₂
Group 7 - Sulphates, Chromates, Molybdates and Tungstates
ⓘ	Baryte	7.AD.35	BaSO₄
Unclassified
ⓘ	'Biotite'	-	K(Fe²⁺/Mg)₂(Al/Fe³⁺/Mg/Ti)([Si/Al/Fe]₂Si₂O₁₀)(OH/F)₂
ⓘ	'Calcium Amphibole Subgroup var. Hornblende'	-	A_nCa₂(Z²⁺_5-mZ³⁺_m)(Si_8-(n+m)Al_(n+m))(OH,F,Cl)₂
ⓘ	'Monazite Group'	-	REE(PO₄)
ⓘ	'Plagioclase'	-	(Na,Ca)[(Si,Al)AlSi₂]O₈
ⓘ	'Apatite'	-	Ca₅(PO₄)₃A
ⓘ	'Calcium Amphibole Subgroup'	-	A_nCa₂(C²⁺_5-mC³⁺_m)(Si_8-(n+m)Al_(n+m))W₂

List of minerals for each chemical element

H	Hydrogen
H	ⓘ Azurite	Cu₃(CO₃)₂(OH)₂
H	ⓘ Biotite	K(Fe²⁺/Mg)₂(Al/Fe³⁺/Mg/Ti)([Si/Al/Fe]₂Si₂O₁₀)(OH/F)₂
H	ⓘ Calcium Amphibole Subgroup var. Hornblende	A_nCa₂(Z²⁺_5-mZ_m³⁺)(Si_8-(n+m)Al_(n+m))(OH,F,Cl)₂
H	ⓘ Malachite	Cu₂(CO₃)(OH)₂
C	Carbon
C	ⓘ Ankerite	Ca(Fe²⁺,Mg)(CO₃)₂
C	ⓘ Azurite	Cu₃(CO₃)₂(OH)₂
C	ⓘ Calcite	CaCO₃
C	ⓘ Malachite	Cu₂(CO₃)(OH)₂
C	ⓘ Siderite	FeCO₃
O	Oxygen
O	ⓘ Ankerite	Ca(Fe²⁺,Mg)(CO₃)₂
O	ⓘ Azurite	Cu₃(CO₃)₂(OH)₂
O	ⓘ Baryte	BaSO₄
O	ⓘ Biotite	K(Fe²⁺/Mg)₂(Al/Fe³⁺/Mg/Ti)([Si/Al/Fe]₂Si₂O₁₀)(OH/F)₂
O	ⓘ Calcite	CaCO₃
O	ⓘ Calcium Amphibole Subgroup var. Hornblende	A_nCa₂(Z²⁺_5-mZ_m³⁺)(Si_8-(n+m)Al_(n+m))(OH,F,Cl)₂
O	ⓘ Malachite	Cu₂(CO₃)(OH)₂
O	ⓘ Monazite Group	REE(PO₄)
O	ⓘ Quartz	SiO₂
O	ⓘ Rutile	TiO₂
O	ⓘ Siderite	FeCO₃
O	ⓘ Plagioclase	(Na,Ca)[(Si,Al)AlSi₂]O₈
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	ⓘ Calcium Amphibole Subgroup var. Hornblende	A_nCa₂(Z²⁺_5-mZ_m³⁺)(Si_8-(n+m)Al_(n+m))(OH,F,Cl)₂
Na	Sodium
Na	ⓘ Plagioclase	(Na,Ca)[(Si,Al)AlSi₂]O₈
Mg	Magnesium
Mg	ⓘ Ankerite	Ca(Fe²⁺,Mg)(CO₃)₂
Mg	ⓘ Biotite	K(Fe²⁺/Mg)₂(Al/Fe³⁺/Mg/Ti)([Si/Al/Fe]₂Si₂O₁₀)(OH/F)₂
Al	Aluminium
Al	ⓘ Biotite	K(Fe²⁺/Mg)₂(Al/Fe³⁺/Mg/Ti)([Si/Al/Fe]₂Si₂O₁₀)(OH/F)₂
Al	ⓘ Calcium Amphibole Subgroup var. Hornblende	A_nCa₂(Z²⁺_5-mZ_m³⁺)(Si_8-(n+m)Al_(n+m))(OH,F,Cl)₂
Al	ⓘ Plagioclase	(Na,Ca)[(Si,Al)AlSi₂]O₈
Al	ⓘ Calcium Amphibole Subgroup	A_nCa₂(C²⁺_5-mC_m³⁺)(Si_8-(n+m)Al_(n+m))W₂
Si	Silicon
Si	ⓘ Biotite	K(Fe²⁺/Mg)₂(Al/Fe³⁺/Mg/Ti)([Si/Al/Fe]₂Si₂O₁₀)(OH/F)₂
Si	ⓘ Calcium Amphibole Subgroup var. Hornblende	A_nCa₂(Z²⁺_5-mZ_m³⁺)(Si_8-(n+m)Al_(n+m))(OH,F,Cl)₂
Si	ⓘ Quartz	SiO₂
Si	ⓘ Plagioclase	(Na,Ca)[(Si,Al)AlSi₂]O₈
Si	ⓘ Calcium Amphibole Subgroup	A_nCa₂(C²⁺_5-mC_m³⁺)(Si_8-(n+m)Al_(n+m))W₂
P	Phosphorus
P	ⓘ Monazite Group	REE(PO₄)
P	ⓘ Apatite	Ca₅(PO₄)₃A
S	Sulfur
S	ⓘ Acanthite	Ag₂S
S	ⓘ Arsenopyrite	FeAsS
S	ⓘ Baryte	BaSO₄
S	ⓘ Chalcopyrite	CuFeS₂
S	ⓘ Chalcocite	Cu₂S
S	ⓘ Galena	PbS
S	ⓘ Gersdorffite	NiAsS
S	ⓘ Millerite	NiS
S	ⓘ Pyrite	FeS₂
S	ⓘ Sphalerite	ZnS
Cl	Chlorine
Cl	ⓘ Calcium Amphibole Subgroup var. Hornblende	A_nCa₂(Z²⁺_5-mZ_m³⁺)(Si_8-(n+m)Al_(n+m))(OH,F,Cl)₂
K	Potassium
K	ⓘ Biotite	K(Fe²⁺/Mg)₂(Al/Fe³⁺/Mg/Ti)([Si/Al/Fe]₂Si₂O₁₀)(OH/F)₂
Ca	Calcium
Ca	ⓘ Ankerite	Ca(Fe²⁺,Mg)(CO₃)₂
Ca	ⓘ Calcite	CaCO₃
Ca	ⓘ Calcium Amphibole Subgroup var. Hornblende	A_nCa₂(Z²⁺_5-mZ_m³⁺)(Si_8-(n+m)Al_(n+m))(OH,F,Cl)₂
Ca	ⓘ Plagioclase	(Na,Ca)[(Si,Al)AlSi₂]O₈
Ca	ⓘ Apatite	Ca₅(PO₄)₃A
Ca	ⓘ Calcium Amphibole Subgroup	A_nCa₂(C²⁺_5-mC_m³⁺)(Si_8-(n+m)Al_(n+m))W₂
Ti	Titanium
Ti	ⓘ Biotite	K(Fe²⁺/Mg)₂(Al/Fe³⁺/Mg/Ti)([Si/Al/Fe]₂Si₂O₁₀)(OH/F)₂
Ti	ⓘ Rutile	TiO₂
Fe	Iron
Fe	ⓘ Ankerite	Ca(Fe²⁺,Mg)(CO₃)₂
Fe	ⓘ Arsenopyrite	FeAsS
Fe	ⓘ Biotite	K(Fe²⁺/Mg)₂(Al/Fe³⁺/Mg/Ti)([Si/Al/Fe]₂Si₂O₁₀)(OH/F)₂
Fe	ⓘ Chalcopyrite	CuFeS₂
Fe	ⓘ Pyrite	FeS₂
Fe	ⓘ Siderite	FeCO₃
Ni	Nickel
Ni	ⓘ Gersdorffite	NiAsS
Ni	ⓘ Millerite	NiS
Cu	Copper
Cu	ⓘ Azurite	Cu₃(CO₃)₂(OH)₂
Cu	ⓘ Chalcopyrite	CuFeS₂
Cu	ⓘ Chalcocite	Cu₂S
Cu	ⓘ Malachite	Cu₂(CO₃)(OH)₂
Zn	Zinc
Zn	ⓘ Sphalerite	ZnS
As	Arsenic
As	ⓘ Arsenopyrite	FeAsS
As	ⓘ Gersdorffite	NiAsS
Ag	Silver
Ag	ⓘ Acanthite	Ag₂S
Ag	ⓘ Native Silver	Ag
Ba	Barium
Ba	ⓘ Baryte	BaSO₄
Au	Gold
Au	ⓘ Native Gold	Au
Pb	Lead
Pb	ⓘ Galena	PbS

Other Regions, Features and Areas containing this locality

Amur PlateTectonic Plate

AsiaContinent

Eurasian Plate

North China CratonOrogen
- Eastern Block
  - Jiao-Liao-Ji BeltOrogenic Belt

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References

[1]Sun, Nantian; Chen, Peiwen; Chen, Hui; Shi, Chuang; Wu, Songsong; Zeng, Qingdong; Sun, Guotao; Fu, Yong; Yu, Bing (2026) Geological characteristics and genesis of the Qiuguobi gold deposit in the Liaodong Peninsula, NE China: Constraints from in situ sulfide geochemistry and monazite U–Pb geochronology. Ore Geology Reviews, 197. p.107531. doi:10.1016/j.oregeorev.2026.107531

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Qiuguobi Au deposit, Kuandian County, Dandong, Liaoning, ChinaiRegional Level TypesQiuguobi Au depositDeposit Kuandian CountyCounty DandongPrefecture-level City LiaoningProvince ChinaCountry function showexplain() { $("#locexplain").toggle(); if (typeof movemap === "function") movemap(); }

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Detailed Mineral List:

Gallery:

List of minerals arranged by Strunz 10th Edition classification

List of minerals for each chemical element

Other Regions, Features and Areas containing this locality

References

Qiuguobi Au deposit, Kuandian County, Dandong, Liaoning, China i
Regional Level Types
Qiuguobi Au deposit Deposit
Kuandian County County
Dandong Prefecture-level City
Liaoning Province
China Country