Movatterモバイル変換


[0]ホーム

URL:


Log InRegister
AboutSupport UsPhotosDiscussionsSearchLearnMore
Quick Links :The Mindat ManualThe Rock H. Currier Digital LibraryMindat Newsletter [Free Download]
Home PageAbout MindatThe Mindat ManualHistory of MindatCopyright StatusWho We AreContact UsAdvertise on Mindat
Donate to MindatCorporate SponsorshipSponsor a PageSponsored PagesMindat AdvertisersAdvertise on Mindat
Learning CenterWhat is a mineral?The most common minerals on earthInformation for EducatorsMindat ArticlesThe ElementsThe Rock H. Currier Digital LibraryGeologic Time
Minerals by PropertiesMinerals by ChemistryAdvanced Locality SearchRandom MineralRandom LocalitySearch by minIDLocalities Near MeSearch ArticlesSearch GlossaryMore Search Options
Search For:
Mineral Name:
Locality Name:
Keyword(s):
 
The Mindat ManualAdd a New PhotoRate PhotosLocality Edit ReportCoordinate Completion ReportAdd Glossary Item
Mining CompaniesStatisticsUsersMineral MuseumsClubs & OrganizationsMineral Shows & EventsThe Mindat DirectoryDevice SettingsThe Mineral Quiz
Photo SearchPhoto GalleriesSearch by ColorNew Photos TodayNew Photos YesterdayMembers' Photo GalleriesPast Photo of the Day GalleryPhotography

Chakabeishan rare-element pegmatites, Tianjun County, Haixi Mongol and Tibetan Autonomous Prefecture, Qinghai, Chinai
Regional Level Types
Chakabeishan rare-element pegmatitesPegmatite
Tianjun CountyCounty
Haixi Mongol and Tibetan Autonomous PrefecturePrefecture
QinghaiProvince
ChinaCountry

This page is currently not sponsored.Click here to sponsor this page.
PhotosMapsSearch
Standard
Add Photo
Map PagesNearest Localities
Mineral SearchSimilar LocalitiesNearest LocalitiesPredictive MineralogySearch Google
Latitude & Longitude (WGS84):
36° 58' 30'' North , 99° 1' 0'' East
Latitude & Longitude (decimal):
Köppen climate type:
Mindat Locality ID:
423792
Long-form identifier:
mindat:1:2:423792:4
GUID (UUID V4):
e12df3ca-0d11-4e69-8f2f-3e30119d1a7c
Other/historical names associated with this locality:
Chaqiabeishan


The Chakabeishan pegmatite dikes are irregularly distributed along the northern side of the Zongwulongshan Southern Margin Fault, and occur as lenses and veins with widths of 1–6 m and lengths of 5–60 m. The rare-element pegmatites can be divided into barren, spodumene, and lepidolite pegmatites, based on mineralogy. The spodumene pegmatites are further divided into A- and B-type spodumene pegmatites, mainly according to the different wall rocks.

There are ca. 800 LCT-type pegmatite dykes in the CKBS deposit, which were derived from high fractional crystallization of granitic magmas. These pegmatite dykes occurred in the Paleoproterozoic Dakendaban Group schist Formation and the Ordovician quartz diorite. The elongation of these pegmatites varies but generally shows NW-SE trending with varying dipping (23°–83°). These pegmatite dykes are ca. 10–400 m in length and ca. 0.5–5 m in width. Since its first discovery in 2018, Li-Be resources of ca. 14,200 t Li2O and ca. 7000 t BeO have been identified.

(1) Mineralization Belt Ⅰ: The pegmatite belt is distributed in a northwest-southeast direction and is located in the GA21 anomaly site, and it spans approximately 1 km in length and 200 m in width. The surrounding rocks are quartz diorite, and 29 granitic pegmatite dikes were delineated, out of which 17 are ore-bearing pegmatite dikes.
(2) Mineralization Belt Ⅱ: The pegmatite belt is distributed in a northwest-southeast direction and is located on the southern side of Mineralization Belt Ⅰ. It stretches approximately 7 km in length and is 200–700 m in width. The surrounding rocks consist of grayish-brown two-mica quartz schist. A total of 144 pegmatite dikes were delineated, with 60 of them being ore-bearing pegmatite dikes.
(3) Mineralization Belt Ⅲ: The pegmatite belt is distributed in a northwest direction and is located on the south side of the mineralization belt Ⅱ, it stretches for about 7 km in length and is 300–500 m in width. The surrounding rocks primarily consist of mylonitic quartz diorite, along with two-mica quartz schist. A total of 115 pegmatite dikes were delineated, predominantly white granitic pegmatites. These pegmatite dikes generally dip to the northeast and extend approximately 50–150 m on the surface. And only 14 ore-bearing pegmatite dikes are delineated.

Select Mineral List Type

StandardDetailedGalleryStrunzChemical Elements

Detailed Mineral List:

Albite
Formula:Na(AlSi3O8)
References:
Albite var. Oligoclase
Formula:(Na,Ca)[Al(Si,Al)Si2O8]
Almandine
Formula:Fe2+3Al2(SiO4)3
'Apatite'
Formula:Ca5(PO4)3(Cl/F/OH)
References:
Beryl
Formula:Be3Al2(Si6O18)
References:
'Biotite'
Formula:K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Cassiterite
Formula:SnO2
'Columbite-(Fe)-Columbite-(Mn) Series'
References:
'Columbite Group'
Columbite-(Mn)
Formula:Mn2+Nb2O6
'Columbite-Tantalite'
Elbaite
Formula:Na(Li1.5Al1.5)Al6(Si6O18)(BO3)3(OH)3(OH)
'Feldspar Group'
'Feldspar Group var. Perthite'
'Garnet Group'
Formula:X3Z2(SiO4)3
References:
'K Feldspar'
References:
Magnetite
Formula:Fe2+Fe3+2O4
Microcline
Formula:K(AlSi3O8)
Muscovite
Formula:KAl2(AlSi3O10)(OH)2
References:
Muscovite var. Phengite
Formula:KAl1.5(Mg,Fe)0.5(Al0.5Si3.5O10)(OH)2
Orthoclase
Formula:K(AlSi3O8)
'Plagioclase'
Formula:(Na,Ca)[(Si,Al)AlSi2]O8
References:
'Polylithionite-Trilithionite Series'
Quartz
Formula:SiO2
References:
Schorl
Formula:NaFe2+3Al6(Si6O18)(BO3)3(OH)3(OH)
Siderophyllite
Formula:KFe2+2Al(Al2Si2O10)(OH)2
Spessartine
Formula:Mn2+3Al2(SiO4)3
Spodumene
Formula:LiAlSi2O6
References:
'Tantalite'
Formula:(Mn,Fe)(Ta,Nb)2O6
Tantalite-(Fe)
Formula:Fe2+Ta2O6
Tantalite-(Mn)
Formula:Mn2+Ta2O6
'Tourmaline'
Formula:AD3G6 (T6O18)(BO3)3X3Z
Description: Two types of tourmalines from the barren pegmatites are identified: optically homogenous fine-grain tourmalines (HTur) and optically zoned coarse-grain tourmalines (OZ-Tur).The H-Tur grains are acicular, long-columnar and short-columnar, and commonly show khaki-dark blue polychromatism. In contrast to H-Tur, the OZ-Tur crystals are round and long-columnar, and generally display two optical layers with blue cores and khaki-dark blue rims. However, three optical rhythmic layers and blurry polyrhythmic layers are also observed occasionally. Notably, H-Tur commonly coexists with muscovite while OZ-Tur does not.[[3]]
References:
Zircon
Formula:Zr(SiO4)

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 4 - Oxides and Hydroxides
Magnetite4.BB.05Fe2+Fe3+2O4
Quartz4.DA.05SiO2
Cassiterite4.DB.05SnO2
Tantalite-(Fe)4.DB.35Fe2+Ta2O6
Columbite-(Mn)4.DB.35Mn2+Nb2O6
Tantalite-(Mn)4.DB.35Mn2+Ta2O6
Group 9 - Silicates
Almandine9.AD.25Fe2+3Al2(SiO4)3
Spessartine9.AD.25Mn2+3Al2(SiO4)3
Zircon9.AD.30Zr(SiO4)
Beryl9.CJ.05Be3Al2(Si6O18)
Elbaite9.CK.05Na(Li1.5Al1.5)Al6(Si6O18)(BO3)3(OH)3(OH)
Schorl9.CK.05NaFe2+3Al6(Si6O18)(BO3)3(OH)3(OH)
Spodumene9.DA.30LiAlSi2O6
Muscovite9.EC.15KAl2(AlSi3O10)(OH)2
var. Phengite9.EC.15KAl1.5(Mg,Fe)0.5(Al0.5Si3.5O10)(OH)2
Siderophyllite9.EC.20KFe2+2Al(Al2Si2O10)(OH)2
Microcline9.FA.30K(AlSi3O8)
Orthoclase9.FA.30K(AlSi3O8)
Albite9.FA.35Na(AlSi3O8)
var. Oligoclase9.FA.35(Na,Ca)[Al(Si,Al)Si2O8]
Unclassified
'Biotite'-K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
'Feldspar Group'-
'Tantalite'-(Mn,Fe)(Ta,Nb)2O6
'Tourmaline'-AD3G6 (T6O18)(BO3)3X3Z
'Feldspar Group
var. Perthite'
-
'Columbite-(Fe)-Columbite-(Mn) Series'-
'Plagioclase'-(Na,Ca)[(Si,Al)AlSi2]O8
'K Feldspar'-
'Garnet Group'-X3Z2(SiO4)3
'Columbite-Tantalite'-
'Polylithionite-Trilithionite Series'-
'Apatite'-Ca5(PO4)3(Cl/F/OH)
'Columbite Group'-

List of minerals for each chemical element

HHydrogen
HBiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
HElbaiteNa(Li1.5Al1.5)Al6(Si6O18)(BO3)3(OH)3(OH)
HMuscoviteKAl2(AlSi3O10)(OH)2
HMuscovite var.PhengiteKAl1.5(Mg,Fe)0.5(Al0.5Si3.5O10)(OH)2
HSchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
HSiderophylliteKFe22+Al(Al2Si2O10)(OH)2
HApatiteCa5(PO4)3(Cl/F/OH)
LiLithium
LiElbaiteNa(Li1.5Al1.5)Al6(Si6O18)(BO3)3(OH)3(OH)
LiSpodumeneLiAlSi2O6
BeBeryllium
BeBerylBe3Al2(Si6O18)
BBoron
BElbaiteNa(Li1.5Al1.5)Al6(Si6O18)(BO3)3(OH)3(OH)
BSchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
BTourmalineAD3G6 (T6O18)(BO3)3X3Z
OOxygen
OAlbiteNa(AlSi3O8)
OAlmandineFe32+Al2(SiO4)3
OBiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
OBerylBe3Al2(Si6O18)
OCassiteriteSnO2
OElbaiteNa(Li1.5Al1.5)Al6(Si6O18)(BO3)3(OH)3(OH)
OTantalite-(Fe)Fe2+Ta2O6
OColumbite-(Mn)Mn2+Nb2O6
OTantalite-(Mn)Mn2+Ta2O6
OMagnetiteFe2+Fe23+O4
OMicroclineK(AlSi3O8)
OMuscoviteKAl2(AlSi3O10)(OH)2
OAlbite var.Oligoclase(Na,Ca)[Al(Si,Al)Si2O8]
OOrthoclaseK(AlSi3O8)
OMuscovite var.PhengiteKAl1.5(Mg,Fe)0.5(Al0.5Si3.5O10)(OH)2
OQuartzSiO2
OSchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
OSiderophylliteKFe22+Al(Al2Si2O10)(OH)2
OSpessartineMn32+Al2(SiO4)3
OSpodumeneLiAlSi2O6
OTantalite(Mn,Fe)(Ta,Nb)2O6
OTourmalineAD3G6 (T6O18)(BO3)3X3Z
OZirconZr(SiO4)
OPlagioclase(Na,Ca)[(Si,Al)AlSi2]O8
OGarnet GroupX3Z2(SiO4)3
OApatiteCa5(PO4)3(Cl/F/OH)
FFluorine
FBiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
FApatiteCa5(PO4)3(Cl/F/OH)
NaSodium
NaAlbiteNa(AlSi3O8)
NaElbaiteNa(Li1.5Al1.5)Al6(Si6O18)(BO3)3(OH)3(OH)
NaAlbite var.Oligoclase(Na,Ca)[Al(Si,Al)Si2O8]
NaSchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
NaPlagioclase(Na,Ca)[(Si,Al)AlSi2]O8
MgMagnesium
MgBiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
MgMuscovite var.PhengiteKAl1.5(Mg,Fe)0.5(Al0.5Si3.5O10)(OH)2
AlAluminium
AlAlbiteNa(AlSi3O8)
AlAlmandineFe32+Al2(SiO4)3
AlBiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
AlBerylBe3Al2(Si6O18)
AlElbaiteNa(Li1.5Al1.5)Al6(Si6O18)(BO3)3(OH)3(OH)
AlMicroclineK(AlSi3O8)
AlMuscoviteKAl2(AlSi3O10)(OH)2
AlAlbite var.Oligoclase(Na,Ca)[Al(Si,Al)Si2O8]
AlOrthoclaseK(AlSi3O8)
AlMuscovite var.PhengiteKAl1.5(Mg,Fe)0.5(Al0.5Si3.5O10)(OH)2
AlSchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
AlSiderophylliteKFe22+Al(Al2Si2O10)(OH)2
AlSpessartineMn32+Al2(SiO4)3
AlSpodumeneLiAlSi2O6
AlPlagioclase(Na,Ca)[(Si,Al)AlSi2]O8
SiSilicon
SiAlbiteNa(AlSi3O8)
SiAlmandineFe32+Al2(SiO4)3
SiBiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
SiBerylBe3Al2(Si6O18)
SiElbaiteNa(Li1.5Al1.5)Al6(Si6O18)(BO3)3(OH)3(OH)
SiMicroclineK(AlSi3O8)
SiMuscoviteKAl2(AlSi3O10)(OH)2
SiAlbite var.Oligoclase(Na,Ca)[Al(Si,Al)Si2O8]
SiOrthoclaseK(AlSi3O8)
SiMuscovite var.PhengiteKAl1.5(Mg,Fe)0.5(Al0.5Si3.5O10)(OH)2
SiQuartzSiO2
SiSchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
SiSiderophylliteKFe22+Al(Al2Si2O10)(OH)2
SiSpessartineMn32+Al2(SiO4)3
SiSpodumeneLiAlSi2O6
SiZirconZr(SiO4)
SiPlagioclase(Na,Ca)[(Si,Al)AlSi2]O8
SiGarnet GroupX3Z2(SiO4)3
PPhosphorus
PApatiteCa5(PO4)3(Cl/F/OH)
ClChlorine
ClApatiteCa5(PO4)3(Cl/F/OH)
KPotassium
KBiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
KMicroclineK(AlSi3O8)
KMuscoviteKAl2(AlSi3O10)(OH)2
KOrthoclaseK(AlSi3O8)
KMuscovite var.PhengiteKAl1.5(Mg,Fe)0.5(Al0.5Si3.5O10)(OH)2
KSiderophylliteKFe22+Al(Al2Si2O10)(OH)2
CaCalcium
CaAlbite var.Oligoclase(Na,Ca)[Al(Si,Al)Si2O8]
CaPlagioclase(Na,Ca)[(Si,Al)AlSi2]O8
CaApatiteCa5(PO4)3(Cl/F/OH)
TiTitanium
TiBiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
MnManganese
MnColumbite-(Mn)Mn2+Nb2O6
MnTantalite-(Mn)Mn2+Ta2O6
MnSpessartineMn32+Al2(SiO4)3
MnTantalite(Mn,Fe)(Ta,Nb)2O6
FeIron
FeAlmandineFe32+Al2(SiO4)3
FeBiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
FeTantalite-(Fe)Fe2+Ta2O6
FeMagnetiteFe2+Fe23+O4
FeMuscovite var.PhengiteKAl1.5(Mg,Fe)0.5(Al0.5Si3.5O10)(OH)2
FeSchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
FeSiderophylliteKFe22+Al(Al2Si2O10)(OH)2
FeTantalite(Mn,Fe)(Ta,Nb)2O6
ZrZirconium
ZrZirconZr(SiO4)
NbNiobium
NbColumbite-(Mn)Mn2+Nb2O6
NbTantalite(Mn,Fe)(Ta,Nb)2O6
SnTin
SnCassiteriteSnO2
TaTantalum
TaTantalite-(Fe)Fe2+Ta2O6
TaTantalite-(Mn)Mn2+Ta2O6
TaTantalite(Mn,Fe)(Ta,Nb)2O6

Other Regions, Features and Areas containing this locality

AsiaContinent
China
China
Eurasian 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, pleaseregister so you can add to our database. This locality information is for reference purposes only. You should never attempt tovisit any sites listed in mindat.org without first ensuring that you have the permission of the land and/or mineral rights holdersfor access and that you are aware of all safety precautions necessary.

References

 
and/or 
Mindat.org is an outreach project of theHudson Institute of Mineralogy, a 501(c)(3) not-for-profit organization.
Copyright © mindat.org and the Hudson Institute of Mineralogy 1993-2025, except where stated. Most political location boundaries are© OpenStreetMap contributors. Mindat.org relies on the contributions of thousands of members and supporters. Founded in 2000 byJolyon Ralph.
Privacy Policy -Terms & Conditions -Contact Us / DMCA issues -Report a bug/vulnerabilityCurrent server date and time: April 8, 2025 16:11:04 Page updated: January 6, 2025 03:07:52