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Mibale (Mibalei), Nyima Co. (Nima Co.), Nagchu Prefecture (Naqu Prefecture), Tibet, Chinai
Regional Level Types
Mibale (Mibalei)- not defined -
Nyima Co. (Nima Co.)County
Nagchu Prefecture (Naqu Prefecture)Prefecture
TibetAutonomous Region
ChinaCountry

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PhotosMapsSearch
Latitude & Longitude (WGS84):
30° 51' 0'' North , 86° 39' 26'' East
Latitude & Longitude (decimal):
30.85000,86.65722
GeoHash:
G#: tvmxebjf7
GRN:
N21E53
Köppen climate type:
ET : Tundra
Name(s) in local language(s):
米巴勒, 尼玛县 (ཉི་མ་རྫོང་), 那曲地区 (ནག་ཆུ་ས་ཁུལ་), 西藏自治区, 中国


Outcrops of Miocenic leucite phonolite, occurring in a suite of alkaline volcanic rocks.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Mineral List


14 valid minerals.

Detailed Mineral List:

ⓘ Aegirine-augite
Formula: (NaaCabFe2+cMgd)(Fe3+eAlfFe2+gMgh)Si2O6
Reference: Siping Liao, Zhenhua Chen, Xiaochuan Luo, and Aijian Zhou (2002): Geological Bulletin of China 21(11), 735-738
ⓘ Analcime
Formula: Na(AlSi2O6) · H2O
Reference: Siping Liao, Zhenhua Chen, Xiaochuan Luo, and Aijian Zhou (2002): Geological Bulletin of China 21(11), 735-738
ⓘ 'Apatite'
Formula: Ca5(PO4)3(Cl/F/OH)
Reference: Siping Liao, Zhenhua Chen, Xiaochuan Luo, and Aijian Zhou (2002): Geological Bulletin of China 21(11), 735-738; Gao, Y., Hou, Z., Kamber, B. S., Wei, R., Meng, X., & Zhao, R. (2007). Lamproitic rocks from a continental collision zone: evidence for recycling of subducted Tethyan oceanic sediments in the mantle beneath southern Tibet. Journal of Petrology, 48(4), 729-752.
ⓘ 'Biotite'
Formula: K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2
Reference: Siping Liao, Zhenhua Chen, Xiaochuan Luo, and Aijian Zhou (2002): Geological Bulletin of China 21(11), 735-738
ⓘ Brookite
Formula: TiO2
Reference: Siping Liao, Zhenhua Chen, Xiaochuan Luo, and Aijian Zhou (2002): Geological Bulletin of China 21(11), 735-738
ⓘ Calcite
Formula: CaCO3
Reference: Siping Liao, Zhenhua Chen, Xiaochuan Luo, and Aijian Zhou (2002): Geological Bulletin of China 21(11), 735-738
ⓘ 'Clinopyroxene Subgroup'
Reference: Gao, Y., Hou, Z., Kamber, B. S., Wei, R., Meng, X., & Zhao, R. (2007). Lamproitic rocks from a continental collision zone: evidence for recycling of subducted Tethyan oceanic sediments in the mantle beneath southern Tibet. Journal of Petrology, 48(4), 729-752.
ⓘ Diopside
Formula: CaMgSi2O6
Reference: Siping Liao, Zhenhua Chen, Xiaochuan Luo, and Aijian Zhou (2002): Geological Bulletin of China 21(11), 735-738; Gao, Y., Hou, Z., Kamber, B. S., Wei, R., Meng, X., & Zhao, R. (2007). Lamproitic rocks from a continental collision zone: evidence for recycling of subducted Tethyan oceanic sediments in the mantle beneath southern Tibet. Journal of Petrology, 48(4), 729-752.
ⓘ 'Fayalite-Forsterite Series'
Reference: Siping Liao, Zhenhua Chen, Xiaochuan Luo, and Aijian Zhou (2002): Geological Bulletin of China 21(11), 735-738; Gao, Y., Hou, Z., Kamber, B. S., Wei, R., Meng, X., & Zhao, R. (2007). Lamproitic rocks from a continental collision zone: evidence for recycling of subducted Tethyan oceanic sediments in the mantle beneath southern Tibet. Journal of Petrology, 48(4), 729-752.
ⓘ 'Glass'
Reference: Gao, Y., Hou, Z., Kamber, B. S., Wei, R., Meng, X., & Zhao, R. (2007). Lamproitic rocks from a continental collision zone: evidence for recycling of subducted Tethyan oceanic sediments in the mantle beneath southern Tibet. Journal of Petrology, 48(4), 729-752.
ⓘ Ilmenite
Formula: Fe2+TiO3
Reference: Gao, Y., Hou, Z., Kamber, B. S., Wei, R., Meng, X., & Zhao, R. (2007). Lamproitic rocks from a continental collision zone: evidence for recycling of subducted Tethyan oceanic sediments in the mantle beneath southern Tibet. Journal of Petrology, 48(4), 729-752.
ⓘ Leucite
Formula: K(AlSi2O6)
Reference: Siping Liao, Zhenhua Chen, Xiaochuan Luo, and Aijian Zhou (2002): Geological Bulletin of China 21(11), 735-738; Gao, Y., Hou, Z., Kamber, B. S., Wei, R., Meng, X., & Zhao, R. (2007). Lamproitic rocks from a continental collision zone: evidence for recycling of subducted Tethyan oceanic sediments in the mantle beneath southern Tibet. Journal of Petrology, 48(4), 729-752.
ⓘ Magnetite
Formula: Fe2+Fe3+2O4
Reference: Siping Liao, Zhenhua Chen, Xiaochuan Luo, and Aijian Zhou (2002): Geological Bulletin of China 21(11), 735-738
ⓘ Magnetite var. Titanium-bearing Magnetite
Formula: Fe2+(Fe3+,Ti)2O4
Reference: Gao, Y., Hou, Z., Kamber, B. S., Wei, R., Meng, X., & Zhao, R. (2007). Lamproitic rocks from a continental collision zone: evidence for recycling of subducted Tethyan oceanic sediments in the mantle beneath southern Tibet. Journal of Petrology, 48(4), 729-752.
ⓘ Phlogopite
Formula: KMg3(AlSi3O10)(OH)2
Reference: Gao, Y., Hou, Z., Kamber, B. S., Wei, R., Meng, X., & Zhao, R. (2007). Lamproitic rocks from a continental collision zone: evidence for recycling of subducted Tethyan oceanic sediments in the mantle beneath southern Tibet. Journal of Petrology, 48(4), 729-752.
ⓘ 'Pyroxene Group'
Formula: ADSi2O6
Reference: Gao, Y., Hou, Z., Kamber, B. S., Wei, R., Meng, X., & Zhao, R. (2007). Lamproitic rocks from a continental collision zone: evidence for recycling of subducted Tethyan oceanic sediments in the mantle beneath southern Tibet. Journal of Petrology, 48(4), 729-752.
ⓘ Sanidine
Formula: K(AlSi3O8)
Reference: Siping Liao, Zhenhua Chen, Xiaochuan Luo, and Aijian Zhou (2002): Geological Bulletin of China 21(11), 735-738; Gao, Y., Hou, Z., Kamber, B. S., Wei, R., Meng, X., & Zhao, R. (2007). Lamproitic rocks from a continental collision zone: evidence for recycling of subducted Tethyan oceanic sediments in the mantle beneath southern Tibet. Journal of Petrology, 48(4), 729-752.
ⓘ Sodalite
Formula: Na4(Si3Al3)O12Cl
Reference: Siping Liao, Zhenhua Chen, Xiaochuan Luo, and Aijian Zhou (2002): Geological Bulletin of China 21(11), 735-738
ⓘ Spinel
Formula: MgAl2O4
Reference: Gao, Y., Hou, Z., Kamber, B. S., Wei, R., Meng, X., & Zhao, R. (2007). Lamproitic rocks from a continental collision zone: evidence for recycling of subducted Tethyan oceanic sediments in the mantle beneath southern Tibet. Journal of Petrology, 48(4), 729-752.
ⓘ Titanite
Formula: CaTi(SiO4)O
Reference: Siping Liao, Zhenhua Chen, Xiaochuan Luo, and Aijian Zhou (2002): Geological Bulletin of China 21(11), 735-738; Gao, Y., Hou, Z., Kamber, B. S., Wei, R., Meng, X., & Zhao, R. (2007). Lamproitic rocks from a continental collision zone: evidence for recycling of subducted Tethyan oceanic sediments in the mantle beneath southern Tibet. Journal of Petrology, 48(4), 729-752.
ⓘ Zircon
Formula: Zr(SiO4)
Reference: Siping Liao, Zhenhua Chen, Xiaochuan Luo, and Aijian Zhou (2002): Geological Bulletin of China 21(11), 735-738

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 4 - Oxides and Hydroxides
ⓘBrookite4.DD.10TiO2
ⓘIlmenite4.CB.05Fe2+TiO3
ⓘMagnetite4.BB.05Fe2+Fe3+2O4
ⓘvar. Titanium-bearing Magnetite4.BB.05Fe2+(Fe3+,Ti)2O4
ⓘSpinel4.BB.05MgAl2O4
Group 5 - Nitrates and Carbonates
ⓘCalcite5.AB.05CaCO3
Group 9 - Silicates
ⓘAegirine-augite9.DA.20(NaaCabFe2+cMgd)(Fe3+eAlfFe2+gMgh)Si2O6
ⓘAnalcime9.GB.05Na(AlSi2O6) · H2O
ⓘDiopside9.DA.15CaMgSi2O6
ⓘLeucite9.GB.05K(AlSi2O6)
ⓘPhlogopite9.EC.20KMg3(AlSi3O10)(OH)2
ⓘSanidine9.FA.30K(AlSi3O8)
ⓘSodalite9.FB.10Na4(Si3Al3)O12Cl
ⓘTitanite9.AG.15CaTi(SiO4)O
ⓘZircon9.AD.30Zr(SiO4)
Unclassified Minerals, Rocks, etc.
ⓘ'Apatite'-Ca5(PO4)3(Cl/F/OH)
ⓘ'Biotite'-K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2
ⓘ'Clinopyroxene Subgroup'-
ⓘ'Fayalite-Forsterite Series'-
ⓘ'Glass'-
ⓘ'Pyroxene Group'-ADSi2O6

List of minerals for each chemical element

HHydrogen
Hⓘ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2
Hⓘ ApatiteCa5(PO4)3(Cl/F/OH)
Hⓘ AnalcimeNa(AlSi2O6) · H2O
Hⓘ PhlogopiteKMg3(AlSi3O10)(OH)2
CCarbon
Cⓘ CalciteCaCO3
OOxygen
Oⓘ LeuciteK(AlSi2O6)
Oⓘ DiopsideCaMgSi2O6
Oⓘ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2
Oⓘ SanidineK(AlSi3O8)
Oⓘ SodaliteNa4(Si3Al3)O12Cl
Oⓘ MagnetiteFe2+Fe23+O4
Oⓘ ApatiteCa5(PO4)3(Cl/F/OH)
Oⓘ ZirconZr(SiO4)
Oⓘ CalciteCaCO3
Oⓘ TitaniteCaTi(SiO4)O
Oⓘ BrookiteTiO2
Oⓘ AnalcimeNa(AlSi2O6) · H2O
Oⓘ Aegirine-augite(NaaCabFec2+Mgd)(Fee3+AlfFeg2+Mgh)Si2O6
Oⓘ PhlogopiteKMg3(AlSi3O10)(OH)2
Oⓘ Pyroxene GroupADSi2O6
Oⓘ Magnetite var. Titanium-bearing MagnetiteFe2+(Fe3+,Ti)2O4
Oⓘ IlmeniteFe2+TiO3
Oⓘ SpinelMgAl2O4
FFluorine
Fⓘ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2
Fⓘ ApatiteCa5(PO4)3(Cl/F/OH)
NaSodium
Naⓘ SodaliteNa4(Si3Al3)O12Cl
Naⓘ AnalcimeNa(AlSi2O6) · H2O
Naⓘ Aegirine-augite(NaaCabFec2+Mgd)(Fee3+AlfFeg2+Mgh)Si2O6
MgMagnesium
Mgⓘ DiopsideCaMgSi2O6
Mgⓘ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2
Mgⓘ Aegirine-augite(NaaCabFec2+Mgd)(Fee3+AlfFeg2+Mgh)Si2O6
Mgⓘ PhlogopiteKMg3(AlSi3O10)(OH)2
Mgⓘ SpinelMgAl2O4
AlAluminium
Alⓘ LeuciteK(AlSi2O6)
Alⓘ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2
Alⓘ SanidineK(AlSi3O8)
Alⓘ SodaliteNa4(Si3Al3)O12Cl
Alⓘ AnalcimeNa(AlSi2O6) · H2O
Alⓘ Aegirine-augite(NaaCabFec2+Mgd)(Fee3+AlfFeg2+Mgh)Si2O6
Alⓘ PhlogopiteKMg3(AlSi3O10)(OH)2
Alⓘ SpinelMgAl2O4
SiSilicon
Siⓘ LeuciteK(AlSi2O6)
Siⓘ DiopsideCaMgSi2O6
Siⓘ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2
Siⓘ SanidineK(AlSi3O8)
Siⓘ SodaliteNa4(Si3Al3)O12Cl
Siⓘ ZirconZr(SiO4)
Siⓘ TitaniteCaTi(SiO4)O
Siⓘ AnalcimeNa(AlSi2O6) · H2O
Siⓘ Aegirine-augite(NaaCabFec2+Mgd)(Fee3+AlfFeg2+Mgh)Si2O6
Siⓘ PhlogopiteKMg3(AlSi3O10)(OH)2
Siⓘ Pyroxene GroupADSi2O6
PPhosphorus
Pⓘ ApatiteCa5(PO4)3(Cl/F/OH)
ClChlorine
Clⓘ SodaliteNa4(Si3Al3)O12Cl
Clⓘ ApatiteCa5(PO4)3(Cl/F/OH)
KPotassium
Kⓘ LeuciteK(AlSi2O6)
Kⓘ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2
Kⓘ SanidineK(AlSi3O8)
Kⓘ PhlogopiteKMg3(AlSi3O10)(OH)2
CaCalcium
Caⓘ DiopsideCaMgSi2O6
Caⓘ ApatiteCa5(PO4)3(Cl/F/OH)
Caⓘ CalciteCaCO3
Caⓘ TitaniteCaTi(SiO4)O
Caⓘ Aegirine-augite(NaaCabFec2+Mgd)(Fee3+AlfFeg2+Mgh)Si2O6
TiTitanium
Tiⓘ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2
Tiⓘ TitaniteCaTi(SiO4)O
Tiⓘ BrookiteTiO2
Tiⓘ Magnetite var. Titanium-bearing MagnetiteFe2+(Fe3+,Ti)2O4
Tiⓘ IlmeniteFe2+TiO3
FeIron
Feⓘ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2
Feⓘ MagnetiteFe2+Fe23+O4
Feⓘ Aegirine-augite(NaaCabFec2+Mgd)(Fee3+AlfFeg2+Mgh)Si2O6
Feⓘ Magnetite var. Titanium-bearing MagnetiteFe2+(Fe3+,Ti)2O4
Feⓘ IlmeniteFe2+TiO3
ZrZirconium
Zrⓘ ZirconZr(SiO4)

Geochronology

Mineralization age: Miocene : 19.04 ± 0.97 Ma

Important note: This table is based only on rock and mineral ages recorded on mindat.org for this locality and is not necessarily a complete representation of the geochronology, but does give an indication of possible mineralization events relevant to this locality. As more age information is added this table may expand in the future. A break in the table simply indicates a lack of data entered here, not necessarily a break in the geologic sequence. Grey background entries are from different, related, localities.

Geologic TimeRocks, Minerals and Events
Phanerozoic
 Cenozoic
  Neogene
   Miocene
ⓘ Phlogopite19.04 ± 0.97 Ma

References

Sort by

Year (asc) Year (desc) Author (A-Z) Author (Z-A)
Siping Liao, Zhenhua Chen, Xiaochuan Luo, and Aijian Zhou (2002): Discovery of leucite phonolite in the Tangra Yumco area, Tibet and its geological significance. Geological Bulletin of China 21(11), 735-738 (in Chinese with English abstract).

Other Regions, Features and Areas containing this locality

AsiaContinent
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, 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.
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