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Mida nephrite deposit, Qiemo Co. (Qerqen Co.; Cherchen Co.), Bayin'gholin Autonomous Prefecture (Bayingolin Autonomous Prefecture; Bayinguoleng Autonomous Prefecture), Xinjiang, Chinai
Regional Level Types
Mida nephrite depositDeposit
Qiemo Co. (Qerqen Co.; Cherchen Co.)County
Bayin'gholin Autonomous Prefecture (Bayingolin Autonomous Prefecture; Bayinguoleng Autonomous Prefecture)Prefecture
XinjiangAutonomous Region
ChinaCountry

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Latitude & Longitude (WGS84):
37° 8' 52'' North , 85° 24' 24'' East
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Mindat Locality ID:
439607
Long-form identifier:
mindat:1:2:439607:2
GUID (UUID V4):
2da56ed5-a767-47fa-b1b6-a735d5c0bf37


Most Mida nephrites show a typical ivory white color, fine texture, semitranslucent-to-opaque transparency and greasy luster, while a smaller portion shows less transparency than the former and a porcelain-like luster. Mida nephrites show distinctive differences from Xinjiang white nephrite, which is known for its fine-grained texture, semitransparent-to-translucent appearance and greasy luster, as well as Qinghai white nephrite, which shows higher transparency and a vitreous luster.
The Mida nephrite deposit occurs in the Tokuzidaban Formation in Karamiran in the Late Paleozoic trench–arc–basin system between the Altyn fault and Muztag–Jingyu Lake fault. Zircon U–Pb dating of the volcanic rocks in the Tokuzidaban Formation in the Aksu River region indicates the formation age ranges from 364 to 343 Ma. The Tokuzidaban Formation is located in the South Kunlun terrane, which is part of the East Kunlun Orogenic Belt. The East Kunlun Orogenic Belt is divided into North Kunlun, South Kunlun and Bayan Har terranes based on the boundary between the Central Kunlun fault and the South Kunlun fault.
Field investigations have revealed that the nephrite orebodies occur as blocks, veins and irregular banded bodies within gray-white or gray-black carbonate rocks composed mainly of marble and marbleized limestone. The main minerals in the carbonate rocks are calcite, with small quantities of tremolite and graphite, along with carbonaceous bands in the center. The carbonate rocks exhibit a large scale, measuring approximately 30 m in horizontal width and over 300 m in length and extending vertically for about 500 m in the Mida nephrite deposit.

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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.


Mineral List


5 valid minerals.

Rock Types Recorded

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

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Alphabetical List Tree Diagram

Detailed Mineral List:

Calcite
Formula: CaCO3
Diopside
Formula: CaMgSi2O6
Graphite
Formula: C
Quartz
Formula: SiO2
Tremolite
Formula: ◻Ca2Mg5(Si8O22)(OH)2

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
Graphite1.CB.05aC
Group 4 - Oxides and Hydroxides
Quartz4.DA.05SiO2
Group 5 - Nitrates and Carbonates
Calcite5.AB.05CaCO3
Group 9 - Silicates
Diopside9.DA.15CaMgSi2O6
Tremolite9.DE.10◻Ca2Mg5(Si8O22)(OH)2

List of minerals for each chemical element

HHydrogen
H Tremolite◻Ca2Mg5(Si8O22)(OH)2
CCarbon
C CalciteCaCO3
C GraphiteC
OOxygen
O CalciteCaCO3
O DiopsideCaMgSi2O6
O QuartzSiO2
O Tremolite◻Ca2Mg5(Si8O22)(OH)2
MgMagnesium
Mg DiopsideCaMgSi2O6
Mg Tremolite◻Ca2Mg5(Si8O22)(OH)2
SiSilicon
Si DiopsideCaMgSi2O6
Si QuartzSiO2
Si Tremolite◻Ca2Mg5(Si8O22)(OH)2
CaCalcium
Ca CalciteCaCO3
Ca DiopsideCaMgSi2O6
Ca Tremolite◻Ca2Mg5(Si8O22)(OH)2

Other Regions, Features and Areas containing this locality

AsiaContinent
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.

References

 
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