Vote for your favorite mineral in #MinCup26! - Quartz vs. Asagiite
It's a classic vs a newbie as the most common named mineral in the crust Quartz is up against an exceedingly-rare sea foam-green mineral discovered just a few years ago Asagiite.
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Dalong Sn deposit, Zhenkang County, Lincang, Yunnan, Chinai
Regional Level Types
Dalong Sn depositDeposit
Zhenkang CountyCounty
LincangPrefecture-level City
YunnanProvince
ChinaCountry

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Latitude & Longitude (WGS84):
23° 45' 43'' North , 99° 2' 46'' East
Latitude & Longitude (decimal):
Type:
Mindat Locality ID:
453830
Long-form identifier:
mindat:1:2:453830:4
GUID (UUID V4):
0


The deposit hosts 1,855 t Sn with an average grade of 0.4 %. Strata are mainly the Cambrian to Permian sedimentary layers, intercalated with Permian-Triassic basalt. The Upper Cambrian Baoshan Formation (Є3b), serving as the main Sn ore-hosting unit, is subdivided into five lithological members. (1) The first member (Є3b1) consists of banded limestone, intercalated with dolomitic limestone. (2) The second member (Є3b2) consists of silty clay slate and calcareous silty clay slate. The top and bottom parts have higher calcium content and exhibit transitional contacts with the adjacent members. (3) The third member (Є3b3) is composed of light gray and grayish-white medium to thick-bedded banded micritic limestone, intercalated with sandy and calcareous clay slate layers. (4) the fourth member (Є3b4) is gray, grayish-green, and locally purplish-red thin to medium-thick bedded sandy and sandy clay slate. The top and bottom parts exhibit relatively higher calcium content. (5) The fifth member (Є3b5) consists of bedded micritic limestone, intercalated with thin-bedded calcareous and silty clay slate. Members Є3b2, Є3b3, and Є3b4 constitute the primary ore-bearing unit.
he Dalong deposit comprises 11 tin ore bodies and several scattered tin-mineralized bodies. The ore bodies are controlled by both structure and stratigraphy, primarily occurring within the NE-trending fault system and their associated interlayer compressional fracture zones. Based on the host strata, three ore zones can be delineated: the Upper Ore Zone (Є3b4), the Middle Ore Zone (Є3b3), and the Lower Ore Zone (Є3b2). The area covered by mineralized bodies is approximately 2 km2. The ore bodies strike 240°–260°, dip NW at 20°–80° (consistent with wall rock attitudes), 40–430 m in length, 10–250 m in depth, and 0.5–10 m in thickness, with Sn grades varying between 0.21 % and 1.59 %. Among the ore bodies, V2, V3, V8, and V9 are the largest, accounting for 85 % of the total reserves. Three ore types are recognized at Dalong: (1) cassiterite-tourmaline-sulfide-quartz ore (main ore type; hosted in sulfide-quartz veins), (2) cassiterite-tourmaline-sulfide-sericite ore (hosted in wallrocks with intensive sericitization), and (3) oxidized limonite-cassiterite ore. Ores exhibit disseminated, veinlet, stockwork, or honeycomb morphologies.

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.


Mineral List


12 valid minerals.

Rock Types Recorded

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

Select Rock List Type

Alphabetical List Tree Diagram

Detailed Mineral List:

Arsenopyrite
Formula: FeAsS
Atelestite
Formula: Bi2(AsO4)O(OH)
Bismuthinite
Formula: Bi2S3
Cassiterite
Formula: SnO2
Chalcopyrite
Formula: CuFeS2
'Limonite'
Marcasite
Formula: FeS2
'Micrite'
Muscovite
Formula: KAl2(AlSi3O10)(OH)2
Muscovite var. Sericite
Formula: KAl2(AlSi3O10)(OH)2
Pyrite
Formula: FeS2
Pyrrhotite
Formula: Fe1-xS
Quartz
Formula: SiO2
Sphalerite
Formula: ZnS
Stannite
Formula: Cu2FeSnS4
'Tetrahedrite Subgroup'
Formula: Cu6(Cu4C2+2)Sb4S12S
'Tourmaline'
Formula: AD3G6(T6O18)(BO3)3X3Z

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 2 - Sulphides and Sulfosalts
Sphalerite2.CB.05aZnS
Chalcopyrite2.CB.10aCuFeS2
Stannite2.CB.15aCu2FeSnS4
Pyrrhotite2.CC.10Fe1-xS
Bismuthinite2.DB.05Bi2S3
Pyrite2.EB.05aFeS2
Marcasite2.EB.10aFeS2
Arsenopyrite2.EB.20FeAsS
'Tetrahedrite Subgroup'2.GB.05Cu6(Cu4C2+2)Sb4S12S
Group 4 - Oxides and Hydroxides
Quartz4.DA.05SiO2
Cassiterite4.DB.05SnO2
Group 8 - Phosphates, Arsenates and Vanadates
Atelestite8.BO.15Bi2(AsO4)O(OH)
Group 9 - Silicates
Muscovite9.EC.15KAl2(AlSi3O10)(OH)2
var. Sericite9.EC.15KAl2(AlSi3O10)(OH)2
Unclassified
'Limonite'-
'Tourmaline'-AD3G6(T6O18)(BO3)3X3Z
'Micrite'-

List of minerals for each chemical element

HHydrogen
H AtelestiteBi2(AsO4)O(OH)
H MuscoviteKAl2(AlSi3O10)(OH)2
H Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
BBoron
B TourmalineAD3G6(T6O18)(BO3)3X3Z
OOxygen
O AtelestiteBi2(AsO4)O(OH)
O CassiteriteSnO2
O MuscoviteKAl2(AlSi3O10)(OH)2
O QuartzSiO2
O TourmalineAD3G6(T6O18)(BO3)3X3Z
O Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
AlAluminium
Al MuscoviteKAl2(AlSi3O10)(OH)2
Al Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
SiSilicon
Si MuscoviteKAl2(AlSi3O10)(OH)2
Si QuartzSiO2
Si Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
SSulfur
S ArsenopyriteFeAsS
S BismuthiniteBi2S3
S ChalcopyriteCuFeS2
S MarcasiteFeS2
S PyriteFeS2
S PyrrhotiteFe1-xS
S SphaleriteZnS
S StanniteCu2FeSnS4
S Tetrahedrite SubgroupCu6(Cu4C22+)Sb4S12S
KPotassium
K MuscoviteKAl2(AlSi3O10)(OH)2
K Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
FeIron
Fe ArsenopyriteFeAsS
Fe ChalcopyriteCuFeS2
Fe MarcasiteFeS2
Fe PyriteFeS2
Fe PyrrhotiteFe1-xS
Fe StanniteCu2FeSnS4
CuCopper
Cu ChalcopyriteCuFeS2
Cu StanniteCu2FeSnS4
Cu Tetrahedrite SubgroupCu6(Cu4C22+)Sb4S12S
ZnZinc
Zn SphaleriteZnS
AsArsenic
As ArsenopyriteFeAsS
As AtelestiteBi2(AsO4)O(OH)
SnTin
Sn CassiteriteSnO2
Sn StanniteCu2FeSnS4
SbAntimony
Sb Tetrahedrite SubgroupCu6(Cu4C22+)Sb4S12S
BiBismuth
Bi AtelestiteBi2(AsO4)O(OH)
Bi BismuthiniteBi2S3

Other Regions, Features and Areas containing this locality

AsiaContinent
China
Eurasian PlateTectonic Plate

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