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Dongjiahe Pb-Zn deposit, Chenxi Co., Huaihua, Hunan, Chinai
Regional Level Types
Dongjiahe Pb-Zn depositDeposit
Chenxi Co.County
HuaihuaPrefecture-level City
HunanProvince
ChinaCountry

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Latitude & Longitude (WGS84):
28° 10' 0'' North , 110° 22' 59'' East
Latitude & Longitude (decimal):
Type:
Kรถppen climate type:
Nearest Settlements:
PlacePopulationDistance
Xiuxi1,000 (2012)22.7km
Tanwan1,630 (2004)31.9km
Xiaojiangkou770 (2012)32.4km
Huomachong1,930 (2012)34.9km
Qiaojiang3,290 (2012)38.4km
Mindat Locality ID:
187088
Long-form identifier:
mindat:1:2:187088:9
GUID (UUID V4):
0
Name(s) in local language(s):
่‘ฃๅฎถๆฒณ้“…้”Œ็Ÿฟ, ่พฐๆบชๅŽฟ, ๆ€€ๅŒ–ๅธ‚, ๆน–ๅ—็œ, ไธญๅ›ฝ


Stratabound lead-zinc deposit.

The Dongjiahe deposit consists of Neoproterozoic and Cambrian rocks that form the NE-SW-striking anticline, which has a steeply SE-dipping axial plane. Clastic rocks and glacial diamictites of the Neoproterozoic Nanhua Group are exposed in the core of the anticline, and Ediacaran and Cambrian dolostones and limestones are exposed in the limbs. The Marinoan cap dolostone in the Dongjiahe deposit is divided into three units, each of which is 1โ€“2 m thick. The basal and upper units contain Zn-Pb ores and are referred to as the lower and upper mineralized layers, respectively. The ore grades of the lower and upper mineralized layers are similar and they contain โˆผ 25 % and โˆผ 75 % of the metal resource of the deposit, respectively. The basal unit of the cap dolostone at Dongjiahe has sheet cracks, breccias, tepee, and doming structures, associated with mineral cementation.
Pre-ore stage: The stratiform distribution of the type I pyrite indicates that it probably formed during early diagenesis of the cap dolostone. Chalcedony fills the folding-related fractures within the upper cap dolostone at Dongjiahe, indicating that it formed during or after regional folding associated with the early Mesozoic Xuefeng Mountain Orogeny.
Ore stage: The Zn-Pb mineralization of the Dongjiahe deposit has not been dated radiometrically. However, mineralization must have occurred during or after the regional folding event associated with the early Mesozoic Xuefeng Mountain Orogeny.
Post-ore stage: Quartz and calcite formed after precipitation of sphalerite and galena. They fill open spaces that also contain Zn and Pb sulfides, or occur in veins without sulfides. These minerals occur in unmineralized cap dolostones elsewhere in South China, so they were not associated with the Zn-Pb mineralization.

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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


8 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:

โ“˜ Baryte
Formula: BaSO4
โ“˜ Calcite
Formula: CaCO3
โ“˜ Dolomite
Formula: CaMg(CO3)2
โ“˜ Fluorite
Formula: CaF2
โ“˜ Galena
Formula: PbS
โ“˜ 'Petroleum'
โ“˜ 'Petroleum var. Bitumen'
โ“˜ Pyrite
Formula: FeS2
โ“˜ Quartz
Formula: SiO2
โ“˜ Quartz var. Chalcedony
Formula: SiO2
โ“˜ Sphalerite
Formula: ZnS

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 2 - Sulphides and Sulfosalts
โ“˜Sphalerite2.CB.05aZnS
โ“˜Galena2.CD.10PbS
โ“˜Pyrite2.EB.05aFeS2
Group 3 - Halides
โ“˜Fluorite3.AB.25CaF2
Group 4 - Oxides and Hydroxides
โ“˜Quartz
var. Chalcedony
4.DA.05SiO2
โ“˜4.DA.05SiO2
Group 5 - Nitrates and Carbonates
โ“˜Calcite5.AB.05CaCO3
โ“˜Dolomite5.AB.10CaMg(CO3)2
Group 7 - Sulphates, Chromates, Molybdates and Tungstates
โ“˜Baryte7.AD.35BaSO4
Unclassified
โ“˜'Petroleum
var. Bitumen'
-
โ“˜''-

Other Regions, Features and Areas containing this locality

AsiaContinent
China
Eurasian Plate
Yangtze PlateTectonic Plate

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