登录注册
Quick Links : Mindat手册The Rock H. Currier Digital LibraryMindat Newsletter [Free Download]
主页关于 MindatMindat手册Mindat的历史版权Who We Are联系我们于 Mindat.org刊登广告
捐赠给 MindatCorporate Sponsorship赞助板页已赞助的板页在 Mindat刊登 广告的广告商于 Mindat.org刊登广告
Learning CenterWhat is a mineral?The most common minerals on earthInformation for EducatorsMindat ArticlesThe ElementsThe Rock H. Currier Digital LibraryGeologic Time
搜索矿物的性质搜索矿物的化学Advanced Locality Search随意显示任何一 种矿物Random Locality使用minID搜索邻近产地Search Articles搜索词汇表更多搜索选项
搜索:
矿物名称:
地区产地名称:
关键字:
 
Mindat手册添加新照片Rate Photos产区编辑报告Coordinate Completion Report添加词汇表项目
Mining Companies统计会员列表Mineral MuseumsClubs & Organizations矿物展及活动The Mindat目录表设备设置The Mineral Quiz
照片搜索Photo GalleriesSearch by Color今天最新的照片昨天最新的照片用户照片相集过去每日精选照片相集Photography

Predictive Mineralogy

Possible unrecorded species at La Cena del Depósito concession, Cerro Minado Mines, Cuesta Alta, Huércal-Overa, Almería, Andalusia, Spain

This table is based on statistical analysis of other localities containing similar species to the ones found at this locality.

Possible missing speciesFormulaMatch %Due to recorded presence of
SphaleriteZnS99.99%Acanthite (62.85 %), Adamite (55.00 %), Ankerite (53.36 %), Annabergite (52.59 %), Aurichalcite (70.37 %), Brochantite (50.32 %), Chalcopyrite (50.66 %), Cobaltite (60.74 %), Covellite (64.68 %), Digenite (61.34 %), Erythrite (50.44 %), Galena (65.95 %), Gersdorffite (65.94 %), Hörnesite (52.80 %), Juanitaite (50.00 %), Luanheite (68.42 %), Millerite (50.48 %), Parnauite (50.40 %), Pitticite (60.00 %), Proustite (64.85 %), Pyrargyrite (69.84 %), Rosasite (67.03 %), Schachnerite (68.75 %), Siegenite (68.94 %), Smithsonite (72.43 %), Zincolivenite (54.88 %)
CerussitePbCO399.91%Adamite (60.00 %), Aurichalcite (64.77 %), Capgaronnite (50.00 %), Juanitaite (50.00 %), Parnauite (51.20 %), Rosasite (73.63 %), Smithsonite (55.69 %), Zincolivenite (58.54 %)
ArsenopyriteFeAsS99.56%Gersdorffite (50.38 %), Hörnesite (52.00 %), Luanheite (57.89 %), Pitticite (66.67 %), Schachnerite (50.00 %), Scorodite (74.10 %)
GypsumCaSO4 · 2H2O99.44%Belloite (57.14 %), Clinoatacamite (60.71 %), Hörnesite (62.40 %), Lavendulan (59.65 %), Rouaite (56.25 %), Schachnerite (50.00 %)
MimetitePb5(AsO4)3Cl99.13%Adamite (58.67 %), Capgaronnite (50.00 %), Juanitaite (75.00 %), Parnauite (51.20 %), Zincolivenite (65.85 %)
HemimorphiteZn4Si2O7(OH)2 · H2O91.01%Aurichalcite (50.47 %), Juanitaite (50.00 %), Rosasite (63.74 %)
AnglesitePbSO488.50%Capgaronnite (50.00 %), Rosasite (54.03 %), Zincolivenite (50.00 %)
ArthuriteCuFe3+2(AsO4)2(OH)2 · 4H2O83.33%Auriacusite (66.67 %), Juanitaite (50.00 %)
PharmacosideriteKFe3+4(AsO4)3(OH)4 · 6-7H2O83.33%Auriacusite (83.33 %)
PyrrhotiteFe1-xS79.10%Cobaltite (57.03 %), Gersdorffite (51.37 %)
KettneriteCaBiCO3OF75.00%Juanitaite (75.00 %)
PerrouditeHg5Ag4S5(I,Br)2Cl275.00%Capgaronnite (75.00 %)
AtelestiteBi2(AsO4)O(OH)62.50%Juanitaite (62.50 %)
BeudantitePbFe3(AsO4)(SO4)(OH)662.50%Juanitaite (62.50 %)
BismuthiniteBi2S362.50%Juanitaite (62.50 %)
ClausthalitePbSe57.54%Tiemannite (57.55 %)
MetacinnabarHgS56.41%Eglestonite (56.41 %)
Terlinguaite[Hg3]4+Hg2+Cl2O253.84%Eglestonite (53.85 %)
LangiteCu4(SO4)(OH)6 · 2H2O53.60%Parnauite (53.60 %)
BariopharmacosideriteBa0.5Fe3+4(AsO4)3(OH)4 · 5H2O50.00%Juanitaite (50.00 %)
BayldonitePbCu3(AsO4)2(OH)250.00%Juanitaite (50.00 %)
Bismutite(BiO)2CO350.00%Juanitaite (50.00 %)
CarminitePbFe3+2(AsO4)2(OH)250.00%Juanitaite (50.00 %)
EnargiteCu3AsS450.00%Juanitaite (50.00 %)
LinaritePbCu(SO4)(OH)250.00%Juanitaite (50.00 %)
PreisingeriteBi3(AsO4)2O(OH)50.00%Juanitaite (50.00 %)
StrashimiriteCu8(AsO4)4(OH)4 · 5H2O50.00%Juanitaite (50.00 %)

Key: Mineral matches key element mineralogy of deposit Key element(s) in mineral not listed for deposit (-20% score)


Predicting paragenetic modes of deposit

Green indicates almost certain match based on minerals unique to a certain deposit type. Yellow indicates a possibly poor match, but should not be entirely discounted. Scores > 100 indicate strong confidence.

Paragenetic ModeScore
33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12])

Unique: Proustite, Pyrargyrite, Schachnerite, Tiemannite
484
47g : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Halogen-bearing surface weathering minerals]

Unique: Calomel, Chlorargyrite, Iodargyrite
345
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]256
47d : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates]175
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]

Unique: Smithsonite
142
12 : Hadean hydrothermal subsurface sulfide deposits (see also #33)

Unique: Siegenite
101
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)

Unique: Spherocobaltite
100
31 : Thermally altered carbonate, phosphate, and iron formations

Unique: Hörnesite
100
37 : Layered igneous intrusions and related PGE minerals38
56 : Slag and smelter minerals (see also #51 and #55)34
47h : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]32
52 : Guano- and urine-derived minerals25
49 : Oxic cellular biomineralization (see also #44)14
26 : Hadean detrital minerals13
55 : Anthropogenic mine minerals12
53 : Other minerals with taphonomic origins10