Mineral Evolution Database
Created and maintained by the Mineral Evolution Project in partnership with RRUFF and mindat.
Mineral locality data provided by mindat.org



The Mineral Evolution database is currently under development.

The goal of this page is to present localities at which the mineral is found, and estimates of the oldest possible geologic age of the minerals at these localities.


Locality Name:
Aldama Municipality, Chihuahua, Mexico

Oldest recorded age at locality: 53.8
Youngest recorded age at locality: 1.85

mindat Locality ID: 17024
mindat URL: http://www.mindat.org/loc-17024.html

Tectonic Settings:

Total number of sublocalities beneath "Aldama Municipality, Chihuahua, Mexico": 43
Total number of bottom-level sublocalities: 35

Number of Child Localities: 10
Child Localities:
Aldama
El Pastor
Estacion Trancas
Juan Aldama
Las Choyas
Las Plomosas
Peña Blanca District
Placer De Guadalupe
Puerto Del Aire
Sierra Del Cuervo

Latitude: 29°3'18"N
Longitude: 105°40'40"W
Decimal Degree (lat, lon): 29.055,-105.67777777778

AThis mineral is Anthropogenic.
GThis mineral is directly dated.
BThis mineral is reported as having this age.
YThis mineral is using an age reported as an element mineralization period.
OThis mineral is using an age calculated from all data at the locality.
RThe age displayed for this mineral originates from a different, non-child locality.
PThe age displayed for this mineral is the range of ages for this mineral at all of this locality's children.
This mineral's age has not yet been recorded.

This Mineral list contains entries from this locality, including sub-localities. Minerals in bold are reported by mindat.org as occurring directly at this locality, and do not occur at any children (sublocalities) of this locality.

Elements at this locality, including sub-localities: Al As Au Ba C Ca Cs Cu Fe H K Mg Mn Mo Na Nb O P Pb S Si Sr Ti U V Y Zn 

Elements from minerals reported directly at this locality: 

Structural Groups for minerals in this locality: 
AluniteAmorphousApatiteAragoniteBranneriteCalciteClayCopperCoronaditeCorundum
DiasporeFluoriteFritzscheiteGypsumKaoliniteMicaMolybdeniteMordeniteNonePhosphuranylite
PyriteQuartzRamsdelliteRutileScheeliteSchoepiteSengieriteSmectite-vermiculiteSpinelTitanite

54 IMA Minerals at location:
Alunite  (*)Becquerelite  (*)Beidellite  (*)Birnessite  (*)Boltwoodite  (*)
Calcite  (*)Carnotite  (*)Cerussite  (*)Copper  (*)Cryptomelane  (*)
Fergusonite-(Y)  (*)Goethite  (*)Gold  (*)Gypsum  (*)Haiweeite  (*)
Hematite  (*)Hollandite  (*)Nováčekite-I  (*)Hydroxylapatite  (*)Hydrozincite  (*)
Ianthinite  (*)Ilmenite  (*)Jarosite  (*)Kaolinite  (*)Kasolite  (*)
Magnetite  (*)Margaritasite  (*)Metaschoepite  (*)Metatyuyamunite  (*)Molybdenite  (*)
Montmorillonite  (*)Mordenite  (*)Muscovite  (*)Opal  (*)Orthobrannerite  (*)
Uranophane-β  (*)Phosphuranylite  (*)Powellite  (*)Pyrite  (*)Pyrolusite  (*)
Quartz  (*)Ramsdellite  (*)Ranciéite  (*)Rutile  (*)Schoepite  (*)
Siderite  (*)Soddyite  (*)Titanite  (*)Todorokite  (*)Tyuyamunite  (*)
Uraninite  (*)Uranophane-α  (*)Vorlanite  (*)Weeksite  (*)
Mineral nameStructural GroupsIMA FormulaMax Age (Ma)Min Age (Ma)# of Sublocalities containing mineralLOCALITY IDs, not mindat ids# of localities containing mineral
Alunite  (*)NoneKAl3(SO4)2(OH)644.951.85281648,81651966
Becquerelite  (*)NoneCa(UO2)6O4(OH)6·8H2O13.12.718165192
Beidellite  (*)Clay Smectite-vermiculite(Na,Ca)0.3Al2(Si,Al)4O10(OH)2·nH2O18163985
Birnessite  (*)None(Na,Ca,K)0.6(Mn4+,Mn3+)2O4·1.5H2O181639178
Boltwoodite  (*)None(K,Na)(UO2)(SiO3OH)·1.5H2O13.12.718165167
Calcite  (*)CalciteCa(CO3)44.71.85381639,81651,8166227770
Carnotite  (*)NoneK2(UO2)2(VO4)2·3H2O44.952.7581648,81649,81651,81652,816531184
Cerussite  (*)AragonitePb(CO3)1816344979
Copper  (*)CopperCu1816363846
Cryptomelane  (*)CoronaditeK(Mn4+7Mn3+)O16181639599
Fergusonite-(Y)  (*)ScheeliteYNbO4181669196
Goethite  (*)DiasporeFeO(OH)44.71.85281639,816517437
Gold  (*)CopperAu581660,81662,81666,81669,8167330554
Gypsum  (*)GypsumCa(SO4)·2H2O1816396890
Haiweeite  (*)NoneCa(UO2)2(Si5O12)(OH)2·6H2O44.9538.3281648,8165015
Hematite  (*)CorundumFe2O344.71.85281639,8165114640
Hollandite  (*)CoronaditeBa(Mn4+6Mn3+2)O16181639243
Nováčekite-I  (*)NoneMg(UO2)2(AsO4)2·12H2O18167355
Hydroxylapatite  (*)ApatiteCa5(PO4)3OH181639367
Hydrozincite  (*)NoneZn5(CO3)2(OH)633.9231816411066
Ianthinite  (*)NoneU4+2(UO2)4O6(OH)4·9H2O44.952.7281650,8165131
Ilmenite  (*)CorundumFe2+Ti4+O344.71.851816515433
Jarosite  (*)AluniteKFe3+3(SO4)2(OH)644.951.85381642,81648,816512228
Kaolinite  (*)Clay KaoliniteAl2Si2O5(OH)444.951.85481639,81648,81651,816565591
Kasolite  (*)NonePb(UO2)(SiO4)·H2O44.9538.3181654198
Magnetite  (*)SpinelFe2+Fe3+2O444.71.8518165114899
Margaritasite  (*)SengieriteCs2(UO2)2(VO4)2·H2O44.9538.3281648,816492
Metaschoepite  (*)Schoepite(UO2)8O2(OH)12·10H2O13.12.718165117
Metatyuyamunite  (*)FritzscheiteCa(UO2)2(VO4)2·3H2O181675129
Molybdenite  (*)MolybdeniteMoS244.9538.31816485800
Montmorillonite  (*)Clay Smectite-vermiculite(Na,Ca)0.3(Al,Mg)2Si4O10(OH)2·nH2O44.71.85281651,816561508
Mordenite  (*)Mordenite(Na2,Ca,K2)4(Al8Si40)O96·28H2O181639405
Muscovite  (*)Mica ClayKAl2(Si3Al)O10(OH)218166217380
Opal  (*)AmorphousSiO2·nH2O44.951.85481637,81639,81648,816512994
Orthobrannerite  (*)BranneriteU4+U6+Ti4O12(OH)213.12.71816515
Uranophane-β  (*)NoneCa(UO2)2(SiO3OH)2·5H2O44.952.7381648,81651,81653144
Phosphuranylite  (*)PhosphuranyliteKCa(H3O)3(UO2)7(PO4)4O4·8H2O44.9538.3181648182
Powellite  (*)ScheeliteCa(MoO4)44.951.85281648,81651494
Pyrite  (*)PyriteFeS244.951.85481648,81651,81660,8166239462
Pyrolusite  (*)RutileMnO21816393106
Quartz  (*)QuartzSiO244.951.85681637,81638,81639,81648,81651,8165661156
Ramsdellite  (*)RamsdelliteMnO218163988
Ranciéite  (*)None(Ca,Mn2+)0.2(Mn4+,Mn3+)O2·0.6H2O181639177
Rutile  (*)RutileTiO244.71.851816515614
Schoepite  (*)Schoepite(UO2)4O(OH)6(H2O)644.952.7281650,8165194
Siderite  (*)CalciteFe(CO3)1816396417
Soddyite  (*)None(UO2)2(SiO4)(H2O)244.952.7281650,8165144
Titanite  (*)TitaniteCaTi(SiO4)O44.71.851816514899
Todorokite  (*)None(Na,Ca,K,Ba,Sr)1-x(Mn,Mg,Al)6O12·3-4H2O181639433
Tyuyamunite  (*)NoneCa(UO2)2(VO4)2·5-8H2O44.9538.3181648628
Uraninite  (*)FluoriteUO244.952.71581648,81649,81650,81651,81660,81661,81662,81664,81665,81667,81668,81669,81670,81671,816722718
Uranophane-α  (*)NoneCa(UO2)2(SiO3OH)2·5H2O44.952.7681648,81650,81651,81653,81656,81662890
Vorlanite  (*)FluoriteCaUO413.12.71816515
Weeksite  (*)None(K)2(UO2)2(Si5O13)·4H2O44.952.7581648,81649,81651,81652,8165342



Locality Notes from all Ages at Locality:
Age IDLocality Notes
Giersdorf_00000810The Nopal I deposit is part of a Basin and Range horst composed of Tertiary rhyolitic tufts underlain by carbonate sedimentary rocks as is Yucca Mountain (Mesozoic carbonates at Nopal, Paleozoic carbonates at Yucca Mountain). Further, both the proposed Yucca Mountain repository horizon and the Nopal I deposit are located in the oxidizing, hydrologically unsaturated zone 100 m or more above the water table. The locality is similar chemically to the Yucca Mountain locality and is studied due to the chemical environment being ideal to store nuclear waste.
Giersdorf_00000811The Nopal I deposit is part of a Basin and Range horst composed of Tertiary rhyolitic tufts underlain by carbonate sedimentary rocks as is Yucca Mountain (Mesozoic carbonates at Nopal, Paleozoic carbonates at Yucca Mountain). Further, both the proposed Yucca Mountain repository horizon and the Nopal I deposit are located in the oxidizing, hydrologically unsaturated zone 100 m or more above the water table. The locality is similar chemically to the Yucca Mountain locality and is studied due to the chemical environment being ideal to store nuclear waste.
Giersdorf_00000812The Nopal I deposit is part of a Basin and Range horst composed of Tertiary rhyolitic tufts underlain by carbonate sedimentary rocks as is Yucca Mountain (Mesozoic carbonates at Nopal, Paleozoic carbonates at Yucca Mountain). Further, both the proposed Yucca Mountain repository horizon and the Nopal I deposit are located in the oxidizing, hydrologically unsaturated zone 100 m or more above the water table. The locality is similar chemically to the Yucca Mountain locality and is studied due to the chemical environment being ideal to store nuclear waste.
Giersdorf_00000813The Nopal I deposit is part of a Basin and Range horst composed of Tertiary rhyolitic tufts underlain by carbonate sedimentary rocks as is Yucca Mountain (Mesozoic carbonates at Nopal, Paleozoic carbonates at Yucca Mountain). Further, both the proposed Yucca Mountain repository horizon and the Nopal I deposit are located in the oxidizing, hydrologically unsaturated zone 100 m or more above the water table. The locality is similar chemically to the Yucca Mountain locality and is studied due to the chemical environment being ideal to store nuclear waste.
Giersdorf_00000814The Nopal I deposit is part of a Basin and Range horst composed of Tertiary rhyolitic tufts underlain by carbonate sedimentary rocks as is Yucca Mountain (Mesozoic carbonates at Nopal, Paleozoic carbonates at Yucca Mountain). Further, both the proposed Yucca Mountain repository horizon and the Nopal I deposit are located in the oxidizing, hydrologically unsaturated zone 100 m or more above the water table. The locality is similar chemically to the Yucca Mountain locality and is studied due to the chemical environment being ideal to store nuclear waste.
Giersdorf_00000815The Nopal I deposit is part of a Basin and Range horst composed of Tertiary rhyolitic tufts underlain by carbonate sedimentary rocks as is Yucca Mountain (Mesozoic carbonates at Nopal, Paleozoic carbonates at Yucca Mountain). Further, both the proposed Yucca Mountain repository horizon and the Nopal I deposit are located in the oxidizing, hydrologically unsaturated zone 100 m or more above the water table. The locality is similar chemically to the Yucca Mountain locality and is studied due to the chemical environment being ideal to store nuclear waste.
Giersdorf_00000816The Nopal I deposit is part of a Basin and Range horst composed of Tertiary rhyolitic tufts underlain by carbonate sedimentary rocks as is Yucca Mountain (Mesozoic carbonates at Nopal, Paleozoic carbonates at Yucca Mountain). Further, both the proposed Yucca Mountain repository horizon and the Nopal I deposit are located in the oxidizing, hydrologically unsaturated zone 100 m or more above the water table. The locality is similar chemically to the Yucca Mountain locality and is studied due to the chemical environment being ideal to store nuclear waste.
Giersdorf_00000817The Nopal I deposit is part of a Basin and Range horst composed of Tertiary rhyolitic tufts underlain by carbonate sedimentary rocks as is Yucca Mountain (Mesozoic carbonates at Nopal, Paleozoic carbonates at Yucca Mountain). Further, both the proposed Yucca Mountain repository horizon and the Nopal I deposit are located in the oxidizing, hydrologically unsaturated zone 100 m or more above the water table. The locality is similar chemically to the Yucca Mountain locality and is studied due to the chemical environment being ideal to store nuclear waste.
Giersdorf_00000818The Nopal I deposit is part of a Basin and Range horst composed of Tertiary rhyolitic tufts underlain by carbonate sedimentary rocks as is Yucca Mountain (Mesozoic carbonates at Nopal, Paleozoic carbonates at Yucca Mountain). Further, both the proposed Yucca Mountain repository horizon and the Nopal I deposit are located in the oxidizing, hydrologically unsaturated zone 100 m or more above the water table. The locality is similar chemically to the Yucca Mountain locality and is studied due to the chemical environment being ideal to store nuclear waste.
Giersdorf_00000955The Sierra Peña Blanca is located to the north of Aldama City (Chihuahua State). It corresponds to an uplifted faulted block about 80 km long and 15 to 20 km wide, of Mesozoic and Cenozoic rocks, surrounded by basins to the west and the east. The average elevation of the sierra is 1,800 m, whereas the basins are around 1,600 m and decrease gradually eastward. This sierra,as well as other sierras belonging to the Basin and Range system, presents a general northward strike, with a tilt to the west.
Giersdorf_00000955bThe Sierra Peña Blanca is located to the north of Aldama City (Chihuahua State). It corresponds to an uplifted faulted block about 80 km long and 15 to 20 km wide, of Mesozoic and Cenozoic rocks, surrounded by basins to the west and the east. The average elevation of the sierra is 1,800 m, whereas the basins are around 1,600 m and decrease gradually eastward. This sierra,as well as other sierras belonging to the Basin and Range system, presents a general northward strike, with a tilt to the west.
Giersdorf_00000956The Sierra Peña Blanca is located to the north of Aldama City (Chihuahua State). It corresponds to an uplifted faulted block about 80 km long and 15 to 20 km wide, of Mesozoic and Cenozoic rocks, surrounded by basins to the west and the east. The average elevation of the sierra is 1,800 m, whereas the basins are around 1,600 m and decrease gradually eastward. This sierra,as well as other sierras belonging to the Basin and Range system, presents a general northward strike, with a tilt to the west.
Giersdorf_00000957The Sierra Peña Blanca is located to the north of Aldama City (Chihuahua State). It corresponds to an uplifted faulted block about 80 km long and 15 to 20 km wide, of Mesozoic and Cenozoic rocks, surrounded by basins to the west and the east. The average elevation of the sierra is 1,800 m, whereas the basins are around 1,600 m and decrease gradually eastward. This sierra,as well as other sierras belonging to the Basin and Range system, presents a general northward strike, with a tilt to the west.
Giersdorf_00000958The Sierra Peña Blanca is located to the north of Aldama City (Chihuahua State). It corresponds to an uplifted faulted block about 80 km long and 15 to 20 km wide, of Mesozoic and Cenozoic rocks, surrounded by basins to the west and the east. The average elevation of the sierra is 1,800 m, whereas the basins are around 1,600 m and decrease gradually eastward. This sierra,as well as other sierras belonging to the Basin and Range system, presents a general northward strike, with a tilt to the west.
Giersdorf_00000959The Sierra Peña Blanca is located to the north of Aldama City (Chihuahua State). It corresponds to an uplifted faulted block about 80 km long and 15 to 20 km wide, of Mesozoic and Cenozoic rocks, surrounded by basins to the west and the east. The average elevation of the sierra is 1,800 m, whereas the basins are around 1,600 m and decrease gradually eastward. This sierra,as well as other sierras belonging to the Basin and Range system, presents a general northward strike, with a tilt to the west.
Giersdorf_00000960The Nopal 1 Deposit is confined to a breccia zone or pipe, limited to by faults. The breccia pipe is 100m high x 20m x 40m wide. The deposit is found within the Nopal Rhyolite. Uranium minerals found in the deposit are primarily oxidized.
Giersdorf_00000961The Las Margaritas Deposit is hosedted by the Escuadra Formation and is found on the axis of a tectonic valley.
Giersdorf_00000962The Puerto 3 deposit is located to the northwest of the Las Margaritas deposit and is hosted by the Nopal Rhyolite overlain by the Escuadra Formation.


20 Ages assigned to this locality:

Excel IDMax Age (Ma)Min Age (Ma)Age as listed in referenceDating MethodAge InterpretPrioritized?Sample SourceSample NumRun NumAge from other LocalityDated MineralMinerals explicitely stated as having this ageAge applies to these ElementsMinDat Locality IDDated Locality (Max Age)Location as listed in referenceReferenceReference DOIReference IDAge Notes
Giersdorf_00000823b4444<44      Uraninite 22313Peña Blanca District, Aldama Municipality, Chihuahua, Mexico     
Giersdorf_0000095553.853.853.8-42.2        17023Sierra Peña Blanca, Peña Blanca District, Aldama Municipality, Chihuahua, MexicoPeña BlancaGeorge-Aniel et al. (1991)10.2113/gsecongeo.86.2.233EG86_233The age of 53.8 is given for altered biotites and 42.2 is given for sanidine. This is the referred to in the literature as unit 1.
Giersdorf_00000955b4242         17023Sierra Peña Blanca, Peña Blanca District, Aldama Municipality, Chihuahua, MexicoPeña BlancaGeorge-Aniel et al. (1991)10.2113/gsecongeo.86.2.233EG86_233The age of 53.8 is given for altered biotites and 42.2 is given for sanidine. This is the referred to in the literature as unit 1.
Giersdorf_0000095644.742.943.8±0.9  sanidine   Sanidine  17023Sierra Peña Blanca, Peña Blanca District, Aldama Municipality, Chihuahua, MexicoPeña BlancaGeorge-Aniel et al. (1991)10.2113/gsecongeo.86.2.233EG86_233Age given for the Nopal rhyolite which underlies what was previously referred to as the Escuadra Formation. The two are occasionally separated by a thin layer of pumice, but together make up what is referred to as unit 2 in the literature.
Giersdorf_0000095745.443.644.5±0.9  sanidine   Sanidine  17023Sierra Peña Blanca, Peña Blanca District, Aldama Municipality, Chihuahua, MexicoPeña BlancaGeorge-Aniel et al. (1991)10.2113/gsecongeo.86.2.233EG86_233Age given for what was previously referred to as the Escuadra formation, which overlies the Nopal Rhyolite. The two are occasionally separated by a thin layer of pumice, but together make up what is referred to as unit 2 in the literature.
Giersdorf_0000095838.338.338.3 After approximately a 6 Ma hiatus, which is generalized in all of the surrounding areas, volcanic activity started again and formed the top part of the Escuadra Formation.sanidine   Sanidine  17023Sierra Peña Blanca, Peña Blanca District, Aldama Municipality, Chihuahua, MexicoPeña BlancaGeorge-Aniel et al. (1991)10.2113/gsecongeo.86.2.233EG86_233Age given for the upper part of the Escuadra Formation, still a component of Unit 2.
Giersdorf_0000095937.337.337.3 The age of the Mesa Formation is given to be the youngest volcanogenic rock of the area.sanidine   Sanidine  17023Sierra Peña Blanca, Peña Blanca District, Aldama Municipality, Chihuahua, MexicoPeña BlancaGeorge-Aniel et al. (1991)10.2113/gsecongeo.86.2.233EG86_233The Mesa formation is a component of what is referred to as Unit 5 of the locality.
Giersdorf_0000096144.9538.344.95-38.3      Carnotite, Margaritasite, Molybdenite, Phosphuranylite, Powellite, Tyuyamunite, Uranophane, ParauranophaneU15672Margaritas No. 1 Mine, Sierra Peña Blanca, Peña Blanca District, Aldama Municipality, Chihuahua, MexicoLas MargaritasGeorge-Aniel et al. (1991)10.2113/gsecongeo.86.2.233EG86_233Age of the deposit is given by the window of ages for the Escuadra Formation.
Giersdorf_0000081043.843.843.8 The age of 43.8 is provided as a constrant on the maximum possible uranium mineralization age as that is the age given to the host rock.      17009Nopal No. 1 Mine, Sierra Peña Blanca, Peña Blanca District, Aldama Municipality, Chihuahua, MexicoNopal I minePearcy et al. (1994)10.1016/0883-2927(94)90030-2AG9_713 
Giersdorf_0000081113.12.77.9±5.2U-PbAge is the average age from microprobe analysis on 7 sampleshighuraninite   UraniniteBecquerelite, Boltwoodite, Ianthinite, Schoepite, Soddyite, Uraninite, WeeksiteU17009Nopal No. 1 Mine, Sierra Peña Blanca, Peña Blanca District, Aldama Municipality, Chihuahua, MexicoNopal I minePearcy et al. (1994)10.1016/0883-2927(94)90030-2AG9_713 
Giersdorf_0000081211.587.729.65±1.93U-Pb uraninite32-ts2-p1  UraniniteBecquerelite, Boltwoodite, Ianthinite, Schoepite, Soddyite, Uraninite, WeeksiteU17009Nopal No. 1 Mine, Sierra Peña Blanca, Peña Blanca District, Aldama Municipality, Chihuahua, MexicoNopal I minePearcy et al. (1994)10.1016/0883-2927(94)90030-2AG9_713 
Giersdorf_0000081310.16.088.09±2.01U-Pb uraninite32-ts2-p4  UraniniteBecquerelite, Boltwoodite, Ianthinite, Schoepite, Soddyite, Uraninite, WeeksiteU17009Nopal No. 1 Mine, Sierra Peña Blanca, Peña Blanca District, Aldama Municipality, Chihuahua, MexicoNopal I minePearcy et al. (1994)10.1016/0883-2927(94)90030-2AG9_713 
Giersdorf_000008145.551.853.7±1.85U-Pb uraninite32-ts2-p5  UraniniteBecquerelite, Boltwoodite, Ianthinite, Schoepite, Soddyite, Uraninite, WeeksiteU17009Nopal No. 1 Mine, Sierra Peña Blanca, Peña Blanca District, Aldama Municipality, Chihuahua, MexicoNopal I minePearcy et al. (1994)10.1016/0883-2927(94)90030-2AG9_713 
Giersdorf_0000081515.2111.4113.31±1.9U-Pb uraninite32-ts2-p6  UraniniteBecquerelite, Boltwoodite, Ianthinite, Schoepite, Soddyite, Uraninite, WeeksiteU17009Nopal No. 1 Mine, Sierra Peña Blanca, Peña Blanca District, Aldama Municipality, Chihuahua, MexicoNopal I minePearcy et al. (1994)10.1016/0883-2927(94)90030-2AG9_713 
Giersdorf_0000081612.368.2610.31±2.05U-Pb uraninite1-ts3-p1  UraniniteBecquerelite, Boltwoodite, Ianthinite, Schoepite, Soddyite, Uraninite, WeeksiteU17009Nopal No. 1 Mine, Sierra Peña Blanca, Peña Blanca District, Aldama Municipality, Chihuahua, MexicoNopal I minePearcy et al. (1994)10.1016/0883-2927(94)90030-2AG9_713 
Giersdorf_000008176.222.084.15±2.07U-Pb uraninite1-ts3-p2  UraniniteBecquerelite, Boltwoodite, Ianthinite, Schoepite, Soddyite, Uraninite, WeeksiteU17009Nopal No. 1 Mine, Sierra Peña Blanca, Peña Blanca District, Aldama Municipality, Chihuahua, MexicoNopal I minePearcy et al. (1994)10.1016/0883-2927(94)90030-2AG9_713 
Giersdorf_000008188.124.066.09±2.03U-Pb uraninite1-ts3-p6  UraniniteBecquerelite, Boltwoodite, Ianthinite, Schoepite, Soddyite, Uraninite, WeeksiteU17009Nopal No. 1 Mine, Sierra Peña Blanca, Peña Blanca District, Aldama Municipality, Chihuahua, MexicoNopal I minePearcy et al. (1994)10.1016/0883-2927(94)90030-2AG9_713 
Giersdorf_0000096044.742.943.8±0.9 The Nopal 1 Deposit and similar deposits are described as forming at the same time as the Nopal Rhyolite and are attributed its age.    UraniniteU17009Nopal No. 1 Mine, Sierra Peña Blanca, Peña Blanca District, Aldama Municipality, Chihuahua, MexicoNopal I mineGeorge-Aniel et al. (1991)10.2113/gsecongeo.86.2.233EG86_233The Nopal 1 Deposit is used to describe the formation age of other similar deposits found in the Sierra Peña Blanca area, and are all found within the Nopal Rhyolite.
Giersdorf_0000096244.742.943.8±0.9      Kaolinite, Montmorillonite, Uranophane, ParauranophaneU208595Puerto No. 3 Mine, Sierra Peña Blanca, Peña Blanca District, Aldama Municipality, Chihuahua, MexicoPuerto 3 mineGeorge-Aniel et al. (1991)10.2113/gsecongeo.86.2.233EG86_233The age is derived from the age of the host Nopal Rhyolite.
sedznpb-0031533.923Oligocene     Yes  18802Plomosas Mine, Las Plomosas, Coyame Municipality, Chihuahua, MexicoPlomosasSinger et al. (2009) USGSOFR2009-1252 


SampleSource LocalityReference URL
R060461Margaritas No. 1 Mine, Sierra Peña Blanca, Peña Blanca District, Aldama Municipality, Chihuahua, Mexicohttps://rruff.info/R060461


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