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.
This mineral is using an age reported as an element mineralization period.
O
This mineral is using an age calculated from all data at the locality.
R
The age displayed for this mineral originates from a different, non-child locality.
P
The 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: AlBaCCaCeClFFeHKLnMgNaNbNdOPPbSSiTaThTiZrElements from minerals reported directly at this locality: Al Ba C Ca Ce Cl F Fe H K Ln Mg Na Nb Nd O P Pb S Si Th Ti Zr Structural Groups for minerals in this locality:
MAGMATIC STYLE: Dykes and possible dolomitized carbonatite tuff. ASSOCIATED SILICATE ROCKS: There are extensive peralkaline granites but their relationship, if any, to the carbonatites is not clear. Basic dykes and brecciated peridotite also occur.
Jen_0001115
MAGMATIC STYLE: Dykes and possible dolomitized carbonatite tuff. ASSOCIATED SILICATE ROCKS: There are extensive peralkaline granites but their relationship, if any, to the carbonatites is not clear. Basic dykes and brecciated peridotite also occur.
Jen_0001116
MAGMATIC STYLE: Dykes and possible dolomitized carbonatite tuff. ASSOCIATED SILICATE ROCKS: There are extensive peralkaline granites but their relationship, if any, to the carbonatites is not clear. Basic dykes and brecciated peridotite also occur.
Jen_0001117
MAGMATIC STYLE: Dykes and possible dolomitized carbonatite tuff. ASSOCIATED SILICATE ROCKS: There are extensive peralkaline granites but their relationship, if any, to the carbonatites is not clear. Basic dykes and brecciated peridotite also occur.
Jen_0001118
MAGMATIC STYLE: Dykes and possible dolomitized carbonatite tuff. ASSOCIATED SILICATE ROCKS: There are extensive peralkaline granites but their relationship, if any, to the carbonatites is not clear. Basic dykes and brecciated peridotite also occur.
Jen_0001119
MAGMATIC STYLE: Dykes and possible dolomitized carbonatite tuff. ASSOCIATED SILICATE ROCKS: There are extensive peralkaline granites but their relationship, if any, to the carbonatites is not clear. Basic dykes and brecciated peridotite also occur.
Jen_0001120
MAGMATIC STYLE: Dykes and possible dolomitized carbonatite tuff. ASSOCIATED SILICATE ROCKS: There are extensive peralkaline granites but their relationship, if any, to the carbonatites is not clear. Basic dykes and brecciated peridotite also occur.
Bayan Obo Deposit (Bayun-Obo Deposit; Baiyunebo Deposit), Bayan Obo, Bayan Obo Mining District, Baotou League (Baotou Prefecture), Inner Mongolia, China
Bayan Obo Deposit (Bayun-Obo Deposit; Baiyunebo Deposit), Bayan Obo, Bayan Obo Mining District, Baotou League (Baotou Prefecture), Inner Mongolia, China
Bayan Obo Deposit (Bayun-Obo Deposit; Baiyunebo Deposit), Bayan Obo, Bayan Obo Mining District, Baotou League (Baotou Prefecture), Inner Mongolia, China
Bayan Obo Deposit (Bayun-Obo Deposit; Baiyunebo Deposit), Bayan Obo, Bayan Obo Mining District, Baotou League (Baotou Prefecture), Inner Mongolia, China
Bayan Obo Deposit (Bayun-Obo Deposit; Baiyunebo Deposit), Bayan Obo, Bayan Obo Mining District, Baotou League (Baotou Prefecture), Inner Mongolia, China
Bayan Obo Deposit (Bayun-Obo Deposit; Baiyunebo Deposit), Bayan Obo, Bayan Obo Mining District, Baotou League (Baotou Prefecture), Inner Mongolia, China
Bayan Obo Deposit (Bayun-Obo Deposit; Baiyunebo Deposit), Bayan Obo, Bayan Obo Mining District, Baotou League (Baotou Prefecture), Inner Mongolia, China
Bayan Obo Deposit (Bayun-Obo Deposit; Baiyunebo Deposit), Bayan Obo, Bayan Obo Mining District, Baotou League (Baotou Prefecture), Inner Mongolia, China
The combination of textural evidence and isotopic data from this study indicates that intermittent REE mineralization of the Bayan Obo deposit started at about 555 Ma, and the principal mineralization related to Caledonian subduction occurred between 474 and 400 Ma.; The most important results of this study indicate that (1) the large database of precise chronology, in conjunction with mineral replacement relation, provides evidence for a prolonged period of mineralization within the giant Bayan Obo orebody and (2) lead and neodymium isotopic compositions indicate that the source for the ores was depleted in uranium but enriched in thorium and LREEs.; note spelling as Bastnaesite in lit.
Sample
Source Locality
Reference URL
All locality data graciously provided by mindat.org