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: BaCCaMgOSSrElements from minerals reported directly at this locality: Ba C Ca Mg O S Sr Structural Groups for minerals in this locality:
MAGMATIC STYLE: Irregular sheet, dykes and veins. ASSOCIATED SILICATE ROCKS: Potassic shonkinite, syenite, granite and fenite.
Jen_0001042
MAGMATIC STYLE: Irregular sheet, dykes and veins. ASSOCIATED SILICATE ROCKS: Potassic shonkinite, syenite, granite and fenite.
Jen_0001043
MAGMATIC STYLE: Irregular sheet, dykes and veins. ASSOCIATED SILICATE ROCKS: Potassic shonkinite, syenite, granite and fenite.
Jen_0001044
MAGMATIC STYLE: Irregular sheet, dykes and veins. ASSOCIATED SILICATE ROCKS: Potassic shonkinite, syenite, granite and fenite.
Jen_0001045
MAGMATIC STYLE: Irregular sheet, dykes and veins. ASSOCIATED SILICATE ROCKS: Potassic shonkinite, syenite, granite and fenite.
Jen_0001046
MAGMATIC STYLE: Irregular sheet, dykes and veins. ASSOCIATED SILICATE ROCKS: Potassic shonkinite, syenite, granite and fenite.
Michelle_0261_a
Sahamalite occurs in the Sulphide Queen Mine of the Mountain Pass Deposit, closely associated with parisite and bastnaesite (as described in reference).
Age of carbonatite. Emplacement of carbonatite was the final event in the intrusion of the 1400 ma complex. Clear parisite coexists with younger bastnaesite in sample.
Sample
Source Locality
Reference URL
All locality data graciously provided by mindat.org