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: AlAsAuBBaBiCCaCdCuFeHHgKMgNaNiOPbSSbSiTeTiWZnElements from minerals reported directly at this locality: Structural Groups for minerals in this locality:
Model derived primarily from studies conducted in the Mount Tom Price mine but with supplemental information acquired from the Channar and Mount Whaleback
Giersdorf_00000216
Model derived primarily from studies conducted in the Mount Tom Price mine but with supplemental information acquired from the Channar and Mount Whaleback
Michelle_323
Porphyry intrudes upper members of the Archaean greenstones of the Warrawoona Group
Michelle_510
Deposit occurs in Archean serpentinized peridotite. It is the TL for three carbon minerals, paraotwayite, otwayite, and nullaginite, that occur as secondary mineralization in shear zones of the deposit. The veinlets cut all other minerals and appear to be late stage and low temperature in origin.
Michelle_512
Deposit occurs in Archean serpentinized peridotite. The serpentinite has undergone extensive alteration by shearing and silicification. Otway deposit is the TL for three carbon minerals, paraotwayite, otwayite, and nullaginite, that occur as secondary mineralization in shear zones of the deposit. The veinlets cut all other minerals and appear to be late stage and low temperature in origin.