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: AgAlAsAuBBeBiCCaClCoCrCuFFeHIrKMgMnMoNaNiOOsPPbRuSSbSiSnTiWZnElements from minerals reported directly at this locality: C Fe H Mg O Structural Groups for minerals in this locality:
Lord Brassey Mine is known for unique nickel mineral assemblages. The Lord Brassey Mine can be divided into four unique stages of mineralization; magmatic, metamorphic, hydrothermal and supergene alteration. The magmatic stage formed minerals such as enstatite, forsterite, anorthite, augite, chromite. Little remains as this assemblage has largely been altered to form new minerals.
Michelle_530
Lord Brassey Mine is known for unique nickel mineral assemblages. The Lord Brassey Mine can be divided into four unique stages of mineralization; magmatic, metamorphic, hydrothermal and supergene alteration. The metamorphic stage is either due to greenschist-facies burial or emplacement related metamorphism. The primary magmatic assemblage has largely transformed to serpentine, chlorite, amphibole, epidote, garnet, and minor prehnite, magnetite, talc, magnesite, opal and chalcedony.
Michelle_531
Lord Brassey Mine is known for unique nickel mineral assemblages. The Lord Brassey Mine can be divided into four unique stages of mineralization; magmatic, metamorphic, hydrothermal and supergene alteration. Hydrothermal alteration occurs later in the Devonian, producing serpentinite and introducing nickel. It is thought that a Devonian granitic intrusion postdates the serpentinite, introducing calcium, talc magnesite veins and possibly molybdenite and veins of diopside.
Michelle_532
Lord Brassey Mine is known for unique nickel mineral assemblages. The Lord Brassey Mine can be divided into four unique stages of mineralization; magmatic, metamorphic, hydrothermal and supergene alteration. Exposure by glaciation and the following rapid erosion allowed new supergene and alteration mineralization.
Age of metamorphism. Age described as "Pre-mid-Devonian, possibly Cambrian." The metamorphic stage is either due to greenschist-facies burial or emplacement related metamorphism.
Age of hydrothermal alteration. Age described as "latest stage of Devonian metamorphism." Hydrothermal alteration occurs later in the Devonian, producing serpentinite and introducing nickel. It is thought that a Devonian granitic intrusion postdates the serpentinite, introducing calcium, talc magnesite veins and possibly molybdenite and veins of diopside.
Age of weathering and supergene alteration. Exposure by glaciation and the following rapid erosion allowed the supergene and alteration mineralization.
Sample
Source Locality
Reference URL
R070671
Heazlewood District, Waratah-Wynyard Municipality, Tasmania, Australia