Dollaseite-(Ce)
Encyclopedia
Dollaseite- is a sorosilicate end-member epidote
mineral, with the formula CaREE+3Mg2AlSi3O11F(OH), where cerium
is the dominant rare earth element
(REE). It also includes lanthanum
, neodymium
, praseodymium
, samarium
, and gadolinium
, and since cerium is the dominant REE, it is placed in the name and formula. It was first discovered and described by P. Geijer in 1927, in the Ostanmossa mine, Norberg district, Sweden
, which is the type locality today. It was first named "magnesium
orthite" because of its relation to orthite (orthite being the corresponding end-member rich in iron
). When orthite was renamed to allanite
in 1986, the Mg end-member was included. Peacor and Dunn redefined the Mg end-member in 1988 as dollaseite, after Wayne A. Dollase, a pioneer in the study of epidote and long-time mineralogy
professor
at UCLA. This redefinition was necessary because of a different coupled-substitution between clinozoisite
-allanite and clinozoisite-dollaseite. The clinozoisite-dollaseite substitution is REE + Mg = Ca + Al and Mg + F = Al + O.
Dollaseite is a metamorphic mineral associated with Västmanlandite-(Ce), Fluorbritholite-(Ce), tremolite
, norbergite, and calcite
. It is not considered hazardous, but is radioactive because of the REE content. The mineral neotype specimen (NMNH no. R6505) of dollaseite is on deposit at the Smithsonian Institution
.
Epidote
Epidote is a calcium aluminium iron sorosilicate mineral, Ca2Al2O, crystallizing in the monoclinic system. Well-developed crystals are of frequent occurrence: they are commonly prismatic in habit, the direction of elongation being perpendicular to the single plane of symmetry. The faces are often...
mineral, with the formula CaREE+3Mg2AlSi3O11F(OH), where cerium
Cerium
Cerium is a chemical element with the symbol Ce and atomic number 58. It is a soft, silvery, ductile metal which easily oxidizes in air. Cerium was named after the dwarf planet . Cerium is the most abundant of the rare earth elements, making up about 0.0046% of the Earth's crust by weight...
is the dominant rare earth element
Rare earth element
As defined by IUPAC, rare earth elements or rare earth metals are a set of seventeen chemical elements in the periodic table, specifically the fifteen lanthanides plus scandium and yttrium...
(REE). It also includes lanthanum
Lanthanum
Lanthanum is a chemical element with the symbol La and atomic number 57.Lanthanum is a silvery white metallic element that belongs to group 3 of the periodic table and is the first element of the lanthanide series. It is found in some rare-earth minerals, usually in combination with cerium and...
, neodymium
Neodymium
Neodymium is a chemical element with the symbol Nd and atomic number 60. It is a soft silvery metal that tarnishes in air. Neodymium was discovered in 1885 by the Austrian chemist Carl Auer von Welsbach. It is present in significant quantities in the ore minerals monazite and bastnäsite...
, praseodymium
Praseodymium
Praseodymium is a chemical element that has the symbol Pr and atomic number 59. Praseodymium is a soft, silvery, malleable and ductile metal in the lanthanide group. It is too reactive to be found in native form, and when artificially prepared, it slowly develops a green oxide coating.The element...
, samarium
Samarium
Samarium is a chemical element with the symbol Sm, atomic number 62 and atomic weight 150.36. It is a moderately hard silvery metal which readily oxidizes in air. Being a typical member of the lanthanide series, samarium usually assumes the oxidation state +3...
, and gadolinium
Gadolinium
Gadolinium is a chemical element with the symbol Gd and atomic number 64. It is a silvery-white, malleable and ductile rare-earth metal. It is found in nature only in combined form. Gadolinium was first detected spectroscopically in 1880 by de Marignac who separated its oxide and is credited with...
, and since cerium is the dominant REE, it is placed in the name and formula. It was first discovered and described by P. Geijer in 1927, in the Ostanmossa mine, Norberg district, Sweden
Sweden
Sweden , officially the Kingdom of Sweden , is a Nordic country on the Scandinavian Peninsula in Northern Europe. Sweden borders with Norway and Finland and is connected to Denmark by a bridge-tunnel across the Öresund....
, which is the type locality today. It was first named "magnesium
Magnesium
Magnesium is a chemical element with the symbol Mg, atomic number 12, and common oxidation number +2. It is an alkaline earth metal and the eighth most abundant element in the Earth's crust and ninth in the known universe as a whole...
orthite" because of its relation to orthite (orthite being the corresponding end-member rich in iron
Iron
Iron is a chemical element with the symbol Fe and atomic number 26. It is a metal in the first transition series. It is the most common element forming the planet Earth as a whole, forming much of Earth's outer and inner core. It is the fourth most common element in the Earth's crust...
). When orthite was renamed to allanite
Allanite
Allanite is a sorosilicate group of minerals within the broader epidote group that contain a significant amount of rare earth elements. The mineral occurs mainly in metamorphosed clay rich sediments and felsic igneous rocks...
in 1986, the Mg end-member was included. Peacor and Dunn redefined the Mg end-member in 1988 as dollaseite, after Wayne A. Dollase, a pioneer in the study of epidote and long-time mineralogy
Mineralogy
Mineralogy is the study of chemistry, crystal structure, and physical properties of minerals. Specific studies within mineralogy include the processes of mineral origin and formation, classification of minerals, their geographical distribution, as well as their utilization.-History:Early writing...
professor
Professor
A professor is a scholarly teacher; the precise meaning of the term varies by country. Literally, professor derives from Latin as a "person who professes" being usually an expert in arts or sciences; a teacher of high rank...
at UCLA. This redefinition was necessary because of a different coupled-substitution between clinozoisite
Clinozoisite
Clinozoisite is a mineral, a complex sorosilicate of calcium and aluminium and is usually a grey green colour.Its formula is Ca2Al3[O|OH|SiO4|Si2O7]....
-allanite and clinozoisite-dollaseite. The clinozoisite-dollaseite substitution is REE + Mg = Ca + Al and Mg + F = Al + O.
Dollaseite is a metamorphic mineral associated with Västmanlandite-(Ce), Fluorbritholite-(Ce), tremolite
Tremolite
Tremolite is a member of the amphibole group of silicate minerals with composition: Ca2Mg5Si8O222. Tremolite forms by metamorphism of sediments rich in dolomite and quartz. Tremolite forms a series with actinolite and ferro-actinolite. Pure magnesium tremolite is creamy white, but the color grades...
, norbergite, and calcite
Calcite
Calcite is a carbonate mineral and the most stable polymorph of calcium carbonate . The other polymorphs are the minerals aragonite and vaterite. Aragonite will change to calcite at 380-470°C, and vaterite is even less stable.-Properties:...
. It is not considered hazardous, but is radioactive because of the REE content. The mineral neotype specimen (NMNH no. R6505) of dollaseite is on deposit at the Smithsonian Institution
Smithsonian Institution
The Smithsonian Institution is an educational and research institute and associated museum complex, administered and funded by the government of the United States and by funds from its endowment, contributions, and profits from its retail operations, concessions, licensing activities, and magazines...
.