Mineralogical and
geochemical features of high-alumina fenites of the Mont Saint-Hilaire alkaline
complex,
Yakovleva O.S.*, Pekov I.V.*,**,
Bryzgalov I.A.*, Horváth L.***, Yapaskurt V.O.*, Guseva E.V.*
2Institute of Geochemistry and Analytical
Chemistry of RAS,
Á
The Mont
Saint-Hilaire complex, part of the Monteregian Hills alkaline province, is
situated the contact metamorphism (Currie et
al., 1986). High-alumina rocks found at Mont Saint-Hilaire have not been studied
before, only the occurrence of corundum, columbite and hercynite were noted.
This paper is the first systematic characterization of these rocks, considered by us as specific
fenites.
High-alumina rocks, uncovered in the Poudrette quarry,
form small bodies at the contact of alkaline pegmatites with hornfels and
granites. Also they replace granite veins. These fenites are fine- to medium-grained rocks consisting substantially of feldspars
(albite, K,Na feldspar and potassic feldspars are abundant, albite-oligoclase
is subordinate). Hercynite (in all the rocks discussed below) and biotite (in
almost all rocks) are the other rock-forming minerals. Typically biotite is
high-alumina annite close to siderophyllite. Sporadically nepheline becomes a
rock-forming mineral.
We have subdivided the high-alumina oxide-silicate rocks of Mont
Saint-Hilaire to four types:
(1) A rock with significant biotite content (to 15%). Isolated
spessartine crystals (up to
(2) A rock with
corundum-hercynite intergrowths surrounded by annite rims (sometimes with
muscovite). Siderite is typically observed in cores of hercynite grains. The
rock contains rare impregnation of
pyrrhotite and manganocolumbite.
(3) A rock with
Zn-rich hercynite grains with annite rims and intergrowths of biotite and
muscovite. A lot of zoned well-shaped and skeletal zircon crystals occur there.
The rock is strongly altered and contains different carbonates:
sideriteãmagnesite series members, ankerite, dolomite; calcite, mckelveyite,
Ca,REE fluorocarbonates are
subordinate; late natrolite and fluorite are also present. Accessory minerals
are members of the ferrocolumbiteãmanganocolumbite series, ilmenite, Nb-bearing
rutile (var. ilmenorutile), uedaite-(Ce), pyrrhotite, monazite-(¶È),
xenotime-(Y), and a Ti-free REE
niobate, probably fergusonite-(Ce). Isolated inclusions consisting of quartz
(60%) and biotite (typically annite) (40%) are observed in a rock. Some biotite
crystals contain inclusions of metacrystals of Ti-bearing spinelides of the
magnetite-chromite series.
(4) A rock with
equal impregnation of Zn-rich hercynite (up
to 20%), accessory zircon and ilmenite (with ferrocolumbite microinclusions).
Sporadically, hercynite forms aggregations containing clusters of zircon with
thorite inclusions. There are big (up to
Similar rocks are
known in large fenitized xenoliths in the Khibiny massif (
ÁBesides the common mineralogical features, we
note some differences. Majority of Khibiny high-alumina fenites contain
nepheline that is not typical for the high-alumina Mont Saint-Hilaire rocks.
Carbonates are widespread at Mont Saint-Hilaire unlike at Khibiny.
The oxide-silicate
rocks of Mont Saint-Hilaire and Khibiny are characterized by high contents of Al,
Fe, Na, and K while concentrations of Ca and Mg are low. Similar rare-element speciality of high-alumina rocks of both massifs
should be noted: the majority of accessory minerals contain Nb (+Ta), Zr, Ce (+
other LREE), and Th, less Y (+HREE), Sr, Ba, and U.
When the
geochemistry of high-alumina rocks of both alkaline massifs are compared, we
noted the higher alkalinity (especially Na) for Khibiny and relative enrichment
in CO2 and Mn for Mont Saint-Hilaire rocks. Content of S in
high-alumina rocks of Mont Saint-Hilaire is lower compared to Khibiny, while
contents of rare elements are close. The important common feature at both
localities is the reducing conditions of mineral formation, that is shown by
the abundance of hercynite (both massifs), and the presence of native iron
(Khibiny) or Fe2+ carbonates (Mont Saint-Hilaire).
Geochemically, the
high-alumina fenites contrast sharply with relatively Al-poor host agpaitic
rocks. It can be explained by the nature of a protholite that coud be initially
Al-rich. In Khibiny, the protholite is most likely metamorphic rocks (muscovite
shales or gneisses) formed after clays, whereas in Mont Saint-Hilaire it was hornfels
or granite. High-alumina rocks of Khibiny were altered by alkaline fluids more
strongly compared to their Mont Saint-Hilaire analogues. In the Khibiny
xenoliths, nepheline-bearing rocks are typical products of the fenitization
unlike the majority of Mont Saint-Hilaire high-alumina rocks, in which almost
all Na is concentrated in feldspars. Note that nepheline-free varieties of
high-alumina fenites, very similar to Mont Saint-Hilaire ones, are common also
at Khibiny.
This study was supported by grant of President of
Russain Federation No. 863.2008.5, grant of RFBR No. 08-05-00077-a and grant of
Russian Science Support Foundation (I.V.P.).
References
Currie K.L., Eby G.N., Gittins J. The petrology
of Mont St-Hilaire complex, southern
Shlyukova Z.V. Mineralogy of Contact Formations
of the Khibiny Massif.
Yakovenchuk V., Ivanyuk G., Pakhomovsky Ya.,
Men'shikov Yu. Khibiny. Apatity: Laplandia Minerals, 2005, 468 pp.
Yakovleva O.S., Pekov I.V., Kononkova N.N.
Hercynite from alkaline alumina rocks of fenitized xenoliths in the Khibiny
massif // Proc. All-Russian Conference Geochemistry,
Petrology, Mineralogy and Genesis of Alkaline Rocks, Miass, 2006, pp.
310-313 (in Russian).