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High-Temperature Metasomatism of the Layered Mafic–Ultramafic Massif in Kiy Island, Belomorian Mobile Belt

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Abstract

The paper presents results of a detailed petrologic study of metasomatites and their host metagabbroids in the northwestern part of Kiy Island, Onega Bay, White Sea. The first evidence is acquired that coronitization and amphibolization of the host rocks took place at the peak of Svecofennian metamorphism at Т = 700–640°C, Р = 9–10 kbar, and \({a_{{H_2}O}}\) = 0.2–0.3. Accompanying metasomatism has formed a number of long (up to several meters long) melanocratic hornblendite and garnet–amphibole veins 0.3–2 m thick. In this area, metasomatites of another type make up single relatively thin amphibole–zoisite lenses that sometimes host ruby-like corundum. The fluid phase that induced metasomatism was poor in salts (Na,K)Cl, and hence, the rocks do not contain sodic plagioclase, and their amphibole is tschermakite but not pargasite. The compositions of the metasomatites of the two types are proved to be complementary, and this indicates that they were most likely produced by high-temperature metasomatism but not via the removal of components by fluid from migmatization zones.

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Abbreviations

Cpx :

clinopyroxene

Di :

diopside

Hd :

hedenbergite

Opx :

orthopyroxene

Aug :

augite

Hbl :

amphibole

Grt :

garnet

Prp :

pyrope

Grs :

grossular

Alm :

almandine

Jd :

jadeite

Pl :

plagioclase

An :

anorthite

Ab :

albite

Kfs :

potassic feldspar

Zo :

zoisite

Chl :

chlorite

Ap :

apatite

Ttn :

titanite

Crn :

corundum

Dsp :

diaspore

Ilm :

ilmenite

Mag :

magnetite

Rt :

rutile

Qtz :

quartz

Py :

pyrite

Act :

actinolite

Tr :

tremolite

Ed :

edenite

Rit :

richterite

Eck :

eckermannite

Arf :

arfvedsonite

Ktp :

cataphorite

Gln :

glaucophane

Prg :

pargasite

fPrg :

ferropargasite

Ts :

tschermakite

Rbk :

riebeckite

Mrg :

margarite

Ms :

muscovite. f = FeO/(FeO + MgO) is the Fe mole fraction

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    Article  Google Scholar 

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    Article  Google Scholar 

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    Article  Google Scholar 

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    Google Scholar 

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    Google Scholar 

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    Google Scholar 

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    Article  Google Scholar 

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    Article  Google Scholar 

  • R. C. Newton and C. E. Manning, “Solubility of corundum in the system Al2O3–SiO2–H2O–aCl at 800°C and 10 kbar,” Chem. Geol. 249, 250–261 (2008).

    Article  Google Scholar 

  • R. C. Newton and C. E. Manning, “Role of saline fluids in deep crustal and upper mantle metasomatism: insights from experimental studies,” Geofluids 10, 58–72 (2010).

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  1. Institute of Experimental Mineralogy (IEM), Russian Academy of Sciences, Chernogolovka, Moscow oblast, 142432, Russia

    L. I. Khodorevskaya & D. A. Varlamov

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  1. L. I. Khodorevskaya
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  2. D. A. Varlamov
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Correspondence to L. I. Khodorevskaya.

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Original Russian Text © L.I. Khodorevskaya, D.A. Varlamov, 2018, published in Geokhimiya, 2018, No. 6, pp. 541–558.

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Khodorevskaya, L.I., Varlamov, D.A. High-Temperature Metasomatism of the Layered Mafic–Ultramafic Massif in Kiy Island, Belomorian Mobile Belt. Geochem. Int. 56, 535–553 (2018). https://doi.org/10.1134/S001670291806006X

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