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Table 1 Natural occurrences of metasomatic reaction zones at the contact between crust and mantle rocks

From: Si- versus Mg-metasomatism at the crust–mantle interface: insights from experiments, natural observations and geochemical modeling

 

Setting

Occurences

Metasomatic zones hosted by ultramafic rocks

Metasomatic zones hosted by crustal rocks

Serpentine minerals

Gain/loss during alteration of the ultramafic rock

Gain/loss during alteration of the ultramafic rock

References

Nishisonogi metamorphic rocks

Subduction zone

Serpentinite pods in pelitic schist

Mgs + Qz veins/Tlc + Car (Act)/Car + Qz

Chl/Ms/Ab

Atg

Gain: CO2

Loss: Mg, Ca, H2O

Gain: Mg, Fe, H2O

Loss: Si, K, C

Mori et al. (2007)

Sanbagawa Belt (Higuchi body)

Subduction zone

Serpentinite block in pelitic schist

Car + Tlc veins/Act-Chl schist

Chl

Atg

Gain: Si, Ca, CO2

Loss:Mg, H2O (n.a.)

Gain: Mg, H2O

Loss: Si, Na, K

Okamoto et al. (2021)

Sanbagawa Belt (Tomisato body)

Subduction zone

Serpentinite block in pelitic schist

Tlc + Chl/Tlc veins

Chl/Ms/Ab

Atg

Gain: Si, Ca, Al

Loss:Mg, H2O

Gain: Mg, H2O

Loss: Si, Na, K

Oyanagi et al. (2023)

Livingstone fault

Tectonic fault between the Dun Mountain Ophiolite Belt and the Caples terrane

Schist blocks in Serpentine shear zone

Tr vein, Tlc veins/Tr

Rodingite pods (occationary)

Chry/Liz (minor Atg)

Gain: Si, Ca? (n.a.)

n.d

Tarling et al. (2019a, b)

Voltri massif

Oceanic lithosphere → Subduction zone

Metagabbro block in schistose serpentinite

No reaction zone (Tlc veins)

Ca-Amp + Chl/Chl + Ca-Amp/Ep

Atg

n.a

Gain: Mg, H2O

Loss: Ca (Chl rock)

Collido et al. (2022b)

Flanciscan Complex (Jade Cove)

Oceanic lithosphere → Subduction zone

Serpentine melange

Tr + Chl, Chl + Tlc

Tr overgrowth + Chl

Liz/Chry → Atg

Gains: Si, Ca

Loss: n.a

Gain: Mg? (n.a.)

King et al. (2003); Hirauchi etal. (2020)

  1. Chl, chlorite; Ms, muscovite; Ab, albite; Amp, amphibole; Ep, epidote; Atg, antigorite; Chry, chrysotile; Liz, lizardite; n.d., not described; n.a., not analyzed qunatitatively