Structural petrology of the garnet-peridotite of Alpe Arami (Ticino, Switzerland)
The decomposition of pyrope-rich garnet into spinel-amphibole symplektite and the alteration of the latter into chlorite indicate the presence of three successive mineral parageneses in the peridotite of Alpe Arami: a garnet-peridotite, a spinelamphibole-
Möckel, J.R.
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Generation of carbonated peridotite melts via biogenic sediment recycling in modern subduction zones. [PDF]
Errázuriz-Henao C +9 more
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Continental evolution influenced by relamination of deeply subducted continental crust. [PDF]
Gómez-Frutos D +3 more
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Melt flow control on lithological and geochemical heterogeneity of the oceanic upper mantle. [PDF]
Rui HC +9 more
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Catchment Productivity Controls Local Species Richness of Hyporheic Invertebrate Communities in Tropical New Caledonia Streams. [PDF]
Mouron S +9 more
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Endolithic fungal diversity is present in the unique phosphatized rocks of an environmentally extreme equatorial archipelago revealed by DNA amplicon metagenomics. [PDF]
Rocha LBA +10 more
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Linking electrical anomalies in the upper mantle to petrological and geochemical heterogeneities. [PDF]
Yang X, Xu YG, Xia QK.
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Sublithospheric diamond constraints on the state of deeply subducted slabs. [PDF]
Zhang Q +11 more
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A universal concept for melting in mantle upwellings. [PDF]
Schmidt MW, Paneva N, Giuliani A.
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