The global distribution of CO<sub>2</sub>-rich magmas is determined by lithospheric thickness. [PDF]
Nat GeosciBowman EE, Gibson SA, Sui S, Lebedev S.
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Carbonate- and silicate-metasomatized mantle beneath Himalayan-Tibetan orogenic belt. [PDF]
Commun Earth EnvironLi W, Yang Z, Zajacz Z, Zhou L, Hou Z.
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Linking carbonatites, rare earth ores, and subduction-fertilized mantle lithosphere. [PDF]
Sci AdvSpandler C, Merdith AS, Griffin A.
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Formation of the 15 Å phase as the most expanded hydrated mineral in cold subduction zone. [PDF]
Nat CommunBang Y +9 more
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Enhanced adsorptive removal of ammonia nitrogen from wastewater by EDTA-2Na modified vermiculite. [PDF]
Sci RepQu J, Yang B, Li Y, Ma S, Zheng Y.
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Sulfide-rich continental roots at cratonic margins formed by carbonated melts. [PDF]
NatureChen C +7 more
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Multi-Techniques Analysis of Archaeological Pottery-Potential Pitfalls in Interpreting the Results. [PDF]
MoleculesKozak L +5 more
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Palm phytoliths in subarctic Canada imply ice-free winters 48 million years ago during the late early Eocene. [PDF]
Ann BotSiver PA +4 more
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Coupled hydrothermal venting and hydrocarbon seepage discovered at Conical Seamount, Papua New Guinea. [PDF]
Sci RepBrandl PA +19 more
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The gold content of mafic to felsic potassic magmas. [PDF]
Nat CommunChang J, Audétat A, Pettke T.
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