Breakup of strong cratonic lithosphere causes extensive magmatism at continental margins. [PDF]
Wang S, Leng W.
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Continental evolution influenced by relamination of deeply subducted continental crust. [PDF]
Gómez-Frutos D +3 more
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Olivine and Fe-isotopes in kimberlites indicate an iron-rich substrate for CLIPPIR and other sub-lithospheric diamonds. [PDF]
Howarth GH +4 more
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Ultraslow spreading ridges: slowest but locally thickest. [PDF]
Liu CZ, Zhu RX.
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The location of compression-induced subduction initiation controlled by structural versus thermal inheritance. [PDF]
Oravecz É, Gerya T, Balázs A.
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Modeling of the Arabian/Nubian shield's geothermal structure: a multi-parametric analysis using geophysical and geological tools. [PDF]
Haggag M +5 more
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Mantle-derived fluid flux controls Olympic Dam-style Fe oxide-Cu-Au mineralisation. [PDF]
Thiel S +4 more
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Proto-Tethyan tectonics in East China: a revisit. [PDF]
Meng QR +6 more
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Average physical structure of cratonic lithosphere, from thermodynamic inversion of global surface-wave data. [PDF]
Xu Y, Lebedev S, Fullea J.
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Variable mantle redox states driven by deeply subducted carbon. [PDF]
Gao M, Wang Y, Foley SF, Xu YG.
europepmc +1 more source

