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<p>Text S1: Analytical methods of whole-rock major element analyses, mineral chemistry measurements, zircon U-Pb dating and trace element measurements; Figure S1: P/T-H2O/O diagrams for samples QL2105 and QL2106; Figure S2: P–T diagram calculated with an effective bulk-rock composition for sample QL2106; Figure S3: Representative Raman spectra of mineral inclusions in zircons with different ages from samples QL2105 and QL2106; Table S1: Selected microprobe analyses of garnet, amphibole, biotite, plagioclase, and phengite for samples QL2105, QL2106, and QL2107; Table S2: Zircon U-Pb isotopic and age data as well as trace element compositions of zircons of samples QL2105, QL2106, and QL2107.</p>

Olivine fabrics are described in terms of their relationship to the crystallographic framework (x, y, and z axes), and can provide important information for understanding the evolution of the upper mantle, mantle flow pattern, mantle dynamics and tectonics (

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<p>Text S1: Analytical methods of whole-rock major element analyses, mineral chemistry measurements, zircon U-Pb dating and trace element measurements; Figure S1: P/T-H2O/O diagrams for samples QL2105 and QL2106; Figure S2: P–T diagram calculated with an effective bulk-rock composition for sample QL2106; Figure S3: Representative Raman spectra of mineral inclusions in zircons with different ages from samples QL2105 and QL2106; Table S1: Selected microprobe analyses of garnet, amphibole, biotite, plagioclase, and phengite for samples QL2105, QL2106, and QL2107; Table S2: Zircon U-Pb isotopic and age data as well as trace element compositions of zircons of samples QL2105, QL2106, and QL2107.</p>