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(A–H) X-ray element mapping for garnet from the eclogite GQ–1 (A–D) and GQ–2 (E–H) at Gaoqiao, western Dabie, respectively. (I,J) Travers of point analyses for garnet from the eclogite GQ–1 and GQ–2, respectively. (C) represents garnet core, M represents garnet mantle, R represents garnet rim.

(A–H) X-ray element mapping for garnet from the eclogite GQ–1 (A–D) and GQ–2 (E–H) at Gaoqiao, western Dabie, respectively. (I,J) Travers of point analyses for garnet from the eclogite GQ–1 and GQ–2, respectively. (C) represents garnet core, M represents garnet mantle, R represents garnet rim.

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  • Feb 2023
Lawsonite is of great significance for understanding fluid activity, element migration and crust–mantle interactions in subduction zones. Though studies have predicted lawsonite to be present under the P–T regime during continental subduction, no lawsonite has been documented from natural (U) HP rocks in continental orogenic belt. In this study, we...
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