Neoproterozoic–early Paleozoic evolution of the southern Central Asian Orogenic Belt: Constraints from eclogites in the Beishan Orogenic Belt (NW China)

Mineral precipitation sequence from multi-stage fluids released by eclogite during high-pressure metamorphism

Subduction zone rocks oxidized by supercritical fluid: Constraints from an ultrahigh-pressure eclogite-vein system in the Dabie orogen, China

Bulk and inter-mineral zinc isotopic systematics of continental eclogites from the Dabie orogenic belt, central China

Continental crustal growth in the post-collisional setting: Insights from the Late Triassic high-Mg andesites in the eastern Central Asian Orogenic Belt

Late Triassic continental eclogite in the central Tibetan Plateau reveals 2500-km-long Paleo-Tethys continental subduction

Phanerozoic emergence of global continental collision and onset of massive crustal eclogitization

Ultrahigh-pressure to high-pressure eclogite in Cuban ophiolitic mélange reveals proto-Caribbean spreading ridge subduction

Lawsonite eclogite records subduction rheology and slab detachment, Faro, Yukon-Tanana Terrane, Yukon Territory, Canada

The Subduction of Hydrogen: Deep Water Cycling, Induced Seismicity, and Plate Tectonics

In situ garnet U-Pb dating of granulitized eclogites from NE Sardinia, Italy

Basal erosion during the initiation of continental deep subduction in the North Qaidam ultrahigh-pressure metamorphic belt (NW China): Constraints from geochemistry and geochronology on eclogites and gneisses in the Chachahe unit

U–Pb Age and Mineral Inclusions in Zircon from Diamondiferous Garnet–Pyroxene Rocks of the Kumdy-Kol Microdiamond Deposit in Northern Kazakhstan

The onset of Neo-Tethys subduction in the Early Jurassic: evidence from the eclogites of the North Shahrekord Metamorphic Complex (Sanandaj-Sirjan Zone, W Iran)

Geochronology of the Sanbagawa Belt: Younger and Faster than Before

On the occurrence of a Variscan eclogite in the Argentera-Mercantour Massif, Western Alps: Implications for the evolution of the southern Variscan belt

Discovery of Permian–Triassic eclogite in northern Tibet establishes coeval subduction erosion along an ~3000-km-long arc: REPLY

Discovery of Permian–Triassic eclogite in northern Tibet establishes coeval subduction erosion along an ~3000-km-long arc: COMMENT

Reaction between volatile-bearing eclogite and harzburgite as a function of degree of interaction: Experimental constraints at 4 GPa

The origin of the ultrahigh-pressure Tso Morari complex, NW Himalaya: implication for early Paleozoic rifting