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- W2012021382 abstract "Coesite and graphite were discovered as inclusions in zircon separates from pelitic gneiss associated with a large eclogite body in the North Qaidam UHP terrane. This finding suggests UHP metamorphism at pressures below the diamond stability field. This supports previous indirect UHP evidences, such as polycrystalline quartz inclusions in eclogitic garnet, quartz lamellae in omphacite and P–T estimates for both eclogite and garnet peridotite. The U/Pb and Sm/Nd isotopic ages from the North Qaidam eclogite indicated that continental subduction occurred in Early Palaeozoic, most probably in relation with the collision between the Sino-Korean and Yangtze plates. De la coésite et du graphite ont été identifiés en inclusion dans des zircons de gneiss pélitiques associés à un massif d'éclogite des terrains métamorphiques de très haute pression des chaı̂nons montagneux du Nord du Qaidam, dans le Nord-Est du plateau du Tibet en Chine. Cette découverte suggère un métamorphisme de type UHP dans des conditions de pression inférieures au champ de stabilité du diamant et conforte les observations antérieures de quartz polycristallin en inclusion dans des grenats éclogitiques, de lamelles d'exsolution de quartz dans de l'omphacite et les données P, T préliminaires sur les éclogites et les péridotites. Les âges U/Pb et Sm/Nd des éclogites du Nord-Qaidam indiquent qu'une subduction continentale s'est développée au Paléozoı̈que inférieur, probablement en relation avec la collision des cratons Sino-Koréen et du Yangze." @default.
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- W2012021382 date "2001-12-01" @default.
- W2012021382 modified "2023-09-26" @default.
- W2012021382 title "Discovery of coesite in the North Qaidam Early Palaeozoic ultrahigh pressure (UHP) metamorphic belt, NW China" @default.
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- W2012021382 doi "https://doi.org/10.1016/s1251-8050(01)01718-9" @default.
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