Differential exhumation was petrologically recognized in ultrahigh pressure metamorphic rocks from the southern and northern parts of the Sulu terrane. While a normal exhumation occurred for eclogites and gneisses in ...Differential exhumation was petrologically recognized in ultrahigh pressure metamorphic rocks from the southern and northern parts of the Sulu terrane. While a normal exhumation occurred for eclogites and gneisses in south Sulu, granulite-facies overprinting of ultrahigh pres- sure metamorphic rocks took place with high retrograde temperatures in north Sulu. A study of fluid inclusions re- veals trapping of five type fluid inclusions in high and ultra- high pressure eclogite minerals and vein quartz in the Sulu terrane. These are A-type N2±CO2 inclusion trapped at high and ultra-high pressure eclogite-facies metamorphic condi- tion, B-type pure-CO2 liquid phase inclusion with higher density trapped during granulite-facies overprinting meta- morphism of eclogites, C-type CO2-H2O inclusion and D-type hypersaline inclusion trapped in high pressure eclogite-facies re-crystallization stage, and E-type low salinity H2O inclu- sion trapped in the latest stage of ultrahigh pressure exhu- mation (amphibolite-facies retrogression). Identification of crowded-distributing pure-CO2 liquid inclusions with higher density trapped in garnet of eclogites provides an evidence for granulite-facies overprinting metamorphism in the north Sulu terrane.展开更多
基金State Key Basic Research Developrment Program of China(Grant No.G1999075502) the National Natural ScienceFoundation of China(Grant No.40273024).
文摘Differential exhumation was petrologically recognized in ultrahigh pressure metamorphic rocks from the southern and northern parts of the Sulu terrane. While a normal exhumation occurred for eclogites and gneisses in south Sulu, granulite-facies overprinting of ultrahigh pres- sure metamorphic rocks took place with high retrograde temperatures in north Sulu. A study of fluid inclusions re- veals trapping of five type fluid inclusions in high and ultra- high pressure eclogite minerals and vein quartz in the Sulu terrane. These are A-type N2±CO2 inclusion trapped at high and ultra-high pressure eclogite-facies metamorphic condi- tion, B-type pure-CO2 liquid phase inclusion with higher density trapped during granulite-facies overprinting meta- morphism of eclogites, C-type CO2-H2O inclusion and D-type hypersaline inclusion trapped in high pressure eclogite-facies re-crystallization stage, and E-type low salinity H2O inclu- sion trapped in the latest stage of ultrahigh pressure exhu- mation (amphibolite-facies retrogression). Identification of crowded-distributing pure-CO2 liquid inclusions with higher density trapped in garnet of eclogites provides an evidence for granulite-facies overprinting metamorphism in the north Sulu terrane.
