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Holocene high-resolution quantitative summer temperature reconstruction based on subfossil chironomids from the southeast margin of the Qinghai-Tibetan Plateau

ClimatologyQinghai-tibetan PlateauHoloceneEngineeringGeomorphologySoutheast MarginGeographySubfossil ChironomidsIndia-asia CollisionTibetan PlateauCryospherePaleoecologyGeochronologyPaleoclimatologyEarth ScienceSocial SciencesQuaternary Period