Publication | Open Access

Mid-Holocene climate change in the eastern Xinjiang region indicated by the grain size and stable isotope record from Lake Barkol, northwest China

HoloceneMid-holocene Climate ChangeLake BarkolEngineeringPaleoenvironmental ChangeGeomorphologyNorthwest ChinaGeographyQuaternary ResearchGeochronologySedimentologyEarth ScienceQuaternary PeriodClimate Change