Paleo-environment from isotopes and hydrochemistry of groundwater in East Junggar Basin, Northwest China
详细信息    查看全文
文摘

Paleoenvironment was reconstructed for a non-monsoon region in West China.

Groundwater evolution is well constrained to support the paleo-environment study.

Isotopes indicate air temperature was lower in the late Pleistocene.

13C of groundwater suggests there were more C4 plants in the late Pleistocene.

© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700