Based on the structural evolution and geological framework in northern margin rift of Qaidam basin, this paper presents that the overall course of faults development in middle Qaidam is the main power for controlling the superimposition and assemblage of
详情正文
登录后查看完整内容
使用 DeepEvidence / 梅斯账号登录，新用户可在登录页面注册。
登录 / 注册登录成功后将返回当前页面，继续浏览。