The alternative changes of paleoenvironment favored the formation and imbedding of brine, which is the source of salt-water intrusion; and the paleochannel that formed during regressive of sea level is the path of salt-water intrusion.
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。