吉林大学学报(地球科学版) ›› 2020, Vol. 50 ›› Issue (2): 442-453.doi: 10.13278/j.cnki.jjuese.20190268
王建功1,2, 张道伟3, 石亚军1, 张平1, 孙秀建1, 王爱萍1, 王玉林1, 高妍芳1, 张世铭1, 易定红1
Wang Jiangong1,2, Zhang Daowei3, Shi Yajun1, Zhang Ping1, Sun XiuJian1, Wang Aiping1, Wang Yulin1, Gao Yanfang1, Zhang Shiming1, Yi Dinghong1
摘要: 利用大量地质及地球化学资料,开展了柴达木盆地西部地区渐新世下干柴沟组上段盐湖沉积特征研究,重点识别岩石类型,恢复古沉积环境,建立沉积模式,探讨控制因素。研究认为:盐湖环境主要发育两大类、五小类沉积相组合,盐湖边缘沉积相包括滨岸斜坡带相组合、缓坡带相组合、陡坡带相组合,盆内沉积相包括水下隆起带相组合和盐湖深水区相组合;盐湖可划分早、中、晚3个沉积演化阶段,分别对应半咸水湖泊、咸水湖泊和盐湖;形成碳酸盐岩与钙质砂岩、富含石膏的碳酸盐岩与泥岩、厚层石盐与薄层碳酸盐岩等主要岩石组合;盐湖沉积主控因素为气候、古地貌与构造运动。
中图分类号:
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