The classical turbidite outcrop at San Clemente, California revisited: An example of sandy submarine channels with asymmetric facies architecture
The classical turbidite outcrop at San Clemente, California revisited: An example of sandy submarine channels with asymmetric facies architecture
复制标题
DOI：
10.1016/j.sedgeo.2016.10.001
复制
发表时间：
2016-12
影响因子：
2.8
通讯作者：
Pan Li;B. Kneller;L. Hansen;I. Kane
中科院分区：
文献类型：
--
作者：
Pan Li;B. Kneller;L. Hansen;I. Kane
