作者: C. Hans Nelson , Andrés Maldonado , John H. Barber , Belén Alonso
DOI: 10.1007/978-1-4684-8276-8_8
关键词:
摘要: Base-of-slope aprons that lack significant channel development and are fed by multiple sediment sources (i.e., numerous slope failures or debris chutes) represent an alternative facies organization to submarine fans possess channels canyon point of allochthonous sediment. Two styles base-of-slope apron deposition evident: (1) sand-rich with rhythmic, gradational sand gravel sheets evolve basin-plain turbidites as exemplified Crater Lake aprons, (2) mud-rich composed chaotic flow lobes without gradation Ebro margin aprons.