Channel‐lobe transition zone development in tectonically active settings: Implications for hybrid bed development
Abstract Channel‐lobe transition zones are dynamic areas located between deepwater channels and lobes. Presented here is a rare example of an exhumed channel‐lobe transition zone from an active‐margin setting, in the Kazusa forearc Basin, Boso Peninsula, Japan. This Plio‐Pleistocene outcrop exposes...
Main Authors: | , , , , |
---|---|
Format: | Article |
Language: | English |
Published: |
Wiley
2022-06-01
|
Series: | The Depositional Record |
Subjects: | |
Online Access: | https://doi.org/10.1002/dep2.180 |