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Coeval Transverse and Axial Sediment Delivery to the Northern Hikurangi Trough During the Late Quaternary (2025)

First Author: Shorrock A

Attributed to: Revealing the geophysical environment of slow slip using core-log-seismic integration funded by NERC

Abstract

No abstract provided

Bibliographic Information

Digital Object Identifier: http://dx.doi.org/10.1111/bre.70019

Publication URI: http://dx.doi.org/10.1111/bre.70019

Type: Journal Article/Review

Parent Publication: Basin Research

Issue: 1