Document is current

Any future updates will be listed below

Geological evidence for shallow ductile-brittle transition zones along subduction interfaces: example from the Shimanto Belt, SW Japan

Crossref DOI link: https://doi.org/10.1186/s40623-014-0141-7

Published Online: 2014-10-16

Published Print: 2014-12

Update policy: https://doi.org/10.1007/springer_crossmark_policy

About CrossMark