Macquarie Island’s Finch-Langdon fault: a ridge-transform inside corner structure
Macquarie Island consists of uplifted oceanic crust, uniquely situated in the ocean basin where it formed, thus allowing onshore structures to be placed into their regional oceanic tectonic context. The Finch-Langdon fault, the most significant spreading-related structure on the island, juxtaposes u...
| Published in: | Geology |
|---|---|
| Main Authors: | , , , |
| Format: | Article in Journal/Newspaper |
| Language: | unknown |
| Published: |
2003
|
| Subjects: | |
| Online Access: | http://nora.nerc.ac.uk/id/eprint/152442/ http://www.gsajournals.org/perlserv/?request=get-abstract&doi=10.1130%2FG19441.1 https://doi.org/10.1130/G19441.1 |