The Ohakuri pyroclastic deposits and the evolution of the Rotorua-Ohakuri volcanotectonic depression.
The caldera-forming Ohakuri pyroclastic deposits (~ 100 km3 magma) were erupted at ~ 240 ka from the newly defined Ohakuri caldera, which is located within the central Taupo Volcanic Zone (TVZ) of New Zealand. The Ohakuri pyroclastic deposits are remarkable for their widespread lateral and vertical...
| Main Author: | |
|---|---|
| Language: | en |
| Published: |
University of Canterbury. Geological Science
2011
|
| Online Access: | http://hdl.handle.net/10092/5465 |
