Cool-water Carbonate Sedimentology and Sequence Stratigraphy of the Waitaki Region, South Island, New Zealand
In the mid-Cenozoic, New Zealand underwent slow subsidence interspersed with unconformity development, however significant controversy exists around both the extent of submergence below sea level during this period of maximum drowning, as well as the causes of these unconformities. Detailed field ob...
| Main Author: | |
|---|---|
| Language: | en |
| Published: |
University of Canterbury. Geological Sciences
2014
|
| Subjects: | |
| Online Access: | http://hdl.handle.net/10092/8799 |