Until about 100 million years ago, New Zealand lay on the Pacific-facing edge of the ancient supercontinent of Gondwana; the formation of our sedimentary rocks provides a fascinating view of the tectonic activity and changes since that time. This volume is the culmination of a comprehensive survey of New Zealand's Cretaceous-Cenozoic strata, begun in 1978, and presents an up-to-date synthesis and interpretation of regional sedimentary information...