The Permian in the intracratonic basins consists of basal glacial to periglacial deposits overlain by marine and finally freshwater deposits. Basin shape was controlled mainly by NW and NE-trending structures that first appeared in the late
Triassic palynology of the Warang Sandstone (Northern Galilee Basin) and its phytogeographic implications in Gondwana Five. Selected papers and abstracts of papers.
Coast of the South Island, while a tectonically-controlled basin developed on the east coast of both islands. This early extensional phase was accompanied by volcanism ranging from rhyolitic to basaltic. The Late Cretaceous transgression and pene