| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 8912964 | Earth-Science Reviews | 2018 | 101 Pages |
Abstract
During later intervals of uplift, the GSM scattered Cambrian-Ordovician, Permian-Triassic, and Cenozoic sediment across East Gondwanaland. In southern Australia, the Early-Middle Ordovician Delamerian Orogen recycled GSM-derived turbidites to the southern part of the Lachlan Orogen; and the Late Ordovician Ross Orogen in North Victoria Land sourced turbidite fans throughout eastern Australia.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geology
Authors
J.J. Veevers,