| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 5755764 | Palaeogeography, Palaeoclimatology, Palaeoecology | 2017 | 98 Pages |
Abstract
Comparison between the stratigraphic record from the East Gondwana interior rift and coeval records from Lhasa and Sibumasu indicate a similar pattern of climate change during the Carboniferous to end Cisuralian. Similar trends probably are present in Eastern Australia although there is confusion over the correlation of some units.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
David W. Haig, Arthur J. Mory, Eujay McCartain, John Backhouse, Eckart HÃ¥kansson, Andrej Ernst, Robert S. Nicoll, Guang R. Shi, Jennifer C. Bevan, Vladimir I. Davydov, Aaron W. Hunter, Myra Keep, Sarah K. Martin, Daniel Peyrot, Olga Kossavaya,