Year-end Sale % OFF 
Abstract
The uplift rates calculated for Tasmania by Shin (2013) are not supported by the data presented in his paper. The OSL ages obtained indicate a Last Glacial age and fluvial origin for many of the deposits analysed. OSL ages obtained on sediments at Mary Ann Bay in southern Tasmania confirm recent research indicating a Last Glacial age and aeolian deposition of the sands rather than marine (Last Interglacial) deposition. Anomalously high uplift rates for southern Tasmania, proposed by earlier researchers and Shin (2013), are discounted.
Published Version
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
