Copy the page URI to the clipboard
Gilmour, I.; Jolley, D.W.; Watson, J. S.; Gilmour, M. A. and Kelley, S. P.
(2013).
URL: http://meetingorganizer.copernicus.org/EPSC2013/EP...
Abstract
Lacustrine sediments from the 24 km diameter Boltysh impact structure record the rapid formation of an intra-crater lake. Stable isotope compositions and organic maturity parameters from the lake sediments deposited post-impact show that they were heated by underlying impactites. This heating is attributed to the establishment of an impact- generated hydrothermal system. Estimates of the duration of heating are ~30 – 40 k.y. consistent with the suggestion that crater lakes extend the longevity of impact-generated hydrothermal systems.
Viewing alternatives
Download history
Item Actions
Export
About
- Item ORO ID
- 37904
- Item Type
- Conference or Workshop Item
- Extra Information
-
EPSC Abstracts
Vol. 8, EPSC2013-177, 2013
European Planetary Science Congress 2013 - Academic Unit or School
-
Faculty of Science, Technology, Engineering and Mathematics (STEM) > Physical Sciences
Faculty of Science, Technology, Engineering and Mathematics (STEM)
Institute of Educational Technology (IET) - Copyright Holders
- © 2013 The Authors
- Related URLs
-
- http://www.abdn.ac.uk/boltysh/(Research Group)
- http://science-people.open.ac.uk/i.gilmo...(Author Website)
- http://www.epsc2013.eu/(Other)
- Depositing User
- Iain Gilmour