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Stockdale, Shannon; Franchi, Ian; Morgan, Dan; Anand, Mahesh and Grady, Monica
(2018).
URL: https://www.hou.usra.edu/meetings/metsoc2018/pdf/6...
Abstract
The cooling rates of chondrules are one of the important constraints on chondrule formation and can be used to distinguish between competing chondrule formation mechanisms. Proposed mechanisms range from shockwaves in the solar nebula to impacts between planetesimals. Dynamic crystallisation experiments are the most widely cited methods of determining chondrule cooling rates and this indirect method has provided cooling rates from 1 to 3000 Kh-1. In order to assess whether this is a true representation of chondrule cooling rates, it should be validated or better constrained by using a more direct method. Modelling of diffusion profiles observed across the boundary between forsteritic- olivine relict grains and more fayalitic overgrowth provides a more direct approach to determining chondrule cooling rates.
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- Item ORO ID
- 62210
- Item Type
- Conference or Workshop Item
- ISSN
- 0161-5297
- Project Funding Details
-
Funded Project Name Project ID Funding Body STFC DTG 2015 - 2016 (2015 Intake) ST/N50421X/1 STFC (Science & Technology Facilities Council) - Academic Unit or School
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Faculty of Science, Technology, Engineering and Mathematics (STEM) > Physical Sciences
Faculty of Science, Technology, Engineering and Mathematics (STEM) - Research Group
- ?? space ??
- Copyright Holders
- © 2019 The Authors
- Related URLs
- Depositing User
- Shannon Stockdale