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  Information - TS9 Paleostress fields from structural kinematics - real or imagined

Event Information
Palaeostress analysis, a major discipline within structural geology, concerns itself with the reconstruction of past geological stress states based on data from microstructures, and aims to provide constraints on regional tectonics. This session will focus on the following aspects of palaeostress analysis:

*methodological advances, using data collected from striated faults, stylolites and tension gashes. The use of joints for regional paleostress analysis.

* the variation of palaeostress states with time. The recognition of successive stress events – strategies and examples.

* The spatial variation of stress and the reconstruction of stress fields, i.e. the integration of several regionally distributed stress estimates to attempt to create palaeostress trajectory patterns. What are the constraints on neighbouring stress tensors imposed by stress compatibility?

* Testing the validity of the results. Are existing methods based on faulty assumptions? Can tests be devised to distinguish the results from coherent datasets from the results derived from random assemblages of slipped faults? If the underlying assumptions are flawed, why are consistent results obtained? If fault-slip methods do not deliver palaeostresses what ARE they delivering?

Preliminary List of Solicited Speakers
Jacques Angelier
David Pollard

Co-Sponsorship

General Statement
The information contained hereafter has been compiled and uploaded by the Session Organizers via the "Organizer Session Form". The Session Organizers have therefore the sole responsibility that this information is true and accurate at the date of publication, and the conference organizer cannot accept any legal responsibility for any errors or omissions that may be made, and he makes no warranty, expressed or implied, with regard to the material published.



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