Dear all,

I’m wondering if sedimentary cross-bedding could be tectonically reactivated, or by a vein formation parallel to the cross-bedding, or even by a sort of ‘bed-on-bed’ movement on the individual layers of the cross-bedding.

Does anyone knows about possible examples in the field or literature?

Any opinion on this idea is welcome.

Cheers,

Manuel

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Manuel Sintubin, PhD FGS
Professor of Geodynamics
Department of Earth & Environmental Sciences
Katholieke Universiteit Leuven
Celestijnenlaan 200E - box 2410
BE-3001 Leuven
Phone: +32 (0)16 32 64 47 - +32 (0)16 32 78 00
Fax: +32 (0)16 32 29 80
Mobile phone: +32 (0)496 50 25 79
E-mail: [log in to unmask]
URL: perswww.kuleuven.be/manuel_sintubin/
Route description: ees.kuleuven.be/geology/contact/howtoreachus/
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International Geoscience Programme
IGCP 567 Earthquake Archaeology
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EOS Scilogs Planeet Aarde. Een uniek kosmisch experiment

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De wetenschap van de Aarde. Over een levende planeet

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