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Charles Rowland Twidale
Department of Geology and Geophysics, School of Physical and Earth Sciences, University of Adelaide
Australia
https://orcid.org/0009-0003-9679-7922
Juan Ramón Vidal Romaní
Instituto Universitario de Xeoloxía, Universidade da Coruña. ESCI, Campus de Elviña. 15071, A Coruña, Spain
Spain
https://orcid.org/0000-0001-7158-4945
Vol. 42 (2020), Articles, pages 29-52
DOI: https://doi.org/10.17979/cadlaxe.2020.42.0.7268
Submitted: Dec 15, 2020 Accepted: Dec 17, 2020 Published: Dec 28, 2020
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Abstract

Many of the so-called corestones have been developed from rocky blocks that have been apparently affected by subsurface physicochemical weathering that results in lamination, granulation, and eventually a puggy or stiff clay. The truth is that weathering takes advantage of a previous deformation structure and does not create it by weathering.

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References

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