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Charles Rowland Twidale
Department of Geology and Geophysics, School of Physical and Earth Sciences, University of Adelaide
Australia
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.

Article Details

References

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