Published July 9, 2013
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Fig. 9 in Recurrent constructional pattern of the crustacean burrow Sinusichnus sinuosus from the Paleogene and Neogene of Spain
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Fig. 9. Depositional setting of the crustacean burrow Sinusichnus sinuosus Gibert, 1996 bearing outcrops in the Vilomara area, Spain. A. Stratigraphic log showing the location of Sinusichnus (indicated by stars) (vf, very fine-grained sand; vc, very coarse-grained sand). B. Correlation panel (from López-Blanco et al. 2000c) showing Sinusichnus occurrences in relation to facies belts on the Sant Llorenç del Munt fan-delta complex and within the regressive sequence set of the Vilomara Composite sequence. Location of A is indicated. C. Panoramic view of the transition from delta front (sandstone beds on the SE) to prodelta (siltstone and mudstone beds on the NW) including Sinusichnus horizons (stars). D. Detail of the tabular alternation of sandstones and siltstone beds on the transition from delta front to prodelta that bears S. sinuosus.
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Related works
- Is part of
- Journal article: 10.4202/app.2012.0092 (DOI)
- Journal article: urn:lsid:plazi.org:pub:FF91E335EA6FFFA48B55FF86FFA4FFBB (LSID)
- Journal article: https://zenodo.org/record/13277520 (URL)