Reorganization of a deeply incised drainage: role of deformation, sedimentation and groundwater flow
Version of Record online: 18 MAY 2011
© 2011 The Authors. Basin Research © 2011 Blackwell Publishing Ltd, European Association of Geoscientists & Engineers and International Association of Sedimentologists
Volume 23, Issue 6, pages 631–651, December 2011
How to Cite
Brocard, G., Teyssier, C., Dunlap, W. J., Authemayou, C., Simon-Labric, T., Cacao-Chiquín, E. N., Gutiérrez-Orrego, A. and Morán-Ical, S. (2011), Reorganization of a deeply incised drainage: role of deformation, sedimentation and groundwater flow. Basin Research, 23: 631–651. doi: 10.1111/j.1365-2117.2011.00510.x
- Issue online: 5 OCT 2011
- Version of Record online: 18 MAY 2011
- Manuscript received 26 February 2010; Manuscript accepted 11 April 2011.
Figure S1. Paleosols of Sicaché.
Figure S2. Grain size of gravel deposits.
Figure S3. Sediment provenance in the paleovalleys of Sicaché (V4) and Chitapol (V5).
Figure S4. Sediment provenance in V7 (Chicruz).
Figure S5.40Ar-39Ar istopic data: step-heating for samples from ignimbrites pertaining to the Colotenango Beds, V0 (2-61), Sicaché paleovalley, V5 (7-71, 7-72), and Chitapol paleovalley, V4 (7-141).
Table S1. General characteristics of the paleovalleys.
Table S2. Major element composition of Miocene ignimbrites and derived Miocene soils, obtained by X-ray fluorescence.
Table S3. Weathering indices in paleosoils developed on top of Ignimbrite 1, V5.
Table S4. Grain size measurements.
Table S5. Clast assortment, paleovalleys V4, V5 and V7.
Table S6. Area occupied by rock source units in the reconstructed paleocatchments of Figures S3 and S4.
Table S7.40Ar/39Ar isotopic analyses.
Appendix S1. General characteristics of the paleovalleys.
Appendix S2. Geochemical analyses of ignimbrites and soils.
Appendix S3. Grain size characteristics of fluvial deposits.
Appendix S4. Clast provenance for paleovalleys V4 (Chitapol), V5 (Sicaché) and V7 (Chicruz).
Appendix S5.40Ar/39Ar isotopic analyses.
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