Mapping of tecto-lineaments and their influence on sedimentological processes in a GIS environment: a case study of the Iberian trough, Spain

Antonio Herrero-Hernández 1 , Francisco Javier López-Moro 2 , María Elena Valle-Feijóo 3 , Fernando Gómez-Fernández 3 , 4 ,  and José Ramón Rodríguez-Pérez 3
  • 1 Research Group of Geological Engineering and Materials (INGEOMAT), Department of Mining Technology, Topography and Structures, Faculty of Mining Engineering, University of Leon, Campus of Vegazana, s/n, 24071 León, Spain
  • 2 Department of Geology, Faculty of Science, University of Salamanca, C/ Plaza de Los Caídos s/n, 37008 Salamanca, Spain
  • 3 Department of Mining Technology, Topography and Structures, Faculty of Mining Engineering, University of Leon, Campus of Vegazana, s/n, 24071 León, Spain
  • 4 Research Group of Geological Engineering and Materials (INGEOMAT), Department of Mining Technology, Topography and Structures, Faculty of Mining Engineering, University of Leon, Campus of Vegazana, s/n, 24071 León, Spain Spain

Abstract

The subsurface sedimentary succession of the Iberian Trough, Spain was examined using geophysical techniques (analogue seismic profiles) and inverse distance weighted (IDW) interpolation algorithm implemented in a gvGIS open source software. The results showed that the Late Cretaceous succession is divided into two depositional sequences: DS-1 (Late Albian-Middle Turonian) and DS-2 (Late Turonian-Campanian). From the analogical seismic sections, digital data and quantitative isopach maps for DS-1 and DS-2 were obtained. The new isopach maps obtained for the DS-1 sequence showed that the deeper sectors of the basin were located to the northeast and the proximal ones to the southwest. The palaeoshoreline was inferred to be situated in the N 150 direction. Across and parallel to this direction several blocks were delimited by faults, with a direction between 30 N and N 65. The thickness of the sediments in these blocks varied in direction NW-SE, with subsidence and depocentres in hangingwall and uplift in the footwall. These variations may have been related to active synsedimentary faults (e.g., Boñar and Yugueros Faults). In the DS-2 sequence, a lineament separated the smaller thicknesses to the southwest from the larger thicknesses (up to 1400 m) to the northeast. This lineament had an N170 orientation and it indicated the position of the palaeoshoreline. In the isopach map for DS-2 there were two groups of lineaments. The first showed a block structure that was limited by N100-120, they were foundering toward the S and had large thicknesses (depocentres), and rose towards the N, where there were smaller thicknesses. The second group of lineaments had a N 50-65 direction and, in this case, they had a similar interpretation as the one in DS-1. The maps obtained are of great help for geologists and permit better understanding of the geological setting and stratigraphic succession of the Late Cretaceous of the Iberian Trough.

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  • Burbank D.W. & Anderson R.S. 2001: Tectonic Geomorphology. Blackwell Science, 1-247.

  • Casas A.M., Cortes A.L., Maestro A., Soriano M.A., Riaguas A. & Bernal J. 2000: LINDENS: A program for lineament length and density analysis. Comput. Geosci. 26, 9-10, 1011-1022.

  • Dercourt J., Zonenshain L.P., Ricou L.E., Kazmin V.G., Le Pichon X., Knipper A.L., Grandjacquet C., Sbortshikov I.M., Geyssant J. & Lepvrier C. 1986: Geological evolution of the Tethys belt from the Atlantic to the Pamir since the Lias. Tectonophysics 123, 241-315.

  • Ekneligoda T.C. & Henkel H. 2010: Interactive spatial analysis of lineaments. Comput. Geosci. 36, 8, 1081-1090.

  • Catuneanu O., Abreu V., Bhattacharya J.P., Blum M.D., Dalrymple R.W., Eriksson P.G., Fielding G.C.R., Fisher W.L., Galloway W.E. & Gibling M.R. 2009: Towards the standardization of sequence stratigraphy. Earth-Sci. Rev. 92, 1-33.

  • Catuneanu O., Galloway W.E., Kendall C.G.St.C., Miall A.D., Posamentier H.W., Strasser A. & Tucker M.E. 2011: Sequence stratigraphy: methodology and nomenclature. Newsletters on Stratigraphy 44, 3, 173-245.

  • Cheng-Shin J., Shih-Kai C. & Yi-Ming K. 2013: Applying indicator-based geostatistical approaches to determine potential zones of groundwater recharge based on borehole data. Catena 101, 178-187.

  • Chorowicz J., Breard J., Guillande R., Morasse C., Prudon D. & Rudant J. 1991: Dip and strike measured systematically on digitised three-dimensional geological map. Photogramm Eng. Rem. S. 57, 431-436.

  • Chorowicz J., Collet B., Bonavia F.F., Mohr P., Parrot J.F. & Korme T. 1998: The Tana basin Ethiopia: intra-plateau uplift rifting and subsidence. Tectonophysics 295, 351-367.

  • Chorowicz J., Dhont D. & Gundogdu N. 1999: Neotectonics in the eastern North Anatolian fault region (Turkey) advocates crustal extension: mapping from SAR ERS imagery and Digital Elevation Model. J. Struct. Geol. 21, 511-532.

  • Ciry R. 1939: Etude géologique d’une partie des provinces de Burgos Palencia León et Santander B. Soc. Hist. Nat. 74, 1-528.

  • Collet B., Taud H., Parrot J.F., Bonavia F. & Chorowicz J. 2000: A new kinematic approach for the Danakil block using a Digital Elevation Model representation. Tectonophysics 316, 343-357.

  • Elmahdy S.I. & Mohamed M.M. 2016a: Automatic Feature Extraction Module for Change Detection in Al Ain, UAE: Analysis by Means of Multi-temporal Remote Sensing Data. Journal of the Indian Society of Remote Sensing 44, 1-10.

  • Elmahdy S.I. & Mohamed M.M. 2016b: Mapping of tecto-lineaments and investigate their association with earthquakes in Egypt: a hybrid approach using remote sensing data. Geomatics, Natural Hazards and Risk 7, 600-619.

  • Elmahdy S.I., Mansor S., Huat B.B. & Mahmod A.R. 2012: Structural geologic control with the limestone bedrock associated with piling problems using remote sensing and GIS: a modified geomorphological method. Environ. Earth Sci. 66, 8, 2185-2195.

  • Evers H.J. 1967: Geology of the Leonides between the Bernesga and Porma rivers. Cantabrian Mountains NW Spain. Leidse Geol Mededelingen 41, 83-151.

  • Galloway W.E. 1989: Genetic stratigraphic sequences in basin analysis I: architecture and genesis of flooding-surface bounded depositional units. AAPG Bull. 73, 125-142.

  • Gómez de Llarena J. 1934: Examples of tertiary tectonic thrust in Asturias, Leon and Palencia. Bol. R. Soc. Esp. Hist. Nat. 34, 2-3,123-127 (in Spanish).

  • Gómez-Fernández F., Méndez-Cecilia A.J. & Bahamonde R.J. 2003: The Boñar Formation (Upper Cretaceous, northern León): Stratigraphy, geochemistry and production potential of natural stone. Rev. Soc. Geol. Esp. 16, 1-2, 61-72 (in Spanish with English abstract).

  • Gossel W., Chudy T. & Falkenhagen M. 2012: Interpolation based on isolines: line-geometry-based inverse distance weighted interpolation (L-IDW) with sample applications from the geosciences. Z. Dtsch. Ges. Geowiss. 163, 4, 493-505.

  • Grijalba-Cuenca A., Torres-Verdín C. & Debeye H.W.J. 2000: Geostatistical inversion of 3-D seismic data to extrapolate petrophysical variables laterally away from the well. Society of Petroleum Engineers Annual International Meeting Dallas Texas (October 1-4) SPE Paper 63283, 1-17.

  • Herrero-Hernández A. 2002: Stratigraphy and sedimentology of the Tertiary deposits of the northern sector of the Duero Basin in the province of León. PhD. thesis: Universidad de Salamanca, 1-435 (in Spanish with English abstract).

  • Herrero-Hernández A. & Gómez-Fernández F. 2012: Palaeoshoreline for the Late Cretaceous marine platform in the Iberian Trough (Leonese Area Spain) deduced from outcrop and subsurface analysis. Cent. Eur. J. Geosci. 4, 3, 395-415.

  • Herrero-Hernández A., Alonso-Gavilán G. & Colmenero R.J. 2004: Subsurface stratigraphy in the northwest sector of the Duero Basin (province of Leon). Rev. Soc. Geol. Esp. 17, 3-4, 197-215 (in Spanish with English abstract).

  • Herrero-Hernández A., Alonso-Gavilán G. & Colmenero R.J. 2010: Depositional sequences in a foreland basin (north-western domain of the continental Duero basin Spain). Sediment. Geol. 223, 235-264.

  • Herrero-Hernández A., Gómez-Fernández F. & López-Moro F.J. 2013: Upper Cretaceous marine-continental transition (Leonese Area NW Spain) defined from integrated outcrop and seismic stratigraphy. Geol. J. 50, 39-55

  • Isaaks E.H. & Srivatava R.M. 1989: An introduction to applied geostatistics Oxford University Press, 1-561.

  • Jonker R.K. 1972: Fluvial sediments of Cretaceous age along the southern border of the Cantabrian Mountains Spain. Leidse Geologische Mededelingen 48, 275-379.

  • Jordan G., Meijninger B.M.L., van Hinsbergen D.J.J., Meulenkamp J.E. & van Dijk P.M. 2005: Extraction of morphotectonic features from DEMs: Development and applications for study areas in Hungary and NW Greece. Int. J. Appl. Earth Obs. 7, 163-182.

  • Jurecka M., Niedzielski T. & Migoń P. 2016: A novel GIS-based tool for estimating present-day ocean reference depth using automatically processed gridded bathymetry data. Geomorphology 260, 91-98.

  • Keller E.A. & Pinter N. 2002: Active Tectonics: earthquakes uplift and landscape. 2nd ed. Prentice Hall, 1-359.

  • Koike K. Nagano S. & Kawaba K. 1998: Construction and analysis of interpreted fracture planes through combination of satellite image derived lineaments and digital elevation model data. Comput. Geosci. 24, 573-583.

  • Krivoruchko K. 2011: Spatial Statistical Data Analysis for GIS Users. Esri Press, DVD-ROM.

  • Lu GY. & Wong DW. 2008: An Adaptive Inverse-Distance Weighting spatial interpolation technique. Comput. Geosci. 34, 1044-1055.

  • Mitchum Jr R.M., Vail P.R. & Thompson III S. 1977: Seismic stratigraphy and global changes of sea-level. Part 2: the depositional sequence as a basic unit for stratigraphic analysis. In: Payton E. (Ed.): Seismic Stratigraphy-Applications to Hydrocarbon Exploration. AAPG Mem. 26, 53-62.

  • Nappi R., Alessio G., Vilardo G. & Bellucci Sessa E. 2009: Integrated morphometric analysis in GIS environment applied to tectonically active areas. Mem. Soc. Geogr. Ital. 87, I-II. (in Italian with English abstract).

  • Sertel E., Demirel H. & Kaya S. 2007: Predictive mapping of air Pollutants: A GIS framework. Proceedings CD of the Fifth International Spatial Data Quality Symposium ITC CD Nm.17 Enschede Hollanda 17, 1-5.

  • Suárez-González, A., Kovács T., Herrero-Hernández A. & Gómez-Fernández F. 2016: Petrophysical characterization of the Dolomitic Member of the Boñar Formation (Upper Cretaceous; Duero Basin, Spain) as a potential CO2 reservoir. Estudios Geológicos 72, 1, e048.

  • Vail P.R., Mitchum Jr R.M. & Thompson III S. 1977: Seismic stratigraphy and global changes of sea level. Part 3: relative changes of sea level from coastal onlap. In: C.E. Payton (Ed.): Seismic Stratigraphy-Applications to Hydrocarbon Exploration. AAPG Mem. 26, 63-81.

  • Van Ameron H.W.J. 1965: Upper Cretaceous pollen and spores assemblages from the so-called «Wealden» of the pronvience of León (Northern Spain). Pollen and Spores 7, 89-93.

  • Vergés J. & Fernández M. 2006: Ranges and basins in the Iberian Peninsula: their contribution to the present topography. In: Gee D.G. & Stephenson R.A. (Eds.): European Lithosphere Dynamics. Geol. Soc. London, Mem. 32, 223-234.

  • Webster R. & Oliver M.A. 2001: Geostatistics for environmental scientists. John Wiley and Sons Ltd., Chichester, 1-271.

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