The Neogene and Quaternary Deposits of the Barcelona City Through the High-Speed Train Line
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Citation: Salvany, J.M., Aguirre, J., 2020. The Neogene and Quaternary deposits of the Barcelona city through the high-speed train line. Geologica Acta, 18.10, 1-19. DOI: 10.1344/GeologicaActa2020.18.10 The Neogene and Quaternary deposits of the Barcelona city through the high-speed train line J.M. Salvany1 and J. Aguirre2 1Departament d’Enginyeria Civil i Ambiental, Universitat Politècnica de Catalunya c/ Jordi Girona 1-3, 08034 Barcelona. E-mail: [email protected] 2Departamento de Estratigrafía y Paleontología, Facultad de Ciencias, Universidad de Granada Avenida Fuentenueva s/n, 18002 Granada. E-mail: [email protected] ABSTRACT A total of 208 boreholes with continuous core sampling, drilled for the construction of the high-speed train line through the city of Barcelona and other nearby infrastructures, were studied. The correlation of the lithologic logs of these boreholes allows identifying five main depositional sequences bounded by sharp erosional surfaces: i) lower Miocene, of alluvial origin; ii) middle Miocene, of deltaic-lacustrine origin; iii) lower Pliocene, of beach-shelf origin; iv) Pleistocene, of alluvial origin and v) Holocene, of deltaic origin. The erosive surfaces that separate these sequences represent important erosive hiatus linked to prolonged sea level falls at regional scale, which eliminated the upper part of each one. Sedimentation took place during decreasing intensity of extensional tectonic activity that mainly affected the Miocene deposits. The Plio-Quaternary units show their original structure apparently without tectonic alterations. Some new biostratigraphic data based on foraminifer assemblages allowed making accurate estimate of the age of the deposits. KEYWORDS Neogene. Quaternary. Barcelona. Boreholes. Foraminifera. INTRODUCTION L’Hospitalet to the proximities of Sants railway station (Adif, 2005) and ii) from Sants to Sagrera railway station In the first decade of 2000, the high-speed train line (Adif, 2007) (Fig. 1). Both sections are separated by an through the Barcelona city subsoil (“Linea de Alta interval of about 500m of length corresponding to Sants Velocidad”, LAV) was projected and constructed. It led to station, which has no subsurface information available (the the excavation of a tunnel of 10km in length, which begins tunnel passes mainly at surface level and no boreholes were in the district of El Gornal, in L’Hospitalet del Llobregat drilled). The sections differentiate three main stratigraphic village, and extends practically continuously till the units: the Quaternary (Holocene) of the Llobregat delta, neighborhood of La Sagrera, in the North end of Barcelona the Quaternary (Pleistocene) of the Barcelona plain, and (Fig. 1). a Tertiary (Neogene) basement. These units are composed of unconsolidated terrigenous materials ranging from fine During the tunnel’s project phase, an important to very coarse grain sizes, which give layers of variable number of boreholes were drilled allowing the elaboration development according to the boreholes. This led to interpret of two geological-geotechnical cross-sections: i) from a complicated structure of facies lateral changes among the J.M. Salvany, J. Aguirre, 2020 CC BY-SA 1 J.M. Salvany and J. Aguirre Neogene and Quaternary of the Barcelona city FIGURE 1. Upper part: simplified geological map of the Barcelona area and location of the studied LAV line from the Llobregat delta to Sagrera, L9 lines from Sagrera and Besòs River, and the boreholes of the L8 line and Catalunya Square. I to V are the sections enlarged in Figures 2, 3 and 4. Lower part: simplified geological cross-section and tunnels of the LAV and L9 lines. different materials, which are difficult to understand from a during the constructive project and the subsequent tunnel sedimentary point of view. construction of the LAV line, as well as of other nearby infrastructures. More especially, this paper provides criteria During the tunnel’s excavation, additional geotechnical to differentiate the Miocene and the Pliocene deposits, and hydrogeological studies were performed in order to commonly difficult to distinguish due to their similar better understand some areas of potential constructive lithological characteristics. Moreover, the paper present problems. Part of these studies were developed to protect new biostratigraphic data that allow constraining the age some sensitive constructions, such as the world heritage and the sedimentary environment of the Neogene deposits. buildings of the Sagrada Familia basilica and Casa Milà Finally, a sedimentary interpretation of the studied units (Alonso and Ledesma, 2015; Ledesma and Alonso, 2017; in the context of the Mediterranean Catalan margin is Pujades et al., 2015; Rodríguez and Blanco, 2012). Other proposed. studies were performed to understand the ground water behaviour during the construction of several deep enclosures (shafts) linked to the Sants-Sagrera tunnel (Culí et al., 2016; GEOLOGICAL SETTING Pujades et al., 2014a, b), the construction of the Sagrera railway station (Candel-Soley and Verbón-Rotllán, 2008; Barcelona is built on five different geological areas of Serrano-Juan et al., 2017), and other parts of the tunnel the Catalan coast: the mountain of Collserola, the Montjuïc (Arroyo et al., 2012; Vilarrasa et al., 2008). These studies hill, the Barcelona plain, and the Llobregat and Besòs present local geological layer-cake type models, obtained deltas (Fig. 1). from correlating sets of close boreholes, sometimes with the help of well-logging (gamma-ray) surveys. The mountain of Collserola, with a height of up to 512m above sea level (Tibidabo), is the part of the Catalan Beyond its constructive purposes, the boreholes of the Litoral Range limited by the valleys of the Besòs River LAV line have provided an excellent opportunity to better to the north and the Llobregat River to the south. It is determine the geology of the subsurface of the city, which made up mainly of metamorphic rocks (slates, hornfels, is still poorly known. With this goal, this paper provides schists, quartzites), as well as sedimentary (limestones, a new Neogene-Quaternary stratigraphic framework and sandstones) and granitic rocks, ranging from Ordovician the sedimentary meaning of the Barcelona subsurface to Carboniferous age (Enrique, 1990; Gil-Ibarguchi and based on the revision of a selection of boreholes made Julivert, 1988; Julivert and Duran, 1990; Llopis-Lladó Geologica Acta, 18.10, 1-19 (2020) 2 DOI: 10.1344/GeologicaActa2020.18.10 J.M. Salvany and J. Aguirre Neogene and Quaternary of the Barcelona city et al., 1969; Sunyer-Coma, 2001; Vaquer, 1973). To the the Tibidabo (or Collserola) fault by the same author. They southeast, these rocks extend below the Neogene and constitute two normal faults related to the extensional Quaternary deposits of the Barcelona plain and deltas, thus tectonics that affected the western Mediterranean during forming its basement. They are rocks strongly folded and the Miocene (Bartrina et al., 1992; Roca et al., 1999). faulted due to Variscan and Alpine tectonics (Santanach et al., 2011), as well as largely weathered from its surface up The Neogene below the Quaternary of the Barcelona to some tens of meters deep. plain includes Pliocene, middle Miocene and lower Miocene deposits. Montjuïc is a gentle coastal relief, up to 175m in height, located between the Barcelona plain and the Llobregat Since the former studies by García-Faria (1893) and delta. It is mainly composed of marls, sands, gravels, and Rubio and Kindelan (1909) it is assumed that the Pliocene conglomerates of deltaic origin, with a total thickness of deposits form an almost continuous bed of marls below de about 200m (Gómez-Gras et al., 2001; Parcerisa et al., 2001; Quaternary, up to 140m in thickness according to a deep Salvany, 2013; Villalta and Rosell, 1965; among others). borehole close to Sagrera station. More recently, the Pliocene Its abundant content of marine fauna led to attribute these has been studied in several excavations and drillings of deposits to the middle Miocene: Vindobonian, according the city (Alborch et al., 1980; Cabañas, 1986; Gillet and to ancient paleontological studies (see Via and Padreny, Vicente, 1961; Vicente-Castells, 1979, 1986, 1990; Vicente 1972), or Serravallian, according to the more recent one by and Fernández, 1993). However, a precise stratigraphy of Parcerisa (2002). this unit remains unknown. This differs from the Pliocene of the neighboring area of the lower Llobregat valley, where The Barcelona plain constitutes a flat surface that a large number of paleontological studies have been carried extends in a gentle slope from the foot of the mountain of out (Almera, 1894; Civis, 1972, 1977a, b, 1979; Gibert- Collserona to the coastline. This plain constitutes the top Atienza, 1995; Gibert and Martinell, 1992, 1993, 1995; of a colluvial-alluvial deposit that ranges from a few meters Martinell and Marquina, 1981; Martinell, 1988; Sanz de to 50m in thickness (Llopis-Lladó, 1942; Ribera-Faig, Siria-Catalán, 1994). These studies have analyzed the 1945; Solé-Sabarís, 1963; Virgili, 1960). Traditionally, outcrops along the valley margins and have established a this deposit is attributed to the Quaternary, in a broad stratigraphy consisting of a lower unit of gray-blue marls sense because it has never been dated. This age is based that grade upwards to an upper unit of yellow clay and sand, on its equivalence to the alluvial terraces of the Llobregat all of which amounts a few tens of meters in thickness. River, dated as Quaternary by Solé-Sabaris (1963). Some These materials contain abundant fossils of marine fauna authors, however, consider it to belong to the late Pliocene and flora, as well as a great variety of biogenic structures. to Pleistocene (Riba and Colombo, 2009). Despite this rich fossil record, there are discrepancies about the precise age and paleoenvironmental meaning of the At the end of the Pleistocene, a drainage network going Pliocene sediments. from Collserola to the coast developed in the Quaternary plain (Julià, 1977; Vila, 1977). This caused the downcutting The characteristics of the middle Miocene below the of a creek network known as “rieres”.