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Relevant bibliographies by topics / South Central Pyrenees

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Academic literature on the topic 'South Central Pyrenees'

Author: Grafiati

Published: 4 June 2021

Last updated: 12 February 2022

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Journal articles on the topic "South Central Pyrenees"

1

Williams, Graham D. "Thrust tectonics in the south central pyrenees." Journal of Structural Geology 7, no. 1 (1985): 11–17. http://dx.doi.org/10.1016/0191-8141(85)90111-7.

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Caus, Esmeralda, and Antonio Gómez-Garrido. "Upper cretaceous biostratigraphy of the south-central Pyrenees (Lleida, Spain)." Geodinamica Acta 3, no. 3 (1989): 221–28. http://dx.doi.org/10.1080/09853111.1989.11105188.

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Simó, Antonio. "Carbonate platform depositional sequences, Upper Cretaceous, south-central Pyrenees (Spain)." Tectonophysics 129, no. 1-4 (1986): 205–31. http://dx.doi.org/10.1016/0040-1951(86)90252-0.

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Bond, R. M. G., and K. R. McClay. "Inversion of a Lower Cretaceous extensional basin, south central Pyrenees, Spain." Geological Society, London, Special Publications 88, no. 1 (1995): 415–31. http://dx.doi.org/10.1144/gsl.sp.1995.088.01.22.

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Ramos, Adrià, Berta Lopez-Mir, Elisabeth P. Wilson, Pablo Granado, and Josep Anton Muñoz. "3D reconstruction of syn-tectonic strata in a salt-related orogen: learnings from the Llert syncline (South-central Pyrenees)." Geologica Acta 18 (December 11, 2020): 1–19. http://dx.doi.org/10.1344/geologicaacta2020.18.20.

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The Llert syncline is located in the South-central Pyrenees, between the eastern termination of the EW-trending Cotiella Basin and the north-western limb of the NS-trending Turbón-Serrado fold system. The Cotiella Basin is an inverted upper Coniacian-lower Santonian salt-floored post-rift extensional basin developed along the northern Iberian rift system. The Turbón-Serrado fold system consists of upper Santonian – Maastrichtian contractional salt-cored anticlines developed along an inverted transfer zone of the Pyrenean rift system. Based on field research, this paper presents a 3D reconstruction of the Llert syncline in order to further constrain the transition between these oblique salt-related structures. Our results suggest that the evolution of the Llert syncline was mainly controlled by tectonic shortening related to the tectonic inversion of the Cotiella Basin synchronously to the growth of the Turbón-Serrado detachment anticline, and by the pre-compressional structural framework of the Pyrenean rift system. Our contribution provides new insight into the geometric and kinematic relationships of structures developed during the inversion of passive margins involving salt.

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López-Vicente, M., A. Navas, and J. Machín. "Modelling soil detachment rates in rainfed agrosystems in the south-central Pyrenees." Agricultural Water Management 95, no. 9 (2008): 1079–89. http://dx.doi.org/10.1016/j.agwat.2008.04.004.

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Granet, Michel, Sebastien Judenherc, and Annie Souriau. "Des images du systeme lithosphere-asthenosphere sous la France et leurs implications geodynamiques; l'apport de la tomographie telesismique et de l'anisotropie sismique." Bulletin de la Société Géologique de France 171, no. 2 (2000): 149–67. http://dx.doi.org/10.2113/171.2.149.

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Abstract From seismic tomography and seismic anisotropy, images of the lithosphere-asthenosphere system beneath France for some remarkable tectonic areas have been computed : a continental rift system (the Upper Rhinegraben), an Hercynian structure reactivated by Neogene volcanism (Massif central), a region of a recent continental collision (Pyrenees) and finally a region of an ancient orogeny (Armorican Massif). These images have a horizontal spatial resolution of the order of 10 km and show not only the geometry of the deep geological structures but will also illustrate the link between surface observations and structures detected at depth. The images demonstrate the passive character of the Rhinegraben mainly because no low-velocity was found below the Moho, show the presence of a thermal anomaly beneath the Massif central interpreted as caused by a mantle plume in the decaying phase of its evolution and prove the lithospheric scale of the North Pyrenean fault and of the South-Armorican shear zone. The anisotropic measurements suggest a lithospheric deformation related to the most recent tectonic event. In the Pyrenees, the Armorican Massif or the Rhinegraben areas, the directions of the fast-polarisation azimuth (the polarisation direction of the fast shear wave) are parallel to the tectonic texture of the last events, but suggest also a reactivation of inherited Hercynian discontinuities. In the Massif central, the splitting parameters distinguish between two lithospheric units regions marked by a distinct fast-polarisation azimuth on each side of the Sillon Houiller fault zone.

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López-Martínez, Nieves, María A. ÁLvarez-Sierra, Remmert Daams, Pablo Peláez-Campomanes, and Paloma Sevilla. "Vertebrate Succession from Late Cretaceous to Early Tertiary, South-Central Pyrenees (Lleida, Spain)." Paleontological Society Special Publications 8 (1996): 246. http://dx.doi.org/10.1017/s2475262200002483.

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Navas, A., L. Gaspar, M. López-Vicente, and J. Machín. "Spatial distribution of natural and artificial radionuclides at the catchment scale (South Central Pyrenees)." Radiation Measurements 46, no. 2 (2011): 261–69. http://dx.doi.org/10.1016/j.radmeas.2010.11.008.

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Donaire, Mario, and Nieves López-Martínez. "Porosity of Late Paleocene Ornitholithus eggshells (Tremp Fm, south-central Pyrenees, Spain): Palaeoclimatic implications." Palaeogeography, Palaeoclimatology, Palaeoecology 279, no. 3-4 (2009): 147–59. http://dx.doi.org/10.1016/j.palaeo.2009.05.011.

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Dissertations / Theses on the topic "South Central Pyrenees"

1

Jones, Stuart Jason. "The evolution of alluvial systems in the south central Pyrenees, Spain." Thesis, University of Reading, 1998. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.301956.

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Michael, Nikolaos. "Functioning of an ancient routing system, the Escanilla Formation, South Central Pyrenees." Thesis, Imperial College London, 2013. http://hdl.handle.net/10044/1/12633.

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The thesis topic concerns the analysis of a well-exposed Eocene sediment routing system in the wedge-top zone of the southern Pyrenees. The Escanilla sediment routing system can be used as a case study of generic value in understanding the dynamics of an ancient source-to-sink system. The Escanilla Formation is a mid-upper Eocene (Bartonian – Priabonian) siliciclastic sedimentary system that was sourced from the Axial Zone of the Pyrenees and deposited on top of the fold-thrust belt of the south-central tectonic unit. Its deposits are found in the Tremp-Graus and Ainsa basins and distal time equivalent units are found in the Jaca basin. The project involves the definition of the sediment routing system linking source area catchments and depositional sinks. It investigates the provenance of sediment in the basin-fill, tracks down-system sedimentological and granulometric trends, and evaluates the volumetric budget of the entire sediment routing system. The reconstruction of the sediment routing system fairway was aided by new provenance data comprising U/Pb dating of detrital zircons, detrital apatite fission track analysis, and evaluation of clast lithologies in fluvial conglomerates, compilation of palaeoflow indicators from sedimentary structures, and a pilot study of heavy minerals. A correlation panel is proposed dividing the Escanilla system into three time intervals. Sedimentary facies changes, grain-size of conglomerate and grain-size fractions are analysed quantitatively from proximal to distal stations within these three time intervals. The fairway, combined with sedimentary logs, allows a sediment budget to be constructed. Depositional volumes and surface fluxes are calculated for the three time intervals, allowing the temporal evolution of the sediment routing system to be constrained. Knowledge of the evolution of sediment budgets and fluxes through time allows an assessment of the sediment effluxes of catchment areas feeding the Escanilla system, and helps an understanding of how supply signals (grain-size fractions and sediment volumes) are propagated down-system. Such propagation is a vital tool in stratigraphic prediction.

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Garcia, Sellés Albert. "Oological Record of Dinosaurs in South-Central Pyrenees (SW Europe): Parataxonomy, diversity and biostratigraphical implications." Doctoral thesis, Universitat de Barcelona, 2012. http://hdl.handle.net/10803/84108.

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Southern Pyrenees has provided an abundant fossil record of dinosaur eggs and eggshells. Historically, the oofamily Megaloolithidae has shown its predominance over any other group of fossil eggs in this region. In addition, this oofamily is world-wide distributed being represented by, at least, four oogenus and 20 oospeices. Considering that the eggshell is a high stable structure, this number of Megaloolithus‘s oospecies is too high for such a relatively short time-interval (Campanian to Maastrichtian; less than 7 My). The structural characters used to define these oospecies are critically revised. As a consequence, three structural groups have been identified, and only ten oospecies have been considered valid. Four of those oospecies have been recognized in Southern Pyrenees: M. aureliensis, M. sirugei, M. mamillare and M. baghensis. The oogenus Cairanoolithus, historically included in Megaloolithidae oofamily, is reevaluated. All evidences suggest that this type of fossil egg is, definitively, different from any other Megaloolithus. Consequently, a new oofamily is erected (Cairanoolithidae oofam. nov), which emphasizes the singularity of cairanoolithid eggs. Phylogenetical analysis also suggests that the eggs of Cairanoolithidae oofam. nov. could be laid by ornithischian dinosaurs. New oological material is described here, including the first spheroolithid oospecies (Spheroolithus oosp. nov.) from the Upper Cretaceous of Europe. Several oospecies of Prismatoolithus (Prismatoolithus oosp. nov, Prismatoolithus cf. levis, Prismatoolithus oosp. indet.) and few eggshells of ratite-morphotype (cf. Ageroolithus fontllonguensis) have been identified. In addition, the great number of specimens attributed to Pseudogeckoolithus oogenus allows re-describing and re-assigning this ootaxon to Mesozoic lizards. The space-temporal variation of the oological diversity in the Southern Pyrenees could be a consequence of environmental changes during the end-Cretaceous or even due to preferences in the nesting-site of each group of dinosaurs. Finally, biostratigraphical studies based on the successions of megaloolithid oospecies have been performed in Coll de Nargó and Àger-Tremp basins, and the European Megaloolithus succession has been updated. As a result, three oozonones have been described: M. aureliensis + Cairanoolithus oozone dates the Late Campanian, M. siruguei oozone the Early Maastrichtian and M. mamillare + M. baghensis oozone the Late Maastrichtian.

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López, Mir Berta. "Extensional salt tectonics in the Cotiella post-rift basin (south-central Pyrenees): 3D structure and evolution." Doctoral thesis, Universitat de Barcelona, 2013. http://hdl.handle.net/10803/132321.

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The Cotiella Massif in the southern Pyrenees constitutes a seismic-scale exposure of an extensional basin developed during the Late Cretaceous by the gravity-driven collapse of the post-rift platform above Upper Triassic salt. The internal structure is dominated by four main middle Coniacian-early Santonian sub-basins with large rollover anticlines. They involve the carbonates of the post-rift succession which unconformably overlies the Lower Cretaceous syn-rift basins. The extensional faults are only partially inverted despite is transported tens of kilometres southwards in the Pyrenean nappes. Data presented in this Thesis reveal that the tectono-sedimentary evolution of the basin has not only been controlled by the growth of extensional faults above salt, but also by the rising and falling of diapirs, as well as by salt migration and the development of transfer faults. At late Santonian, the extensional faults were partially inverted, salt was expulsed and salt welds were produced, leaving little trace of the original salt volume. Even though, the extensional features are outstandingly preserved. The excellent exposures offer a unique opportunity to investigate in outcrop the structure and infilling of a post-rift salt basin and gain insight into the understanding of other salt-involved passive margins. Thus, the main purposes of the Thesis are twofold: 1) describe the structure and the facies distribution of the inverted Cotiella basin with more detail than existing works and 2) decipher the role of salt tectonics in its development. To reach these objectives, the structure has been investigated through geological mapping and structural field data acquisition, integrated with a three-dimensional (3D) 1:5.000 digital terrain model. A surface-data based 3D reconstruction; cross-sections along strike and across strike, interpretation of oblique photographs. The middle Coniacian – early Santonian succession has been sub-divided into litostratigraphic units which make the investigation of the tectono-sedimentary evolution of the Cotiella basin possible. The data presented is compared with similar structures of the world and the given interpretations are validated with sequential restorations of the salt structures. Ultimately, a structural evolutionary model of the Cotiella basin is proposed.

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Beamud, Amorós Elisabet. "Paleomagnetism and Thermochronology in Tertiary systectonic sediments of the South-central Pyrenees: Chronostratography, kinematic and exhumation constraints." Doctoral thesis, Universitat de Barcelona, 2013. http://hdl.handle.net/10803/129314.

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This PhD Thesis presents the Tertiary kinematic evolution of the South-Central Pyrenees from the integration of magnetostratigraphic, magnetotectonic and thermochronological analyses on its synorogenic sedimentary record. One of the main contributions of this PhD thesis is the continuous absolute dating of the syntectonic conglomerates of La Pobla de Segur, Senterada and Sis. Magnetostratigraphy of these materials establishes their deposition during Middle Eocene-Late Oligocene times (from chron 19r up to chron 9n). Integration of these results with previous magnetostratigraphic works within the Ainsa Basin has allowed the establishment of a new chronostratigraphy for the Eocene-Oligocene materials of the South-Central Pyrenees. The obtained chronostratigraphy has biochronological implications as it substantially changes the traditionally accepted ages of the European reference levels MP14 to MP17. MP14 and MP15 reference levels are proposed to correlate to Lutetian whereas MP16 and MP17 would be Bartonian in age. These results reveal that the correlation between the continental and marine Paleogene record needs further refinement and therefore, that the chronostratigraphic age attributions based on MP reference levels should be taken with caution. The magnetostratigraphic ages have been combined with detrital thermochronology on 13 granitic cobbles enclosed in the syntectonic conglomerates. The detrital apatite fission track ages obtained vary from 63 to 27 Ma. When these ages are combined with the stratigraphic ages, samples define 5 groups with thermochronological ages generally increasing down-section except in the most deeply buried ones due to post-depositional partial annealing. Thermal models reveal three periods of rapid-cooling within the Axial Zone due to movement on large-thrust sheets. A dramatic increase in exhumation rate occurred during the latest Eocene-Early Oligocene related to the onset of movement in the Rialp thrust sheet and the increase in structural relief of the Axial Zone by underthrusting. The magnetostratigraphic and thermochronological ages obtained permit the link between the sedimentation rates in the surrounding basins and the exhumation rates in the hinterland, and reveal that accommodation space exerted the main control on sedimentation rates within the piggy-back basins. Post-depositional annealing of the stratigraphically lowest samples suggests about 2 km of burial by the younger synorogenic materials during progressive burial of the South Pyrenean fold and thrust belt. Thermal models also suggest a rapid exhumation event during the Late Neogene, linked to re-excavation caused by the base level drop during the Ebro River capture to the Mediterranean Sea. Sedimentation of the studied synorogenic materials during Middle Eocene-Oligocene times occurred coeval to the development of thrust salients in the southern Pyrenees. The magnetotectonic study of 36 sites carried out in the Ainsa Oblique Zone reveal clockwise vertical-axis rotations varying from ~80° in the lower Lutetian materials of the Mediano anticline to ~20° in middle Ilerdian materials cropping out at the northern edge of the Añisclo anticline. Sites in the central part of the Montsec and Bóixols thrust sheets don’t record any significant rotation as neither do the syntectonic materials of La Pobla, Sis and Senterada. The age of the main rotation event within the Gavarnie thrust sheet is constrained to Lutetitan to Bartonian times, when all the structures of the Ainsa Oblique Zone were active. This vertical-axis rotation stage obeys to a difference of ~50 km in the amount of displacement on the Gavarnie thrust sheet controlled by the NE-SW pinch out of the Triassic salts at its basal detachment. A second rotation event of ~ 10° took place since Priabonian times, as a result of the differential displacement of about 22 km of the Serres Marginals thrust sheet, respect the Gavarnie one, on top of the upper Eocene-Oligocene evaporites. The synchronicity between thrusting and vertical-axis rotations suggests that the curved fold and thrust belt formed by progressive curvature with divergent thrust transport. The results exposed in this Thesis reveal a strong relationship between the stratigraphic record of the synorogenic materials, thrusting and exhumation in the Axial Zone and the structural evolution of the South Pyrenean thrust system. Tectonic forces controlled the observed patterns of exhumation, the evolution of the synorogenic topography of the piggy-back and foreland basins and the depositional features of the synorogenic sediments.<br>Aquesta tesi presenta l’evolució cinemàtica dels Pirineus centre-meridionals durant el Terciari a partir de la integració de dades magnetostratigràfiques, termocronològiques I magnetotectòniques del seu registre sinorogènic. La datació magnetostratigràfica dels conglomerats sintectònics de La Pobla de Segur, Senterada i Sis, fixa la seva edat en Eocè mig-Oligocè superior (cron 19r a cron 9n). Aquests resultats permeten establir una nova cronostratigrafia pels materials eocens-oligocens dels Pirineus centre-meridionals de la que deriven implicacions biocronològiques, ja que canvia substancialment les edats acceptades del nivells de referència europeus MP14 a MP17. Les edats magnetostratigràfiques s’han combinat amb termocronologia detrítica de blocs de granit dels conglomerats sintectònics. La termocronologia obtinguda varia de 63 a 27 Ma. Els models tèrmics revelen tres períodes de refredament ràpid relacionats amb el moviment de grans encavalcaments a la Zona Axial, destacant l’ocorregut a l’Eocè superior-Oligocè inferior degut al moviment de l’encavalcament de Rialp i a l’increment de relleu a la Zona Axial per underthrusting. L’annealing post-deposicional de les mostres estratigràficament més baixes suggereix que el cinturó de plecs i encavalcaments pirinenc va estar cobert per 2 km de materials. Els models tèrmics també suggereixen una exhumació ràpida al Miocè superior, relacionada amb la captura de l’Ebre al Mediterrani. Durant la sedimentació dels materials sinorogènics estudiats té lloc la formació de thrust salients als Pirineus meridionals entre els que destaca la Zona Obliqua d’Ainsa. L’estudi magnetotectònic dut a terme en aquesta zona revela rotacions verticals que varien de ~80º a Mediano a ~20º al nord d’Añisclo. L’edat de la rotació principal a la làmina de Gavarnie s’estableix en el Lutecià-Bartonià, quan eren actives totes les estructures de la Zona Obliqua d’Ainsa, i estaria causada per una diferència de 50 km en la quantitat de desplaçament de la làmina de Gavarnie controlada per la distribució de les sals triàsiques al seu desenganxament basal. La sincronia entre encavacalments i rotacions apunta a un model d’arc progressiu amb transport divergent. Aquests resultats revelen una estreta relació entre el registre estratigràfic dels materials sinorogènics, els encavalcaments i l’exhumació a la Zona Axial i l’evolució estructural del sistema d’envacalments dels Pirineus meridionals. Les forces tectòniques van controlar els patrons d’exhumació, l’evolució de la topografia sinorogènica de les conques intramuntanyoses i d’avantpaís i les característiques deposicionals dels sediments sinorogènics.

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Jirutthitijaroen, Preeya. "Application of ground penetrating radar image shallow-water carbonate, South-central Pyrenees, Spain." 2006. http://catalog.hathitrust.org/api/volumes/oclc/86078739.html.

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Thesis (M.S.)--University of Wisconsin--Madison, 2006.<br>Typescript. eContent provider-neutral record in process. Description based on print version record. Includes bibliographical references (leaves 70-73).

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Soriano, Katherine Anne. "Stratigraphy and sedimentology of Cenomanian-Santonian carbonate platforms, Montsec Mountains, South-Central Pyrenees, Spain." 1992. http://catalog.hathitrust.org/api/volumes/oclc/25841996.html.

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Thesis (M.S.)--University of Wisconsin--Madison, 1992.<br>Two folded plates in pocket. Typescript. eContent provider-neutral record in process. Description based on print version record. Includes bibliographical references (leaves 112-116).

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Drzewiecki, Peter Anthony. "Mid-cretaceous carbonate platform evolution, south-central Pyrenees, Spain interactions among eustasy, tectonics, environmental factors, and biological factors /." 1996. http://catalog.hathitrust.org/api/volumes/oclc/35745921.html.

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Bens, Ashley Elizabeth. "Architecture of deposits formed in a tectonically generated tidal strait, upper Baronia Fm., Ager Basin, South Central Pyrenees, Spain." Thesis, 2011. http://hdl.handle.net/2152/ETD-UT-2011-05-3429.

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The upper Baronia Fm. of the Ager Basin, Spain, is composed of a hierarchy of prominently stacked sets of primarily unidirectional cross-strata in units up to 40m thick. These large sets of cross-strata are interpreted as deposits of migrating subaqueous tidal simple dunes, compound dunes, and compound dune complexes within an approximately 10km wide north-east to south-west oriented seaway with water depths of a calculated 60-90m. These interpretations are opposed to prior interpretations of the upper Baronia Fm. which suggests deposits were formed by tidal bars within a deltaic environment (Mutti et al., 1985). Dunes developed due to dominantly north-east directed tidal currents driven through the strait by tidal phase differences between the two bodies of water (Mediterranean and Atlantic basins) connected by the seaway. Evidence for syn-tectonic deposition further constrains timing of movement of the northern basin bounding Montsec thrust to the early Eocene. Indicators for movement on the Montsec thrust include the development of the Ager Basin elongate to the thrust front, and syn-tectonic signals in the fill of the basin such as local conglomerate wedges and emplacement of olistoliths. Individual cross-stratified successions are interpreted to have formed with variable flow velocity and orientation, resulting in a basin wide stacking of compound dune complexes. These compound dune complexes form cross stratified successions which are distributed throughout the basin according to the variable current speeds, dune size which impacts migration, and sediment availability during deposition. This results in the observed distributions of muddy and sandy sediments, where finer grained materials accumulate preferentially in the low energy troughs of the hierarchy of compound dunes.<br>text

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Freiberg, Philip George. "Facies description and interpretation of the Senyus Sequence, south-central Pyrenees the evolution of an Aptian carbonate platform along a rift basin margin /." 1994. http://catalog.hathitrust.org/api/volumes/oclc/32718626.html.

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Thesis (M.S.)--University of Wisconsin--Madison, 1994.<br>Typescript. Three folded leaves of illustrations in pocket. eContent provider-neutral record in process. Description based on print version record. Includes bibliographical references (leaves 132-136).

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Books on the topic "South Central Pyrenees"

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Speksnijder, Arie. Geological analysis of Paleozoic large-scale faulting in the south-central Pyrenees. Geologisch Instituut der Rijksuniversiteit, 1986.

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Speksnijder, Arie. Geological analysis of Paleozoic large-scale faulting in the south-central Pyrenees =: Geologische analyse van Paleozoische grootschalige breukbewegingen in de zuidelijke centrale Pyreneeën. Geologisch Instituut der Rijksuniversiteit te Utrecht], 1986.

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Gozalo, Margarita C. Cuevas. Sedimentary facies and sequential architecture of tide-influenced alluvial deposits: An example from the Middle Eocene Capella Formation, south-central Pyrenees, Spain. Institut voor Aardwetenschappen der Rijksuniversiteit te Utrecht, 1989.

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Book chapters on the topic "South Central Pyrenees"

1

Clark, J. D. "Detailed section across the Ainsa II Channel complex, south central Pyrenees, Spain." In Atlas of Deep Water Environments. Springer Netherlands, 1995. http://dx.doi.org/10.1007/978-94-011-1234-5_21.

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Dominici, Stefano, and Thorsten Kowalke. "Early Eocene Cerithioidean Gastropods from a Subtropical Coast Environment (South–Central Pyrenees, Spain)." In Springer Geology. Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-04364-7_17.

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Schuppers, J. D. "Quantification of Turbidite Facies in a Reservoir-Analogous Submarine-Fan Channel Sandbody, South-Central Pyrenees, Spain." In The Geological Modelling of Hydrocarbon Reservoirs and Outcrop Analogues. Blackwell Publishing Ltd., 2009. http://dx.doi.org/10.1002/9781444303957.ch5.

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Marfil, R., H. Mansurbeg, D. Garcia, et al. "Dolomite-Rich Condensed Sections in Overbank Deposits of Turbidite Channels: The Eocene Hecho Group, South-Central Pyrenees, Spain." In Linking Diagenesis to Sequence Stratigraphy. John Wiley & Sons, Inc., 2013. http://dx.doi.org/10.1002/9781118485347.ch9.

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Remacha, E., O. Oms, and J. Coello. "The Rapitán turbidite channel and its related eastern levee-overbank deposits, Eocene Hecho group, south-central Pyrenees, Spain." In Atlas of Deep Water Environments. Springer Netherlands, 1995. http://dx.doi.org/10.1007/978-94-011-1234-5_22.

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Millington, J., and J. D. Clark. "Submarine canyon and associated base-of-slope sheet system: the Eocene Charo-Arro system, south-central Pyrenees, Spain." In Atlas of Deep Water Environments. Springer Netherlands, 1995. http://dx.doi.org/10.1007/978-94-011-1234-5_23.

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Mellere, D. "Thrust-Generated, Back-Fill Stacking of Alluvial Fan Sequences, South-Central Pyrenees, Spain (La Pobla De Segur Conglomerates)." In Tectonic Controls and Signatures in Sedimentary Successions. Blackwell Publishing Ltd., 2009. http://dx.doi.org/10.1002/9781444304053.ch14.

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Gallemi, J. "Upper Cretaceous echinoids from south central Pyrenees*." In Echinoderms through Time. CRC Press, 2020. http://dx.doi.org/10.1201/9781003077831-156.

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Simo, J. A. Toni. "Cretaceous Carbonate Platforms and Stratigraphic Sequences, South-Central Pyrenees, Spain." In Cretaceous Carbonate Platforms. American Association of Petroleum Geologists, 1993. http://dx.doi.org/10.1306/m56578c26.

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Pickering, Kevin T., and Jordi Corregidor. "3D Reservoir-Scale Study of Eocene Confined Submarine Fans, South-Central Spanish Pyrenees." In Deep-Water Reservoirs of the World: 20th Annual. SOCIETY OF ECONOMIC PALEONTOLOGISTS AND MINERALOGISTS, 2000. http://dx.doi.org/10.5724/gcs.00.15.0776.

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Conference papers on the topic "South Central Pyrenees"

1

Drzewiecki, Peter, David W. Hunt, Wayne R. Wright, et al. "TECTONIC, SEA-LEVEL, AND PALEOECOLOGICAL CONTROLS ON CARBONATE FACIES DISTRIBUTION, SANTONIAN SANT CORNELI FORMATION, SOUTH-CENTRAL PYRENEES, SPAIN." In 53rd Annual GSA Northeastern Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018ne-310946.

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2

Fitzgerald, Paul G., Thomas S. Warfel, Marco G. Malusa, et al. "COBBLE THERMOCHRONOLOGY AND ITS APPLICATION TO CONSTRAINING HINTERLAND EXHUMATION: LESSONS LEARNT FROM THE PYRENEES AND SOUTH-CENTRAL ALASKA." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-322617.

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3

Llaguno, Jose, and Florentin J.-M. R. Maurrasse. "PETROGRAPHIC AND GEOCHEMICAL CHARACTERIZATION OF THE UPPERMOST BARREMIAN - LOWEST APTIAN OF THE EASTERN PRADA QUARRY SECTION OF THE RESTRICTED ORGANYÀ BASIN, SOUTH-CENTRAL PYRENEES." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-285934.

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4

Thomson, Kelly, Daniel F. Stockli, Margaret Odlum, Julian Clark, Cai Puigdefabregas, and Andrea Fildani. "EXPLORING THE EFFECTS OF SEDIMENT MIXING AND HYDRAULIC SORTING ON DETRITAL ZIRCON SIGNAL PROPAGATION: EXAMPLES FROM THE EOCENE CASTISSENT FORMATION, SOUTH CENTRAL PYRENEES, SPAIN." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-324934.

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Thomson, Kelly, Margaret Odlum, Daniel F. Stockli, Andrea Fildani, Julian Clark, and Cai Puigdefabregas. "TRACING ENVIRONMENTAL SIGNALS FROM SOURCE TO SINK: ZIRCON (U-TH)/(HE-PB) DOUBLE DATING APPLIED TO FORELAND BASIN FILL OF THE SOUTH CENTRAL PYRENEES, SPAIN." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-287126.

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Socorro, Jander, and Florentin J.-M. R. Maurrasse. "GEOCHEMICAL AND LITHOLOGICAL CHARACTERISTICS OF CHANGING PALEOENVIRONMENTAL CONDITIONS ASSOCIATED WITH THE END OF CARBON ISOTOPE SEGMENT C5 OF OAE 1A IN THE SOUTH-CENTRAL SPANISH PYRENEES." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-340572.

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