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Autor López Gómez, José |
Documentos disponibles escritos por este autor (63)
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López Gómez, José ; Galán Abellán, Ana Belén ; Horra del Barco, Raúl de la ; Fernández Barrenechea, José María ; Arche, Alfredo ; Bourquin, Sylvie ; Marzo Carpio, Mariano ; Durand, Marc | Elsevier | 2012The Permian–Triassic transition (P–T) was marked by important geochemical perturbations and the largest known life crisis. Consequences of this event, as oxygen-depleted conditions and the unusual behavior of the carbon cycle, were prolonged dur[...]texto impreso
Kietzmann, Diego A. ; Palma, Ricardo Manuel ; Riccardi, A.C. ; Martín Chivelet, Javier ; López Gómez, José | Elsevier | 2014The Vaca Muerta Formation (early Tithonian–early Valanginian) is a rhythmic succession of marls and limestones, cropping out in the Neuquén Basin, west-central Argentina. This lithostratigraphic unit was traditionally interpreted as basinal to s[...]texto impreso
Barrenechea, José F. ; López Gómez, José ; Horra del Barco, Raúl de la | Geological Society | 2018-05-17This study examines rainfall variations of the Mid-Carnian Pluvial Episode (CPE) based on the continental fluvial sedimentology, palaeosol and clay mineralogy records of the Stable Meseta (E Spain). In the formation examined, Manuel Fm or K2 Fm,[...]texto impreso
Benito Moreno, María Isabel ; Horra del Barco, Raúl de la ; López Gómez, José ; Fernández Barrenechea, José María ; Luque del Villar, Francisco Javier ; Arche, Alfredo | Elsevier | 2011This work is focused on carbonate paleosols developed in three stratigraphic sections (Landete, Talayuelas and Henarejos) of theMiddle–Late Permian Alcotas Formation in the SE Iberian Basin. The Alcotas Formation, of alluvial origin, was deposit[...]texto impreso
Galán Abellán, Ana Belén ; Alonso Azcárate, Jacinto ; Newton, Robert J. ; Bottrell, Simon H. ; Fernández Barrenechea, José María ; Benito Moreno, María Isabel ; Horra del Barco, Raúl de la ; López Gómez, José ; Luque del Villar, Francisco Javier | SEPM (Society for Sedimentary Geology) | 2013Aluminum-phosphate–sulfate (APS) minerals, formed during early diagenesis in relation to acid meteoric waters, are the main host of Sr and S in the Early–Middle Triassic continental sandstones of the Iberian Ranges (east of the Iberian Peninsula[...]texto impreso
The Permian–Triassic transition, a time of phenomenal palaeoenvironmental and palaeogeographical change, represents the largest episode of mass extinctions known to palaeontologists. This episode is, however, very poorly understood, and a lack o[...]texto impreso
The sedimentary record of the Late Permian and Early Triassic of the eastern Iberian Ranges shows four major, sudden, or very rapid, vertical changes in fluvial style. The Late Permian sedimentary cycle starts with the Boniches Formation, of all[...]texto impreso
Lloret, Joan ; Ronchi, Ausonio ; López Gómez, José ; Gretter, Nicola ; Horra, Raúl de la ; Barrenechea, José F. ; Arche, Alfredo | Elsevier | 2018-10-15The break-up of Pangea remains one of the most interesting moments in the Earth's history. In the Pyrenees this geological moment is represented by continental successions, giving rise to a magnificent example of the creation of new basins and t[...]texto impreso
The Eslida Fm is an alluvial unit of the Buntsandstein Facies of the Iberian Ranges deposited in a half-graben basin over a period of 2–2.5 Ma during the lower Anisian (Middle Triassic). It can be subdivided into six cycles that can be correlate[...]texto impreso
Wees, Jan Dierik van ; Arche, Alfredo ; Beijdorff, C.G. ; López Gómez, José ; Cloetingh, Sierd A.P.L. | Elsevier Science B.V | 1998By subsidence analysis on eighteen surface sections and 6 wells, which cover large part of the Iberian Basin (E Spain) and which are marked by high-resolution stratigraphy of the Permian, Triassic, Jurassic and Cretaceous, we quantify the comple[...]texto impreso
Gretter, N. ; Ronchi, A. ; López Gómez, José ; Arche, Alfredo ; Horra, R. De la ; Barrenechea, José F. ; Lago San José, Marceliano | Elsevier | 2015-11The Eastern Catalan Pyrenees form the southernmost segment of the Pyrenean Axial Zone. They experienced complex multistage process as the result of both the Variscan and the Pyrenean orogenic cycles. After the Late Palaeozoic, several small exte[...]texto impreso
The tiny outcrop of the mining area of Minas de Henarejos is unique among the early post-Variscan basins of the Iberian Ranges, Central Spain, for several reasons: Its age, considered up now to be Late Carboniferous (Stephanian B-C), its syn-sed[...]texto impreso
Bourquin, Sylvie ; Bercovici, Antoine ; López Gómez, José ; Diez Ferrer, José B. ; Broutin, Jean ; Ronchi, Ausonio ; Durand, Marc ; Arche, Alfredo ; Linol, Bastien ; Amour, Frédéric | Elsevier | 2011The main aim of this paper is to review Middle Permian through Middle Triassic continental successions in European. Secondly, areas of Middle–Late Permian sedimentation, the Permian–Triassic Boundary (PTB) and the onset of Triassic sedimentation[...]texto impreso
Arche, Alfredo ; López Gómez, José ; Marzo Carpio, Mariano ; Vargas, Henar | Instituto de Ciencias de la Tierra "Jaume Almera" (Barcelona) | 2004The siliciclastic deposits of the Iberian, Ebro and Catalan Basins have been described for more than a century, but facies similarities and a lack of biostratigaphic data have difficulted the correlation of the local stratigraphic units in a gen[...]texto impreso
The Boniches Conglomerates Fm. (Upper Permian) represents the first episode of sedimentation in the southeast border margin of the Iberian Basin, central Spain. The Iberian Basin commenced development as a rift basin running mainly NW-SE during [...]