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Relevant bibliographies by topics / Karstic infilling

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Academic literature on the topic 'Karstic infilling'

Author: Grafiati

Published: 7 June 2025

Last updated: 2 August 2025

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Journal articles on the topic "Karstic infilling"

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Fagoaga, Ana, Francisco Javier Molina, Vicente D. Crespo, César Laplana, Rafael Marquina, and Francisco J. Ruíz-Sánchez. "Geological context and micromammal fauna characterisation from the karstic infilling of La Pedrera (Albaida, Valencia, E Spain)." Spanish Journal of Palaeontology 32, no. 2 (2020): 241. http://dx.doi.org/10.7203/sjp.32.2.17042.

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Conrad, Georges, and Gérard Onoratini. "Le remplissage karstique de la grotte de l'Adaouste et sa genèse (Jouques, B.D.R) [The karstic infilling of Adaouste cave.]." Quaternaire 8, no. 2 (1997): 159–74. http://dx.doi.org/10.3406/quate.1997.1570.

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Sebe, Krisztina, Mihály Gasparik, Zoltán Szentesi, Gergely Surányi, Ágnes Novothny, and Luca Pandolfi. "New Pleistocene vertebrate assemblages from the Villány Hills (SW Hungary): Siklós and Palkonya." Fragmenta Palaeontologica Hungarica 38 (2023): 75–94. http://dx.doi.org/10.17111/fragmpalhung.2023.38.75.

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The Villány Hills in SW Hungary have the richest archive of Pliocene–Quaternary vertebrate faunas in the Pannonian Basin, mostly in karstic cavities. Here we present three new sites that extend the list of Pleistocene vertebrate locations for the area and add information to the evolution history of the region. In the northern part of the Siklós quarry, bone breccia was found coming from fissures in Jurassic or Cretaceous limestones. Its lithofacies and fossil content are similar to those of other well-known Plio-Pleistocene karst infills of the region. As it contained mostly snake vertebrae, i

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Camus, Hubert. "Caractérisation morphokarstique de l'Igue du Gral." Revue de Paléobiologie 43, no. 2 (2024): 107–49. https://doi.org/10.5281/zenodo.13860476.

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The Igue du Gral, as a largely vertical cavity, has functioned as a natural trap during several periods, and the distribution of the filling is linked to the opening and to the closing of entrance vents over time. The prolonged periods when it was closed allowed the good conservation of paleontological material, while the episodic karst functioning of the cavity was determined by the morpho-dynamic and climatic factors, both on the surface of the plateau and underground. The alternation of overture and closure controls the conditions of deposition, alteration, or degradation, particularly when

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Hodnett, John-Paul M., and David K. Elliott. "Carboniferous chondrichthyan assemblages from the Surprise Canyon and Watahomigi formations (latest Mississippian–Early Pennsylvanian) of the western Grand Canyon, Northern Arizona." Journal of Paleontology 92, S77 (2018): 1–33. http://dx.doi.org/10.1017/jpa.2018.72.

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AbstractTwo chondrichthyan assemblages of Late Mississippian/Early Pennsylvanian age are now recognized from the western Grand Canyon of northern Arizona. The latest Serpukhovian Surprise Canyon Formation has yielded thirty-one taxa from teeth and dermal elements, which include members of the Phoebodontiformes, Symmoriiformes, Bransonelliformes, Ctenacanthiformes, Protacrodontoidea, Hybodontiformes, Neoselachii (Anachronistidae), Paraselachii (Gregoriidae, Deeberiidae, Orodontiformes, and Eugeneodontiformes), Petalodontiformes, and Holocephali. The euselachian grade taxa are remarkably diverse

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Baqués, Vinyet, Estibalitz Ukar, Stephen E. Laubach, Stephanie R. Forstner, and András Fall. "Fracture, Dissolution, and Cementation Events in Ordovician Carbonate Reservoirs, Tarim Basin, NW China." Geofluids 2020 (April 18, 2020): 1–28. http://dx.doi.org/10.1155/2020/9037429.

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Ordovician carbonate rocks of the Yijianfang Formation in the Tabei Uplift, Tarim Basin, contain deeply buried (>6000 m), highly productive oil and gas reservoirs associated with large cavities (>10 m). Previous workers inferred that large cavities are paleocaves (paleokarst) formed near the surface and subsequently buried. Alternately, caves may have formed by dissolution at depth along faults. Using 227 samples from 16 cores, we document textures and cement compositions bearing on cavity histories with petrographic, high-resolution scanning electron microscopy (SEM), isotopic, and flui

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Mocochain, Ludovic, Philippe Audra, and Jean-Yves Bigot. "Base level rise and per ascensum model of speleogenesis (PAMS). Interpretation of deep phreatic karsts, vauclusian springs and chimney-shafts." Bulletin de la Société Géologique de France 182, no. 2 (2011): 87–93. http://dx.doi.org/10.2113/gssgfbull.182.2.87.

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Abstract In Mediterranean karsts, the Messinian salinity crisis induced first a deepening of the karst systems, then a flooding after the Pliocene transgression, and finally a reorganization of the drains after this base level rise. This reorganization mainly corresponds to the development of phreatic lifts: the chimney-shafts and the vauclusian springs. Such a per ascensum speleogenesis appears with a base level rise, which is caused by eustatism, by fluvial aggradation or valley infilling, or by continental subsidence. Consequently, we explain the origin of most of the deep phreatic cave sys

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Veress, Márton. "Postglacial evolution of paleodepressions in glaciokarst areas of the Alps and Dinarides." Zeitschrift für Geomorphologie 60, no. 4 (2016): 343–58. http://dx.doi.org/10.1127/zfg/2016/0331.

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The karstification of the paleodolines of glaciokarst is studied. Our methods included topographical mapping, geomorphological mapping and analysis, vertical electrical sounding (VES) measurements, areal imaging, investigation of the material of the superficial deposit. On glaciokarst, the paleodolines without cover are the bare karst patches, while paleodolines with cover belong to allogenic karst (if the cover is impermeable) or covered karst (if the cover is permeable). The covered karst also occur in patches, their pattern depends on the distribution of paleodolines, the size of glacier va

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Dobrowolski, Radosław, Marta Ziółek, Krystyna Bałaga, Jerzy Melke, and Andrij Bogucki. "Radiocarbon Age and Geochemistry of the Infillings of Small Closed Depressions from Western Polesie (Poland Se, Ukraine Nw)." Geochronometria 36, no. -1 (2010): 39–46. http://dx.doi.org/10.2478/v10003-010-0010-8.

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Radiocarbon Age and Geochemistry of the Infillings of Small Closed Depressions from Western Polesie (Poland Se, Ukraine Nw)In this paper we report the results of interdisciplinary investigations of deposits filling small closed depressions in the Western Polesie region. There were reconstructed the environmental changes and the main evolution phases of four morphometrically similar forms (=research sites) situated in the Lublin and Volhynia parts of the Polesie region. The gathered sedimentological, chronostratigraphical, palynological and geochemical data evidence great lithological (peats, g

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Jabrane, Oussama, Pedro Martínez-Pagán, Marcos A. Martínez-Segura, et al. "Integration of Electrical Resistivity Tomography and Seismic Refraction Tomography to Investigate Subsiding Sinkholes in Karst Areas." Water 15, no. 12 (2023): 2192. http://dx.doi.org/10.3390/w15122192.

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Operational and safety issues associated with subsiding sinkholes in karst areas start with the definition of fractures and joints, causing ground weakness. Conventional geotechnical boreholes and geological mapping must be complemented with indirect subsurface exploration techniques to detail those structures. This work aims to use electrical resistivity tomography (ERT) and seismic refraction tomography (SRT) near-surface geophysical techniques to infer the 2D and 3D geometry of sediment-infilled sinkholes formed by the conjunction of fractures and joints in karst areas. Geophysical surveys

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Book chapters on the topic "Karstic infilling"

1

Mhanna, R., A. Naveau, F. Battaglia, et al. "Leaching behavior of arsenic from Upper Cretaceous karst infillings materials in a fractured limestone aquifer (HESP, France)." In Arsenic in the Environment: Bridging Science to Practice for Sustainable Development As2021. CRC Press, 2024. http://dx.doi.org/10.1201/9781003317395-65.

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