Letteratura scientifica selezionata sul tema "Datation par les traces de fission"
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Articoli di riviste sul tema "Datation par les traces de fission":
Jonckheere, Raymond, Michel Mars, Peter Van den haute, Michel Rebetez e Alain Chambaudet. "L'apatite de Durango (Mexique): Analyse d'un minéral standard pour la datation par traces de fission". Chemical Geology 103, n. 1-4 (gennaio 1993): 141–54. http://dx.doi.org/10.1016/0009-2541(93)90297-v.
Dorighel, Olivier, Gérard Poupeau, Jean-François Bouchard e Erika Labrin. "Datation par traces de fission et étude de provenance d'artefacts en obsidienne des sites archéologiques de la Tolita (Equateur) et Inguapi (Colombie)". Bulletin de la Société préhistorique française 91, n. 2 (1994): 133–44. http://dx.doi.org/10.3406/bspf.1994.9726.
Doperé, Frans. "Introduction à la datation des maçonneries de l’Hôtel de Ville par l’étude des techniques de taille des pierres". Studia Bruxellae N° 12, n. 1 (2 ottobre 2018): 37–42. http://dx.doi.org/10.3917/stud.012.0037.
Imrani, Abdelhakim El, Hassan Zine El Abidine, Gérard Poupeau, Mohammed Limouri e Abderahmane Essaîd. "Modélisation inverse des histoires thermiques par traces de fission dans l'apatite". Comptes Rendus de l'Académie des Sciences - Series IIA - Earth and Planetary Science 327, n. 3 (agosto 1998): 161–66. http://dx.doi.org/10.1016/s1251-8050(98)80003-7.
Weitz, Armelle, Christophe Maggi, Sarah Crémer, Pascale Fraiture e Patrick Hoffsummer. "Les charpentes de l’Hôtel de Ville de Bruxelles : témoin caché du xviii e siècle". Studia Bruxellae N° 12, n. 1 (2 ottobre 2018): 76–79. http://dx.doi.org/10.3917/stud.012.0076.
Storzer, D., e M. Selo. "Chrono-thermométrie par traces de fission : une perspective nouvelle pour la prospection pétrolière". Revue de l'Institut Français du Pétrole 40, n. 3 (maggio 1985): 301–21. http://dx.doi.org/10.2516/ogst:1985020.
Jakni, Bouchra, Gérard Poupeau, Marc Sosson, Philippe Rossi, Jean Ferrandini e Pol Guennoc. "Dénudations cénozoïques en Corse : une analyse thermochronologique par traces de fission sur apatites". Comptes Rendus de l'Académie des Sciences - Series IIA - Earth and Planetary Science 331, n. 12 (dicembre 2000): 775–82. http://dx.doi.org/10.1016/s1251-8050(00)01494-4.
Rousse, Corinne, Souen Fontaine, Corinne Landure, Frédéric Marty, Yoan Quesnel, Claude Vella, Philippe Dussouliez, Jules Fleury e Minoru Uheara. "Le canal de Marius : réflexions autour d’une nouvelle hypothèse de tracé dans le secteur des Marais du Vigueirat". Revue archéologique de Narbonnaise 52, n. 1 (2019): 109–20. http://dx.doi.org/10.3406/ran.2019.1980.
Canak-Medic, Milka. "Polychromie et représentations apotropaïques sur la façade de l'église du Saint-sauveur a Zica". Zbornik radova Vizantoloskog instituta, n. 43 (2006): 561–78. http://dx.doi.org/10.2298/zrvi0643561c.
Carpéna, Joëlle, Isabelle Gagnol, Didier Mailhé e Jean-Pierre Pupin. "L'uranium marqueur de la croissance cristalline : mise en évidence par les traces de fission dans les zircons gemmes d'Espaly (Haute-Loire, France)". Bulletin de Minéralogie 110, n. 4 (1987): 459–63. http://dx.doi.org/10.3406/bulmi.1987.8041.
Tesi sul tema "Datation par les traces de fission":
Sabil, Naïma. "La datation par les traces de fission : aspects méthodologiques et applications thermochronologiques en contexte alpin et marge continentale". Phd thesis, Grenoble 1, 1995. http://www.theses.fr/1995GRE10066.
Sabil, Naïma. "La datation par les traces de fission : aspects méthodologiques et applications thermochronologiques en contexte alpin et marge continentale". Phd thesis, Université Joseph Fourier (Grenoble), 1995. http://tel.archives-ouvertes.fr/tel-00534619.
Genge, Marie. "Tectonic evolution of the north-central Patagonia : a thermochronological approach". Electronic Thesis or Diss., Université de Lille (2018-2021), 2021. http://www.theses.fr/2021LILUR013.
The change in plate kinematics, which may have affected slab dip, can deeply influence the interplate coupling and consequently the deformation of the overriding plate. The north-central Patagonia represents a unique region to study the impact of slab-dip changes as this area is characterized by alternating episodes of steep to flat-slab since the onset of subduction below the South American Plate. The alternation of the upper plate subsidence and exhumation events related with slab steepening and shallowing episodes, respectively, or with changes in kinematics has been widely studied in the recent years along the Andes. However, some topics remain highly debated, and especially the magnitude of the vertical movements through time and space. Low-temperature thermochronology systems, which are sensitive to events involving the upper first kilometers of the upper crust, represent an efficient approach for dating and quantifying significant episodes of burial and exhumation. This thesis investigates the thermal history of the north-central Patagonian broken foreland and the Cordillera. The latter area has been widely studied through bedrock thermochronology studies compared with data from the Patagonian foreland, where only few data are available. Thus, this work aims at improving our knowledge on the relationships between the surface cooling record and the geodynamic evolution.Three apatites thermochronometers (U-Pb, fission tracks and (U-Th-Sm)/He) were used on bedrocks, Mesozoic and Cenozoic sandstones as well as on modern sediments. All samples were collected from the inner part of the north-central Patagonian Cordillera to the distal part of the broken foreland along the Atlantic coast. Compilation of these diverse thermochronology datasets, integrated by inverse thermal modeling and provenance analysis, is discussed here and compared with the different geodynamic processes proposed for Patagonia (e.g. convergence changes, slab dip variations). The new thermochronology records indicate that main unroofing of Patagonia (~3 – 4 km), Cordillera and broken foreland included, occurred during a slab-shallowing episode from late Early Cretaceous to early Paleogene, after a Jurassic – Early Cretaceous heating episode related to a significant burial below a thick sedimentary cover. This regional exhumation phase was followed by a period between the late Eocene and the early Miocene of foreland subsidence associated with slab rollback, characterized by a steady-state post-shortening low exhumation rates. During this period of relative quiescence, detrital analysis point to the Cordillera as a primary contributor of sediments for the entire foreland with a local input from the broken foreland reliefs. Finally, Miocene substantial exhumation is recognized into the Cordillera after a change of convergence rates and obliquity, especially along a dextral strike-slip fault zone active along the Cordillera. However, this exhumation phase is not detected regionally in the broken foreland. Since no regional sedimentary burial or relevant exhumation events affected the north-central Patagonian foreland, the few Oligo-Miocene ages identified along the foreland have been ascribed to the coeval intraplate magmatic processes
Toro, Villegas Gloria Elena. "Tephrochronologie de la Colombie centrale (département d'Antioquia et abanico de Pereira) : une approche stratigraphique, géochimique, minéralogique et géochronologique (par C14 et traces de fission)". Université Joseph Fourier (Grenoble), 1999. http://www.theses.fr/1999GRE10036.
Akkouche, Madjid. "Application de la datation par traces de fission à l'analyse de la thermicité de bassins à potentialités pétrolières : exemple de la cuvette de Sbaâ et du bassin de l'Ahnet-Nord (plate-forme saharienne occidentale, Algérie)". Bordeaux 1, 2007. http://www.theses.fr/2007BOR13367.
Jakni, Bouchra. "Thermochronologie par traces de fission des marges conjuguées du bassin liguro-provençal : la Corse et le massif des Maures-Tanneron". Phd thesis, Grenoble 1, 2000. http://www.theses.fr/2000GRE10008.
Lelarge, Maria Lidia Meideros Vignol. "Thermochronologie par la méthode des traces de fission d'une marge passive (dôme de Ponta Grossa, se Brésil) et au sein d'une chaîne de collision (zone externe de l'arc alpin, France)". Université Joseph Fourier (Grenoble), 1993. https://tel.archives-ouvertes.fr/tel-00603209.
Mars, Michel. "Analyse thermique et géochronologie par traces de fission de l'uranium dans les minéraux : simulation et applications". Besançon, 1989. http://www.theses.fr/1989BESA2035.
Bermudez, Cella Mauricio Alberto. "Exhumation cénozoïque dans les Andes vénézuéliennes : apport de la thermochronologie par traces de fission". Phd thesis, Grenoble 1, 2009. http://www.theses.fr/2009GRE10224.
This dissertation presents the results and observations of an investigation on the long-term (Miocene to present) exhumation history of the Venezuelan Andes, and the relationships between inherited structures and development of topography in response to tectonic and surface processes. The Venezuelan Andes are ideal for understanding the relationships between these processes, because they have involved through inversion and reactivation of pre-existing structures, they are associated with a major climatic gradient due to the orograpic effect of the belt and extensive data is available concerning their recent tectonic evolution. This mountain belt is the result of transpression caused by oblique convergence of the continental Maracaibo block and the South America Plate, controlled, on a larger scale, by the triple junction between the South American, Caribbean and Nazca plates. The complex kinematics of triple plate interaction and the continuous evolution of related structures coupled with surface processes have profoundly affected the evolution of the Venezuelan Andes
Bermudez, Cella Mauricio Alberto. "Exhumation Cénozoïque dans les Andes Vénézuéliennes: apport de la thermochronologie par traces de fission". Phd thesis, Université Joseph Fourier (Grenoble), 2009. http://tel.archives-ouvertes.fr/tel-00450838.
Libri sul tema "Datation par les traces de fission":
Galbraith, Rex F. Statistics for Fission Track Analysis (Interdisciplinary Statistics). Chapman & Hall/CRC, 2005.