Orogenic Processes in the Alpine Collision Zone

Total Page:16

File Type:pdf, Size:1020Kb

Orogenic Processes in the Alpine Collision Zone Orogenic Processes in the Alpine Collision Zone Guest Editors: Nikolaus Froitzheim Stefan M. Schmid Vol. 101 Swiss Journal of Geosciences Supplement 1 formerly Eclogae Geologicae Helvetiae 2008 Pages S1–S 310 ISSN 1661-8726 Journal of the Swiss Geological Society Swiss Society of Mineralogy and Petrology Swiss Palaeontological Society and affiliated organisations and specialist groups: Platform Geosciences of the Swiss Academy of Sciences Swiss Geological Survey Swiss Tectonic Studies Group SwissSed Swiss Group of Geophysicists Contents FROITZHEIM, N., SCHMID, S. M.: HERWARTZ, D., MÜNKER, C., SCHERER, E. E., NAGEL, T. J., Orogenic processes in the Alpine collision zone, Preface ....... S1 PLEUGER, J., FROITZHEIM, N.: Lu-Hf garnet geochronology of eclogites from the Balma ROURE, F.: Unit (Pennine Alps): implications for Alpine paleotectonic Foreland and Hinterland basins: what controls their evolution? S5 reconstructions .......................................... S173 MIKES, T., CHRIST, D., PETRI, R., DUNKL, I., FREI, D., KURZ, W., HANDLER, R., BERTOLDI, C.: BÁLDI-BEKE, M., REITNER, J., WEMMER, K., HRVATOVIĆ, H., Tracing the exhumation of the Eclogite Zone (Tauern Window, VON EYNATTEN, H.: Eastern Alps) by 40Ar/39Ar dating of white mica in eclogites .... S191 Provenance of the Bosnian Flysch .......................... S31 LUTH, S. W., WILLINGSHOFER, E.: ORTNER, H., USTASZEWSKI, M., RITTNER, M.: Mapping of the post-collisional cooling history of the Eastern Late Jurassic tectonics and sedimentation: breccias in the Unken Alps ................................................... S207 syncline, central Northern Calcareous Alps .................. S55 DANIŠÍK, M., KOHÚT, M., DUNKL, I., HRAŠKO, L., FRISCH, W.: VESELÁ, P., LAMMERER, B.: Apatite fission track and (U-Th)/He thermochronology of the The Pfitsch-Mörchner Basin, an example of the post-Variscan Rochovce granite (Slovakia) – implications for the thermal sedimentary evolution in the Tauern Window (Eastern Alps) . S73 evolution of the Western Carpathian-Pannonian region........ S225 DUMONT, T., CHAMPAGNAC, J.-D., CROUZET, C., ROCHAT, P.: PISCHINGER, G., KURZ, W., ÜBLEIS, M., EGGER, M., FRITZ, H., Multistage shortening in the Dauphiné zone (French Alps): BROSCH, F. J., STINGL, K.: the record of Alpine collision and implications for pre-Alpine Fault slip analysis in the Koralm Massif (Eastern Alps) and con- restoration.............................................. S89 sequences for the final uplift of “cold spots” in Miocene times . S235 THÖNY, W. F., T ROPPER, P., SCHENNACH, F., KRENN, E., FODOR, L. I., GERDES, A., DUNKL, I., KOROKNAI, I., FINGER, F., KAINDL, R., BERNHARD, F., HOINKES, G.: The metamorphic evolution of migmatites from the Ötztal PÉCSKAY, Z., TRAJANOVA, M., HORVÁTH, P., VRABEC, M., Complex (Tyrol, Austria) and constraints on the timing of the JELEN, B., BALOGH, K., FRISCH, W.: pre-Variscan high-T event in the Eastern Alps ............... S111 Miocene emplacement and rapid cooling of the Pohorje pluton at the Alpine-Pannonian-Dinaridic junction, Slovenia ......... S255 WIEDERKEHR, M., BOUSQUET, R., SCHMID, S. M., BERGER, A.: From subduction to collision: thermal overprint of HP/LT meta- USTASZEWSKI, K., SCHMID, S. M., FÜGENSCHUH, B., sediments in the north-eastern Lepontine Dome (Swiss Alps) TISCHLER, M., KISSLING, E., SPAKMAN, W.: and consequences regarding the tectono-metamorphic evolution A map-view restoration of the Alpine-Carpathian-Dinaridic of the Alpine orogenic wedge.............................. S127 system for the Early Miocene.............................. S273 RÜTTI, R., MARQUER, D., THOMPSON, A. B.: TUECKMANTEL, C., SCHMIDT, S., NEISEN, M., GEORGIEV, N., Tertiary tectono-metamorphic evolution of the European NAGEL, T. J., FROITZHEIM, N.: margin during Alpine collison: example of the Leventina Nappe The Rila-Pastra Normal Fault and multi-stage extensional un- (Central Alps, Switzerland)................................ S157 roofing in the Rila Mountains (SW Bulgaria) ................ S295 1661-8726/08/01S001-3 Swiss J. Geosci. 101 (2008) Supplement 1, S1–S3 DOI 10.1007/s00015-008-1296-7 Birkhäuser Verlag, Basel, 2008 Orogenic processes in the Alpine collision zone Preface to the Special Issue of the Swiss Journal of Geosciences devoted to “Orogenic processes in the Alpine collision zone” NIKOLAUS FROITZHEIM1 & STEFAN M. SCHMID2 INVITED EDITORS The papers in this issue further elaborate themes that were pre- What controls their evolution?, (7) From Neogene to present- sented at the 8th Workshop on Alpine Geological Studies held day Alps: Neotectonics, brittle tectonics, big tunnels, and finally, in Davos on 10–12 October 2007. Ever since a first meeting in (8) Coupling of climate, uplift, erosion, and topography. Grenoble that took place in 1993, a series of successor Work- Keynote lectures opening the sessions were given by shops on Alpine Geological Studies has continued in a two-year Thorsten Nagel (Bonn), Edi Kissling (Zürich), Onno Oncken rhythm: 1995 Basel, 1997 Biella – Oropa, 1999 Tübingen, 2001 (Potsdam), Alfons Berger (Bern), Liviu Matenco (Amster- Obergurgl, 2003 Sopron, 2005 Opatija. Gradually, the study area dam), Francois Roure (Paris), and Sean Willett (Zürich). Ben encompassed by these meetings was enlarged beyond the Alps Reinhardt (Dornach) offered an introduction to the geologic in the strict sense. More and more contributions touched on results of and problems encountered along the construction of other parts of the Alpine Collision Zone such as the Carpath- the Lötschberg and Gotthard base tunnels in a public lecture ians, Dinarides or Apennines. Thereby an increasing multitude entitled “Lange Tunnels durch die Alpen: NEAT aus der Sicht of various processes leading to collisional mountain building in des Geologen”. general could be discussed. Consequently, this present volume The presentations and discussions during the workshop re- captures a part of that same diversity. The 8th workshop in 2007 flected the recent development of Alpine geology. An increas- took place with 117 participants from 14 countries. ing part of Alpine geological research deals with the Neogene Two excursions to the high Alpine area around Davos were to recent evolution of the earth’s surface and with the interplay carried out before and after the workshop, favoured by clear, of climate and tectonics. For this field of research, the Alps are warm autumn weather prevailing during the entire conference. ideally suited as a natural laboratory because of their limited The pre-workshop field trip on October 9, guided by Daniel size, well-constrained boundary conditions, and high density of Bernoulli (Basel) and Othmar Müntener (Lausanne), was de- data. Several presentations dealt with the tectonic continua- voted to the ophiolites at Totalp, where lithologies and struc- tions of the Alps into the Carpathians and Dinarides and as far tures testify for the exhumation of subcontinental mantle rocks as the Balkan Peninsula. The intense, border-crossing research during the opening of the Piemont-Ligurian Ocean in Jurassic in these areas is proceeding towards a stage where a synoptic times. The second field trip of October 13 was a hike from St. picture of the tectonic evolution emerges. Important new find- Antönien near Klosters to the Tilisuna area, across the Alpine ings were also presented by several groups working on bio- and nappe stack at the Penninic-Austroalpine boundary. It was lithostratigraphy in basin sediments around the Alpine orogen. guided by Thorsten Nagel and Niko Froitzheim (Bonn). It was remarkable that this particular Alpine Workshop finally During the three lecture days, 50 oral and 68 poster contri- managed to bring together geologists working on the tectono- butions were presented, organized into the following topical metamorphic history of the Alps with those working on the sessions: (1) Alpine oceans: Rifting, break-up, spreading, and stratigraphy of adjacent foreland basins. paleogeography, (2) Deep structure, lithospheric strength, and This volume captures some highlights of the 2007 Davos mantle dynamics, (3) From subduction to collision, (4) Tectonic Workshop. 16 articles cover a multitude of Alpine-type work- and metamorphic processes and the role of HP/UHP metamor- ing areas and processes active in collisional mountain build- phic rocks, (5) Orogenic curvature and kinematics of the Alps- ing. We wish to acknowledge the financial contributions of Carpathians-Dinarides, (6) Foreland and hinterland basins: the Schweizerische Nationalfonds and the Swiss Academy of 1 Steinmann-Institut für Geologie Mineralogie und Paläontologie, Universität Bonn, Meckenheimer Allee 171, 53115 Bonn, Germany. E-mail: niko.froitzheimuni-bonn.de 2 Geologisch-Paläontologisches Institut, Universität Basel, Bernoullistr. 32, 4056 Basel, Switzerland. E-mail: [email protected] Preface S1 Sciences towards the organization of the 8th Workshop on Al- orogeny in the French external Alps (Dauphiné Zone). The pine Geological Studies in Davos and the publication of this authors show that Eocene or older deformation was followed series of articles. We are also grateful to the editors of the Swiss by N to NW-oriented basement thrusting so far only reported Journal of Geosciences who agreed to host this Special Issue, for more internal parts of the Western Alps. The classical main particularly Stefan Bucher who assisted the technical aspects WNW-directed compression represents a third event, indicat- of editing, and the three supporting Swiss Earth Science Soci-
Recommended publications
  • Tectonics and Sedimentation in Foreland Basins: Results from the Integrated Basin Studies Project
    Downloaded from http://sp.lyellcollection.org/ by guest on September 30, 2021 Tectonics and sedimentation in foreland basins: results from the Integrated Basin Studies project ALAIN MASCLE 1 & CAI PUIGDEFABREGAS 2,3 IIFP School, 228-232 avenue Napoldon Bonaparte, 92852 Rueil-Malmaison Cedex, France (e-mail: [email protected]) 2Norsk Hydro Research Centre, Bergen, Norway. 3Institut de Ciences de la Terra, (?SIC, Barcelona, Spain. Why foreland basins? to a better understanding of some basic interact- ing tectonic, sedimentary and hydrologic pro- Over the last ten years or so, since the Fribourg cesses (More & Vrolijk 1992; Touret & van meeting in 1985 (Homewood et al. 1986), the Hinte 1992). Additional data have also been attention given by sedimentologists and struc- obtained through the development of analogue tural geologists to the geology of foreland basins and numerical models (Larroque et al. 1992; has been growing continuously, parallel to the Zoetemeijer 1993). The physical parameters increase of co-operative links between scientists controlling the forward propagation of d6colle- from the two disciplines. A number of reasons ments and thrusts (fluid pressure, roughness, lie behind this development. Attempting to sediment thickness, etc.) have been determined understand the growth of an orogen without and tested. The relationships between rapidly paying due attention to the stratigraphic record subsiding piggyback basins and growing ramp of the derived sediments would be unrealistic. It anticlines have also been imaged, although the would, moreover, be equally unrealistic to con- lack of deep-sea well control still prevents accu- struct restored sections across the chain without rate sedimentological studies. More significant considering the constraints imposed by the has been the progress in our understanding of basin-fill architecture, or to describe the basin- the role of fluids and pore pressure in the fill evolution disregarding the development of development of thrust belts.
    [Show full text]
  • French Massif Armoricain
    The Léon Domain (French Massif Armoricain): a westward extension of the Mid-German Crystalline Rise? Structural and geochronological insights Michel Faure, Claire Sommers, Jérémie Melleton, Alain Cocherie, Olivier Lautout To cite this version: Michel Faure, Claire Sommers, Jérémie Melleton, Alain Cocherie, Olivier Lautout. The Léon Domain (French Massif Armoricain): a westward extension of the Mid-German Crystalline Rise? Structural and geochronological insights. International Journal of Earth Sciences, Springer Verlag, 2010, 99 (1), pp.65-81. 10.1007/s00531-008-0360-x. insu-00352053 HAL Id: insu-00352053 https://hal-insu.archives-ouvertes.fr/insu-00352053 Submitted on 12 Jan 2009 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. The Léon Domain (French Massif Armoricain): a westward extension of the Mid-German Crystalline Rise? Structural and geochronological insights Michel Faure1 , Claire Sommers1, Jérémie Melleton1, 2, Alain Cocherie2 and Olivier Lautout1 (1) ISTO Campus Géosciences, Orléans University, 1A Rue de la Férollerie, 45071 Orléans Cedex 2, France (2) BRGM, Av. Claude-Guillemin, 45060 Orléans Cedex 2, France Abstract The Léon Domain in the NW part of the French Massif Armoricain is a stack of synmetamorphic nappes displaced from south to north in ductile conditions.
    [Show full text]
  • Cessenon Sur Orb Assignan Babeau-Bouldoux Pierrerue Prades
    Assignan Cessenon sur Orb Pierrerue 7 Départ : Cave des vignerons Distance : 28 km - Dénivelé : + 930 m Départ : Parking Piboulade Départ : Parking Mairie 4 17 Un circuit sportif, demandant Distance : 28 km - Dénivelé : + 640 m Distance : 10 km - Dénivelé : + 270 m Le circuit 10 passe au une bonne condition physique cœur du village et les 3 et mais pas de grosse difficulté 15 sont tout proches. Un circuit bleu difficile qui aurait pu être rouge car la technique. montée se fait en deux temps avec deux passages un peu rudes (un peu de poussette ?) attention au retour une petite La montée est « rude » mais la partie de la descente est assez technique. récompense est au rdv avec Circuit difficile. Des montées courtes mais pentues une très belle descente coupée de passages un peu plus techniques et des vues à Babeau-Bouldoux et quelques passages techniquement difficiles, voire Mais l’ensemble constitue un remarquable circuit couper le souffle sur Saint-Chinian et la mer. dangereux pour des pratiquants non avertis. d’entraînement et de découverte de très beaux paysages. Départ : Parking babeau Ces passages sont reliés par de longues liaisons sans 16 Départ : Cave des vignerons Distance : 7 km - Dénivelé : + 90 m difficultés. Vous admirerez les rapides de Réals et sa base 22 de canoë ouverte à tous. Distance : 9 km - Dénivelé : + 230 m 8 Départ : Parking Mairie Circuit commun en partie avec le 9 bleu. Les deux circuits se Distance : 23 km - Dénivelé : + 530 m Pas de réelle difficulté technique mais un peu de pilotage séparent puis se retrouvent, se séparent à nouveau etc..
    [Show full text]
  • Dépliant PPN (Carto Rando)
    D152E5 St-Félix St-Jean D130 Commune de de-l'Héras D152 de-Buèges D151 D152E1 D33 Laval Roquecezière Lergue D9 Romiguières Belmont Camarès 02 Rocozels D142E2 D142E4 Pas de l’Escalette Commune de D142E2 D25 Pégairolles Masnau sur-Rance 2 Orb Grotte de Labeil Église St-Jacques Temple bouddhiste de-Buèges Massuguiès D902 D82 Fayet Pégairolles D9 Rance Église St-Jean-Baptiste l’Engayresque St-Pierre D130 la Claparède de-l'Escalette la Vacquerie St-Salvi 1 D152 Ceilhes-et-Rocozels 51 de-la-Fage et-St-Martin de-Carcavès D12 D902 A75 de-Castries St-Paul Plan d’eau D138 Roqueredonde Cirque du Bout du Monde de-Massuguiès St-Sever D149 du Bouloc D122 du-Moustier La Méridienne D4 Lac d’Avène D151 Panorama depuis le Caroux © G. Souche G. © Caroux le depuis Panorama Tauriac de-Camarès D89 D142 D151E4 D25 D607 Lauroux D138E2 D32 Brusque D8 D138 Soubès N D902 St-Étienne Secteur GRAND ORB Poujols de-Gourgas D89 52 les Moulières D149 les Salces Senaux D151 Avène Joncelets les Plans D9 D9E1D 3 D138E5 Église Orthodoxe D138 D149 St-Privat D163 Fozières D54 Vinas 5 Mont 4 D153 St-Michel de D153E1Mourcairol © CDRP34St-Baudille la Rouquette D4 Lacaze Joncels D142 Cathédrale (847m) Balisage des randonnéesViane Escroux Prieuré St-Michel St-Guilhem D81 le Coural St-Fulcran D144 Cloître le-Désert Les itinéraires de randonnée pédestre Arnac Chapelle Truscas de Grandmont Gijou sur-Dourdou D163 D153E Soumont sont jalonnés de marques conformes au St-André D35 Lodève D153E5 Usclas modèle en vigueur reproduit ci-dessous. de Rieussec D8 53 6 7 D153E4 Secteur grand orb
    [Show full text]
  • Mesozoic and Cenozoic Sequence Stratigraphy of European Basins
    Downloaded from http://pubs.geoscienceworld.org/books/book/chapter-pdf/3789969/9781565760936_frontmatter.pdf by guest on 26 September 2021 Downloaded from http://pubs.geoscienceworld.org/books/book/chapter-pdf/3789969/9781565760936_frontmatter.pdf by guest on 26 September 2021 MESOZOIC AND CENOZOIC SEQUENCE STRATIGRAPHY OF EUROPEAN BASINS PREFACE Concepts of seismic and sequence stratigraphy as outlined in To further stress the importance of well-calibrated chronos- publications since 1977 made a substantial impact on sedimen- tratigraphic frameworks for the stratigraphic positioning of geo- tary geology. The notion that changes in relative sea level shape logic events such as depositional sequence boundaries in a va- sediment in predictable packages across the planet was intui- riety of depositional settings in a large number of basins, the tively attractive to many sedimentologists and stratigraphers. project sponsored a biostratigraphic calibration effort directed The initial stratigraphic record of Mesozoic and Cenozoic dep- at all biostratigraphic disciplines willing to participate. The re- ositional sequences, laid down in response to changes in relative sults of this biostratigraphic calibration effort are summarized sea level, published in Science in 1987 was greeted with great, on eight charts included in this volume. albeit mixed, interest. The concept of sequence stratigraphy re- This volume also addresses the question of cyclicity as a ceived much acclaim whereas the chronostratigraphic record of function of the interaction between tectonics, eustasy, sediment Mesozoic and Cenozoic sequences suffered from a perceived supply and depositional setting. An attempt was made to estab- absence of biostratigraphic and outcrop documentation. The lish a hierarchy of higher order eustatic cycles superimposed Mesozoic and Cenozoic Sequence Stratigraphy of European on lower-order tectono-eustatic cycles.
    [Show full text]
  • Arrêté Du 24 Mai 2016 Portant Modification Des Circonscriptions
    BULLETIN OFFICIEL DU MINISTÈRE DE L’INTÉRIEUR MINISTÈRE DE L’INTÉRIEUR _ Arrêté du 24 mai 2016 portant modification des circonscriptions des brigades territoriales de Capestang, d’Olonzac, de Saint-Chinian et de Valras-Plage (Hérault) NOR : INTJ1612225A Le ministre de l’intérieur, Vu le code de la défense ; Vu le code de procédure pénale, notamment ses articles 15-1 et R. 15-22 à R. 15-26 ; Vu le code de la sécurité intérieure, notamment son article L. 421-2, Arrête : Article 1er Les circonscriptions des brigades territoriales de Capestang, d’Olonzac, de Saint-Chinian et de Valras-Plage (Hérault) sont modifiées à compter du 1er juin 2016 dans les conditions précisées en annexe. Article 2 Les officiers, gradés et gendarmes des brigades territoriales de Capestang, d’Olonzac, de Saint-Chinian et de Valras-Plage exercent les attributions attachées à leur qualité d’officier ou d’agent de police judiciaire dans les conditions fixées aux articles R. 13 à R. 15-2 et R. 15-24 (1o) du code de procédure pénale. Article 3 Le directeur général de la gendarmerie nationale est chargé de l’exécution du présent arrêté, qui sera publié au Bulletin officiel du ministère de l’intérieur. FFi l 24 mai 2016. Pour le ministre et par délégation : L’inspecteur général de l’administration, directeur des soutiens et des finances, P. DEBROSSE 15 JUILLET 2016. – INTÉRIEUR 2016-7 – PAGE 297 BULLETIN OFFICIEL DU MINISTÈRE DE L’INTÉRIEUR ANNEXE BRIGADE TERRITORIALES CIRCONSCRIPTION ACTUELLE CIRCONSCRIPTION NOUVELLE Capestang Capestang Capestang Colombiers Colombiers
    [Show full text]
  • Assignan, Babeau-Bouldoux, Cazedarnes, Cébazan, Cessenon
    OU --- WHERE QUAND QUOI --- WHATWHATWHAT €€€ QUI --- WHOWHOWHO WHEN ℡℡℡ AOUT AUGUST SaintSaintSaint-Saint --- Domaine de 010101 9h309h309h30 Balade vigneronne --- Stroll int he RRR 04 67 38 19 13 ChinianChinianChinian Canimals le vineyard, tasting and lunch 131313 HautHautHaut SaintSaintSaint-Saint --- Jardin de la 020202 08h08h08h-08h ---12h12h12h12h Foire aux produits régionaux Art et Terroir ChinianChinianChinian MairieMairieMairie Local products fair Ht Languedoc Townhall gar- den SaintSaintSaint-Saint --- Promenade 040404 TLJTLJTLJ Vide Grenier --- Car boot sale GGG Philatélie ChinianChinianChinian Cazedarnes Salle 040404 NCNCNC Soirée Tapas --- Spanish food evening NCNCNC CDFCDFCDF polyvalente Cazedarnes Domaine des 060606 18h3018h3018h30 Balade vigneronne --- stroll in the RRR 06 83 33 51 69 Mathurins vineyard, wine tasting and lunch Cébazan VillageVillageVillage 070707 18h18h18h-18h ---22h22h22h22h Marché Paysan avec buvette et Asso CLIC restautation --- Farming market 06 32 07 33 33 Cébazan Salle Polyva- Du 10h --- Exposition de peintures de Georges GGG MairieMairieMairie lentelentelente 10 12h et12h et Blondeau. Vernissage le 10 à 19h Multipurpose au 17h --- Georges Blondeau painting exhibi- Assignan, hall 121212 20h20h20h tion Preview the 10th at 7.00 pm Babeau-Bouldoux, Cessenon Cave de 101010 8h458h458h45 Balade vigneronne --- stroll in the RRR 04 67 89 39 18 sur Orbsur Orb Cessenon vineyard, wine tasting and lunch Cazedarnes, Cébazan, SaintSaintSaint-Saint --- Cave des 101010 TLJTLJTLJ Journée portes ouvertes. Repas et RRR
    [Show full text]
  • SDGCH Réglementation Agrainage 2019 2025
    ANNEXES ANNEXES Annexe 2 : Afin de vérifier les zones potentielles où l’agrainage de dissuasion peut se pratiquer, un lien dynamique est disponible sur le site internet de la DDTM 34 : La réglementation sur l’agrainage de dissuasion http://carto.geo-ide.application.developpement- durable.gouv.fr/134/CEP_Chasse_Agrainage.map - Mise en place d’une zone test sans agrainage : A) Argumentaire Le précédent SDGC interdisait déjà l’agrainage dans de nombreuses communes de l’Hérault situées essentiellement en plaine viticole et sur le littoral (agrainage demeure interdit sur ces CONSIDERANT que la plaine viticole et la zone littorale ne permettent pas une gestion du communes). sanglier compatible avec le maintien de l’équilibre agro-cynégétique compte tenu de la Conformément au protocole du 5 avril 2018, le présent SDGC interdit l’agrainage de dissuasion présence de cultures agricoles et de l’urbanisation importante de ces secteurs, sur des communes supplémentaires afin de mettre en place une expérimentation sur une zone CONSIDERANT que le nourrissage (agrainage et affouragement) visant à cantonner le grand test (cf. cartographie de la zone test) dès la saison 2019/2020. gibier sur un territoire donné contribue à une perte du caractère sauvage des animaux et à des surpopulations, et par conséquent augmente le risque de déséquilibre agro-sylvo-cynégétique, 2. Période le risque de collisions routières, le risque de dégâts en zone urbaine et péri-urbaine et le risque Sur les territoires où il peut se pratiquer, l’agrainage de dissuasion est autorisé uniquement à de propagation des épizooties, compter du 1er avril jusqu’à la date d’ouverture de la chasse dans les vignes.
    [Show full text]
  • Télécharger La Liste Des MSAP De L'hérault (18
    18 MAISONS DE SERVICES AU PUBLIC A VOTRE DISPOSITION Alco Olonzac 101 Rue Robert Fabre 16 Boulevard Louis Blazin 34 080 Montpellier 34 210 Olonzac 04 99 23 17 69 04 68 27 83 67 LODEVE [email protected] [email protected] LE CAYLAR CLARET ST GERVAIS LE CAYLAR MONTPELLIERCLARET Centre Cebenna Roujan Avenue du champ des Horts 35 Avenue du Pézenas LA SALVETAT OLARGUES 34 320 Roujan LODEVE SAINT MARTIN DE 34 390 Olargues LONDRES LODEVE ST PARGOIRE 04 67 97 88 02 04 67 24 50 80 ST GERVAIS ROUJAN MONTPELLIER [email protected] [email protected] ST GERVAIS Alco ST CHINIAN FRONTIGNAN Saint-Gervais sur Mare LA SALVETAT LE CAYLAR CLARETAdages Claret (LA POSTE) LA SALVETAT MAUREILHAN ( LA POSTE) OLARGUE MONTPELLIER Place de l’Hermet 34 Rue de Castres AGDEST PARGOIRE 34 270 Claret ROUJAN ST PARGOIRE 34 610 Saint-Gervais-sur-Mare OLONZAC OLARGUES 04 67 59 00 38 CAPESTANG LODEVEROUJAN 04 67 97 64 94 ST CHINIAN FRONTIGNANFRONTIGNAN MSAP Classique MURVIELS [email protected] [email protected] ST GERVAIS MONTPELLIER ST CHINIAN MAUREILHAN LES BEZIERS MSAP La Poste MSAP Itinérante Frontignan Saint-Pargoire (LA POSTE) AGDE LA SALVETAT MAUREILHAN 5 Rue Lucien Salette 10 Rue de la Paix OLARGUE CAPESTANG 34 110 Frontignan OLONZAC 34 230 Saint-Pargoire ST PARGOIRE ROUJAN 04 67 18 50 64 SERIGNAN AGDE [email protected] Sud Hérault – Capestang MSAP Classique 1 Rue Georges Brassens ST CHINIAN FRONTIGNAN MSAP La Poste 34 310 Capestang Le Caylar ( LA POSTE ) MSAP Itinérante 04 67 26 37 10 Centre
    [Show full text]
  • Liste Des Zones Infra-Departementales Pour Les Partipants Obligatoires
    LISTE DES ZONES INFRA-DEPARTEMENTALES POUR LES PARTIPANTS OBLIGATOIRES 4 zones infra-départementales sont offertes : 4 MUG sont offerts : Zone A, B, C et D 1-DIR. 2 à 7 classes 2-ASH 3-REMPLACEMENT 4- ENSEIGNEMENT ZONE A ZONE B AGEL PORTIRAGNES ABEILHAN LE POUJOL-SUR-ORB AIGNE PREMIAN AGDE LE PRADAL AIGUES-VIVES PUIMISSON ALIGNAN-DU-VENT LES AIRES AZILLANET PUISSERGUIER AUMES LEZIGNAN-LA-CEBE BASSAN QUARANTE AUTIGNAC LUNAS BELARGA RIOLS AVENE MAGALAS BEZIERS SAUVIAN BEDARIEUX MARGON BOUJAN-SUR-LIBRON SERIGNAN BERLOU MARSEILLAN CAPESTANG SIRAN BESSAN MONTAGNAC CAZOULS-LES-BEZIERS ST-ETIENNE-D'ALBAGNAN CABREROLLES MONTBLANC CERS ST-PONS-DE-THOMIERES CAMPAGNAN MURVIEL-LES-BEZIERS CESSERAS ST-THIBERY CAMPLONG NEFFIES COLOMBIERS THEZAN-LES-BEZIERS CASTANET-LE-HAUT NEZIGNAN-L'EVEQUE CORNEILHAN VALRAS-PLAGE CASTELNAU-DE-GUERS NIZAS COURNIOU VENDRES CAUSSES-ET-VEYRAN PEZENAS CREISSAN VILLENEUVE-LES-BEZIERS CAUX PINET CRUZY CAZEDARNES POMEROLS FELINES-MINERVOIS CAZOULS-D'HERAULT POUZOLLES FERRALS-LES-MONTAGNES CEBAZAN PUISSALICON FRAISSE-SUR-AGOUT CEILHES-ET-ROCOZELS ROQUEBRUN LA CAUNETTE CESSENON-SUR-ORB ROUJAN LA LIVINIERE COLOMBIERES-SUR-ORB SERVIAN LA SALVETAT-SUR-AGOUT COULOBRES ST-CHINIAN LESPIGNAN ESPONDEILHAN ST-GENIES-DE-FONTEDIT LIEURAN-LES-BEZIERS FAUGERES ST-GENIES-DE-VARENSAL LIGNAN-SUR-ORB FLORENSAC ST-GERVAIS-SUR-MARE MARAUSSAN GABIAN ST-NAZAIRE-DE-LADAREZ MAUREILHAN GRAISSESSAC ST-PARGOIRE MONTADY HEREPIAN ST-PONS-DE-MAUCHIENS NISSAN-LEZ-ENSERUNE JONCELS TOURBES OLARGUES LA TOUR-SUR-ORB VALROS OLONZAC LAMALOU-LES-BAINS VIAS PAILHES
    [Show full text]
  • L'organisation Institutionnelle Du Pays
    L’ORGANISATION INSTITUTIONNELLE DU PAYS Le Pays Haut Languedoc et Vignobles comprend : 89 communes 11 Communautés de communes 4 communes hors communautés La ville de Bédarieux, seule ville du Pays, comprenant 6 518 habitants n’est pas en intercommunalité. La population totale du Pays s’élève à 58 967 habitants (Population légale au 1 er janvier 2009). a) Les communes COMMUNES COMMUNES 1 AGEL 46 MARGON 2 AIGNE 47 MINERVE 3 AIGUES VIVES 48 MONS LA TRIVALLE 4 ASSIGNAN 49 MONTELS 5 AVÈNE 50 MONTESQUIEU 6 AZILLLANET 51 MONTOULIERS 7 BABEAU-BOULDOUX 52 MURVIEL LES BÉZIERS 8 BEAUFORT 53 NEFFIÈS 9 BÉDARIEUX 54 OLARGUES 10 BERLOU 55 OLONZAC 11 BOISSET 56 OUPIA 12 BRENAS 57 PAILHÈS 13 CABREROLLES 58 PARDAILHAN 14 CAMPLONG 59 PÉZENES LES MINES 15 CAPESTANG 60 PIERRERUE 16 CARLENCAS ET LEVAS 61 POILHES 17 CASSAGNOLES 62 POUZOLLES 18 CAUSSES ET VEYRAN 63 PRADES-SUR-VERNAZOBRES 19 CAUSSINIOJOULS 64 PREMIAN 20 CAZEDARNES 65 PUISSERGUIER 21 CÉBAZAN 66 QUARANTE 22 CEILHES ET ROCOZELS 67 RIEUSSEC 23 CESSENON 68 RIOLS 24 CESSERAS 69 ROQUEBRUN 25 COLOMBIÈRES SUR ORB 70 ROUJAN 26 COMBES 71 SIRAN 27 COURNIOU 72 ST CHINIAN 28 CREISSAN 73 ST ÉTIENNE D'ALBAGNAN 29 CRUZY 74 ST ÉTIENNE D'ESTRECHOUX 30 DIO ET VALQUIÈRES 75 ST GENIÈS DE VARENSAL 31 FAUGÈRES 76 ST GERVAIS SUR MARE 32 FÉLINES MINERVOIS 77 ST JEAN DE MINERVOIS 33 FERRALS LES MONTAGNES 78 ST JULIEN 34 FERRIÈRES POUSSAROU 79 ST MARTIN DE L'ARCON 35 FOS 80 ST NAZAIRE DE LADAREZ 36 GABIAN 81 ST PONS DE THOMIÈRES 37 GRAISSESSAC 82 ST VINCENT D'OLARGUES 38 JONCELS 83 TAUSSAC LA BILLIÈRE 39 LA CAUNETTE
    [Show full text]
  • Nelles Circo-2
    Circonscriptions législatives de l'Hérault, découpage par cantons Nelles COMMUNES CANTONS ARDTS CIRCONS VILLENEUVE LES MAGUELONE FRONTIGNAN 03 01 LATTES LATTES 03 01 PALAVAS LES FLOTS LATTES 03 01 PEROLS LATTES 03 01 MONTPELLIER-05 MONTPELLIER-5 03 01 MONTPELLIER-06 MONTPELLIER-6 03 01 LAVERUNE MONTPELLIER-8 03 01 MONTPELLIER-08 MONTPELLIER-8 03 01 SAINT JEAN DE VEDAS MONTPELLIER-8 03 01 MONTPELLIER-01 MONTPELLIER-1 03 02 MONTPELLIER-03 MONTPELLIER-3 03 02 MONTPELLIER-07 MONTPELLIER-7 03 02 MONTPELLIER-09 MONTPELLIER-9 03 02 CASTELNAU LE LEZ CASTELNAU LE LEZ 03 03 CRES (LE) CASTELNAU LE LEZ 03 03 ASSAS CASTRIES 03 03 BAILLARGUES CASTRIES 03 03 BEAULIEU CASTRIES 03 03 BUZIGNARGUES CASTRIES 03 03 Nelles COMMUNES CANTONS ARDTS CIRCONS CASTRIES CASTRIES 03 03 GALARGUES CASTRIES 03 03 GUZARGUES CASTRIES 03 03 JACOU CASTRIES 03 03 MONTAUD CASTRIES 03 03 RESTINCLIERES CASTRIES 03 03 SAINT BRES CASTRIES 03 03 SAINT DREZERY CASTRIES 03 03 SAINT GENIES DES MOURGUES CASTRIES 03 03 SAINT HILAIRE DE BEAUVOIR CASTRIES 03 03 SAINT JEAN DE CORNIES CASTRIES 03 03 SUSSARGUES CASTRIES 03 03 TEYRAN CASTRIES 03 03 VENDARGUES CASTRIES 03 03 CAMPAGNE CLARET 03 03 GARRIGUES CLARET 03 03 BOISSERON LUNEL 03 03 SAINT CHRISTOL LUNEL 03 03 SAINT SERIES LUNEL 03 03 SATURARGUES LUNEL 03 03 SAUSSINES LUNEL 03 03 VERARGUES LUNEL 03 03 Nelles COMMUNES CANTONS ARDTS CIRCONS VILLETELLE LUNEL 03 03 CLAPIERS MONTPELLIER-2 03 03 MONTFERRIER SUR LEZ MONTPELLIER-2 03 03 MONTPELLIER-02 MONTPELLIER-2 03 03 ANIANE ANIANE 02 04 ARGELLIERS ANIANE 02 04 BOISSIERE (LA) ANIANE 02 04
    [Show full text]