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Gravimetry for Geothermal Exploration
GRAVIMETRY FOR GEOTHERMAL EXPLORATION METHODOLOGY, COMPUTER PROGRAMS AND TWO CASE STUDIES IN THE SWISS MOLASSE BASIN Thesis defended on January 8, 2015 at the FACULTY OF SCIENCES INSTITUTE OF HYDROGEOLOGY AND GEOTHERMICS (CHYN) UNIVERSITY OF NEUCHÂTEL for the degree of DOCTOR OF NATURAL SCIENCES presented by PIERRICK ALTWEGG Accepted by the following Jury: PROF. PHILIPPE RENARD PROF. STEPHEN ANDREW MILLER PROF. GUILLAUME CAUMON PROF. JON MOSAR DR. EVA SCHILL DR. FRANÇOIS-DAVID VUATAZ DR. PIER-VITTORIO RADOGNA To my beloved wife and children, Alexandrine, Elanor and Aurèle. Acknowledgments A PhD thesis is something unique in the life of a scientist but is not a project that one can carry alone. In this respect, many individuals, institutions and societies contributed to it and I want to gratefully thank them. First, I owe much to Dr. François-David Vuataz who introduced me to the world of geothermal energy, saved me countless hours by being a living database and for her active participation in the project. I also would like to thank Prof. Eva Schill who made this project possible. A special thanks to Prof. Philippe Renard who agreed to supervise this work after three years and for his availability and his advice. I also want to thank Prof. Daniel Hunkeler and Prof. Pierre Perrochet for their support. My gratitude to all the members of the jury for their availability and their input after the critical review of this PhD thesis. I would like to especially thank Prof. Jon Mosar of the University of Fribourg for his time and input as well as for teaching me how to avoid formal errors in this work. -
Calcareous Nannofossils, Ammonites
De Kaenel et al. Swiss J Palaeontol (2020) 139:6 https://doi.org/10.1186/s13358-020-00209-5 Swiss Journal of Palaeontology RESEARCH ARTICLE Open Access New biostratigraphical data (calcareous nannofossils, ammonites) and Early to Late Barremian transition in the Urgonien Jaune facies and Marnes de la Russille complex of the Swiss Jura Mountains Eric De Kaenel1*, Pierre‑Olivier Mojon2 and Antoine Pictet3 Abstract In the central Jura Mountains (Western Switzerland), the Urgonien Jaune (UJ) facies with the Marnes de la Russille beds (MRu) have provided very rich nannoforas associated with very rare Tethyan ammonites. A late Early Barremian nannofora of the Mid‑Barremian Event (MBE, following a regional tectonic event of an earliest Barremian synsedimentary tectonic crisis) was found in MRu of the lower UJ and includes 42 genera with 90 species. Among them, Biscutum jurensis De Kaenel, n. sp., Flabellites eclepensensis De Kaenel, n. sp., Palaeopontosphaera giraudii De Kaenel, n. sp., Rhagodiscus buisensis De Kaenel, n. sp., and Vagalapilla rutledgei De Kaenel, n. sp., are recognized as fve new species. This nannofora is a mixture of Boreal and Tethyan taxa with 20 nannofossil markers (Assipetra terebrodentarius, Broinsonia galloisii, Calcicalathina oblongata, Cyclagelosphaera rotaclypeata, Diloma placinum, Ethmorhabdus hauterivianus, Flabellites eclepensensis, Gorkaea pseudoanthophorus, Nannoconus abundans, Nannoconus pseudoseptentrionalis, Palaeopontosphaera giraudii, Palaeopontosphaera pinnata, Placozygus howei, Placozygus reticulatus, Reinhardtites scutula, Rhagodiscus buisensis, Rhagodiscus eboracensis, Tegulalithus septentrionalis, Tubodiscus jurapelagicus, Zeugrhabdotus moulladei) indicating very precisely the nannofossil Zones LK19 (Boreal)–NC5D (Tethyan) as well as the Elegans (Boreal) and Moutonianum (Tethyan) ammonite Zones of the latest Early Barremian. The ammonites in the basal UJ facies of Early Barremian age are reworked Lyticoceras claveli (Nodosoplicatum Zone, Early Hauterivian) and reworked Cruasiceras cf. -
Découverte Celtique Exceptionnelle En 2006 Le «Sanctuaire»
Découverte celtique exceptionnelle en 2006 Le «sanctuaire» Le site au sommet du Mormont, en cours de fouille. helvète du Mormont par Gilbert Kaenel et Alors que la communauté scientifique s’apprêtait à commémo- Denis Weidmann rer le cent cinquantième anniversaire de la découverte de La Tène en novembre 1857, le canton de Vaud mettait au jour en 2006, au sommet du Mormont, de manière inattendue, un site appelé à devenir une référence, au même titre que le site épo- nyme du Second âge du fer européen; référence non seule- ment pour l’archéologie des Helvètes du Plateau suisse, entre la fin du IIe et le début du Ier siècle av. J.-C., mais pour l’étu- de des pratiques rituelles et cultuelles des Celtes en général. 16 NIKE-Bulletin 4 /2007 NIKE-Bulletin 4 /2007 17 La Section de l’archéologie cantonale Venoge, au sud: le Mormont sépare ainsi les vaudoise a dû gérer une nouvelle interven- bassins versants du Rhin et du Rhône. Fosses et puits à offrandes tion nécessitant la mise en œuvre de moyens L’occupation de la fin de l’âge du Fer au sein d’un vaste ensemble à importants, affectés à l’organisation d’une s’est développée dans le fond d'un secteur vocation cultuelle fouille préventive de grande ampleur. Le légèrement encaissé, encadré par des fail- Quelque 300 structures (fosses, trous de po- Musée cantonal d’archéologie et d’histoire les, et proche du sommet (604 m). La sur- teau, foyers, blocs de signalisation, petits de Lausanne de son côté, responsable de la face rocheuse, retravaillée par l’érosion et fossés) ont été mises au jour; parmi ces der- conservation des vestiges exhumés, a dû en particulier par l’activité glaciaire qua- nières, plus de 260 fosses sont interprétées adapter l’activité de son laboratoire à l’arri- ternaire, présente un aspect moutonné avec comme de véritables puits à offrandes. -
Mitochondrial D-Loop Variation, Coat Colour and Sex Identification of Late
Journal of Archaeological Science: Reports 6 (2016) 386–396 Contents lists available at ScienceDirect Journal of Archaeological Science: Reports journal homepage: www.elsevier.com/locate/jasrep Mitochondrial d-loop variation, coat colour and sex identification of Late Iron Age horses in Switzerland Julia Elsner a,⁎, Sabine Deschler-Erb a, Barbara Stopp a, Michael Hofreiter b,JörgSchiblera, Angela Schlumbaum a a Integrative Prehistory and Archaeological Science, Department of Environmental Sciences, Basel University, Spalenring 145, 4055 Basel, Switzerland b Institute for Biochemistry and Biology, University of Potsdam, Karl-Liebknecht-Str. 24–25, D-14476 Potsdam, Germany article info abstract Article history: In the Celtic world, horses enjoyed a prominent position as status symbols and objects of veneration, yet little is Received 26 November 2015 known about these Celtic horses except that they were rather small. The Late Iron Age was a time defined by in- Accepted 7 March 2016 creasing inter-cultural contact between Celtic peoples and the Romans. This is, amongst other features, observ- Available online 14 March 2016 able in the phenotypes of domestic livestock such as horses. Amongst the usually small animals, larger ones are rarely but regularly encountered in the archaeological record. We have investigated mitochondrial (mt) Keywords: Genetic diversity DNA d-loop diversity, sex and coat colour using bones from 34 horses of different size from three Swiss sites Ancient DNA (Mormont, Basel-Gasfabrik, Aventicum) most of them dating from 150 to 50 BCE. The aim was to characterise Iron Age the diversity of matrilineages and coat colourations of Iron Age horses, and to identify molecular sex. -
De L'âge Du Fer À L'usage Du Verre
Cahiers d'archéologie romande 151 De l'âge du Fer à l'usage du verre Mélanges offerts à Gilbert Kaenel, dit «Auguste», à l'occasion de son 65e anniversaire Textes réunis par Jérôme Bullinger, Pierre Crotti et Claire Huguenin Lausanne 2014 Sommaire Avant-propos Jérôme BULLINGER, Pierre CROTTI et Claire HUGUENIN 9 Préface d'un coéditeur Denis WEIDMANN 11 «Rendez-vous à la Couronne !» Suzanne et Daniel FIBBI-AEPPLI 13 A propos d'une formule orale usuelle en contexte vaudois : approche analytique, interprétative et tout le commerce Laurent FLUTSCH 15 Clin d'oeil sur la portée du temps... Daniel PAUNIER 21 Frontière... quelle frontière ? Gilbert Kaenel et la valorisation hors de Suisse de la recherche sur l'âge du Fer chez les Helvètes : l'archéologie à saute-frontière Marie-Jeanne ROULIÈRE-LAMBERT, Philippe BARRAL, Philippe CURDY, Cynthia DUNNING-THIERSTEIN, 25 Olivier BUCHSENSCHUTZ, Jean-Loup FLOUEST et François SCHIFFERDECKER De Naef à Auguste : La Tène et les Vaudois Marc-Antoine KAESER et Gianna REGINELLI SERVAIS 37 Les archives en musées et en bibliothèques Gilbert COUTAZ 43 De Lausanne à Lattes : réflexions sur les expositions d'archéologie Lionel PERNET 49 L'église-musée. Réflexions sur l'exposition des vestiges archéologiques dans les églises de Suisse romande au 20e siècle Dave LUTH! en collaboration avec Claire HUGUENIN 59 De la fouille aux restitutions en Protohistoire : l'exemple du sanctuaire de Gournay-sur-Aronde Stephan FICHTL 69 Bien culturel et valeur économique : un conflit devenu omniprésent Marc-André HALDIMANN 77 Processus -
Geothermal State of the Deep Western Alpine Molasse Basin, France-Switzerland
Published in Geothermics 67, 48-65, 2017 1 which should be used for any reference to this work Geothermal state of the deep Western Alpine Molasse Basin, France-Switzerland Cyril Chelle-Michou a,b,∗, Damien Do Couto a, Andrea Moscariello a, Philippe Renard c, Elme Rusillon a a University of Geneva, Department of Earth Sciences, 13 rue des Maraîchers, 1205 Geneva, Switzerland b Univ. Lyon, UJM-Saint-Etienne, UBP, CNRS, IRD, Laboratoire Magmas et Volcans UMR 6524, F-42023 Saint Etienne, France c University of Neuchâtel, Center for Hydrogeology and Geothermics (CHYN), 11 rue Emile Argand, 2000 Neuchâtel, Switzerland abstract Keywords: Over the last few years the Western Alpine Molasse Basin (WAMB) has been attracting large institutional, Geothermal anomaly industrial and scientific interest to evaluate the feasibility of geothermal energy production. However, Geostatistics the thermal state of the basin, which is instrumental to the development of such geothermal projects, Structure has remained to date poorly known. Here, we compile and correct temperature measurements (mostly Alpine Molasse Basin bottom hole temperature) from 26 existing well data mostly acquired during former hydrocarbon explo- Fluid circulations ration in the basin. These data suggest that the average geothermal gradient of the WAMB is around Bottom hole temperature 25–30 ◦C/km. We further use these data to build the first well data-driven 3D geostatistical temper- ature model of the whole basin and generate probabilistic maps of isotherms at 70 and 140 ◦C. This model highlights a number of positive and negative thermal anomalies that are interpreted in the con- text of heat advection caused by fluid circulation along faults and/or karst systems. -
Le Sanctuaire Celtique Du Mormont, Vaud, Suisse Eduard Dietrich
Le sanctuaire celtique du Mormont, Vaud, Suisse Eduard Dietrich To cite this version: Eduard Dietrich. Le sanctuaire celtique du Mormont, Vaud, Suisse. Bulletin de l’Association française pour l’étude de l’âge du fer, AFEAF, 2007, 25, pp.61-64. hal-02516109 HAL Id: hal-02516109 https://hal.archives-ouvertes.fr/hal-02516109 Submitted on 20 Aug 2020 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. Distributed under a Creative Commons Attribution - NonCommercial - NoDerivatives| 4.0 International License Bulletin de l'Association Française pour /'Étude de l'Âge du Fer, n° 25, 2007 LE SANCTUAIRE CELTIQUE DU MORMONT, VAUD, SUISSE EDUARD DIETRICH, ARCHEODUNUM SA 1. Introduction La deuxième phase d'exploitation du / I calcaire de la colline du Mormont a nécessité Î -t la mise en place d'une campagne de sondages r , ,>j ) qui a révélé un site celtique d'une importance y Yve~d9Jl ) / exceptionnelle. En effet, il apparaît que le site / Orbe / \ { fut utilisé comme sanctuaire pendant La Tène 1 ·( f K LE MORMONT (/ r 1 D 1, où un nombre important de puits et de y Cossonay ~ fosses à offrandes ont été creusés. -
Cartographie Géologique Du Canton De Vaud Et Cartographie Du
Geology mapping with an emphasis on the Quaternary deposits in the Swiss Prealps and Molasse Plateau Valérie Baumann, Marc-Henri Derron, Jean-Luc Epard, Michel Jaboyedoff Institute of Earth Sciences, University of Lausanne Location for 2 test areas Digital detailed geological maps (scale 1:25000) Montreux Les Mosses Monthey Les Diablerets Maps source: Atlas géologique 1:25000, Federal Office of Topography, swisstopo Detailed geological maps have been produced for the whole Switzerland since about a century. In the last decades maps were converted to digital maps. However, often the limits for each formation (or name) are different from one sheet to the other. Main Goals ➢ Harmonise the different geological maps (scale 1:25.000) ➢ Improve the Quaternary deposits mapping of “canton de Vaud” in Switzerland Methodology The geology mapping was performed using different data: ➢ The geological maps (scale: 1:25000) ➢ Geological publications for the studied areas ➢ High resolution LiDAR data and derived hillshades ➢ Aerial photographs ➢ Boreholes data and field work in order to solve specific problems Hillshade map for the region of Leysin (Prealps) The hillshade is derived from high resolution LiDAR data (LiDAR 2015, Etat de Vaud). The possibility to remove the trees in the forested areas allows the detection and interpretation of new morphologic features. 3D geological map of the Leysin area (Prealps) Leysin In order to produce the geological map for the test area from the 4 pre-existent geological maps, we adjusted and modified the geological limits for the different formations and linear structures, such as faults. Also, new glacial deposits related to the Last Glacial maximum (LGM) and paraglacial rock slope deformations have been mapped. -
Juin 2006 340 (P.D
JUIN 2006 340 (P.D. 08/06) (R. 08/06) EXPOSE DES MOTIFS ET PROJET DE DECRET modifiant le Plan directeur cantonal et RAPPORT COMPLEMENTAIRE DU CONSEIL D'ETAT AU GRAND CONSEIL sur le postulat Charles-Pascal Ghiringhelli : voie navigable du Rhône au Rhin : Un symbole pour l’Expo 01 !? et REPONSE DU CONSEIL D’ETAT AU GRAND CONSEIL sur l’interpellation André Marendaz concernant le plan d’extension cantonal N° 112. Canal d’Entreroches. Quel avenir ! 1. EXPOSE DES MOTIFS ET PROJET DE DECRET MODIFIANT LE PLAN DIRECTEUR CANTONAL...........................................................2 1.1 Introduction ..........................................................................................2 1.2 Protection du tracé du Canal du Rhône au Rhin...................................2 1.3 Evolution du contexte politique et technique .......................................3 1.3.1 Position de la Confédération et des autres cantons ..................3 1.3.2 Plan d’affectation cantonal de la Venoge .................................4 1.3.3 Résultats de l’étude GESORBE.................................................4 1.4 Modification du Plan directeur cantonal...............................................5 1.5 Concept d’aménagement des terrains concernés par la modification du Plan directeur cantonal ....................................................................6 1.6 Conséquences du projet de décret ........................................................7 – 2 – 2. REPONSE DU CONSEIL D’ETAT A L’INTERPELLATION MARENDAZ ET RAPPORT COMPLEMENTAIRE DU -
Geological and Archeological Visit of Geneva
Geological and archeological Update July 3rd 2014 visit of Geneva Walter Wildi, Pierre Corboud, Stéphanie Girardclos, Georges Gorin Geological and archeological visit of Geneva Key words: geology, archeology, field trip, Geneva Walter Wildi, Pierre Corboud, Stéphanie Girardclos, Georges Gorin Christian [email protected] Section of Earth and Environmental Sciences Rue des Maraîchers 13, CH-1211 Genève 4 Copyright 2014 Document available on the website http://www.unige.ch/forel/Services/Visitegeologique_en.html 1 Table of contents Foreword ………………………………………………………………………………………………………………………………………………………………………........ 3 1.Introduction ……………………………………………………………………………………………………………………………………………………………………… 3 1.1. The natural site ……………...................................................................................................................................................... 3 1.2. Geological history of the Geneva Basin ………………………………………………………………………………………………………………………… 5 1.3. Human occupation of the Geneva site …………………………………………………………………………………………………………………………. 15 2. Site visit ……………………………………………………………………………………………………………………………………………………………………………. 24 Ge 1: Geological visit of Geneva City ……………………………………………………………………………………………………………………………….. 25 Ge 1.1: The Arve River: an Alpine river and its alluvial plain…………………………………………………………………………………………………. 27 Ge 1.2: Bois de la Bâtie: the «Alluvion ancienne», deposits of an old proglacial plain covered by the Upper Basal Moraine of the Rhône Glacier………………………………………………………………………………………………………………………………………………… 30 Ge 1.3: From the -
Le Sanctuaire Helvète Du Mormont
Le sanctuaire helvète du Mormont Autor(en): Dietrich, Eduard / Kaenel, Gilbert / Weidmann, Denis Objekttyp: Article Zeitschrift: AS : Archäologie Schweiz : Mitteilungsblatt von Archäologie Schweiz = Archéologie Suisse : Bulletin d'Archéologie Suisse = Archeologia Svizzera : Bollettino di Archeologia Svizzera Band(Jahr): 30(2007) Heft 1 Erstellt am: 28 mars 2014 Persistenter Link: http://dx.doi.org/10.5169/seals-109261 Nutzungsbedingungen Mit dem Zugriff auf den vorliegenden Inhalt gelten die Nutzungsbedingungen als akzeptiert. Die angebotenen Dokumente stehen für nicht-kommerzielle Zwecke in Lehre, Forschung und für die private Nutzung frei zur Verfügung. Einzelne Dateien oder Ausdrucke aus diesem Angebot können zusammen mit diesen Nutzungsbedingungen und unter deren Einhaltung weitergegeben werden. Die Speicherung von Teilen des elektronischen Angebots auf anderen Servern ist nur mit vorheriger schriftlicher Genehmigung möglich. Die Rechte für diese und andere Nutzungsarten der Inhalte liegen beim Herausgeber bzw. beim Verlag. Ein Dienst der ETH-Bibliothek Rämistrasse 101, 8092 Zürich, Schweiz [email protected] http://retro.seals.ch as. 30.2007.1 Le Mormont (VD) S S *f- :r- r- Le sanctuaire helvète du Mormont Eduard Dietrich, avec la collaboration de Gilbert Kaenel et Denis Weidmann et des contributions de Peter Jud, Patrice Méniel et Patrick Moinat Fig. 1 Vue aérienne du site en cours de fouille. Les falaises qui bordent l'ensel- L'année 2006 a été la lure sur les côtés nord et sud forment marquée par Aucun indice archéologique n'était répertorié sur la une limite naturelle de l'aire cultuelle. découverte inattendue d'un sanc¬ colline du Mormont avant les découvertes de 2006. Luftbild der Fundstelle während der Néanmoins, le service archéologique cantonal, qui Ausgrabung. -
Potential for Deep Geological Sequestration of CO2 in Switzerland: a first Appraisal
Swiss J Geosci (2010) 103:427–455 DOI 10.1007/s00015-010-0030-4 Potential for deep geological sequestration of CO2 in Switzerland: a first appraisal Gabriel Chevalier • Larryn W. Diamond • Werner Leu Received: 10 February 2009 / Accepted: 10 August 2010 / Published online: 24 November 2010 Ó Swiss Geological Society 2010 Abstract Possibilities to sequester anthropogenic CO2 in aquifers within the preferred 800–2,500 m depth interval, deep geological formations are being investigated world- and to its low seismicity, low geothermal gradient, low wide, but the potential within Switzerland has not yet been fault density, and long groundwater residence times. evaluated. This study presents a first-order appraisal based Smaller areas with good potential lie between Zu¨rich and solely on geological criteria collated from the literature. St. Gallen. In contrast, western Switzerland, the Jura and The Swiss Molasse Basin (SMB) and the adjacent Folded the southern SMB have markedly poorer potential. Con- Jura are the only realms of the country where CO2 could sidering only the portions of the aquifers with potential conceivably be stored in saline aquifers. Evaluation of above 0.6, the theoretical, effective storage capacity of the geological criteria at the basin-wide scale shows that the basin is estimated to be 2,680 million tonnes of CO2. SMB–Jura has moderate potential (score of 0.6 on a scale from 0 to 1) when compared to basins elsewhere. At the Keywords Sequestration Á Carbon dioxide Á Switzerland Á intrabasinal scale, inspection of the stratigraphy reveals Swiss Molasse basin Á CO2 storage potential Á Geology Á four regional candidate aquifers that are sealed by suitable Aquifer caprocks: top Basement plus basal Mesozoic sandstones, all sealed by the Anhydrite Group; Upper Muschelkalk sealed by the Gipskeuper; Hauptrogenstein sealed by the Introduction Effinger Member, and Upper Malm plus Lower Cretaceous sealed by the Lower Freshwater Molasse.