Low Temperature Deep Geothermal Operations for Direct Use in France: Development of a National Geothermal Database and Last Review Virginie Hamm, Camille Maurel
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THE DEVELOPMENT of MESOZOIC SEDIMENTARY IBASINS AROUND the MARGINS of the NORTH ATLANTIC and THEIR HYDROCARBON POTENTIAL D.G. Masson and P.R
INTERNAL DOCUMENT IIL THE DEVELOPMENT OF MESOZOIC SEDIMENTARY IBASINS AROUND THE MARGINS OF THE NORTH ATLANTIC AND THEIR HYDROCARBON POTENTIAL D.G. Masson and P.R. Miles Internal Document No. 195 December 1983 [This document should not be cited in a published bibliography, and is supplied for the use of the recipient only]. iimsTit\jte of \ OCEANOGRAPHIC SCIENCES % INSTITUTE OF OCEANOGRAPHIC SCIENCES Wormley, Godalming, Surrey GU8 5UB (042-879-4141) (Director: Dr. A. S. Laughton, FRS) Bidston Observatory, Crossway, Birkenhead, Taunton, Mersey side L43 7RA Somerset TA1 2DW (051-653-8633) (0823-86211) (Assistant Director: Dr. D. E. Cartwright) (Assistant Director: M.J. Tucker) THE DEVELOPMENT OF MESOZOIC SEDIMENTARY BASINS AROUND THE MARGINS OF THE NORTH ATLANTIC AND THEIR HYDROCARBON POTENTIAL D.G. Masson and P.R. Miles Internal Document No. 195 December 1983 Work carried out under contract to the Department of Energy This document should not be cited in a published bibliography except as 'personal communication', and is supplied for the use of the recipient only. Institute of Oceanographic Sciences, Brook Road, Wormley, Surrey GU8 SUB ABSTRACT The distribution of Mesozoic basins around the margins of the North Atlantic has been summarised, and is discussed in terms of a new earliest Cretaceous palaeogeographic reconstruction for the North Atlantic area. The Late Triassic-Early Jurassic rift basins of Iberia, offshore eastern Canada and the continental shelf of western Europe are seen to be the fragments of a formerly coherent NE trending rift system which probably formed as a result of tensional stress between Europe, Africa and North America. The separation of Europe, North America and Iberia was preceded by a Late Jurassic-Early Cretaceous rifting phase which is clearly distinct from the earlier Mesozoic rifting episode and was little influenced by it. -
New Micropalaeontological Studies on the Type Section of the Campanian-Maastrichtian at Tercis
New micropalaeontological studies on the type section of the Campanian-Maastrichtian at Tercis (SW France): new ostracodes obtained using acetolysis Bernard Andreu, Gilles Serge Odin To cite this version: Bernard Andreu, Gilles Serge Odin. New micropalaeontological studies on the type section of the Campanian-Maastrichtian at Tercis (SW France): new ostracodes obtained using acetolysis. Carnets de Geologie, Carnets de Geologie, 2008, CG2008 (A02), pp.1-14. hal-00235838v2 HAL Id: hal-00235838 https://hal.archives-ouvertes.fr/hal-00235838v2 Submitted on 21 Mar 2008 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. Carnets de Géologie / Notebooks on Geology - Article 2008/02 (CG2008_A02) New micropalaeontological studies on the type section of the Campanian-Maastrichtian at Tercis (SW France): new ostracodes obtained using acetolysis 1 Bernard ANDREU 2 Gilles Serge ODIN Abstract: Through the use of acetolysis new micropalaeontological studies on the type section of the Campanian-Maastrichtian boundary at Tercis (SW France) we obtained additional information on ostracodes. Acetolysis on hard carbonates levels of the Tercis quarry found 22 species in addition to those of the studies published in 2001. Today, 75 species are recognized: they represent 34 known genera, and 4 currently unidentified. -
French Geothermal Resources Survey BRGM Contribution to the Market Study in the LOW-BIN Project
French geothermal resources survey BRGM contribution to the market study in the LOW-BIN project BRGM/RP - 57583 - FR August, 2009 French geothermal resources survey BRGM contribution to the market study in the LOW-BIN project (TREN/05/FP6EN/S07.53962/518277) BRGM/RP-57583-FR August, 2009 F. Jaudin With the collaboration of M. Le Brun, V.Bouchot, C. Dezaye IM 003 ANG – April 05 Keywords: French geothermal resources, geothermal heat, geothermal electricity generation schemes, geothermal Rankine Cycle, cogeneration, geothermal binary plants In bibliography, this report should be cited as follows: Jaudin F. , Le Brun M., Bouchot V., Dezaye C. (2009) - French geothermal resources survey, BRGM contribution to the market study in the LOW-BIN Project. BRGM/RP-57583 - FR © BRGM, 2009. No part of this document may be reproduced without the prior permission of BRGM French geothermal resources survey BRGM contribution to the market study in the LOW-BIN Project BRGM, July 2009 F.JAUDIN M. LE BRUN, V. BOUCHOT, C. DEZAYE 1 / 33 TABLE OF CONTENT 1. Introduction .......................................................................................................................4 2. The sedimentary regions...................................................................................................5 2.1. The Paris Basin ........................................................................................................5 2.1.1. An overview of the exploitation of the low enthalpy Dogger reservoir ..............7 2.1.2. The geothermal potential -
In Retrospect: Leibniz's Protogaea
NATURE|Vol 455|4 September 2008 OPINION In Retrospect: Leibniz’s Protogaea The first English translation of Gottfried Leibniz’s earth science treatise records the difficulties of understanding our planet before geologists appreciated deep time, Richard Fortey discovers. Protogaea When considering the origin of minerals, by Gottfreid Wilhelm Leibniz Leibniz has an intuitive sense that a kind Translated by Claudine Cohen and of natural cookery is involved: “One is thus Andre Wakefield inclined to suspect that nature, using volca- University of Chicago Press: 2008. noes as furnaces and mountains as alembics, 204 pp. $55. has accomplished in her mighty works what we play at with our little examples [in labo- It is something of a game among historians ratories].” That the furnaces of the ‘chymist’ to try and detect the earliest hints of a major might simulate Earth’s processes is a hope scientific breakthrough in a little-known work that still drives research into petrology and discovered through recondite scholarship. geochemistry today. Charles Darwin’s supposed debt to his grandfa- Why then did Leibniz’s shrewd obser- ther Erasmus is an example, or maybe geologist vations fail to move geology significantly Charles Lyell’s insufficient acknowledgement towards becoming a mature science? For all its of the early geological work of Nicolaus Steno. insights, Protogaea does not seem to a modern When the savant in question is Gottfried Wil- geologist like the natural ancestor of Lyell’s helm Leibniz (1646–1716) — the man who Principles of Geology. The missing ingredient developed calculus independently of Isaac is an awareness of geological time. -
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. -
The Cenozoic History of the Armorican Massif: New Insights
C. R. Geoscience 348 (2016) 387–397 Contents lists available at ScienceDirect Comptes Rendus Geoscience ww w.sciencedirect.com Stratigraphy, Sedimentology The Cenozoic history of the Armorican Massif: New insights from the deep CDB1 borehole (Rennes Basin, France) a, b c d Hugues Bauer *, Paul Bessin , Pierre Saint-Marc , Jean-Jacques Chaˆteauneuf , e a f Chantal Bourdillon , Robert Wyns , Franc¸ois Guillocheau a Bureau de recherches ge´ologiques et minie`res (BRGM), 3, avenue Claude-Guillemin, 45060 Orle´ans cedex 2, France b Universite´ du Maine, Ge´osciences Le Mans, avenue Olivier-Messiaen, 72085 Le Mans cedex 09, France c SEMM Logging, Les Maufras, 18360 Vesdun, France d BRGM (retired), 8, quai du Chaˆtelet, 45000 Orle´ans, France e ERADATA, 170, avenue Fe´lix-Geneslay, 72100 Le Mans, France f Universite´ de Rennes-1, UMR 6118 Ge´osciences Rennes, campus de Beaulieu, 35042 Rennes cedex, France A R T I C L E I N F O A B S T R A C T Article history: Borehole CDB1 (675.05 m) crosses the deepest Cenozoic sedimentary basin of the Received 30 November 2015 Armorican Massif, the Rennes Basin, to reach the underlying basement at a depth of Accepted after revision 25 February 2016 404.92 m, made up of the Late Neoproterozoic to Early Cambrian Brioverian Group, Available online 31 March 2016 weathered down to 520 m depth. The basin’s Cenozoic deposits are divided into seven formations, ranging from Early–Middle Bartonian to Late Pliocene in age. Coastal Handled by Sylvie Bourquin sediments at the very base, along with a thick Priabonian lacustrine episode, imply a major revision of the regional palaeogeography, whilst a very steady and low-energy lacustrine- Keywords: palustrine environment throughout the Priabonian and Early Rupelian argue for an Eocene aggradational system associated with uniform subsidence. -
Paleoclimate Variations and Impact on Groundwater
Paleoclimate variations and impact on groundwater recharge in multi-layer aquifer systems using a multi-tracer approach (northern Aquitaine basin, France) Marc Saltel, Romain Rebeix, Bertrand Thomas, Michel Franceschi, Bernard Lavielle, Pascal Bertran To cite this version: Marc Saltel, Romain Rebeix, Bertrand Thomas, Michel Franceschi, Bernard Lavielle, et al.. Paleo- climate variations and impact on groundwater recharge in multi-layer aquifer systems using a multi- tracer approach (northern Aquitaine basin, France). Hydrogeology Journal, 2019, 27, pp.1439-1457. 10.1007/s10040-019-01944-x. hal-02154742 HAL Id: hal-02154742 https://hal.archives-ouvertes.fr/hal-02154742 Submitted on 21 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| 4.0 International License Paleoclimate variations and impact on groundwater recharge in multi-layer aquifer systems using a multi-tracer approach (northern Aquitaine basin, France) Marc Saltel1 & Romain Rebeix2,3 & Bertrand Thomas2,3 & Michel Franceschi4,5 & Bernard Lavielle2,3 & Pascal Bertran6,7 Abstract The northern Aquitaine basin (southwest France) is a large multi-layer aquifer system that contains groundwater with strong residence-time variability ranging from years to tens of thousands of years. -
A Review of the Late Jurassic–Early Cretaceous Charophytes from The
A review of the Late Jurassic–Early Cretaceous charophytes from the northern Aquitaine Basin in south-west France Roch-Alexandre Benoit, Didier Néraudeau, Carles Martin-Closas To cite this version: Roch-Alexandre Benoit, Didier Néraudeau, Carles Martin-Closas. A review of the Late Jurassic– Early Cretaceous charophytes from the northern Aquitaine Basin in south-west France. Cretaceous Research, Elsevier, 2017, 79, pp.199-213. <10.1016/j.cretres.2017.07.009>. <insu-01574653> HAL Id: insu-01574653 https://hal-insu.archives-ouvertes.fr/insu-01574653 Submitted on 16 Aug 2017 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. Accepted Manuscript A review of the Late Jurassic–Early Cretaceous charophytes from the northern Aquitaine Basin in south-west France Roch-Alexandre Benoit, Didier Neraudeau, Carles Martín-Closas PII: S0195-6671(17)30121-0 DOI: 10.1016/j.cretres.2017.07.009 Reference: YCRES 3658 To appear in: Cretaceous Research Received Date: 13 March 2017 Revised Date: 5 July 2017 Accepted Date: 17 July 2017 Please cite this article as: Benoit, R.-A., Neraudeau, D., Martín-Closas, C., A review of the Late Jurassic–Early Cretaceous charophytes from the northern Aquitaine Basin in south-west France, Cretaceous Research (2017), doi: 10.1016/j.cretres.2017.07.009. -
Brittle Tectonics and Fluids Overpressure During the Early
Brittle tectonics and fluids overpressure during the early stage of the Bay of Biscay opening in the Jard-sur-Mer area, (northern Aquitaine Basin, France) Pierre Strzerzynski, Louise Lenoir, Paul Bessin, Loic Bouat To cite this version: Pierre Strzerzynski, Louise Lenoir, Paul Bessin, Loic Bouat. Brittle tectonics and fluids overpressure during the early stage of the Bay of Biscay opening in the Jard-sur-Mer area, (northern Aquitaine Basin, France). Bulletin de la Société Géologique de France, Société géologique de France, 2020, 191, 10.1051/bsgf/2020025. insu-03231747 HAL Id: insu-03231747 https://hal-insu.archives-ouvertes.fr/insu-03231747 Submitted on 21 May 2021 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| 4.0 International License BSGF - Earth Sciences Bulletin 2020, 191, 38 © P. Strzerzynski et al., Published by EDP Sciences 2020 https://doi.org/10.1051/bsgf/2020025 Available online at: www.bsgf.fr Brittle tectonics and fluids overpressure during the early stage of the Bay of Biscay opening in the Jard-sur-Mer area, (northern Aquitaine Basin, France) Pierre Strzerzynski1,*, Louise Lenoir2, Paul Bessin1 and Loic Bouat1 1 Laboratoire de Planétologie et Géodynamique, UMR 6112, CNRS, Le Mans Université, Avenue Olivier Messiaen, 72085 Le Mans Cedex 9, France 2 UMR CNRS/UPS Géosciences Paris Sud (GEOPS), Bât. -
Estimating the Ultimate Recoverable Reserves of the Paris Basin, France
Oil & Gas Science and Technology – Rev. IFP, Vol. 57 (2002), No. 6, pp. 621-629 Copyright © 2002, Éditions Technip Estimating the Ultimate Recoverable Reserves of the Paris Basin, France J. Wendebourg1 and C. Lamiraux2 1 Institut français du pétrole, 1 et 4, avenue de Bois-Préau, 92852 Rueil-Malmaison Cedex - France 2 Direction générale de l’énergie et des matière premières (DGEMP), 41, boulevard Vincent Auriol, 75703 Paris Cedex 13 - France e-mail: [email protected] Résumé — Estimation des réserves ultimes récupérables du Bassin parisien, France — Le Bassin parisien est un bassin mature en exploration pétrolière. Pas moins de 800 puits exploratoires ont été forés pendant les 40 dernières années et 52 champs de pétrole ont été découverts : 33,4 Mt de pétrole ont été produits jusqu’en 2000. Le potentiel du Bassin parisien est estimé à l’aide de méthodes statistiques. La taille moyenne d’un champ est de 100 000 t avec une probabilité de 5 % de trouver un champ de plus de 2,5 Mt. Les réserves ultimes récupérables étaient de 15 Mt en 1986, 29 Mt en 1991 et 46 Mt en 1996. Aujourd’hui, il y a une probabilité de 5 % de trouver un champ de plus de 4 Mt dans les grès du Dogger ou du Keuper. Le taux de succès augmente de 1/66 dans la formation du Néocomien, le réservoir le moins profond, à 1/8 dans le Keuper, le réservoir le plus profond et le plus récemment foré. L’analyse présentée s’appuie sur des données de production et ne prend pas en compte une production supplémentaire éventuelle grâce à des méthodes de récupération assistée ou grâce à des découvertes basées sur de nouveaux concepts d’exploration, susceptibles d’augmenter les réserves de façon significative, bien au-delà des chiffres présentés comme cela est démontré par l’analyse de la courbe crémière. -
Originally Published As
Originally published as: Schintgen, T. V., Förster, A. (2013): Geology and basin structure of the Trier-Luxembourg Basin - implications for the existence of a buried Rotliegend graben. - Zeitschrift der Deutschen Gesellschaft für Geowissenschaften, 164, 4, p. 615-637(23). DOI: http://doi.org/10.1127/1860-1804/2013/0025 Geology and basin structure of the Trier–Luxembourg Basin – implications for the existence of a buried Rotliegend graben Tom Schintgen, Andrea Förster Published in: Z. Dt. Ges. Geowiss. 164 (4), 615–637. http://dx.doi.org/10.1127/1860-1804/2013/0025 Geology and basin structure of the Trier–Luxembourg Basin Abstract This paper presents the geology of the TrierLuxembourg Basin (TLB) in a comprehensive and updated manner. It describes the structural and lithological features of the basin, which comprises sediments of Permian to Mesozoic age. The regional geological assessment profited from recently published information on the geology and regional tectonics, as well as from borehole data from Luxembourg and adjoining areas in France, Belgium and Germany. The paper specifically focuses on the location of major synsedimentary faults and weakness zones, which gave rise to a new conceptual model of basin structure and evolution. The total depth of the basin as well as the thickness estimates of the fault-controlled subunits are supported by the interpretation of a Bouguer gravity map. In addition, the stratigraphy of the Cessange borehole and the depositional conditions of the Luxembourg Sandstone have been reinterpreted in accordance with the new concept. Supported by numerous geological cross sections it is suggested that the TLB has developed along a SW–NE trending weakness zone above a Permian Graben in direct prolongation of the Wittlicher Senke. -
75 Proc. 7Th NZ Geothermal Workshop 1985 JEAN-MICHEL COUDERT
75 Proc. 7th NZ Geothermal Workshop 1985 REINJECTION: A FRENCH APPROACH JEAN-MICHEL COUDERT Gkothermal Public Service, BRGN, BP 6009, 45060 Orleans Cedex, France. The' Paris Basin ABSTRACT This large sedimentary basin, 3 km deep under the Brie, extends a5 far as England. It is distin- This paper gives a brief introduction to the guished by calm tectonics, with the geological geothermal resources of France. These are all of beds arranged regularly like a stack of plates, the low temperature (T < 100°C) type, initially and by the considerable development of porous identified in the sedimentary basins by petroleum formations. Hence the resource displays a exploration. "continuous" character. The geothermal "doublet" reinjection technique is The main aquifers appearing in the section (Fig. described. More than 40 doublets have been - 2) are designated by their standard geological drilled and are exploited in the Paris Basin. name. These geothermal developments have taken place only during the past 6 years, and so far no major A well drilled at the centre of the basin will problems have occurred. Mathematical modelling encounter the following sequence: has been carried out, and computer programs developed. Albian and Neocomian sands: the water is fresh and the temperature about 30°C under the Paris urban area. These aquifers are tapped for air- conditioning of buildings (the Albian for the Introduction National Radio Agency in 1956 and the Neocomian at Bruysres-le-Chhtel, south of Paris, in 1980). In 1973 France was importing 80% of its energy. Very stringent legislation now protects the Albian Among major occidental countries only Japan and aquifer, which was over-used at the turn of the Italy were more dependent on energy imports.