Young Tectonic Evolution of the Northern Alpine Foreland Basin

Total Page:16

File Type:pdf, Size:1020Kb

Young Tectonic Evolution of the Northern Alpine Foreland Basin Dissertation zur Erlangung des Doktorgrades der Naturwissenschaften an der Fakultät für Geowissenschaften der Ludwig-Maximilians-Universität München Young tectonic evolution of the Northern Alpine Foreland Basin, southern Germany, based on linking geomorphology and structural geology Markus Hoffmann München, 15. März 2017 II 1. Gutachterin: Prof. Dr. Anke M. Friedrich 2. Gutachterin: Prof. Dr. Miriam Dühnforth Tag der mündlichen Prüfung: 24. Juli 2017 III IV Für Horst† und Irene V VI Brick walls are there for a reason. The brick walls are not there to keep us out, they let us prove how badly we want something. (Randy Pausch, 2012) VII VIII TABLE OF CONTENTS ABSTRACT ................................................................................................................................. 1 ZUSAMMENFASSUNG ............................................................................................................. 3 ACKNOWLEDGEMENTS ........................................................................................................ 7 DANKSAGUNG .......................................................................................................................... 8 CHAPTER 1 .............................................................................................................................. 11 INTRODUCTION ........................................................................................................................ 11 1. History of basin discovery and exploration ................................................................. 16 2. Dynamic landscapes .................................................................................................... 18 3. Paleo-coastal research and topography ....................................................................... 21 4. General remark ............................................................................................................ 23 5. References ................................................................................................................... 24 CHAPTER 2 .............................................................................................................................. 29 MORPHOTECTONIC ANALYSIS OF THE ASYMMETRIC TERTIARY HILLS AND POSSIBLE CONNECTION TO BASEMENT FAULTS – NORTHERN ALPINE FORELAND BASIN, GERMANY ... 29 1. Abstract ....................................................................................................................... 29 2. Introduction ................................................................................................................. 30 3.1. Surface morphology and study site setting .......................................................... 36 3.2. Regional fault data ............................................................................................... 37 4. Methods ....................................................................................................................... 38 4.1. Geomorphic mapping ........................................................................................... 38 4.2. Shallow coring ..................................................................................................... 39 4.3. Resistivity tomography ........................................................................................ 39 4.4. Geologic field mapping ........................................................................................ 40 5. Results ......................................................................................................................... 43 5.1. Study site Paindlkofen ......................................................................................... 43 5.1.1. Geomorphic analysis ......................................................................................... 43 5.1.2. Coring................................................................................................................ 45 5.1.3. Resistivity Tomography .................................................................................... 47 5.2. Study site Tunzenberg .......................................................................................... 50 5.2.1. Geomorphic analysis ......................................................................................... 50 5.2.2. Geologic field mapping ..................................................................................... 50 6. Interpretation ............................................................................................................... 52 7. Discussion ................................................................................................................... 54 7.1. Composite climatic landscape (Fig. 2.12): ........................................................... 57 IX 7.2. Composite tectonic landscape (Fig. 2.13): ........................................................... 57 8. Conclusions ................................................................................................................. 62 9. Acknowledgements ..................................................................................................... 62 10. References ................................................................................................................. 63 11. Appendix ................................................................................................................... 66 CHAPTER 3 .............................................................................................................................. 67 EROSIONAL AND TECTONIC OVERPRINT OF THE MID-MIOCENE MARINE CLIFF LINE AND ITS APPLICABILITY AS A PALEO-GEODETIC MARKER OF REGIONAL-SCALE TILTING, SWABIAN ALB, SOUTHWESTERN GERMANY ............................................................................................ 67 1. Abstract ....................................................................................................................... 67 2. Introduction ................................................................................................................. 68 2.1. History of ancient rocky shore research ............................................................... 68 3. Regional Background and Stratigraphic Setting ......................................................... 75 3.1. Fault Systems and Seismotectonics ..................................................................... 77 3.2. The mid-Miocene coast ........................................................................................ 78 3.3. The Heldenfingen study site (A) .......................................................................... 79 3.4. The Burgmagerbein study site (B) ....................................................................... 80 4. Methods ....................................................................................................................... 82 4.1. Geomorphic mapping ........................................................................................... 82 4.2. Field mapping and analysis of bio-erosion features ............................................. 82 4.3. Estimating local surface uplift ............................................................................. 83 4.4. Onlap and facies analysis ..................................................................................... 84 5. Results ......................................................................................................................... 85 5.1. Site Heldenfingen (A) .......................................................................................... 85 5.1.1. Geomorphology ................................................................................................ 85 5.1.2. Coastal features ................................................................................................. 87 5.2. Site Burgmagerbein (B) ....................................................................................... 87 5.2.1. Geomorphology ................................................................................................ 87 5.2.2. Coastal features ................................................................................................. 88 5.3. Uplift estimates for the sites Heldenfingen and Burgmagerbein ......................... 91 5.4. Sequence stratigraphic analysis............................................................................ 94 6. Interpretation ............................................................................................................... 98 7. Discussion ................................................................................................................. 101 7.1. Evolution of the coastal region along the northern margin of the NAFB .......... 101 8. Conclusions ............................................................................................................... 109 9. References ................................................................................................................. 110 X CHAPTER 4 ............................................................................................................................ 117 QUATERNARY TECTONIC ACTIVITY OF THE NORTHERN ALPINE FORELAND BASIN - ANALYSIS OF EROSION PATTERNS AND GEOMORPHIC MARKERS .......................................... 117 1. Abstract ..................................................................................................................... 117 2. Introduction
Recommended publications
  • 9 Rhein Traverse Wolfgang Schirmer
    475 INQUA 1995 Quaternary field trips in Central Europe Wolfgang Schirmer (ed.) 9 Rhein Traverse Wolfgang Schirmer with contributions by H. Berendsen, R. Bersezio, A. Bini, F. Bittmann, G. Crosta, W. de Gans, T. de Groot, D. Ellwanger, H. Graf, A. Ikinger, O. Keller, U. Schirmer, M. W. van den Berg, G. Waldmann, L. Wick 9. Rhein Traverse, W. Schirmer. — In: W. Schirmer (ed.): Quaternary field trips hl Central Europe, vo1.1, p. 475-558 ©1995 by Verlag Dr. Friedrich Pfeil, Munchen, Germany ISBN 3-923871-91-0 (complete edition) —ISBN 3-923871-92-9 (volume 1) 476 external border of maximum glaciation Fig.1 All Stops (1 61) of excursion 9. Larger setting in Fig. 2. Detailed maps Figs. 8 and 48 marked as insets 477 Contents Foreword 479 The headwaters of the Rhein 497 Introductory survey to the Rhein traverse Stop 9: Via Mala 498 (W. ScI-~uvtER) 480 Stop 10: Zillis. Romanesque church 1. Brief earth history of the excursion area 480 of St. Martin 499 2. History of the Rhein catchment 485 The Flims-Tamins rockslide area 3. History of valley-shaping in the uplands 486 (W. SCHIItMER) 499 4. Alpine and Northern glaciation 486 Stop 11: Domat/Ems. Panoramic view of the rockslide area 500 5. Shape of the Rhein course 486 Stop 12: Gravel pit of the `Kieswerk Po plain and Southern Alps Reichenau, Calanda Beton AG' 500 (R. BERSEZIO) 488 Stop 13: Ruinaulta, the Vorderrhein gorge The Po plain subsurface 488 piercing the Flims rockslide 501 The Southern Alps 488 Retreat Stades of the Würmian glaciation The Periadriatic Lineament (O.
    [Show full text]
  • Geologic Storage Formation Classification: Understanding Its Importance and Impacts on CCS Opportunities in the United States
    BEST PRACTICES for: Geologic Storage Formation Classification: Understanding Its Importance and Impacts on CCS Opportunities in the United States First Edition Disclaimer This report was prepared as an account of work sponsored by an agency of the United States Government. Neither the United States Government nor any agency thereof, nor any of their employees, makes any warranty, express or implied, or assumes any legal liability or responsibility for the accuracy, completeness, or usefulness of any information, apparatus, product, or process disclosed, or represents that its use would not infringe privately owned rights. Reference therein to any specific commercial product, process, or service by trade name, trademark, manufacturer, or otherwise does not necessarily constitute or imply its endorsement, recommendation, or favoring by the United States Government or any agency thereof. The views and opinions of authors expressed therein do not necessarily state or reflect those of the United States Government or any agency thereof. Cover Photos—Credits for images shown on the cover are noted with the corresponding figures within this document. Geologic Storage Formation Classification: Understanding Its Importance and Impacts on CCS Opportunities in the United States September 2010 National Energy Technology Laboratory www.netl.doe.gov DOE/NETL-2010/1420 Table of Contents Table of Contents 5 Table of Contents Executive Summary ____________________________________________________________________________ 10 1.0 Introduction and Background
    [Show full text]
  • Goalscorers Bärencup 2017 (Vorrunde)
    Bärencup 2017 (Vorrunde) No. 1, Gr. A Bärencup 2017 (Vorrunde) No. 2, Gr. A 09.07. 09:00 09.07. 09:00 TSV Grafing I : ASV Glonn ATSV Kirchseeon : TSV Poing II Goalscorers Goalscorers Made with passion by tournej Made with passion by tournej Bärencup 2017 (Vorrunde) No. 3, Gr. A Bärencup 2017 (Vorrunde) No. 4, Gr. A 09.07. 09:19 09.07. 09:19 SpVgg Markt : SV Anzing SV Bruck : TSV Grafing I Schwabener Au Goalscorers Goalscorers Made with passion by tournej Made with passion by tournej Bärencup 2017 (Vorrunde) No. 5, Gr. A Bärencup 2017 (Vorrunde) No. 6, Gr. A 09.07. 09:38 09.07. 09:38 SpVgg Markt ASV Glonn : ATSV Kirchseeon TSV Poing II : Schwabener Au Goalscorers Goalscorers Made with passion by tournej Made with passion by tournej Bärencup 2017 (Vorrunde) No. 7, Gr. A Bärencup 2017 (Vorrunde) No. 8, Gr. A 09.07. 09:57 09.07. 09:57 SV Anzing : SV Bruck TSV Grafing I : ATSV Kirchseeon Goalscorers Goalscorers Made with passion by tournej Made with passion by tournej Bärencup 2017 (Vorrunde) No. 9, Gr. A Bärencup 2017 (Vorrunde) No. 10, Gr. A 09.07. 10:16 09.07. 10:16 SpVgg Markt : ASV Glonn SV Bruck : TSV Poing II Schwabener Au Goalscorers Goalscorers Made with passion by tournej Made with passion by tournej Made with passion by tournej Bärencup 2017 (Vorrunde) No. 11, Gr. A Bärencup 2017 (Vorrunde) No. 12, Gr. A 09.07. 10:35 09.07. 10:35 SpVgg Markt SV Anzing : TSV Grafing I ATSV Kirchseeon : Schwabener Au Goalscorers Goalscorers Made with passion by tournej Made with passion by tournej Bärencup 2017 (Vorrunde) No.
    [Show full text]
  • Wohnberechtigungsschein 1 2 1 2 3 1 1 1 1 - 1 1 2 1 1 2 2 1 1 2 - 1 2
    Landratsamt Miesbach – Fachbereich Gesundheit, Betreuung und Senioren – Altenhilfeplanung Stand 31.12.2016 Gemeinde Bad Bayrischzell Fischbachau Gmund Hausham Holzkirchen Irschenberg Kreuth Miesbach Otterfing Rottach- Schliersee Tegernsee Valley Waakirchen Warngau Weyarn Wiessee Egern Wohnberechtigungsschein 1 2 1 2 3 1 1 1 1 - 1 1 2 1 1 2 2 1 1 2 - 1 2 Wohngeldantrag 1 2 1 2 3 1 1 2 1 - 1 1 2 1 1 2 1 1 1 2 1 3 1 2 Rentenantrag 3 1 2 3 - 1 2 - 1 3 1 1 2 2 3 - 2 1 1 2 1 2 Sozialversicherungsangelegenheiten 3 1 2 3 1 1 2 - 1 3 1 1 2 2 3 - - 1 1 - 1 2 Vertriebenenangelegenheiten - - - - 2 - - - 1 2 - - - - - - - - Pflegegeld - 1 2 3 - - - - - - - - - - - 1 - - - Sozialhilfe-/Grundsicherungsantrag 3 1 2 3 1 1 2 1 - 1 1 2 1 1 2 1 1 1 1 1 3 1 2 Antrag auf Übernahme ungedeckter 3 - 1 - 2 1 - 1 1 2 1 - 1 - 1 - - - Heimkosten Heizungsbeihilfe - 1 2 3 1 1 2 1 - 1 1 2 1 - 1 - 1 - 1 3 - Rundfunkgebührenbefreiung 1 2 1 2 3 1 1 2 1 1 2 3 1 1 2 1 1 2 1 1 1 1 1 3 1 2 Antrag auf Feststellung des Grades 3 1 2 3 1 1 2 1 2 1 2 3 1 1 2 - 1 2 1 1 1 1 1 3 1 2 der Behinderung Schwerbehindertenparkausweis 3 1 2 3 1 2 2 1 1 2 3 1 1 2 1 4 1 3 1 3 1 3 3 Holzkirchenkarte 1 Ansprechpartner der Gemeinde-/Stadt-/Marktverwaltung im Bereich Soziales im Alter S e i t e | 1 Landratsamt Miesbach – Fachbereich Gesundheit, Betreuung und Senioren – Altenhilfeplanung Stand 31.12.2016 Bad Wiessee 1 Karen Lange 08022/8602-23 [email protected] Otterfing 1 Wachinger Kornelia 08024/2063-113 [email protected] 2 Edo Memic 08022/8602-46 [email protected] 2 Eder
    [Show full text]
  • Understanding Mediterranean Tectonics to Recognise Earthquake-Prone Zones
    Understanding Mediterranean Tectonics to Recognise Earthquake-prone Zones Professor Enzo Mantovani UNDERSTANDING MEDITERRANEAN TECTONICS TO RECOGNISE EARTHQUAKE-PRONE ZONES Precisely predicting when earthquakes will happen is still a distant goal. However, local authorities could reduce the damage caused by such disasters if scientists could identify zones that are most likely to be affected by earthquakes. Gaining this information requires an in-depth knowledge of the ongoing tectonic situation in a given area. In the Mediterranean region, this knowledge is surrounded by considerable uncertainty, as different researchers have different hypotheses to explain tectonic processes in this area. Professor Enzo Mantovani and his team at the University of Siena, Italy, propose a new geodynamic interpretation that offers a plausible explanation for all major tectonic features observed in this area. Using their hypothesis, along with the seismic history of the region, the team has recognised a connection between the short-term development of tectonic processes and the distribution of major earthquakes. Tectonic Evolution of the and Eurasian plates. However, Mediterranean since convergence mostly produces ‘compressional’ deformations, causing Over the last 30 million years, the the Earth’s crust to become thicker and tectonic and morphological situation mountains to form, some researchers in the Mediterranean region has propose that other driving forces undergone profound change. In this caused the formation of basins in the area, elongated regions of deformation Mediterranean. where the African and Eurasian tectonic plates converge – called ‘orogenic The most frequently cited hypothesis belts’ – migrated by distances of several assumes that basin formation is hundreds of kilometres and some also driven by the gravitational sinking of underwent strong distortions.
    [Show full text]
  • Directions By
    HOW TO GET TO LTN SERVOTECHNIK GMBH © cevahir87 / fotolia © andylimberger / fotolia HOW TO GET TO LTN HOW TO GET TO LTN BY CAR FROM THE NORTH/WEST BY CAR FROM THE EAST/SOUTH From Munich or the motorway ring road A99 or A995 take the A8 From Rosenheim take the A8 and drive in the direction of Nurem- driving in the direction of Salzburg / Austria / Italy / Innsbruck. berg / Stuttgart / Munich. Take exit 96 Hofolding / Aying / Dietramszell / Sauerlach. Take exit 97 Holzkirchen / Tegernsee / Bad Wiessee. After you have taken the exit, turn right at the set of first traffic After you have taken the exit turn right and then left onto the lights and drive towards Sauerlach until you reach Tegernseer main road. Then on the roundabout take the first exit and at the Landstraße B 13. Turn left onto Tegernseer Landstraße B 13 and second roundabout take the first exit again and continue until you drive towards Otterfing. Take the third exit at the roundabout reach Otterfing. Take the first exit at the roundabout (Hienlohe- (Hienlohestraße), then turn right onto Lehrer-Holl-Straße. straße), then turn right onto Lehrer-Holl-Straße. The LTN building will be on your left. The LTN building will be on your left. You will find the visitor’s entrance on Ludwig-Ganghofer-Straße. You will find the visitor’s entrance on Ludwig-Ganghofer-Straße. The delivery entrance is located on Georg-Hardt-Straße. The delivery entrance is located on Georg-Hardt-Straße. LTN SERVOTECHNIK GMBH Georg-Hardt-Strasse 4 83624 Otterfing, Germany T +49 8024 6080-0 [email protected] www.ltn-servotechnik.com.
    [Show full text]
  • Perspectives Annual Report 2012 Perspectives
    Perspectives Annual Report 2012 Perspectives We are an airport operator. We run a major piece of aviation infrastructure – part of an international, interconnected transport network that sustains global mobility and unites people across national boundaries. We are also a responsible corporate citizen who seeks an open, fair and balanced dialogue with stake holders and inter- est groups and for whom the long-term protection of the environment, climate and natural resources is paramount. As such, we pursue a forward-looking business strategy intended to strike a successful balance between business, environmental and social objectives. We provide our dedicated workforce with the training and continuing education they need to be their best; we offer attractive, long-term employment; and we deliver valuable economic and labor-market stimulus with a reach far beyond the bounds of our airport. Our goal: to create value – for our customers, employees, owners and host region. Markets As a hub, Munich Airport plays an important role for German and international aviation. We meet the needs of our varied customers with a comprehen- sive range of services and products. In the avia- tion segment, we handle the air traffic – including passenger services and all air-side and land-side services concerning aircraft handling. With Retail and Hospitality, as well as the Consumer Activities and Real Estate divisions, we also provide a broad portfolio of products and services in the non-avia- tion segment. Both markets make an almost bal- anced contribution to our consolidated revenue. Our corporate policy is systematically aligned toward sustainability. The quality and variety of our ser vices make us one of the most attractive airports in the world.
    [Show full text]
  • Geomorphological Studies of the Sedimentary Cuddapah Basin, Andhra Pradesh, South India
    SSRG International Journal of Geoinformatics and Geological Science (SSRG-IJGGS) – Volume 7 Issue 2 – May – Aug 2020 Geomorphological studies of the Sedimentary Cuddapah Basin, Andhra Pradesh, South India Maheswararao. R1, Srinivasa Gowd. S1*, Harish Vijay. G1, Krupavathi. C1, Pradeep Kumar. B1 Dept. of Geology, Yogi Vemana University, Kadapa-516005, Andhra Pradesh, India Abstract: The crescent shaped Cuddapah basin located Annamalai Surface - at an altitude of over 8000’ (2424 mainly in the southern part of Andhra Pradesh and a m), ii. Ootacamund Surface – at 6500’-7500’ (1969- little in the Telangana State is one of the Purana 2272 m) on the west and at 3500’ (1060m) on the east basins. Extensive work was carried out on the as noticed in Tirumala hills, iii. Karnataka Surface - stratigraphy of the basin, but there is very little 2700’-3000’ (Vaidynathan, 1964). 2700-3300 reference (Vaidynathan,1964) on the geomorphology of (Subramanian, 1973) 2400-3000 (Radhakrishna, 1976), the basin. Hence, an attempt is made to present the iv. Hyderabad Surface – at 1600’ – 2000’v. Coastal geomorphology of the unique basin. The Major Surface – well developed east of the basin.vi. Fossil Geomorphic units correspond to geological units. The surface: The unconformity between the sediments of the important Physiographic units of the Cuddapah basin Cuddapah basin and the granitic basement is similar to are Palakonda hill range, Seshachalam hill range, ‘Fossil Surface’. Gandikota hill range, Velikonda hill range, Nagari hills, Pullampet valley and Kundair valley. In the Cuddapah Basin there are two major river systems Key words: Topography, Land forms, Denudational, namely, the Penna river system and the Krishna river Pediment zone, Fluvial.
    [Show full text]
  • Geological Excursion BASE-Line Earth
    Geological Excursion BASE-LiNE Earth (Graz Paleozoic, Geopark Karavanke, Austria) 7.6. – 9.6. 2016 Route: 1. Day: Graz Paleozoic in the vicinity of Graz. Devonian Limestone with brachiopods. Bus transfer to Bad Eisenkappel. 2. Day: Visit of Geopark Center in Bad Eisenkappel. Walk on Hochobir (2.139 m) – Triassic carbonates. 3. Day: Bus transfer to Mezica (Slo) – visit of lead and zinc mine (Triassic carbonates). Transfer back to Graz. CONTENT Route: ................................................................................................................................... 1 Graz Paleozoic ...................................................................................................................... 2 Mesozoic of Northern Karavanke .......................................................................................... 6 Linking geology between the Geoparks Carnic and Karavanke Alps across the Periadriatic Line ....................................................................................................................................... 9 I: Introduction ..................................................................................................................... 9 II. Tectonic subdivision and correlation .............................................................................10 Geodynamic evolution ...................................................................................................16 Alpine history in eight steps ...........................................................................................17
    [Show full text]
  • LP NVK Anhang (PDF, 7.39
    Landschaftsplan 2030 Nachbarschaftsverband Karlsruhe 30.11.2019 ANHANG HHP HAGE+HOPPENSTEDT PARTNER INHALT 1 ANHANG ZU KAP. 2.1 – DER RAUM ........................................................... 1 1.1 Schutzgebiete ................................................................................................................. 1 1.1.1 Naturschutzgebiete ................................................................................... 1 1.1.2 Landschaftsschutzgebiete ........................................................................ 2 1.1.3 Wasserschutzgebiete .................................................................................. 4 1.1.4 Überschwemmungsgebiete ...................................................................... 5 1.1.5 Waldschutzgebiete ...................................................................................... 5 1.1.6 Naturdenkmale – Einzelgebilde ................................................................ 6 1.1.7 Flächenhaftes Naturdenkmal .................................................................... 10 1.1.8 Schutzgebiete NATURA 2000 .................................................................... 11 1.1.8.1 FFH – Gebiete 11 1.1.8.2 Vogelschutzgebiete (SPA-Gebiete) 12 2 ANHANG ZU KAP. 2.2 – GESUNDHEIT UND WOHLBEFINDEN DER MENSCHEN ..................... 13 3 ANHANG ZU KAP. 2.4 - LANDSCHAFT ..................................................... 16 3.1 Landschaftsbeurteilung ...............................................................................................
    [Show full text]
  • Characterization of a Deep Fault Zone in Upper Jurassic Carbonates of the Northern Alpine Foreland Basin for Geothermal Production (South Germany)
    PROCEEDINGS, 43rd Workshop on Geothermal Reservoir Engineering Stanford University, Stanford, California, February 12-14, 2018 SGP-TR-213 Characterization of a Deep Fault Zone in Upper Jurassic Carbonates of the Northern Alpine Foreland Basin for Geothermal Production (South Germany) Michael Dussel1, Inga Moeck1,2, Markus Wolfgramm3, Robert Straubinger4 1Leibniz Institute for Applied Geophysics (LIAG), Section Geothermics and Information Systems, Hannover, Germany 2Georg-August-Universität Göttingen, Department of Applied Geology, Göttingen, Germany 3Geothermie Neubrandenburg GmbH (GTN), Neubrandenburg, Germany 4Enex Power Germany GmbH (Enex), Kirchseeon, Germany [email protected] Keywords: fault intersection, permeability structure, 3D seismic interpretation, Y-shaped grabens, fractured carbonate cores, geothermal play type ABSTRACT The fractured and karstified Upper Jurassic carbonates of the South German Molasse Basin, the northern foreland basin of the European Alps, constitute the most important reservoir for deep geothermal energy use in Germany. Over the last 15 years more than 20 deep geothermal heating facilities and power plants were successfully installed. Currently, new wells are drilled deeper and nearer closer to the frontal fault of the Alpine fold belt. The new targets are associated with challenging drilling and detailed target determination like damage zones and intersection of faults of Y-shaped graben structures. One of the wells into the deep basin is the well GEN-1ST, drilled into 4.7 km deep dolomitic carbonates. An intensive research program was carried out to determine the permeability structure across the drilled fault zone including vertical seismic profiling, core drilling and logging. 1. INTRODUCTION The Bavarian Molasse Basin in South Germany is the most important region for the use of deep geothermal energy in Germany.
    [Show full text]
  • Gemeinde Pastetten Landkreis Erding
    Planungsverband Äußerer Wirtschaftsraum München GEMEINDEDATEN PV Gemeinde Pastetten Landkreis Erding Gemeindedaten Ausführliche Datengrundlagen 2017 www.pv-muenchen.de Impressum Herausgeber Planungsverband Äußerer Wirtschaftsraum München (PV) v.i.S.d.P. Geschäftsführer Christian Breu Arnulfstraße 60, 3. OG, 80335 München Telefon +49 (0)89 53 98 02-0 Telefax +49 (0)89 53 28 389 [email protected] www.pv-muenchen.de Redaktion: Christian Breu, Daniel Gromotka, Brigitta Walter, Annette Wild Satz und Layout: Brigitta Walter Statistische Auswertungen: Brigitta Walter Kontakt: Brigitta Walter, Tel. +49 (0)89 53 98 02-13, Mail: [email protected] Quellen Grundlage der Gemeindedaten sind die amtlichen Statistiken des Bayerischen Landesamtes für Statistik und der Ar beitsagentur Nürnberg. Aufbereitung und Darstellung durch den Planungsverband Äußerer Wirtschaftsraum München (PV). Titelbild: Foliage_539413_1920_claude05alleva, Pixabay Hinweis Alle Angaben wurden sorgfältig zusammengestellt; für die Richtigkeit kann jedoch keine Haftung übernommen werden. In der vorliegenden Publikation werden für alle personenbezogenen Begriffe die Formen des grammatischen Geschlechts ver- wendet. Der Planungsverband Äußerer Wirtschaftsraum München (PV) wurde 1950 als kommunaler Zweckverband gegründet. Er ist ein freiwilliger Zusammenschluss von rund 150 Städten, Märkten und Gemeinden, acht Landkreisen und der Landeshauptstadt München. Der PV vertritt kommunale Interessen und engagiert sich für die Zusammenarbeit seiner Mitglieder sowie für eine zukunftsfähige
    [Show full text]