The Eastern Alps: Result of a Two-Stage Collision Process
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The Structure of the Alps: an Overview 1 Institut Fiir Geologie Und Paläontologie, Hellbrunnerstr. 34, A-5020 Salzburg, Austria
Carpathian-Balkan Geological pp. 7-24 Salzburg Association, XVI Con ress Wien, 1998 The structure of the Alps: an overview F. Neubauer Genser Handler and W. Kurz \ J. 1, R. 1 2 1 Institut fiir Geologie und Paläontologie, Hellbrunnerstr. 34, A-5020 Salzburg, Austria. 2 Institut fiir Geologie und Paläontologie, Heinrichstr. 26, A-80 10 Graz, Austria Abstract New data on the present structure and the Late Paleozoic to Recent geological evolution ofthe Eastem Alps are reviewed mainly in respect to the distribution of Alpidic, Cretaceous and Tertiary, metamorphic overprints and the corresponding structure. Following these data, the Alps as a whole, and the Eastem Alps in particular, are the result of two independent Alpidic collisional orogens: The Cretaceous orogeny fo rmed the present Austroalpine units sensu lato (including from fo otwall to hangingwall the Austroalpine s. str. unit, the Meliata-Hallstatt units, and the Upper Juvavic units), the Eocene-Oligocene orogeny resulted from continent continent collision and overriding of the stable European continental lithosphere by the Austroalpine continental microplate. Consequently, a fundamental difference in present-day structure of the Eastem and Centrai/Westem Alps resulted. Exhumation of metamorphic crust fo rmed during Cretaceous and Tertiary orogenies resulted from several processes including subvertical extrusion due to lithospheric indentation, tectonic unroofing and erosional denudation. Original paleogeographic relationships were destroyed and veiled by late Cretaceous sinistral shear, and Oligocene-Miocene sinistral wrenching within Austroalpine units, and subsequent eastward lateral escape of units exposed within the centrat axis of the Alps along the Periadriatic fault system due to the indentation ofthe rigid Southalpine indenter. -
Present-Day Uplift of the European Alps Evaluating Mechanisms And
Earth-Science Reviews 190 (2019) 589–604 Contents lists available at ScienceDirect Earth-Science Reviews journal homepage: www.elsevier.com/locate/earscirev Invited review Present-day uplift of the European Alps: Evaluating mechanisms and models T of their relative contributions ⁎ Pietro Sternaia, ,1, Christian Sueb, Laurent Hussonc, Enrico Serpellonid, Thorsten W. Beckere, Sean D. Willettf, Claudio Faccennag, Andrea Di Giulioh, Giorgio Spadai, Laurent Jolivetj, Pierre Vallac,k, Carole Petitl, Jean-Mathieu Nocquetm, Andrea Walpersdorfc, Sébastien Castelltorta a Département de Sciences de la Terre, Université de Genève, Geneva, Switzerland b Chrono-Environnement, CNRS, Université de Bourgogne Franche-Comté, Besançon, France c Université Grenoble Alpes, CNRS, IRD, IFSTAR, ISTERRE, Université Savoie Mont Blanc, Grenoble 38000, France d Istituto Nazionale di Geofisica e Vulcanologia, Centro Nazionale Terremoti, Bologna, Italy e Institute for Geophysics, Department of Geological Sciences, Jackson School of Geosciences, The University Texas at Austin, Austin, TX, USA f Erdwissenschaften, Eidgenössische Technische Hochschule Zürich (ETH), Zurich, Switzerland g Dipartimento di Scienze, Università di Roma III, Rome, Italy h Dipartimento di Scienze della Terra e dell'Ambiente, Università di Pavia, Pavia, Italy i Università degli Studi di Urbino “Carlo Bo”, Urbino, Italy j Sorbonne Université, Paris, France k Institute of Geological Sciences, Oeschger Center for Climate Research, University of Bern, Switzerland l Geoazur, IRD, Observatoire de la Côte d'Azur, CNRS, Université de Nice Sophia-Antipolis, Valbonne, France m Institut de Physique du Globe de Paris, Paris, France ARTICLE INFO ABSTRACT Keywords: Recent measurements of surface vertical displacements of the European Alps show a correlation between vertical European Alps velocities and topographic features, with widespread uplift at rates of up to ~2–2.5 mm/a in the North-Western Vertical displacement rate and Central Alps, and ~1 mm/a across a continuous region from the Eastern to the South-Western Alps. -
Maps of Aegidius Tschudi
146 The Alpin~ Maps of Aegidius Tschudi. We arrived at 4.30 at the tents and after hot drinks soon recovered our strength. Also Kesar's eyesight became normal again. At 7.30 we arrived down at Camp I, evacuated everything to the Base Camp on 22nd, and on 27th arrived at Tapoban. p ACHMARHI, INDIA, C.P. 2-10-33. DEAR DocTOR LoNGSTAFF, The mistake about times was due to my carelessness in the account I sent you. I suppose I did not look it through with thoroughness. The actual times were these: Left Camp II (ca. 19,000 ft.) . 7.45 A.M. At the site we meant to have Camp III (about 11.15 , 21,000 ft.) 11.30 " Summit 2.45 P.M. • • • • • • • • 2.52 " ' Camp III ' (ca. 21,000 ft.) . 4.30 " • . 5.00 '' Camp II . • • • . .. 6.00 " ' Camp I (ca. 17,000 ft.) • • . 7.30 '' This gives my times: Of. [T. G. L.] ' A.J.' 24, 120 : Up: 4500 ft. in 7 hrs. 6000 ft. in 10 hrs. 650 ft. per hour. 600 ft. per hr. Down : 6500 ft. in 4! hrs. 7000 ft. in 3 hrs. 1440 ft. per hour. 2333 ft. per hr. These times are incI uding rests. Ditto. p. R. OLIVER . • [Lieut. Oliver followed our 1907 route except perhaps at the commencement. There is no doubt at all that he attained the summit, which is the first (N.) . small flattish dome : the very slightly lower and corniched S. top, across a small gap, would have been invisible in such weather. -
Rapid Formation and Exhumation of the Youngest Alpine Eclogites: a Thermal Conundrum to Barrovian Metamorphism
Earth and Planetary Science Letters 306 (2011) 193–204 Contents lists available at ScienceDirect Earth and Planetary Science Letters journal homepage: www.elsevier.com/locate/epsl Rapid formation and exhumation of the youngest Alpine eclogites: A thermal conundrum to Barrovian metamorphism Andrew J. Smye a,⁎, Mike J. Bickle a, Tim J.B. Holland a, Randall R. Parrish b, Dan J. Condon b a Department of Earth Sciences, University of Cambridge, Cambridge, CB2 3EQ, UK b NERC National Isotope Geoscience Laboratories, Kinglsey Dunhem Centre, Keyworth, Nottingham, NG12 5GG, UK article info abstract Article history: Eclogite facies metamorphic rocks provide critical information pertaining to the timing of continental collision Received 15 December 2010 in zones of plate convergence. Despite being amongst Earth's best studied orogens, little is understood about Received in revised form 28 March 2011 the rates of Alpine metamorphism within the Eastern Alps. We present LA–MC–ICPMS and ID–TIMS U–Pb Accepted 29 March 2011 ages of metamorphic allanite from the Eclogite Zone, Tauern Window, which when coupled with rare earth Available online 30 April 2011 element analysis and thermobarometric modelling, demonstrate that the European continental margin was – fi Editor: R.W. Carlson subducted to between 8 and 13 kbar (30 45 km) by 34.2±3.6 Ma. These data de ne: (i.) an upper limit on the timing of eclogite facies metamorphism at 26.2±1.8 kbar (70–80 km) and 553±12 °C, (ii.) plate velocity −1 Keywords: (1–6 cm·a ) exhumation of the Eclogite Zone from mantle to mid-crustal depths, and (iii.) a maximum eclogite duration of 10 Ma (28–38 Ma) for juxtaposition of Alpine upper-plate and European basement units and Barrovian metamorphism subsequent conductive heating thought to have driven regional Barrovian (re)crystallisation at ca. -
Ivrea Mantle Wedge, Arc of the Western Alps, and Kinematic Evolution of the Alps–Apennines Orogenic System
Swiss J Geosci DOI 10.1007/s00015-016-0237-0 Ivrea mantle wedge, arc of the Western Alps, and kinematic evolution of the Alps–Apennines orogenic system 1 1 1 2 Stefan M. Schmid • Eduard Kissling • Tobias Diehl • Douwe J. J. van Hinsbergen • Giancarlo Molli3 Received: 6 June 2016 / Accepted: 9 December 2016 Ó Swiss Geological Society 2017 Abstract The construction of five crustal-scale profiles related to the lateral indentation of the Ivrea mantle slice across the Western Alps and the Ivrea mantle wedge towards WNW by some 100–150 km. (4) The final stage of integrates up-to-date geological and geophysical informa- arc formation (25–0 Ma) is associated with orogeny in the tion and reveals important along strike changes in the Apennines leading to oroclinal bending in the southern- overall structure of the crust of the Western Alpine arc. most Western Alps in connection with the 50° counter- Tectonic analysis of the profiles, together with a review of clockwise rotation of the Corsica-Sardinia block and the the existing literature allows for proposing the following Ligurian Alps. Analysis of existing literature data on the multistage evolution of the arc of the Western Alps: (1) Alps–Apennines transition zone reveals that substantial exhumation of the mantle beneath the Ivrea Zone to shal- parts of the Northern Apennines formerly suffered Alpine- low crustal depths during Mesozoic is a prerequisite for the type shortening associated with an E-dipping Alpine sub- formation of a strong Ivrea mantle wedge whose strength duction zone and were backthrusted to the NE during exceeds that of surrounding mostly quartz-bearing units, Apenninic orogeny that commences in the Oligocene. -
Field Trip - Alps 2013
Student paper Field trip - Alps 2013 Evolution of the Penninic nappes - geometry & P-T-t history Kevin Urhahn Abstract Continental collision during alpine orogeny entailed a thrust and fold belt system. The Penninic nappes are one of the major thrust sheet systems in the internal Alps. Extensive seismic researches (NFP20,...) and geological windows (Tauern-window, Engadin-window, Rechnitz-window), as well as a range of outcrops lead to an improved understanding about the nappe architecture of the Penninic system. This paper deals with the shape, structure and composition of the Penninic nappes. Furthermore, the P-T-t history1 of the Penninic nappes during the alpine orogeny, from the Cretaceous until the Oligocene, will be discussed. 1 The P-T-t history of the Penninic nappes is not completely covered in this paper. The second part, of the last evolution of the Alpine orogeny, from Oligocene until today is covered by Daniel Finken. 1. Introduction The Penninic can be subdivided into three partitions which are distinguishable by their depositional environment (PFIFFNER 2010). The depositional environments are situated between the continental margin of Europe and the Adriatic continent (MAXELON et al. 2005). The Sediments of the Valais-trough (mostly Bündnerschists) where deposited onto a thin continental crust and are summarized to the Lower Penninic nappes (PFIFFNER 2010). The Middle Penninic nappes are comprised of sediments of the Briançon-micro-continent. The rock compositions of the Lower- (Simano-, Adula- and Antigori-nappe) and Middle- Penninic nappes (Klippen-nappe) encompass Mesozoic to Cenozoic sediments, which are sheared off from their crystalline basement. Additionally crystalline basement form separate nappe stacks (PFIFFNER 2010). -
Mapping of the Post-Collisional Cooling History of the Eastern Alps
1661-8726/08/01S207-17 Swiss J. Geosci. 101 (2008) Supplement 1, S207–S223 DOI 10.1007/s00015-008-1294-9 Birkhäuser Verlag, Basel, 2008 Mapping of the post-collisional cooling history of the Eastern Alps STEFAN W. LUTH 1, * & ERNST WILLINGSHOFER1 Key words: Eastern Alps, Tauern Window, geochronology, cooling, mapping, exhumation ABSTRACT We present a database of geochronological data documenting the post-col- High cooling rates (50 °C/Ma) within the TW are recorded for the tem- lisional cooling history of the Eastern Alps. This data is presented as (a) geo- perature interval of 375–230 °C and occurred from Early Miocene in the east referenced isochrone maps based on Rb/Sr, K/Ar (biotite) and fission track to Middle Miocene in the west. Fast cooling post-dates rapid, isothermal exhu- (apatite, zircon) dating portraying cooling from upper greenschist/amphibo- mation of the TW but was coeval with the climax of lateral extrusion tectonics. lite facies metamorphism (500–600 °C) to 110 °C, and (b) as temperature maps The cooling maps also portray the diachronous character of cooling within documenting key times (25, 20, 15, 10 Ma) in the cooling history of the Eastern the TW (earlier in the east by ca. 5 Ma), which is recognized within all isotope Alps. These cooling maps facilitate detecting of cooling patterns and cooling systems considered in this study. rates which give insight into the underlying processes governing rock exhuma- Cooling in the western TW was controlled by activity along the Brenner tion and cooling on a regional scale. normal fault as shown by gradually decreasing ages towards the Brenner Line. -
An Overview of Glacier Lakes in the Western Italian Alps from 1927 To
Geogr. Fis. Dinam. Quat. DOI 10.4461/GFDQ.2016.39.19 39 (2016). 203-214, 9 figg., 3 tabb. CRISTINA VIANI (*), MARCO GIARDINO (*,**), CH RISTIAN GLHUG E (***), LUIGI PEROTTI (*,**) & GIO VANNI MORTARA (**) AN OVERVIEW OF GLACIER LAKES IN THE WESTERN ITALIAN ALPS FROM 1927 TO 2014 BASED ON MULTIPLE DATA SOURCES (HISTORICAL MAPS, ORTHOPHOTOS AND REPORTS OF THE GLACIOLOGICAL SURVEYS) ABSTRT AC : VIANI C., GIARDINO M., HUGLG E C., PEROTTI L. & MOR- Alps (Monte Rosa Group). Moreover, in a dedicated database, we collect- TARA G., An overview of glacier lakes in the Western Italian Alps form ed information (descriptions, photos, maps) about glacier lakes from the 1927 to 2014 based on multiple data sources (historical maps, orthophotos reports of the annual glaciological surveys published by the Italian Gla- and reports of the glaciological surveys). (IT ISSN 0391-9839, 2016) ciological Committee (CGI) since 1928. Finally, we reported two cases of glacier lakes at the Tzére Glacier (Monte Rosa Group, Pennine Alps) Since the end of the Little Ice Age (LIA, ca. 1850 AD) a general and at the Ban Glacier (Monte Leone-Blinnenhorn Chain, Lepontine and progressive retreat of glaciers started in the European Alps, causing Alps), in order to demonstrate the importance of integrating data from a important environmental changes in this high mountain region. The ap- diversity of sources (historical maps, orthophotos and reports of the gla- pearance of glacier lakes is one of the most evident environmental effects ciological surveys) for better detailed reconstructions of the condition of in the Alps as well as in newly deglaciated areas worldwide. -
Monitoraggio Dei Pops Sul Territorio Alpino Monitoring Pops in the Alps
Agenzia Regionale per la Protezione dell’Ambiente della Lombardia Dipartimento di Sondrio C. A. Belis - T. Magnani Editors C. A. Belis - T. Magnani C. A. Belis - T. Monitoraggio dei POPs S P sul territorio alpino IN THE AL Monitoring POPs RING POPS O in the Alps NIT O M - - O IN P AL O RI ATTI DELLA CONFERENZA O Monitoraggio degli inquinanti organici persistenti sul territorio alpino: uno sguardo sulla situazione europea, italiana e lombarda UL TERRIT UL S PROCEEDINGS OF THE CONFERENCE S Monitoring persistent organic pollutants in the Alps: An overview on the situation in Europe, Italy and Lombardy DEI POP DEI O ISBN 978-88-903167-0-8 RAGGI O NIT O 9 788890 316708 > M 31 ottobre 2007 - Bormio (SO) - 31st october 2007 C. A. Belis - T. Magnani Editors Monitoraggio dei POPs sul territorio alpino Monitoring POPs in the Alps Agenzia Regionale per la Protezione dell’Ambiente della Lombardia Dipartimento di Sondrio Copyright © 2007 Agenzia Regionale per la Protezione dell’Ambiente Lombardia ISBN 978-88-903167-0-8 Finito di stampare nel mese di ottobre 2007 dalla Tipografia Polaris di Sondrio INDICE GLI INQUINANTI ORGANICI PERSISTENTI IN UNA PROSPETTIVA NAZIONALE ED EUROPEA Le Alpi e i progetti transnazionali 7 Environmental protection and transnational cooperation in the alpine space: results and perspectives 11 Present and future in the risk assessment of chemicals with PBT properties 13 I RISULTATI DEL PROGETTO MONARPOP Synthesis of the findings of the project MONARPOP 21 Idrocarburi policiclici aromatici negli ecosistemi alpini (progetto -
New Aspects on the Timing of Deformation Along the South
Originally published as: Bachmann, R., Glodny, J., Oncken, O., Seifert, W. (2009): Abandonment of the South Penninic-Austroalpine palaeosubduction zone, Central Alps, and shift from subduction erosion to accretion: constraints from Rb/Sr geochronology. - Journal of the Geological Society London, 166, 2, 217-231 DOI: 10.1144/0016-76492008-024. Abandonment of the South Penninic-Austroalpine palaeo-subduction zone, Central Alps, and shift from subduction erosion to accretion: constraints from Rb/Sr geochronology Raik Bachmann Deutsches GeoForschungsZentrum (GFZ), Telegrafenberg, 14473 Potsdam, Germany. [email protected] Present address: Horizon Energy Partners, Prinses Margrietplantsoen 81, 2595 BR The Hague, The Netherlands [email protected] Johannes Glodny Deutsches GeoForschungsZentrum (GFZ), Telegrafenberg, 14473 Potsdam, Germany, [email protected] Onno Oncken Deutsches GeoForschungsZentrum (GFZ), Telegrafenberg, 14473 Potsdam, Germany, [email protected] Wolfgang Seifert Deutsches GeoForschungsZentrum (GFZ), Telegrafenberg, 14473 Potsdam, Germany, [email protected] Corresponding author: Raik Bachmann 1 Abstract We present new age data for the evolution of the suture zone between lower-plate South Penninic and upper-plate Austroalpine units in the Central European Alps. Rb/Sr deformation ages for mylonitized rocks of the South Penninic palaeo-subduction mélange and for deformed Austroalpine basement (Eastern Switzerland) shed light on the pre-Alpine and Alpine deformation history along the suture, as well as on syn-subduction interplate mass transfer. Rb/Sr age data define two age groups. The first group reflects pre-Alpine events within the upper plate basement, with varying degree of resetting by subsequent Alpine overprints. The second group marks the waning of subduction-related deformation along the South Penninic-Austroalpine suture zone, at around 50 Ma, and termination at ~47 Ma. -
2017 ANNUAL POPULATION STATUS REPORT for BROWN BEARS in NORTHERN DINARIC MOUNTAINS and CENTRAL- EASTERN ALPS Action C.5: Population Surveillance
2017 ANNUAL POPULATION STATUS REPORT FOR BROWN BEARS IN NORTHERN DINARIC MOUNTAINS AND CENTRAL- EASTERN ALPS Action C.5: Population surveillance Prepared by Tomaž Skrbinšek, Natalia Bragalanti, Sonia Calderola, Claudio Groff, Đuro Huber, Petra Kaczensky, Aleksandra Majić Skrbinšek, Anja Molinari-Jobin, Paolo Molinari, Georg Rauer, Slaven Reljić, Matija Stergar and Maja Jelenčič July, 2017 Introduction This is the third of annual Population Status Reports planned within LIFE DINALP BEAR. It provides an overview of both how population is being managed and its current status over the entire area in question. With these reports, we’d like to give the basic tool to wildlife managers dealing with bear management in each respective country/region, to include the situation in neighboring areas in their conservation and management planning. Understanding the status of populations of conservation concern is essential for effective conservation and management, which is also true for brown bears in the area covered by LIFE DINALP BEAR. Such population-level understanding is the foremost condition that must be met if we are to transcend the national or regional-level conservation and management practices that are the current norm in wildlife management and conservation. In this third report we’ve again had some problems in production. Since we’re still ironing-out the common information infrastructure, we decided to stick with the expert approach. Each of the experts updated the text for his or her geographic area with the most recent available data on all recorded aspects of bear monitoring to produce an up to date picture of the status of the bears in our area. -
Deciphering the Evolution of the Bleis Marscha Rock Glacier (Val
The Cryosphere, 15, 2057–2081, 2021 https://doi.org/10.5194/tc-15-2057-2021 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. Deciphering the evolution of the Bleis Marscha rock glacier (Val d’Err, eastern Switzerland) with cosmogenic nuclide exposure dating, aerial image correlation, and finite element modeling Dominik Amschwand1,a, Susan Ivy-Ochs1,2, Marcel Frehner1, Olivia Steinemann2, Marcus Christl2, and Christof Vockenhuber2 1Department of Earth Sciences, ETH Zurich, 8092, Zurich, Switzerland 2Laboratory of Ion Beam Physics, ETH Zurich, 8093, Zurich, Switzerland anow at: Department of Geosciences, University of Fribourg, 1700, Fribourg, Switzerland Correspondence: Dominik Amschwand ([email protected]) Received: 21 July 2020 – Discussion started: 10 August 2020 Revised: 21 January 2021 – Accepted: 25 February 2021 – Published: 26 April 2021 Abstract. We constrain the Holocene development of the ders on a moving rock glacier ideally record time since depo- active Bleis Marscha rock glacier (Err–Julier area, east- sition on the rock glacier root but are stochastically altered by ern Swiss Alps) with 15 cosmogenic nuclide exposure ages boulder instabilities and erosional processes. This work con- (10Be, 36Cl), horizontal surface creep rate quantification by tributes to deciphering the long-term development and the correlating two orthophotos from 2003 and 2012, and finite past to quasi-present climate sensitivity of rock glaciers. element modeling. We used the latter to separate the con- trol on surface movement exerted by topography and ma- terial properties. Bleis Marscha is a stack of three over- riding lobes whose formation phases are separated by time gaps expressed morphologically as over-steepened terrain 1 Introduction steps and kinematically as a sharp downslope decrease in surface movement.