DOCSLIB.ORG

Mezzolombardo

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Mezzolombardo ISPRA Istituto Superiore per la Protezione e la Ricerca Ambientale SERVIZIO GEOLOGICO D’ITALIA Organo cartografico dello Stato (legge 68 del 2.2.1960) ERLÄUTERUNGEN zur GEOLOGISCHEN KARTE VON ITALIEN im Maßstab 1:50.000 Blatt 043 MEZZOLOMBARDO Erstellt von: Marco Avanzini1 Giuseppe Maria Bargossi2, Andrea Borsato1, Maurizio Cucato3, Corrado Morelli3, Vincenzo Picotti2, Luigi Selli2 Mit Beiträgen von: Tiziano Abbà3, Mariangela Balboni4, Gianfranco Bazzoli3, Paolo Campedel4, Claudio Carraro5, Oscar Groaz4, Lorenz Keim5, Paolo Ferretti1, Luca Froner4, Pierpaolo Macconi2, Mattia Marini6, Gianluca Piccin3, Matteo Rinaldo3, Ernesto Santuliana4,Claudia Strada5, Riccardo Tomasoni3, Alfio Viganò4, Giorgio Zampedri4, MauroPROGETTO Zambotto4 1 Museo Tridentino di Scienze Naturali, Trento 2 Dipartimento di Scienze della Terra e Geologico - Ambientali, Università di Bologna 3 Freiberuflicher Geologe 4 Servizio Geologico - Provincia Autonoma di Trento 5 Amt für Geologie und Baustoffprüfung - Autonome Provinz Bozen - Südtirol 6 SEA Srl, Torino Ausführende Körperschaften Provincia Autonoma di Trento AutonomeProvincia Provinz Autonoma Bozen di Bolzano- Südtirol Servizio GeologicoCARGAmt Ufficio für Geologie Geologia und e prove Baustoffprüfung materiali Direktor des Geologischen Dienstes von Italien - ISPRA: C. Campobasso Verantwortlicher des Projekts CARG des Geologischen Dienstes von Italien - ISPRA: F. Galluzzo Verantwortlicher des Projekts CARG der Autonomen Provinz Trient: S. Cocco Verantwortlicher des Projekts CARG der Autonomen Provinz Bozen – Südtirol: V. Mair Für den Geologischen Dienst von Italien – ISPRA: Wissenschaftliche Revision: D. Berti, R. Graciotti, M.L. Pampaloni, M. Pantaloni Kartographische Leitung: D. Tacchia, S. Falcetti Leitung der Herausgabe und der Druckvorbereitung: M.L. Vatovec, S. Falcetti Überprüfung der Informatisierung der geologischen Daten: L. Battaglini, V. Campo, A. Fiorentino (ASC) Für den Geologischen Dienst der Autonomen Provinz Trient: Operative Leitung: S. Cocco, M. Balboni Informatisierung der geologischen Daten: G. Fucarino, P. Trainotti Für das Amt für Geologie und Baustoffprüfung der Autonomen Provinz Bozen - Südtirol: Operative Leitung: L. Keim, C. Morelli Informatisierung der geologischen Daten: M. Cucato, L. Keim, C. Morelli Übersetzung aus dem Italienischen: PROGETTOL. Montresor, A. Stofner, L. Keim, M. Stefani Kartographische Ausarbeitung zum Druck: B. Monopoli - Land Technology & Services - Padova e Treviso Technisch-administrative Verwaltung des Projekts CARG: M.T. Lettieri - Geologischer Dienst von Italien - ISPRA M. Balboni - Geologischer Dienst der Autonomen Provinz Trient L. Keim, C. Morelli - Amt für Geologie und Baustoffprüfung der Autonomen Provinz Bozen – Südtirol Dank an die Mitarbeiter der vorhergehenden CARGGeologischen Komitees für ihren wissenschaftlichen Beitrag INHALT I - EINLEITUNG................................................................... Seite 7 II - GEOMORPHOLOGISCHER UND GEOLOGISCHER ÜBERBLICK ....................................................................... » 11 1. - GEOMORPHOLOGIE .......................................................... » 11 2. - KARST .................................................................................. » 15 3. - ANMERKUNGEN ZUR GEOLOGIE .................................. » 16 III - FRÜHERE UNTERSUCHUNGEN ................................... » 17 IV - STRATIGRAPHIE DER VULKANITE ........................... » 23 1. - ETSCHTALER VULKANIT-GRUPPE (GA) ...................... » 23 1.1. - GARGAZON-FORMATION (IGG) ................................................. » 24 1.2. - GRIES-FORMATION (IGR) ........................................................ » 27 1.3. - ANDRIAN-FORMATION (LAN) ................................................... » 28 1.4. - TREGIOVO-FORMATION (TGV) .................................................. » 30 1.5. - AUER-FORMATION (ORA) ........................................................ » 32 1.5.1. - Perdonig-Member (ORA1) .................................................... » 35 2. - VULKANO-tektonische ENTWICKLUNG DES ABLAGERUNGSGEBIETES DER ETSCHTALER VULKANIT-GRUPPE (GA) IM Blatt MEZZOLOMBARDO .......................................................... » 37 3. - GEOCHEMIE DER PERMISCHEN VULKANISCHEN PRODUKTE .......................................................................... » 41 V - STRATIGRAPHIE DER PERMO-MESO-KÄNOZOISCHEN SEDIMENT- UND VULKANIT-ABFOLGEN ................. » 43 1. - GRÖDEN-Formation (GAR) .......................................... » 43 2. - BELLEROPHON-FORMATION (BEL) .............................. » 44 3.PROGETTO - WERFEN-FORMATION (WER) ......................................... » 46 3.1. - TESERO- UND MAZZIN-MEMBER (WER1-2) ............................... » 46 3.2. - ANDRAZ- UND SEIS-MEMBER (WER3-4) .................................... » 48 3.3. - GASTROPODENOOLITH- UND CAMPILL-MEMBER (WER5-6) .......... » 49 3.4. - VAL BADIA-, CENCENIGHE- UND SAN LUCANO-MEMBER (WER7-8-9) . » 50 4. - UNTERER SARLDOLOMIT (SLI) ..................................... » 52 5. - Voltago-Konglomerat (VTG) ................................. » 52 6. - GIOVO-FORMATION (GIV) ............................................... » 54 6.1. - KURTATSCH-MEMBER (GIV2) ................................................... » 54 6.2. - MONTE OZOL -M EMBER CARG (GIV3) ...............................................................» 55 7. - CONTRIN-FORMATION (CTR) ...................................... Seite 57 8. - MOENA-FORMATION (MNA) ........................................... » 58 9. - SCHLERN-FormaTION (SCI) .......................................... » 58 9.1. - HANGFAZIES (SCIa) .................................................................. » 60 9.2. - BIOSTRATIGRAPHIE UND PALÄOGEOGRAPHIE ................................ » 61 10. - BUCHENSTEIN-Formation (BHL) ............................... » 64 11. - VAL VELA KALK (VVL) .................................................... » 66 12. - BASALTISCHE VULKANITE (VAB) ................................. » 67 13. - Travenanzes-FORMATION (TVZ) .............................. » 69 13.1. - FOSSILE SPUREN VON CASTELLO DI SAN GOTTARDO.................... » 76 13.2. - FOSSILE SPUREN VON MOSTIZZOLO ............................................ » 79 14. - HAUPTDOLOMIT (DPR) .................................................... » 80 15. - ZU KALK (ZUU) .................................................................. » 83 15.1. - GROSTÈ-MEMBER (ZUU1) ....................................................... » 83 15.2. - TREMALZO-MEMBER (ZUU3) ................................................... » 84 16. - GRAUKALK-Gruppe ........................................................ » 84 16.1. - MONTE ZUGNA-FORMATION (FMZ) .......................................... » 85 16.2. - LOPPIO-OOLITHKALK (LOP) ..................................................... » 88 16.3. - ROTZO-FORMATION (RTZ) ........................................................ » 89 16.3.1. - Tovel-Member (RTZ1) ....................................................... » 91 17. - PELLER-ENCRINIT (EPE) .................................................. » 91 18. - ROSSO ammonitico VERONESE (ARV) ..................... » 92 19. - MAIOLICA (MAI) ................................................................ » 93 20. - SCAGLIA VARIEGATA ALPINA (VAA) ............................ » 94 21. - SCAGLIA ROSSA (SAA) ..................................................... » 97 22. - VAL d’AGOLA-Formation (VAG) ................................ » 98 22.1. - COSTE DI GRUAL-MEMBER (VAG2) .......................................... » 99 22.2. - SARCA DI CAMPIGLIO-MEMBER (VAG3) .................................... » 100 23. - PONTE PIÀ-Formation (FPP) ........................................ » 101 VIPROGETTO - STRATIGRAPHIE DER QUARTÄREN ABLAGERUNGEN ............................................................. » 103 1. - EINLEITUNG ZUR Stratigraphie DER QuartÄREN ABLAGERUNGEN .............................................................. » 103 2. - Stratigraphische EINHEITEN VOR DEM LETZTEN GLAZIALEN HochstanD ............................................... » 104 2.1. - FAEDO-FORMATION (FAD) ....................................................... » 106 2.2. - FORTE CASARA-GRUPPE (FC) ................................................... » 106 2.3. - NOGARÉ-SUPERSYNTHEM (NG) ................................................. » 109 2.4. - RIO PES CARA -S YNTHEM CARG (RPS) ................................................. » 110 2.5. - RIO BARNES-SYNTHEM (RBR) .............................................. Seite 111 2.6. - PENON-SYNTHEM (NON) ......................................................... » 114 2.7. - KALTERN-SYNTHEM (CLD) ...................................................... » 117 3. - EINHEITEN DES LETZTEN glazialen HochstanDES („LAST GLACIAL MAXIMUM“) .............. » 125 3.1. - GARDA-SYNTHEM (SGD) ......................................................... » 128 3.2. - CLOZ-SUBSYNTHEM (SGD3) ..................................................... » 137 3.3. - MALÈ-SUBSYNTHEM (SGD1) .................................................... » 140 3.4. - MOLLARO-SUBSYNTHEM (SGD14)............................................. » 146 3.5. - LISIGNAGO-SUBSYNTHEM (SGD12) ........................................... » 150 3.6. - S T . P AULS -S UBSYNTHEM (SGD6) ..................................... » 155 4. - ALPINES Postglaziales SYNTHEM (PTG)............... » 158 4.1. - ALLGEMEINER ÜBERBLICK ........................................................
Load more

Recommended publications
  • Promozione Promozione Trentino Alto Adige
    TRENTINO 3 Giovedì 22 agosto 2019 CALENDARI CALCIO REGIONALE Promozione Promozione Trentino Alto Adige 1 Set. 2019 1ª Giornata 9 Feb. 2020 8 Set. 2019 2ª Giornata 16 Feb. 2020 15 Set. 2019 3ª Giornata 23 Feb. 2020 1 Set. 2019 1ª Giornata 16 Feb. 2020 8 Set. 2019 2ª Giornata 23 Feb. 2020 15 Set. 2019 3ª Giornata 1 Mar. 2020 CALCIOCHIESE - MEZZOCORONA GARDOLO - BORGO AQUILA TRENTO - CALCIOCHIESE VALLE AURINA - PARCINES RAIFF. BRUNICO - VALLE AURINA VALLE AURINA - VAL PASSIRIA AQUILA TRENTO - ALENSE NAGO TORBOLE - CAVEDINE LASINO BORGO - ROVERETO ALBES - BRUNICO CAMPO TRENS - STRADA D. VINO SUD ALBES - APPIANO PINZOLO V. RENDENA - BORGO CALCIOCHIESE - TELVE VOLANO - RAVINENSE NATURNO - VORAN LEIFERS APPIANO - NAZ NAZ - CAMPO TRENS VOLANO - NAGO TORBOLE ALENSE - VOLANO BASSA ANAUNIA - GARDOLO NAZ - VAL PASSIRIA LACES - NATURNO PARCINES RAIFF. - BRUNICO BENACENSE - BASSA ANAUNIA PINZOLO V. RENDENA - BASSA ANAUNIA CAVEDINE LASINO - ALENSE SCENA - CAMPO TRENS MILLAND - SCENA SCENA - VORAN LEIFERS CAVEDINE LASINO - ROVERETO MEZZOCORONA - BENACENSE PINZOLO V. RENDENA - BENACENSE STEGONA - MILLAND PARCINES RAIFF. - TERLANO STEGONA - LACES SACCO S.GIORGIO - GARDOLO ROVERETO - SACCO S.GIORGIO SACCO S.GIORGIO - NAGO TORBOLE TERLANO - LACES VAL PASSIRIA - ALBES TERLANO - NATURNO TELVE - RAVINENSE RAVINENSE - AQUILA TRENTO TELVE - MEZZOCORONA STRADA D. VINO SUD - APPIANO VORAN LEIFERS - STEGONA STRADA D. VINO SUD - MILLAND 22 Set. 2019 4ª Giornata 1 Mar. 2020 29 Set. 2019 5ª Giornata 8 Mar. 2020 6 Ott. 2019 6ª Giornata 15 Mar. 2020 18 Set. 2019 4ª Giornata 8 Mar. 2020 22 Set. 2019 5ª Giornata 15 Mar. 2020 29 Set. 2019 6ª Giornata 22 Mar. 2020 GARDOLO - PINZOLO V. RENDENA GARDOLO - BENACENSE MEZZOCORONA - CAVEDINE LASINO BRUNICO - TERLANO VALLE AURINA - CAMPO TRENS CAMPO TRENS - PARCINES RAIFF.
    [Show full text]
  • Post-Carboniferous Stratigraphy, Northeastern Alaska by R
    Post-Carboniferous Stratigraphy, Northeastern Alaska By R. L. DETTERMAN, H. N. REISER, W. P. BROSGE,and]. T. DUTRO,JR. GEOLOGICAL SURVEY PROFESSIONAL PAPER 886 Sedirnentary rocks of Permian to Quaternary age are named, described, and correlated with standard stratigraphic sequences UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON 1975 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. MORTON, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress Cataloging in Publication Data Detterman, Robert L. Post-Carboniferous stratigraphy, northeastern Alaska. (Geological Survey Professional Paper 886) Bibliography: p. 45-46. Supt. of Docs. No.: I 19.16:886 1. Geology-Alaska. I. Detterman, Robert L. II. Series: United States. Geological Survey. Professional Paper 886. QE84.N74P67 551.7'6'09798 74-28084 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 Stock Number 024-001-02687-2 CONTENTS Page Page Abstract __ _ _ _ _ __ __ _ _ _ _ _ _ _ _ _ _ _ _ __ __ _ _ _ _ _ _ __ __ _ _ __ __ __ _ _ _ _ __ 1 Stratigraphy__:_Continued Introduction __________ ----------____ ----------------____ __ 1 Kingak Shale ---------------------------------------- 18 Purpose and scope ----------------------~------------- 1 Ignek Formation (abandoned) -------------------------- 20 Geographic setting ------------------------------------ 1 Okpikruak Formation (geographically restricted) ________ 21 Previous work and acknowledgments ------------------ 1 Kongakut Formation ----------------------------------
    [Show full text]
  • BCT1 (Fondo Miscellaneo). Archivi Di Famiglie 2018
    BCT1 (Fondo miscellaneo). Archivi di famiglie 2018 AGOSTINI COLLOCAZIONE: BCT1–3088/16, BCT1–3088/29 ESTREMI CRONOLOGICI: 1754-1773 DATA DI ACQUISIZIONE E PROVENIENZA: i documenti collocati al ms. BCT1–3088 sono stati donati da Pietro Zanolini nell’anno 1908 e fanno parte di una raccolta di 43 documenti, relativi a diverse famiglie trentine, rilegati in due volumi. DESCRIZIONE: 1. Contratti di compravendita - 1754 aprile 28, Leonardo Segata di Sopramonte vende a Valentino Agostini di quel luogo un prato ubicato nelle pertinenze di Sopramonte: BCT1–3088/16 - 1773 maggio 20, Contratto di permuta concluso tra Gianantonio Rosat di Sopramonte e Antonio Agostini del medesimo luogo: BCT1–3088/29 ALBERTINI COLLOCAZIONE: BCT2 ESTREMI CRONOLOGICI:1590 DATA DI ACQUISIZIONE E PROVENIENZA: Hippoliti, famiglia DESCRIZIONE: 1. Contratti - 1590 febbraio 10, Maria fu Tomeo Pazzo da Cinte, vedova di Pellegrino Alde da Scurelle e Zaneto suo figlio vendono a Nicolò Albertino una pezza di terra sita a Scurelle, in luogo det- to ‘a Pra de Ponte’: BCT2–884 ALESSANDRINI DI NEUENSTEIN COLLOCAZIONE: BCT1–482, BCT1–905, BCT1–1038, BCT1–2409, BCT2 DATA DI ACQUISIZIONE E PROVENIENZA: raccolta Mazzetti e altre provenienze fondo manoscritti BCT1–1696, BCT1–1818, BCT1–2224, BCT1–2518, BCT1–2668, vedi anche BCT2 DESCRIZIONE: - De anatome humani corporis, auctore Julio Alexandrino cum notis, copia del sec. XVII: BCT1–2409 ALIPRANDI COLLOCAZIONE: BCT1–1188 ESTREMI CRONOLOGICI:1654 DATA DI ACQUISIZIONE E PROVENIENZA: Raccolta Antonio Mazzetti DESCRIZIONE: 1. Privilegi di nobiltà - 1654: BCT1–1188 ALMERICO 1 BCT1 (Fondo miscellaneo). Archivi di famiglie dicembre 2014 COLLOCAZIONE: BCT1–2478 ESTREMI CRONOLOGICI:1820 DESCRIZIONE: 1. Eredità - 1820, Pretesa Mazani sull’eredità di famiglia: BCT1–2478 ALTENBURGER COLLOCAZIONE: BCT1–3322 ESTREMI CRONOLOGICI:1733 DATA DI ACQUISIZIONE E PROVENIENZA: Lascito Tranquillini dell’aprile 1923, pervenuta con i docu- menti della famiglia Valentini di Calliano e della famiglia Zambaiti di Vezzano.
    [Show full text]
  • A Palaeoenvironmental Reconstruction of the Middle Jurassic of Sardinia (Italy) Based on Integrated Palaeobotanical, Palynological and Lithofacies Data Assessment
    Palaeobio Palaeoenv DOI 10.1007/s12549-017-0306-z ORIGINAL PAPER A palaeoenvironmental reconstruction of the Middle Jurassic of Sardinia (Italy) based on integrated palaeobotanical, palynological and lithofacies data assessment Luca Giacomo Costamagna1 & Evelyn Kustatscher2,3 & Giovanni Giuseppe Scanu1 & Myriam Del Rio1 & Paola Pittau1 & Johanna H. A. van Konijnenburg-van Cittert4,5 Received: 15 May 2017 /Accepted: 19 September 2017 # The Author(s) 2017. This article is an open access publication Abstract During the Jurassic, Sardinia was close to con- diverse landscape with a variety of habitats. Collection- tinental Europe. Emerged lands started from a single is- and literature-based palaeobotanical, palynological and land forming in time a progressively sinking archipelago. lithofacies studies were carried out on the Genna Selole This complex palaeogeographic situation gave origin to a Formation for palaeoenvironmental interpretations. They evidence a generally warm and humid climate, affected occasionally by drier periods. Several distinct ecosystems can be discerned in this climate, including alluvial fans This article is a contribution to the special issue BJurassic biodiversity and with braided streams (Laconi-Gadoni lithofacies), paralic ^ terrestrial environments . swamps and coasts (Nurri-Escalaplano lithofacies), and lagoons and shallow marine environments (Ussassai- * Evelyn Kustatscher [email protected] Perdasdefogu lithofacies). The non-marine environments were covered by extensive lowland and a reduced coastal Luca Giacomo Costamagna and tidally influenced environment. Both the river and the [email protected] upland/hinterland environments are of limited impact for Giovanni Giuseppe Scanu the reconstruction. The difference between the composi- [email protected] tion of the palynological and palaeobotanical associations evidence the discrepancies obtained using only one of those Myriam Del Rio [email protected] proxies.
    [Show full text]
  • Climatic Control of Arenites: an Example from the Carnian (Upper Triassic) of the Dolomites (Northern Italy) R
    Geophysical Research Abstracts, Vol. 8, 08628, 2006 SRef-ID: 1607-7962/gra/EGU06-A-08628 © European Geosciences Union 2006 Climatic control of arenites: an example from the Carnian (Upper Triassic) of the Dolomites (northern Italy) R. Meneguolo (1), N. Preto (1), A. Breda (1) (1) Università degli Studi di Padova - Dip.to di Geologia, Paleontologia e Geofisica, Via Giotto, 1. 35137, Padova (Italy) Sedimentology and arenite composition have been investigated in the Upper Triassic of the Dolomites (Southern Alps, northern Italy). The siliciclastics of two superim- posed mixed terrigenous-carbonate, Carnian formations have been studied. The tran- sitional to shallow-marine Heiligkreuz Formation of the Dolomites records at least 8 high-frequency sedimentary cycles. The siliciclastic portions of each cycle are de- posited in a shallow-water subtidal setting, always including high-density flow de- posits in the lower part. Composition of arenites displays a short-term trend from lithic to quartzose. Mixed, high frequency cycles can be recognized also within the continental to transitional Travenanzes Formation. Arenites deposits are found in spo- radic, channelized bodies, and in their related overbank sheets, representing flooding events of ephemeral streams. Fluctuations in the composition of arenites can still be recognized, with a strong quartz enrichment in the upper part of each cycle. Siliciclastic constituents (quartz, feldspars and lithics of volcaniclastic origin) remain constant through time. Volcaniclastic grains may be either substantially unaltered or strongly altered, with altered volcaniclastic grains prevailing in the more quartzose facies. An upwards increase in quartz content is observed also through the whole suc- cession. An influence of tectonics and/or source area changes on the compositional variations of arenites can be excluded.
    [Show full text]
  • USGS Geologic Investigations Series I-2673, Pamphlet
    U.S. DEPARTMENT OF THE INTERIOR TO ACCOMPANY MAP I–2673 U.S. GEOLOGICAL SURVEY GEOLOGIC MAP OF THE ARCTIC QUADRANGLE, ALASKA By W.P. Brosgé, H.N. Reiser, J.T. Dutro, Jr., R.L. Detterman, and I.L. Tailleur INTRODUCTION parts of the quadrangle in 1926 and 1927 and published his results in 1930 (Mertie, 1930). This rapid reconnaissance, GEOLOGIC SETTING AND LAND USE made mostly on foot under extremely difficult conditions, sketched out the rudimentary distribution of rock types, but The Arctic quadrangle is well located to shed light on little of the modern stratigraphy was discerned. The distri- the basic geologic relations of northern Alaska. The rocks bution of the Lisburne Limestone in the eastern part of the represent all of the stratigraphic systems from Cambrian to quadrangle was roughly shown; and the approximate distri- Cretaceous and all but one of the tectono-stratigraphic bution of the Devonian clastic rocks between the East Fork subterranes of the Brooks Range, from the autochthonous of the Chandalar and the Sheenjek valley was also shown subterrane in the north to the allochthonous subterranes far- although details of the history of these strata were not known. ther south. Most of the pre-Mississippian carbonate rocks were mapped Among the distinctive geologic features displayed in the by Mertie as Skajit Limestone, supposedly of Silurian ages. Arctic quadrangle are voluminous volcanic rocks of prob- He mapped the chert and slate unit between Old Woman able Devonian age, a wide array of Carboniferous carbonate Creek and the East Fork of the Chandalar, and tentatively facies in the Lisburne Group (which here extends up into the assigned it a Mississippian or Late Devonian age.
    [Show full text]
  • Serie D1 Maschile Calendario 2020 Gironi
    FEDERAZIONE ITALIANA TENNIS TN SERIE D1 MASCHILE 2020 SERIE D1 MASCHILE - Girone 1 SQUADRA CAMPI PALLE SEDE DI GIOCO Dunlop Fort All Court CT PREDAZZO Terra rossa Tournament Select VIA RODODENDRI, Predazzo 38037 (TN) CT BORGO Terra rossa Dunlop Australian Open PIAZZA AL MERCATO, Borgo Valsugana 38051 (TN) Dunlop Fort All Court CT MEZZOCORONA Terra rossa Tournament Select VIA SOTTODOSSI, Mezzocorona 38016 (TN) Dunlop Fort All Court CT TRENTO B Terra rossa Tournament Select PIAZZA VENEZIA, Trento 38122 (TN) Dunlop Fort All Court AT DARZO Sintetico - Play-it Tournament Select VIA CAPITELLO - DARZO, Storo 38089 (TN) CT ARGENTARIO Terra rossa Wilson US Open VIA DEI COLLI PARCO URBANO, Lavis 38015 (TN) CLASSIFICA CALENDARIO RIS. PEN. squadra g v n p pen. i.v. P domenica 5 luglio 2020 CT ARGENTARIO 5 5 0 0 0 19 10 09:00 CT PREDAZZO - CT TRENTO B 2 2 0 0 CT MEZZOCORONA 5 3 1 1 0 12 7 09:00 CT MEZZOCORONA - AT DARZO 3 1 0 0 CT PREDAZZO 5 2 2 1 0 10 6 09:00 CT ARGENTARIO - CT BORGO 4 0 0 0 CT TRENTO B 5 1 2 2 0 7 4 domenica 12 luglio 2020 AT DARZO 5 1 0 4 0 7 2 09:00 AT DARZO - CT TRENTO B 1 3 0 0 CT BORGO 5 0 1 4 0 5 1 09:00 CT MEZZOCORONA - CT ARGENTARIO 0 4 0 0 09:00 CT BORGO - CT PREDAZZO 1 3 0 0 domenica 19 luglio 2020 09:00 CT TRENTO B - CT MEZZOCORONA 0 4 0 0 09:00 CT PREDAZZO - CT ARGENTARIO 0 4 0 0 09:00 AT DARZO - CT BORGO 3 1 0 0 domenica 26 luglio 2020 09:00 CT ARGENTARIO - CT TRENTO B 4 0 0 0 09:00 CT BORGO - CT MEZZOCORONA 1 3 0 0 09:00 CT PREDAZZO - AT DARZO 3 1 0 0 domenica 2 agosto 2020 09:00 CT TRENTO B - CT BORGO 2 2 0 0 09:00 CT MEZZOCORONA - CT PREDAZZO 2 2 0 0 09:00 AT DARZO - CT ARGENTARIO 1 3 0 0 CT MEZZOCORONA - AT DARZO ROSINI CLAUDIO FESTA MATTIA 63 63 PANCHERI MASSIMO FONTANA NICOLA 61 40 RIT.
    [Show full text]
  • Mezzolombardo
    ISPRA Istituto Superiore per la Protezione e la Ricerca Ambientale SERVIZIO GEOLOGICO D’ITALIA Organo cartografico dello Stato (legge 68 del 2.2.1960) NOTE ILLUSTRATIVE della CARTA GEOLOGICA D’ITALIA alla scala 1:50.000 foglio 043 MEZZOLOMBARDO A cura di Marco Avanzini1 Giuseppe Maria Bargossi2, Andrea Borsato1, Maurizio Cucato3, Corrado Morelli3, Vincenzo Picotti2, Luigi Selli2 Con la collaborazione di: Tiziano Abbà3, Mariangela Balboni4, Gianfranco Bazzoli3, Paolo Campedel4, Claudio Carraro5, Oscar Groaz4, Lorenz Keim5, Paolo Ferretti1, Luca Froner4, Pierpaolo Macconi2, Mattia Marini6, Gianluca Piccin3, Matteo Rinaldo3, Ernesto Santuliana4,Claudia Strada5, Riccardo Tomasoni3, Alfio Viganò4, Giorgio Zampedri4, Mauro Zambotto4 1 MuseoPROGETTO Tridentino di Scienze Naturali, Trento 2 Dipartimento di Scienze della Terra e Geologico - Ambientali, Università di Bologna 3 Geologo, libero professionista 4 Servizio Geologico - Provincia Autonoma di Trento 5 Ufficio Geologia e prove materiali - Provincia Autonoma di Bolzano - Alto Adige 6 SEA Srl, Torino Enti realizzatori Provincia Autonoma di Trento ProvinciaProvincia Autonoma Autonoma di Bolzano di Bolzano - Alto Adige Servizio Geologico CARGUfficio Geologia e prove materiali Ufficio Geologia e prove materiali Direttore del Servizio Geologico d’Italia - ISPRA: C. Campobasso Responsabile del Progetto CARG per il Servizio Geologico d’Italia - ISPRA: F. Galluzzo Responsabile del progetto CARG per la Provincia Autonoma di Trento: S. Cocco Responsabile del Progetto CARG per la Provincia Autonoma di Bolzano: V. Mair Per il Servizio Geologico d’Italia – ISPRA Revisione scientifica: D. Berti, R. Graciotti, M.L. Pampaloni, M. Pantaloni Coordinamento cartografico: D. Tacchia, S. Falcetti Coordinamento editoriale ed allestimento per la stampa: M.L. Vatovec, S. Falcetti Revisione informatizzazione dei dati geologici: L.
    [Show full text]
  • Report 2010-11
    Research Report 2010-2011 Research at Museo delle Scienze Science Science at Museo delle Scienze | Research Report 2010-2011 Science at Museo delle Scienze Research Report 2010-2011 MUSEO DELLE SCIENZE President Giuliano Castelli (Marco Andreatta since October 16th, 2011) Director Michele Lanzinger MdS Research Report 2010-2011 © 2012 Museo delle Scienze, Via Calepina 14, 38122 Trento, Italy Managing editor Valeria Lencioni Editorial committee Marco Avanzini, Costantino Bonomi, Marco Cantonati, Giampaolo Dalmeri, Valeria Lencioni, Paolo Pedrini, Francesco Rovero Editorial assistant Nicola Angeli Cover and layout design Roberto Nova Printing Tipografia Esperia Srl - Lavis (TN) 978-88-531-0019-1 SCIENCE at MUSEO DELLE SCIENZE RESEARCH REPOrt 2010-2011 5 Preface Part 1 7 1. Introducing MdS as museum and research centre 11 2. The research programmes 12 Programme 1R Ecology and biodiversity of mountain ecosystems in relation to environmental and climate change 12 Programme 2R Documenting and conserving nature 13 Programme 3R Plant conservation: seedbanking and plant translocation 13 Programme 4R Tropical Biodiversity 14 Programme 5R Earth sciences 14 Programme 6R Alpine Prehistory 15 3. The research staff and activities 19 4. The scientific collections 23 5. The main results and projects Part 2 57 Appendix 1: The staff of the scientific sections 85 Appendix 2: The staff of the science communicators 91 Appendix 3: Research projects, high education and teaching 105 Appendix 4: Publications 127 Appendix 5: Collaborations: the research national network 131 Appendix 6: Collaborations: the research international network Science at Museo delle Scienze: Research Report 2010-2011 1R 2R 3R 4R 5R 6R 4 Preface Fully developed as a natural history museum since the beginning of the 1900, the Museo Tridentino di Scienze Naturali, since May 2011 named Museo delle Scienze (MdS) over the past decade has developed a new cultural approach through innovative exhibitions and public programmes which prompted a wi- der interpretation of its strictly naturalistic institutional scope.
    [Show full text]
  • Why Didn't You Take Advantage of the Chance to Disco
    Are you looking for a unique experience to enrich your holiday in Trentino? Why didn't you take advantage of the chance to discover local wines and distillates along the Wine and Flavour Route of the Region? Here is the list of the open wineries during the weekends on June. We are waiting for you…Cheers! th Wednesday | 2nd JUNE Saturday | 5th JUNE Sunday | 6 JUNE Ala – Azienda Agricola La Cadalora Ala – Azienda Agricola La Cadalora Ala – Azienda Agricola La Cadalora Cembra Lisignago – Cembra cantina di montagna Cembra Lisignago – Cembra cantina di montagna Cembra Lisignago – Cembra cantina di montagna Lavis – Azienda Agricola Maso Grener Giovo - Villa Corniole Mezzocorona - Azienda Agricola Donati Marco Mezzocorona - Azienda Agricola Donati Marco Isera - Cantina d'Isera Riva del Garda - Comai - Azienda Agricola Riva del Garda - Cantina Agraria Riva del Garda Lavis – Azienda Agricola Maso Grener San Michele all'Adige - Cantina Endrizzi Riva del Garda - Comai - Azienda Agricola Lavis - Cantina La Vis Trento - Mas dei Chini San Michele all'Adige - Cantina Endrizzi Mezzocorona - Azienda Agricola Donati Marco Trento - Mas dei Chini Mezzocorona – Dorigati Nogaredo – Distilleria Marzadro Nogaredo – Vivallis Nomi - Azienda Agricola Grigoletti Riva del Garda - Cantina Agraria Riva del Garda Riva del Garda - Comai - Azienda Agricola Rovereto – Letrari Soc. Agr. San Michele all'Adige - Cantina Endrizzi Trento - Mas dei Chini Saturday | 12 th JUNE Sunday | 13 th JUNE Nogaredo – Distilleria Marzadro Ala – Azienda Agricola La Cadalora Ala – Azienda Agricola La Cadalora Nogaredo – Vivallis Cembra Lisignago – Cembra cantina di montagna Cembra Lisignago – Cembra cantina di montagna Nomi - Azienda Agricola Grigoletti Giovo - Villa Corniole Mezzocorona - Azienda Agricola Donati Marco Riva del Garda - Cantina Agraria Riva del Garda Isera - Cantina d'Isera Riva del Garda - Comai - Azienda Agricola Riva del Garda - Comai - Azienda Agricola Lavis – Azienda Agricola Maso Grener Rovereto – Letrari Soc.
    [Show full text]
  • An Early Cretaceous Astropectinid (Echinodermata, Asteroidea)
    Andean Geology 41 (1): 210-223. January, 2014 Andean Geology doi: 10.5027/andgeoV41n1-a0810.5027/andgeoV40n2-a?? formerly Revista Geológica de Chile www.andeangeology.cl An Early Cretaceous astropectinid (Echinodermata, Asteroidea) from Patagonia (Argentina): A new species and the oldest record of the family for the Southern Hemisphere Diana E. Fernández1, Damián E. Pérez2, Leticia Luci1, Martín A. Carrizo2 1 Instituto de Estudios Andinos Don Pablo Groeber (IDEAN-CONICET), Departamento de Ciencias Geológicas, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires, Intendente Güiraldes 2160, Pabellón 2, Ciudad Universitaria, Ciudad Autónoma de Buenos Aires, Argentina. [email protected]; [email protected] 2 Museo de Ciencias Naturales Bernardino Rivadavia, Ángel Gallardo 470, Ciudad Autónoma de Buenos Aires, Argentina. [email protected]; [email protected] ABSTRACT. Asterozoans are free living, star-shaped echinoderms which are important components of benthic marine faunas worldwide. Their fossil record is, however, poor and fragmentary, probably due to dissarticulation of ossicles. In particular, fossil asteroids are infrequent in South America. A new species of starfish is reported from the early Valanginian of the Mulichinco Formation, Neuquén Basin, in the context of a shallow-water, storm-dominated shoreface environment. The specimen belongs to the Astropectinidae, and was assigned to a new species within the genus Tethyaster Sladen, T. antares sp. nov., characterized by a R:r ratio of 2.43:1, rectangular marginals wider in the interbrachial angles, infero- marginals (28 pairs along a median arc) with slightly convex profile and flat spines (one per ossicle in the interbrachials and two per ossicle in the arms).
    [Show full text]
  • Exine Morphology and Ultrastructure of Duplicisporites from the Triassic of Italy
    Grana 44: 337–342, 2005 Exine morphology and ultrastructure of Duplicisporites from the Triassic of Italy NATALIA E. ZAVIALOVA and GUIDO ROGHI Zavialova, N. E. & Roghi, G. 2005. Exine morphology and ultrastructure of Duplicisporites from the Triassic of Italy. – Grana 44: 337–342. ISSN 0017-3134. A morphological study of dispersed Circumpolles pollen grains from the Upper Triassic of the Southern Alps has been initiated with the genus Duplicisporites. Individual pollen grains were studied by means of scanning electron microscopy (SEM) and transmission electron microscopy (TEM). Seen with SEM the pollen surface is finely verrucate with low verrucae of different sizes. A sub-equatorial continuous rimula is clearly visible. The proximal trilete scar is small and indistinct. TEM images reveal a bi-layered exine. The ectexine is formed by numerous small, closely packed, granulae subdivided by irregularly-spaced cavities. In the region of the subequatorial canal, the ectexine becomes thinner, about 1/3 of the usual thickness. At places, the ectexine is slightly separated from the underlying endexine. The endexine is prominent and significantly darker than the ectexine. It is homogeneous and of constant thickness. On the basis of its older age, with respect to Classopollis, the present ultrastructural dataset provides information on the possible origin of cheirolepidiaceous-type morphology. Natalia E. Zavialova*, Laboratory of Palaeobotany, Palaeontological Institute, Russian Academy of Sciences, Profsoyusnaya str., 123, Moscow, 117647 Russia & Guido Roghi, Institute of Geosciences and Earth Resources (IGG-CNR), Corso Garibaldi 37, Padova I -35137, Italy. *Corresp. Author (Manuscript received 19 November 2004; accepted 5 June 2005) The fossil pollen group Circumpolles is of interest to of Italy, Austria and Hungary have revealed rich palyno- palynologists and evolutionary biologists due to its complex logical assemblages, which contain members of Circum- morphology and parallelisms to angiospermoid characters polles (De Zanche et al.
    [Show full text]