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PROGETTO ANTARTIDE Rapporto Sulla Campagna Antartica Estate Australe 1996
PROGRAMMA NAZIONALE DI RICERCHE IN ANTARTIDE Rapporto sulla Campagna Antartica Estate Australe 1996 - 97 Dodicesima Spedizione PROGETTO ANTARTIDE ANT 97/02 PROGRAMMA NAZIONALE DI RICERCHE IN ANTARTIDE Rapporto sulla Campagna Antartica Estate Australe 1996 - 97 Dodicesima Spedizione A cura di J. Mϋller, T. Pugliatti, M.C. Ramorino, C.A. Ricci PROGETTO ANTARTIDE ENEA - Progetto Antartide Via Anguillarese,301 c.p.2400,00100 Roma A.D. Tel.: 06-30484816,Fax:06-30484893,E-mail:[email protected] I N D I C E Premessa SETTORE 1 - EVOLUZIONE GEOLOGICA DEL CONTINENTE ANTARTICO E DELL'OCEANO MERIDIONALE Area Tematica 1a Evoluzione Geologica del Continente Antartico Progetto 1a.1 Evoluzione del cratone est-antartico e del margine paleo-pacifico del Gondwana.3 Progetto 1a.2 Evoluzione mesozoica e cenozoica del Mare di Ross ed aree adiacenti..............11 Progetto 1a.3 Magmatismo Cenozoico del margine occidentale antartico..................................17 Progetto 1a.4 Cartografia geologica, geomorfologica e geofisica ...............................................18 Area Tematica 1b-c Margini della Placca Antartica e Bacini Periantartici Progetto 1b-c.1 Strutture crostali ed evoluzione cenozoica della Penisola Antartica e del margine coniugato cileno ......................................................................................25 Progetto 1b-c.2 Indagini geofisiche sul sistema deposizionale glaciale al margine pacifico della Penisola Antartica.........................................................................................42 -
Abstract List – Poster (Mon/Tue)
Abstract List – Poster (Mon/Tue) 5 Poster Presentation No. Day Time Presenter E-mail Institution/Organization Abstract no. Session no. Title 1 MON/TUE 13:45-15:00 Seongchan Hong [email protected] Korea University, Korea A088 01 OSL dating of raised beach in Terra Nova Bay, Antarctica with tectonic implications 2 MON/TUE 13:45-15:00 Jeremy Lee [email protected] University of Melbourne, Australia A183 01 Revisiting the Admiralty Suite and its link to southeastern Australia 3 MON/TUE 13:45-15:00 Yingchun Cui [email protected] First Institute of Oceanography, MNR, China A194 01 The early Paleozoic magmatism in northern Victoria Land, Antarctica 4 MON/TUE 13:45-15:00 Taeyoon Park [email protected] Korea Polar Research Institute, Korea A235 01 Jurassic phreatoicid isopods from Victoria Land, Antarctica 5 MON/TUE 13:45-15:00 Changhwan Oh [email protected] Chungbuk National University, Korea A236 01 New occurrence of Triassic gymnosperm wood at the Ricker Hills, southern Victoria Land, Antarctica 6 MON/TUE 13:45-15:00 Sangbong Yi [email protected] Korea Polar Research Institute, Korea A251 01 Paleozoic metamorphism identified in the Mountaineer Range of northern Victoria Land, Antarctica 7 MON/TUE 13:45-15:00 Simon Cox [email protected] GNS Science, New Zealand A254 01 The Convoy Range mapping project, Victoria Land, Antarctica Federal institute for geosciences and natural resources (BGR), Dating the Granite Harbour Intrusives of northern Victoria Land (Antarctica) - Magmatic ages, inheritance 8 MON/TUE 13:45-15:00 Andreas Laeufer -
USGS Open-File Report 2007-1047 Extended Abstract
U.S. Geological Survey and The National Academies; USGS OF-2007-1047, Extended Abstract 043 Inside the Granite Harbour Intrusives of northern Victoria Land: Timing and origin of the intrusive sequence R. M. Bomparola and C. Ghezzo Dipartimento di Scienze della Terra, Università di Siena, via Laterina 8, 53100 Siena, Italy, [email protected] Summary Cambro-Ordovician Granite Harbour Intrusives define, in northern Victoria Land, a complex intrusive sequence composed of metaluminous and peraluminous granitoids, and minor ultramafic and mafic rocks, with variable K-enrichment and magmatic arc affinity. The main intrusive units cropping out in the Wilson Terrane between the Prince Albert Mountains and the Mountaineer Range have been dated by means of in-situ U-Pb LA -ICPMS analyses of zircons. The obtained results constrain the timing of emplacement of major crustal-derived anatectic melts in this area between 521 and 481 Ma, a time interval of 40 Ma. The mantle -derived mafic-ultramafic rocks, associated to the main high-K granitoids in the Deep Freeze Range-Northern Foothills, cover a time interval between 521 and 487 Ma. The long-lasting intrusive mafic and felsic magmatism caused the slow cooling of the basement responsible, together with local deformation and fluid circulation, of the common young reset ages observed in some of the studied intrusions. Citation: Bomparola, R. M. and Ghezzo, C. (2007), Guidelines for extended abstracts in the 10th ISAES X Online Proceedings, in Antarctica: A Keystone in a Changing World – Online Proceedings of the 10th ISAES X, edited by A. K. Cooper and C. R. Raymond et al., USGS Open-File Report 2007-1047, Extended Abstract 043, 4 p. -
High Altitude Geothermal Sites Of
Measure 13 (2014) Annex Management Plan For Antarctic Specially Protected Area No. 175 HIGH ALTITUDE GEOTHERMAL SITES OF THE ROSS SEA REGION (including parts of the summits of Mount Erebus, Ross Island and Mount Melbourne and Mount Rittmann, northern Victoria Land) Introduction: There exist a few isolated sites in Antarctica where the ground surface is warmed by geothermal activity above the ambient air temperature. Steam emissions from fumaroles (openings at the Earth’s surface that emit steam and gases) condense forming a regular supply of water which, coupled with warm soil temperatures, provides an environment that selects for a unique and diverse assemblage of organisms. Geothermal sites are rare and small in extent covering no more than a few hectares on the Antarctic continent and circumpolar islands (or maritime sites). The biological communities that occur at continental geothermal sites are at high altitude and differ markedly to those communities that occur at maritime geothermal sites due to the differences in the abiotic environment. There are three high altitude geothermal sites in the Ross Sea region, known to have unique biological communities. These are the summits of Mount Erebus, on Ross Island, and Mount Melbourne and Mount Rittmann, both in northern Victoria Land. The only other known high altitude site in Antarctica where evidence of fumarolic activity has been seen is at Mount Berlin in Marie Byrd Land, West Antarctica, although no biological research has been conducted at this site. High altitude geothermal sites are vulnerable to the introduction of new species, particularly from human vectors, as they present an environment where organisms typical of more temperate regions can survive. -
Management Plan for Antarctic Specially Protected Area No. 175
Measure 13 (2014) Annex Management Plan For Antarctic Specially Protected Area No. 175 HIGH ALTITUDE GEOTHERMAL SITES OF THE ROSS SEA REGION (including parts of the summits of Mount Erebus, Ross Island and Mount Melbourne and Mount Rittmann, northern Victoria Land) Introduction: There exist a few isolated sites in Antarctica where the ground surface is warmed by geothermal activity above the ambient air temperature. Steam emissions from fumaroles (openings at the Earth’s surface that emit steam and gases) condense forming a regular supply of water which, coupled with warm soil temperatures, provides an environment that selects for a unique and diverse assemblage of organisms. Geothermal sites are rare and small in extent covering no more than a few hectares on the Antarctic continent and circumpolar islands (or maritime sites). The biological communities that occur at continental geothermal sites are at high altitude and differ markedly to those communities that occur at maritime geothermal sites due to the differences in the abiotic environment. There are three high altitude geothermal sites in the Ross Sea region, known to have unique biological communities. These are the summits of Mount Erebus, on Ross Island, and Mount Melbourne and Mount Rittmann, both in northern Victoria Land. The only other known high altitude site in Antarctica where evidence of fumarolic activity has been seen is at Mount Berlin in Marie Byrd Land, West Antarctica, although no biological research has been conducted at this site. High altitude geothermal sites are vulnerable to the introduction of new species, particularly from human vectors, as they present an environment where organisms typical of more temperate regions can survive. -
The Antarctic Treaty
The Antarctic Treaty Measures adopted at the Thirty-seventh Consultative Meeting held at Brasilia 28 April – 07 May 2014 Presented to Parliament by the Secretary of State for Foreign and Commonwealth Affairs by Command of Her Majesty December 2015 Cm 9150 © Crown copyright 2015 This publication is licensed under the terms of the Open Government Licence v3.0 except where otherwise stated. To view this licence, visit www.nationalarchives.gov.uk/doc/open-government- licence/version/3/ or write to the Information Policy Team, The National Archives, Kew, London TW9 4DU, or email: [email protected] Where we have identified any third party copyright information you will need to obtain permission from the copyright holders concerned. This publication is available at www.gov.uk/government/publications Any enquiries regarding this publication should be sent to us at Treaty Section, Foreign and Commonwealth Office, King Charles Street, London, SW1A 2AH Print ISBN 9781474125475 Web ISBN 9781474125482 Printed in the UK by the Williams Lea Group on behalf of the Controller of Her Majesty’s Stationery Office ID P002767088 12/15 51958 19585 Printed on paper containing 30% recycled fibre content minimum MEASURES ADOPTED AT THE THIRTY-SEVENTH ANTARCTIC TREATY CONSULTATIVE MEETING Brasilia, Brazil, 28 April - 07 May 2014 The Measures1 adopted at the Thirty-seventh Antarctic Treaty Consultative Meeting are reproduced below from the Final Report of the Meeting. In accordance with Article IX, paragraph 4, of the Antarctic Treaty, the Measures adopted at Consultative Meetings become effective upon approval by all Contracting Parties whose representatives were entitled to participate in the meeting at which they were adopted (i.e. -
No Printed Publication, Digital Data Only
Gazetteer of German-language Antarctic place-names, Third Edition, Version 3.1 (no printed publication, digital data only) – Complete revision of the Second Edition according to the specifications of the SCAR Composite Gazetteer of Antarctica (CGA), with contributions by Karsten Brunk, Rosbach v.d. Höhe, compiled and arranged by Jörn Sievers, Neu-Isenburg, on behalf of Ständiger Ausschuss für geographische Namen (StAGN), Frankfurt am Main, 2021-JUN-08 BKG- Alti- BKG-Nr. Place name Feature type Latitude Longitude Date approved Country Quelle tude 482 Acapulcofelsen 27, 30, 31 Cliff -70,5500000 164,0333333 200 1985-APR-19 Germany 499 Adlerwand 28, 30, 31 Bluff -73,2500000 167,1833333 800 1985-APR-19 Germany 515 Aklestadberg 28, 30, 31 Mountain -72,8166667 166,3000000 2450 1985-APR-19 Germany 5 Alexander-von-Humboldt- 25 Range -71,6666667 11,5000000 2895 1952-JUL-12 Germany Gebirge 33 Altar 25 Mountain -71,6500000 11,3833333 2200 1952-JUL-12 Germany 35 Am Überlauf 25 Pass -71,5500000 11,6166667 1700 1952-JUL-12 Germany 92 Amelangplatte 25 Mountain -74,0833333 -5,6666667 2430 1952-JUL-12 Germany 540 Ampfererberg 28, 30, 31 Mountain -72,8000000 167,3166667 3080 1985-APR-19 Germany 481 Andalusitgrat 27, 30, 31 Ridge -71,5500000 160,1666667 2100 1985-APR-19 Germany 548 Armbrustspitze 28, 30, 31 Peak -73,4166667 166,9333333 1290 1985-APR-19 Germany 678 Atka-Eiskuppel 46, 50, 51 Ice rise -70,7000000 -7,8333333 83 1990-APR-02 Germany 1 Gazetteer of German-language Antarctic place-names, Third Edition (no printed publication, digital data only) – Complete revision of the Second Edition according to the specifications of the SCAR Composite Gazetteer of Antarctica (CGA), with contributions by Karsten Brunk, Rosbach v.d. -
Programma Nazionale Di Ricerche in Antartide
PROGRAMMA NAZIONALE DI RICERCHE IN ANTARTIDE Rapporto sulla campagna antartica Estate Australe 1988 - 89 A cura di G. Casazza, col contributo dei partecipanti alla Spedizione ENEA PAS PROGETTO ANTARTIDE Casaccia - S.P. Anguillarese 301 - Cas. Post. 2400 00100 ROMA - Telex 613290 ENEACA I - Tel. (06)30484816 ANT 89/4 INDICE Pag. 1. - INTRODUZIONE 1.1 - Obiettivi della Spedizione 4 1.2 - Principali adempimenti istituzionali 5 1.3 - Programma 1988/89 5 1.4 – Finanziamenti 5 2. - PROGRAMMI DI RICERCA SCIENTIFICA Sommario 6 2.1-IV Spedizione a Baia Terra Nova 6 - Introduzione 6 2.1.1 - Oceanografia 8 2.1.2 - Fisica dell'atmosfera e meteorologia 11 1- Climatologia 11 2- Aerosol e Spettrofotometria 12 3- Sodar 13 4- Meteorologia 14 5- Analisi e Previsioni Meteo 14 2.1.3.- Scienze della Terra 21 1- Geologia regionale, Tettonica, Stratigrafia, Cartografia geologica e Telerilevamento; 22 2- Petrologia, Geochimica e Metallogenesi del Basamento igneo e metamorfico; 24 3- Vulcanologia e Geotermia; 25 4- Geomorfologia, Glaciologia, Paleoclimatologia; 28 5- Geomagnetismo, Gravimetria; 30 6- Osservatori Geofisici. 32 2.1.4 - Biologia 42 1- Floristica 42 2- Faunistica 43 3- Limnologia 44 4- Biologia evoluzionistica 44 5- Fisiologia e Tossicologia 45 6- Biochimica dell'adattamento 46 2.1.5 - Impatto ambientale - Metodologie chimiche 52 2.1.6.- Impatto ambientale a terra 55 2.2.- Ricerche geofisiche a mare condotte dalla M/V OGS-Explora 60 2.3 - Esperienza LIDAR presso la Base americana Amundsen-Scott (Polo Sud). 65 2.4 - Esperienza LIDAR presso la Base francese di Dumont D'Urville. 65 2.5 - Campagna oceanografica EPOS, a bordo della M/V Polarstem. -
Gazetteer of the Antarctic
NOIJ.VQNn OJ3ON3133^1 VNOI±VN r o CO ] ] Q) 1 £Q> : 0) >J N , CO O The National Science Foundation has TDD (Telephonic Device for the Deaf) capability, which enables individuals with hearing impairment to communicate with the Division of Personnel and Management about NSF programs, employment, or general information. This number is (202) 357-7492. GAZETTEER OF THE ANTARCTIC Fourth Edition names approved by the UNITED STATES BOARD ON GEOGRAPHIC NAMES a cooperative project of the DEFENSE MAPPING AGENCY Hydrographic/Topographic Center Washington, D. C. 20315 UNITED STATES GEOLOGICAL SURVEY National Mapping Division Reston, Virginia 22092 NATIONAL SCIENCE FOUNDATION Division of Polar Programs Washington, D. C. 20550 1989 STOCK NO. GAZGNANTARCS UNITED STATES BOARD ON GEOGRAPHIC NAMES Rupert B. Southard, Chairman Ralph E. Ehrenberg, Vice Chairman Richard R. Randall, Executive Secretary Department of Agriculture .................................................... Sterling J. Wilcox, member Donald D. Loff, deputy Anne Griesemer, deputy Department of Commerce .................................................... Charles E. Harrington, member Richard L. Forstall, deputy Henry Tom, deputy Edward L. Gates, Jr., deputy Department of Defense ....................................................... Thomas K. Coghlan, member Carl Nelius, deputy Lois Winneberger, deputy Department of the Interior .................................................... Rupert B. Southard, member Tracy A. Fortmann, deputy David E. Meier, deputy Joel L. Morrison, deputy Department -
Rock Mapping of Glaciated Areas by Satellite Image Processing
Rock mapping of glaciated areas by satellite image processing FRANCESCO SALVINI. ROBERTO DELLA MAGGIORE, LUCIAN0 FORTUNATI, and FRANCESCO MAZZARINI Salvini. F., della Maggiore, R., Fortunati, L. & Mazzarini, F. 1994: Rock Mapping of Glaciated Areas by Satellite Image Processing. Polar Research 13, 23-33. A model is presented that performs spectral deicing of mixed pixels in satellite images of glaciated areas. The model was tested in Northern Victoria Land, Antarctica. For this region we assumed that pixels could be grouped in two broad categories representing pure ice and pure rock. Naturally mixed ice and rock pixels are present in satellite images; these were recomputed to separate the spectral component related to the rock fraction. We used Landsat TM images as input data and aerial photographs, maps and field surveys as reference data. By making use of sample populations of pixels corresponding to pure ice and to pure rock groundels (it. ground elements, the ground portions corresponding to each pixel), we detected the linear correlation between pairs of bands and selected the two most suitable bands. For every pixel falling between the correlation lines of the two categories, the rock fraction in the corresponding groundel was computed. This fractional value was then used to perform the automatic deicing process with which the DNs of the selected mixed pixels were recomputed. In the utilised Antarctic image, this process increases about 2.7 times the number of pixels in the pure rock category, allowing the production of enhanced images and, as a side product, a thematic map of rock percentage in the groundels. F. -
COMPOSITE GAZETTEER of ANTARCTICA (CGA) Draft Of
Draft July 2002 Letter “A” only COMPOSITE GAZETTEER OF ANTARCTICA (CGA) Draft of Volume 2, letter A only Shanghai, July 2002 1 . 2 INTRODUCTION From 1998 to 2000 At the meeting of the WG on Geodesy and Geographic Information held in Concepción, Chile, July 1998, the first edition of the SCAR Composite Gazetteer of Antarctica (CGA) was presented and discussed. As a consequence of the discussion, the WG decided the upgrading of the CGA in order to include in future editions the dates of approval of names and the descriptions of the geographical features. All Member Countries were asked to send their contributions to the Italian team charged with the new task. An additional requirement, mainly addressed to those Countries that had already got the required supplementary information in their Gazetteers, was that the descriptions should be shortened in order to not exceed, on the average, 300 characters. The request was issued on 15 June 1999. At the meeting of the WG Program Leaders held in Heppenheim, Germany, July 1999, the difficulties of assembling a large amount of data in a comparatively short time appeared quite evident. It was decided, accordingly, that only the geographical names beginning with the letter "A" should be taken into consideration at the present stage. During the two year span between Concepción meeting (1998) and Tokyo meeting (2000) the work on the CGA went on along two lines: on the one side, dates of approval and descriptions were added to existing names; on the other side, new names were collected and included in the CGA, those new names coming most often complete with dates and descriptions.