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LEADER 00000cam  2200553Ii 4500 
001    676700680 
003    OCoLC 
005    20181101045515.3 
006    m     o  d         
007    cr cn||||||||| 
008    101101s2010    ne abc  ob    001 0 eng d 
010    2010931610 
019    670292522|a771422726|a771422727|a780394585|a908039521
020    9789048193905|q(electronic bk.) 
020    9048193907|q(electronic bk.) 
020    |z9781402084065 
020    |z1402084064 
035    (OCoLC)676700680|z(OCoLC)670292522|z(OCoLC)771422726
037    978-1-4020-8406-5|bSpringer|n 
040    GW5XE|beng|epn|erda|cGW5XE|dEBLCP|dYDXCP|dCEF|dOCLCQ|dMHW
043    t------ 
049    MAIN 
050  4 QE350|b.F38 2010 
072  7 SCI|x019000|2bisacsh 
082 04 559.89|222 
100 1  Faure, Gunter.|0
245 14 The transantarctic mountains :|brocks, ice, meteorites and
       water /|cGunter Faure, Teresa M. Mensing. 
264  1 Dordrecht ;|aNew York :|bSpringer,|c2010. 
300    1 online resource (xxvi, 804 pages) :|billustrations (some
       color), maps (some color), portraits (some color) 
336    text|btxt|2rdacontent 
337    computer|bc|2rdamedia 
338    online resource|bcr|2rdacarrier 
340    |gpolychrome|2rdacc|0
347    text file|2rdaft|0
504    Includes bibliographical references and indexes. 
505 0  Chapter 1: The Exploration of Antarctica; Chapter 2: 
       Antarctica: The Continent; Chapter 3: Southern Victoria 
       Land; Basement Rocks; Chapter 4: Northern Victoria Land; 
       Chapter 5: Central Transantarctic Mountains; Chapter 6: 
       The Queen Maud Mountains; Chapter 7: Horlick Mountains; 
       Chapter 8: The Far-Eastern Mountains; Chapter 9: From 
       Rodinia to Gondwana; Chapter 10: The Beacon Supergroup; 
       Chapter 11: Beacon Supergroup; Special topics; Chapter 12:
       The Ferrar Group: Kirkpatrick Basalt; Chapter 13: Ferrar 
       Group: Dolerite Sills and the Dufek Intrusion; Chapter 14:
       Kirwan Volcanics, Queen Maud Land. 
520    This book is intended for Earth scientists who want to do 
       fieldwork in the Transantarctic Mountains or who are 
       interested in the geology of this region. The 
       Transantarctic Mountains are relevant even from a global 
       perspective because most of the rocks of which they are 
       composed formed at a time when Antarctica was an integral 
       part of the supercontinent of Gondwana, which subsequently
       broke apart during the Mesozoic Era to form the continents
       of the southern hemisphere. The first two chapters 
       summarize the history of exploration of Antarctica leading
       up to the signing of the Antarctic Treaty (C. 
588 0  Print version record. 
650  0 Geology|zAntarctica|0
       subjects/sh2008117897|zTransantarctic Mountains.|0http:// 
651  0 Transantarctic Mountains (Antarctica)|0
651  0 Transantarctic Mountains (Antarctica)|0
       authorities/subjects/sh85136872|xDiscovery and 
655  4 Electronic books. 
700 1  Mensing, Teresa M.|0
776 08 |iPrint version:|aFaure, Gunter.|tTransantarctic 
       Mountains.|dDordrecht ; New York : Springer, 2010
990    SpringerLink|bSpringer English/International eBooks 2011 -
       Full Set|c2018-10-31|yNew collection 
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