Continent formation through time /
- 出版日期：2015.
- 出版者：The Geol. Soc.,
- 页数：362 pages :
- 出版地：London :
- 第一责任说明：edited by N.M.W. Roberts, NERC Isotope Geosciences Laboratory, UK, M. Van Kranendonk, University of New South Wales, Australia, S. Parman, Brown University, USA, S. Shirey, Carnegie Institution of Washington, USA, and P.D. Clift, Louisiana State University, USA.
- 尺寸：26 cm
- 分类号：a240
- ISBN：9781862393752(hardback) :
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02h0073298 20151124160134.0 151030s2015 enkab frb |001|||eng d 9781862393752(hardback) : CNY1181.00 CDX eng rda CDX OCLCQ ; FUG ; OCLCQ ; MUU ; EQO ; OCLCQ ; YDXCP ; ERL ; Z@L ; BTCTA ; OCLCF ; DLC ; CNNGL QE511 .C66 2015 551.13 23 a240 Continent formation through time / edited by N.M.W. Roberts, NERC Isotope Geosciences Laboratory, UK, M. Van Kranendonk, University of New South Wales, Australia, S. Parman, Brown University, USA, S. Shirey, Carnegie Institution of Washington, USA, and P.D. Clift, Louisiana State University, USA. London : The Geol. Soc., 2015. aLondon : bThe Geological Society, c2015. 362 pages : illustrations (some color), maps (some color) ; 26 cm atext btxt 2rdacontent aunmediated bn 2rdamedia avolume bnc 2rdacarrier Geological Society special publication, 0305-8719 ; no. 389 Includes bibliographical references and index. Geophysics and numerical modelling -- Geology and geochemistry -- Zircon. The continental crust is our archive of Earth history, and the store of many natural resources; however, many key questions about its formation and evolution remain debated and unresolved: What processes are involved in the formation, differentiation and evolution of continental crust, and how have these changed throughout Earth history? How are plate tectonics, the supercontinent cycle and mantle cooling linked with crustal evolution? What are the rates of generation and destruction of the continental crust through time? How representative is the preserved geological record? A range of approaches are used to address these questions, including field-based studies, petrology and geochemistry, geophysical methods, palaeomagnetism, whole-rock and accessory-phase isotope chemistry and geochronology. Case studies range from the Eoarchaean to Phanerozoic, and cover many different cratons and orogenic belts from across the continents. Continental crust ; Formations (Geology) History. ; History. aRoberts, N. M. W. ; q(Nick M. W.), ; eeditor. ; aVan Kranendonk, Martin, ; eeditor. ; aParman, S. ; q(Stephen), ; eeditor. ; aShirey, Steven Bottome, ; eeditor. ; aClift, P. D. ; q(Peter D.), ; eeditor. Geological Society special publication ; no. 389. aCN b010001 http://0-sp.lyellcollection.org.wam.leeds.ac.uk/content/389/1 View this book online, via Lyell Collection, both on- and off-campus 010001 P 206.4 Sp3p v389 ; h1 ; rCNY1181.00 gljx1506