000 06605nam a22006255i 4500
001 978-3-540-48684-8
003 DE-He213
005 20161121230825.0
007 cr nn 008mamaa
008 100301s2006 gw | s |||| 0|eng d
020 _a9783540486848
_9978-3-540-48684-8
024 7 _a10.1007/978-3-540-48684-8
_2doi
050 4 _aQE1-996.5
072 7 _aRBG
_2bicssc
072 7 _aSCI031000
_2bisacsh
082 0 4 _a551
_223
245 1 4 _aThe Andes
_h[electronic resource] :
_bActive Subduction Orogeny /
_cedited by Onno Oncken, Guillermo Chong, Gerhard Franz, Peter Giese, Hans-Jürgen Götze, Victor A. Ramos, Manfred R. Strecker, Peter Wigger.
264 1 _aBerlin, Heidelberg :
_bSpringer Berlin Heidelberg,
_c2006.
300 _aXXII, 569 p.
_bonline resource.
336 _atext
_btxt
_2rdacontent
337 _acomputer
_bc
_2rdamedia
338 _aonline resource
_bcr
_2rdacarrier
347 _atext file
_bPDF
_2rda
490 1 _aFrontiers in Earth Sciences,
_x1863-4621
505 0 _aThe Big Picture -- Deformation of the Central Andean Upper Plate System — Facts, Fiction, and Constraints for Plateau Models -- The Time-Space Distribution of Cenozoic Volcanism in the South-Central Andes: a New Data Compilation and Some Tectonic Implications -- Crustal Evolution at the Central Andean Continental Margin: a Geochemical Record of Crustal Growth, Recycling and Destruction -- Long-Term Signals in the Present-Day Deformation Field of the Central and Southern Andes and Constraints on the Viscosity of the Earth’s Upper Mantle -- Tectonic Processes along the Chile Convergent Margin -- Elements of the Subduction System -- Oblique Convergence along the Chilean Margin: Partitioning, Margin-Parallel Faulting and Force Interaction at the Plate Interface -- Seismic Images of Accretive and Erosive Subduction Zones from the Chilean Margin -- Geophysical Signatures and Active Tectonics at the South-Central Chilean Margin -- Latitudinal Variation in Sedimentary Processes in the Peru-Chile Trench off Central Chile -- Subduction Erosion — the “Normal” Mode of Fore-Arc Material Transfer along the Chilean Margin? -- Subduction Channel Evolution in Brittle Fore-Arc Wedges — a Combined Study with Scaled Sandbox Experiments, Seismological and Reflection Seismic Data and Geological Field Evidence -- Tectonics and Surface Processes — Responses to Change -- Tectonics, Climate, and Landscape Evolution of the Southern Central Andes: the Argentine Puna Plateau and Adjacent Regions between 22 and 30°S -- Exhumation and Basin Development Related to Formation of the Central Andean Plateau, 21° S -- The Salar de Atacama Basin: a Subsiding Block within the Western Edge of the Altiplano-Puna Plateau -- Upper-Crustal Structure of the Central Andes Inferred from Dip Curvature Analysis of Isostatic Residual Gravity -- Central and Southern Andean Tectonic Evolution Inferred from Arc Magmatism -- The Segmented Overriding Plate and Coupling at the South-Central Chilean Margin (36–42°S) -- Episodic Neogene Southward Growth of the Andean Subduction Orogen between 30°S and 40°S — Plate Motions, Mantle Flow, Climate, and Upper-Plate Structure -- Long-Term Geological Evolution and Mass-Flow Balance of the South-Central Andes -- Links between Mountain Uplift, Climate, and Surface Processes in the Southern Patagonian Andes -- The System at Depth: Images and Models -- Seismological Studies of the Central and Southern Andes -- Partial Melting in the Central Andean Crust: a Review of Geophysical, Petrophysical, and Petrologic Evidence -- Controls on the Deformation of the Central and Southern Andes (10–35° S): Insight from Thin-Sheet Numerical Modeling -- Numerical Study of Weakening Processes in the Central Andean Back-Arc -- Mechanism of the Andean Orogeny: Insight from Numerical Modeling -- The Andean Information System: Data, Maps and Movies -- Data Management of the SFB 267 for the Andes — from Ink and Paper to Digital Databases -- Digital Geological Map of the Central Andes between 20°S and 26°S -- Bouguer and Isostatic Maps of the Central Andes -- Digital Geological Map of the Southern and Central Puna Plateau, NW Argentina -- Morphotectonic and Geologic Digital Map Compilations of the South-Central Andes (36°–42°S) -- to the Attached DVD.
520 _aConvergent plate margins and subduction zones are first order features shaping the Earth. Convergent continental margins combine the majority of processes that affect the internal architecture thermal and geochemical character of continental lith- phere. In addition, the close relationships between active deformation and uplift, m- matism and associated crustal growth, ore formation, the release of more than 90% of global seismic energy at convergent margins, make these plate boundaries imp- tant natural laboratories where mass and energy flux rates can be studied at various scales. Since the advent of plate tectonic theory, it has been recognized that all of these phenomena are intimately related and often governed by feedback mechanisms. Accordingly, subduction orogeny has become an international, high-priority theme in process-oriented, earth-system analysis. In this context, Dewey and Bird (1970) have defined the Andes as the type representative for orogeny and associated p- cesses at convergent margins in their benchmark paper. The Andes, therefore, p- vide an excellent natural laboratory for studying the above processes.
650 0 _aEarth sciences.
650 0 _aGeology.
650 0 _aSedimentology.
650 0 _aGeophysics.
650 0 _aAtmospheric sciences.
650 0 _aGeographical information systems.
650 1 4 _aEarth Sciences.
650 2 4 _aGeology.
650 2 4 _aGeophysics/Geodesy.
650 2 4 _aEarth Sciences, general.
650 2 4 _aSedimentology.
650 2 4 _aGeographical Information Systems/Cartography.
650 2 4 _aAtmospheric Sciences.
700 1 _aOncken, Onno.
_eeditor.
700 1 _aChong, Guillermo.
_eeditor.
700 1 _aFranz, Gerhard.
_eeditor.
700 1 _aGiese, Peter.
_eeditor.
700 1 _aGötze, Hans-Jürgen.
_eeditor.
700 1 _aRamos, Victor A.
_eeditor.
700 1 _aStrecker, Manfred R.
_eeditor.
700 1 _aWigger, Peter.
_eeditor.
710 2 _aSpringerLink (Online service)
773 0 _tSpringer eBooks
776 0 8 _iPrinted edition:
_z9783540243298
830 0 _aFrontiers in Earth Sciences,
_x1863-4621
856 4 0 _uhttp://dx.doi.org/10.1007/978-3-540-48684-8
912 _aZDB-2-EES
950 _aEarth and Environmental Science (Springer-11646)
999 _c504514
_d504514