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|a 978354076035
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|c WAA
|a WAA
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|a spa
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|a Frisch, Wolfgang
|9 21051
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|a Plate tectonics :
|b continental drift and mountain building /
|c Wolfgang Frisch, Martin Meschede and Ronald Blakey
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250 |
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|a 1st ed.
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260 |
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|a Berlin :
|b Springer,
|c 2011
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300 |
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|a 212 p. :
|b il., grafs., maps. ;
|c 29 cm.
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500 |
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|a Incluye índice analítico
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505 |
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|a 1. Contractional theory, continental drift and plate tectonics -- Plate tectonics – a change in the paradigm of the geosciences -- Early history of geodynamic thought -- From continental drift to plate tectonics -- The plate tectonic concept -- The pattern of magnetic polarity stripes -- Plate motions and earthquake zones -- Two kinds of continental margins -- Magmatism and plate tectonics -- What drives the plates and what slows them down? -- Collision and mountain building -- 2. Plate movements and their geometric relationships -- Helpful transform faults -- Relative movements and triple junctions -- Two RTF triple junctions off North America -- Relative plate velocities – past and present -- Direct measurement of plate movements -- Apparent contradictions in the plate motion pattern -- Fault-plane-solutions of earthquakes -- Seismic tomography -- 3. Continental graben structures -- Active and passive graben structures -- Symmetric and asymmetric crustal extension -- Sediments and ore deposits in graben structures -- Volcanism in graben structures -- The Upper Rhine Graben in Germany -- The history of the Upper Rhine Graben -- The Upper Rhine Graben in the Middle European stress field -- Magmatism and heat fl ow in the Upper Rhine Graben -- The large East African rift system -- The Afar Depression -- The Red Sea – from rift to drift -- The extensional area of the Basin and Range Province -- The development of metamorphic domes -- A brief history of the Basin and Range Province -- 4. Passive continental margins and abyssal plains -- Continuous subsidence of the continental margins -- The sedimentary trap at a passive continental margin -- Tracts of sequence stratigraphy -- Processes on continental margins -- Petroleum deposits – the economic signifi - cance of passive continental margins -- The Atlantic – an ocean opens in an intricate manner -- Pangaea and Panthalassa -- The large abyssal plains -- Sediments of the abyssal plains -- Manganese nodules from the deep sea -- Facies changes on the large oceanic conveyor belt -- Th e Bengal deep sea fan -- 5. Mid-ocean ridges -- Topography of the ridges -- Generation of oceanic lithosphere -- Rocks of the oceanic crust -- Pillow lavas -- Seismic layers -- Basalts of mid-ocean ridges -- Fast and slow spreading ridges and rocks of the lithospheric mantle -- Segmentation of ridges by faults -- Graben formation in the Atlantic -- An oceanic crustal profi le in the Atlantic Ocean -- Black and white smokers -- Ocean fl oor metamorphism -- Chromite deposits -- Ophiolites -- The ophiolite of the Semail Nappe in Oman -- Metamorphic sole -- Alpine-Mediterranean ophiolites -- 6. Hot spots -- Hot spots and mid-ocean ridges -- The mysterious D'' layer and the dented Earth -- Hot spots of Pangaea -- Hot spot tracks in the ocean -- A guyot evolves -- Hot spot tracks on the continent -- Flood and trap basalts -- The Azores – hot, cold or wet spot? -- Hawaii – a typical oceanic hot spot -- Iceland -- Yellowstone -- The superplume event in the Cretaceous -- 7 Subduction zones, island arcs and active continental margins -- Structure of plate margin systems with subduction zones -- Spontaneous and forced subduction: Mariana- and Chile-type subduction -- Deep sea trenches as sediment traps -- Accretionary wedge and outer ridge -- Th e accretionary wedge of the Sunda Arc -- Subduction erosion instead of accretion -- The forearc basin -- Earthquakes and Benioff zones -- The secret of deep earthquakes -- High-pressure or subduction metamorphism -- Ultrahigh-pressure meta morphic rocks -- Rapid burial, rapid uplift -- Subduction-related magmatism – a paradox? -- Rocks of the magmatic zone -- Zonation of magmas in space and time -- Explosive stratovolcanoes as indicators for subduction magmatism -- Metamorphism in the magmatic belt -- Paired metamorphic belts -- Ore deposits in the magmatic belt -- The backarc basin -- Splitting of intra-oceanic island arcs -- Gravity and heat flow -- Subduction and collision -- 8 Transform faults -- Oceanic transform faults -- Fracture zones in the ocean floor -- Continental transform faults -- San Andreas – the infamous transform fault of California -- The North Anatolian Fault in Asia Minor and the Alpine Fault in New Zealand -- 9. Terranes -- Documenting terranes -- Terranes in the North American Cordillera -- Suspect terranes in Mexico and Middle America -- 10. Early Precambrian plate tectonics -- Th e oldest rocks and minerals -- Greenstone-granite belts -- Granulite-gneiss belts -- Towards an Archean plate tectonic model -- The growth of continents -- Possible younger equivalents of greenstone-granite belts -- 11. Plate tectonics and mountain building -- Types of active continental margins within orogenic styles -- Continent-continent collision -- Uplift , erosion, and elevation of mountains -- Collapse and crustal escape -- 12. Old orogens -- 2500–2000 million years old ophiolites -- The Wopmay orogen in Canada -- The Grenville orogenic cycle and the formation of the supercontinent Rodinia -- The Panafrican orogeny and the formation of Gondwana -- The Caledonides – a Wilson cycle around the Iapetus Ocean -- The signifi cance of Scotland and the Greek mythology -- The Variscides – a broad mountain belt in central Europe -- A Variscan suture in the southern Black Forest -- The Variscan orogen in the Alps -- Paleozoic mountain building in eastern and southern North America -- How many orogenies? -- 13. Young orogens – the Earth’s loftiest places -- The Himalayas – a mountain range with superlatives -- Tectonic history of the Himalayas -- Nanga Parbat and Namche Barwa syntaxis -- The Alps – an untypical but classic orogen -- Brief history of Alpine evolution -- Lateral tectonic extrusion in the Alps -- The North American Cordillera – a diff erent style of orogen -- Laramide Rocky Mountains – an orogenic mystery solved.
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650 |
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0 |
|a Geología
|9 1052
|
650 |
|
0 |
|a Geodinámica
|9 1050
|
650 |
|
0 |
|a Corteza terrestre
|9 1035
|
700 |
1 |
|
|a Meschede, Martin
|9 21052
|
700 |
1 |
|
|a Blakey, Ronald
|9 21053
|
942 |
|
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