Earth as an Evolving Planetary System

  • Format
  • Bog, paperback
  • Engelsk

Beskrivelse

Earth as an Evolving Planetary System, Fourth Edition discusses key topics dealing with the evolution and interaction through time of Earth’s crust, mantle, core, atmosphere, hydrosphere, and biosphere. It addresses the questions of why Earth is unique among planets of the solar system, and how the various subsystems in the planet have interacted over 4.6 billion years in the habitable planet that we live on. This new edition includes over 100 new pages of material, data, and images and is a key reference for students and researchers in Earth and planetary sciences. Earth as an Evolving Planetary System, Fourth Edition includes new material that has become available since the third edition, including new sections on the Mid-lithosphere discontinuity, geoneutrinos, mantle oxidation, continental emergence, Earth cycles (new chapter) and recycling processes, the evolution of Earth from a stagnant lid to a plate tectonic regime, the controversy over how the continents have grown, when plate tectonics began, and exoplanets.

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Detaljer
  • SprogEngelsk
  • Sidetal406
  • Udgivelsesdato23-09-2021
  • ISBN139780128199145
  • Forlag Academic Press Inc
  • FormatPaperback
Størrelse og vægt
  • Vægt1000 g
  • coffee cup img
    10 cm
    book img
    21,6 cm
    27,6 cm

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    Mars Venus Satellite Asteroid Suture Photosynthesis Core Solar system Exhumation Mercury Mesosphere Plate tectonics Tree of life Planetary volcanism Crust Sea level Continental crust Stromatolites Lithosphere Mantle Sulfur Isotopes Mantle plume Feedback Loops RNA world Ophiolite Geodynamo Paleoclimate Heat Flow Meteorite Earth System Passive Margin Comet Hotspot Carbon cycle Cambrian Explosion Habitable zone Accretionary prism Mantle Convection Craton Arc Extrasolar planet Supercontinent Moho Mass extinction Planetary atmospheres Eukaryotes Rodinia Mineral deposit Transition zone Asthenosphere Accretionary orogen Ancient glaciations Back-arc basin Archean Greenstone Carbon isotope anomaly Atmospheric evolution Continental growth rate Core temperature Crustal type Crustal province Crustal recycling Crustal xenoliths Convergent margin Core age Crustal age gap Crustal origin Earth accretion Earth components Earth Cycles Crustal composition Crustal melting Crustal rheology Crustal secular changes Extinct radioactivity Detrital zircon ages Foreland Basin Flood basalt Earth uniqueness Collisional orogen Comparative planetary evolution Continental size Energy deposit Core origin Episodic zircon ages Cratonization Heat flow age dependency heat production Core composition Core formation Gondwana-Pangea Hotspot volcanism D? layer Earth’s oldest rocks Inner-core anisotropy High-pressure metamorphism Hinterland basin Earth’s thermal history Lithosphere evolution Large igneous province (LIP) Mantle xenolith Juvenile crust production rate Mantle secular changes Mantle transition zone Large low S-wave velocity province Mineral evolution LIP event Oceanic plateau Mantle seismic structure Mantle temperature Giant dyke swarm Oceanic Crust Ocean ridge Hadean crust orogen Paleoclimate feedbacks impact chronology Oceanic island Plate driving forces great events Proterozoic euxinic oceans Seawater temperature Ir anomalies Seismic crustal structure terrane Supercontinent assembly Interacting Earth systems Solar nebula Sr isotopes Supercontinent breakup Supercontinent cycle Mantle geochemical component Metazoan origin Planetary growth Plate Boundaries Magnetic reversals Mantle water Primitive atmosphere Nuna Petrotectonic assemblage Seismic discontinuity Secular changes seawater composition

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