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000725270 019__ $$a897115926$$a899276139$$a908082761
000725270 020__ $$a9783319113883$$qelectronic book
000725270 020__ $$a3319113887$$qelectronic book
000725270 0247_ $$a10.1007/978-3-319-11388-3$$2doi
000725270 035__ $$aSP(OCoLC)ocn900364209
000725270 035__ $$aSP(OCoLC)900364209$$z(OCoLC)897115926$$z(OCoLC)899276139$$z(OCoLC)908082761
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000725270 049__ $$aISEA
000725270 050_4 $$aQB601
000725270 050_4 $$aQB600-701
000725270 08204 $$a523.4$$223
000725270 1001_ $$aMalcuit, Robert J.,$$eauthor.
000725270 24514 $$aThe twin sister planets Venus and Earth$$h[electronic resource] :$$bwhy are they so different? /$$cRobert J. Malcuit.
000725270 264_1 $$aCham :$$bSpringer,$$c2015.
000725270 300__ $$a1 online resource (xix, 401 pages) :$$billustrations (some color)
000725270 336__ $$atext$$btxt$$2rdacontent
000725270 337__ $$acomputer$$bc$$2rdamedia
000725270 338__ $$aonline resource$$bcr$$2rdacarrier
000725270 347__ $$atext file$$bPDF$$2rda
000725270 504__ $$aIncludes bibliographical references and indexes.
000725270 5050_ $$aPreface; Acknowledgements; Contents; Chapter 1; Introduction; 1.1 The Scientific Method; 1.2 Some Special Features of Earth as a Planet; 1.3 Some Special Features of Venus as a Planet; References; Chapter 2; The Origin of the Sun and the Early Evolution of the Solar System; 2.1 List of Some Important Facts to be Explained by a Successful Model; 2.2 A Composite Working Model for Origin and Evolution of the Solar System; Summary; References; Chapter 3; Models for the Origin and Evolution of the Earth-Moon System; 3.1 List of Facts to be Explained by a Successful Model
000725270 5058_ $$a3.2 Fission from the Earth Early in Earth History3.3 Co-formation of the Earth and Moon from the Same Cloud of Dust and Gas; 3.4 Intact Capture of the Moon by the Earth (1952-1986); 3.5 Other Recent Attempts at Intact Capture; 3.6 Orbital Traceback Models Suggesting Intact Capture; 3.7 More on the Singer (1968) Model of Prograde Capture; 3.8 Disintegrative Capture Models; 3.9 A Miltiple-Small-Moon Model; 3.10 A New (Post-Kona) View of the Intact Capture Process; 3.11 Formation of the Moon Resulting from a Giant Impact Early in Earth History
000725270 5058_ $$a3.11.1 The Angular Momentum Problem of the Earth-Moon System3.11.2 The Oxygen Isotope Similarities Between Earth and Moon; 3.11.3 The Mass and Density of the Moon; 3.12 A Report Card for Models of Lunar Origin; References; Chapter4; A Prograde Gravitational Capture Model for℗ the Origin and Evolution of℗ the℗ Earth-Moon℗ System; 4.1 Place of Origin for Luna and Sibling Planetoids and a Model for Magnetization of the Crust of Luna and Sibling Vulcanoid Planetoids; 4.2 Migration History of Luna and Sibling Vulcanoid Planetoids; 4.2.1 Stability of Vulcanoid Planetoid Orbits
000725270 5058_ $$a4.2.2 Transfer of Vulcanoid Planetoids from Orbits of Origin to Venus-Earth Space4.2.3 Summary for the Transfer Scheme; 4.3 Prograde Gravitational Capture of Luna and the Subsequent Orbit Circularization: Two-Body Analysis and a Discussion of theParadoxes Associated with the Capture Process; 4.4 Numerical Simulations of Gravitational Capture of a Lunar-Like Body by an Earth-Like Planet; 4.4.1 Computer Code Information; 4.4.2 Development of the Computer Code; 4.4.3 A Sequence of Typical Orbital Encounter Scenarios Leading to a Stable Capture Scenario
000725270 5058_ $$a4.4.4 Geometry of Stable Capture Zones for Planetoids Being Captured by Planets4.4.5 The Post-Capture Orbit Circularization Calculation; 4.4.6 A Qualitative Model for Generation of a Mare-Age Lunar Magnetic Field; 4.4.7 Subsequent Orbit Expansion due to Angular Momentum Exchange between the Rotating Earth and the Lunar Orbit; 4.5 Summary and Statement of the Fourth Paradox; 4.6 Summary and Conclusions for the Chapter; Appendix; References; Chapter5; Some Critical Interpretations and℗ Misinterpretations of Lunar Features; 5.1 Discussion of Some Speculations of Harold Urey and℗ Zdenek Kopal
000725270 506__ $$aAccess limited to authorized users.
000725270 520__ $$aThis book explains how it came to be that Venus and Earth,℗ℓwhile very similar in chemical composition, zonation, size and heliocentric distance from the Sun, are very different in surface environmental conditions. It is argued here that these differences can be℗ℓaccounted for℗ℓby planetoid capture processes and the subsequent evolution of the planet-satellite system. Venus captured a one-half moon-mass planetoid early in its history in the retrograde direction and underwent its ℓ́ℓfatal attraction scenarioℓ́ℓ with its satellite (Adonis). ℗ℓEarth, on the other hand, captured a moon-mass planetoid (Luna) early in its history in prograde orbit and underwent a benign estrangement scenario with its captured satellite.
000725270 650_0 $$aGeography.
000725270 650_0 $$aGeochemistry.
000725270 650_0 $$aPlanetary science.
000725270 650_0 $$aGeology.
000725270 650_0 $$aExobiology.
000725270 651_0 $$aVenus (Planet)
000725270 651_0 $$aEarth (Planet)
000725270 77608 $$iPrint version:$$z9783319113876
000725270 852__ $$bebk
000725270 85640 $$3SpringerLink$$uhttps://univsouthin.idm.oclc.org/login?url=http://link.springer.com/10.1007/978-3-319-11388-3$$zOnline Access$$91397441.1
000725270 909CO $$ooai:library.usi.edu:725270$$pGLOBAL_SET
000725270 980__ $$aEBOOK
000725270 980__ $$aBIB
000725270 982__ $$aEbook
000725270 983__ $$aOnline
000725270 994__ $$a92$$bISE