Isostasy and Flexure of the LithosphereThis unique book presents an overview of isostasy, a phenomenon of fundamental importance to the earth sciences. Isostasy is a simple concept, yet it has long perplexed students. To overcome this problem, the author uses a simplified mathematical treatment, numerous geological examples and an extensive bibliography. The book begins by tracing the ideas behind local and regional models of isostasy, arguing that only flexure is in accord with geological observations. It then proceeds to describe the theoretical background, the observational evidence and the constraints that flexure has provided on physical properties of the lithosphere. The book concludes with a discussion of flexure's role in understanding the evolution of the surface features of the Earth and its neighboring planets. |
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Contents
IV | 1 |
VI | 2 |
VII | 9 |
VIII | 12 |
IX | 14 |
X | 15 |
XI | 17 |
XII | 22 |
XLVIII | 162 |
XLIX | 174 |
L | 176 |
LII | 177 |
LIII | 180 |
LIV | 192 |
LV | 193 |
LVI | 195 |
XIII | 23 |
XIV | 33 |
XV | 34 |
XVI | 39 |
XVIII | 42 |
XIX | 44 |
XX | 47 |
XXI | 48 |
XXIII | 49 |
XXIV | 52 |
XXV | 58 |
XXVI | 62 |
XXVII | 64 |
XXVIII | 69 |
XXIX | 75 |
XXX | 83 |
XXXI | 85 |
XXXII | 87 |
XXXV | 90 |
XXXVI | 91 |
XXXVII | 96 |
XXXVIII | 108 |
XXXIX | 109 |
XL | 112 |
XLII | 113 |
XLV | 114 |
XLVI | 125 |
XLVII | 150 |
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Common terms and phrases
admittance Airy America applied associated assumed basin beam belts bending beneath Bouguer bulge buried loading calculated caused changes coherence compared compensation considered continental continents crust crustal deflection deformation density depth determined distance Earth effect elastic elastic plate estimate et al evidence example explain fault Figure flank flexure follows force free-air geological given gravity anomaly increases initial islands isostasy isostatic Lake layer lithosphere load lower mantle margin mass material mGal mountain North observed occurs oceanic Pinfill plate Pratt predicted range regions Reproduced from Fig response ridge rift rigidity rise river deltas sea-level seamounts sediment seismic seismic refraction shows similar strength stress structure studies subsidence suggest supported surface Table tectonic thermal thickness topography trenches underlying United uplift values viscoelastic viscosity Watts wavelengths wide Zone
References to this book
Iceland Geodynamics: Crustal Deformation and Divergent Plate Tectonics Freysteinn Sigmundsson No preview available - 2006 |