Электронная книга: Burbank Douglas W. «Tectonic Geomorphology»

Tectonic Geomorphology

Tectonic geomorphology is the study of the interplay between tectonic and surface processes that shape the landscape in regions of active deformation and at time scales ranging from days to millions of years. Over the past decade, recent advances in the quantification of both rates and the physical basis of tectonic and surface processes have underpinned an explosion of new research in the field of tectonic geomorphology. Modern tectonic geomorphology is an exceptionally integrative field that utilizes techniques and data derived from studies of geomorphology, seismology, geochronology, structure, geodesy, stratigraphy, meteorology and Quaternary science. While integrating new insights and highlighting controversies from the ten years of research since the 1st edition, this 2nd edition of Tectonic Geomorphology reviews the fundamentals of the subject, including the nature of faulting and folding, the creation and use of geomorphic markers for tracing deformation, chronological techniques that are used to date events and quantify rates, geodetic techniques for defining recent deformation, and paleoseismologic approaches to calibrate past deformation. Overall, this book focuses on the current understanding of the dynamic interplay between surface processes and active tectonics. As it ranges from the timescales of individual earthquakes to the growth and decay of mountain belts, this book provides a timely synthesis of modern research for upper-level undergraduate and graduate earth science students and for practicing geologists. Additional resources for this book can be found at: www.wiley.com/go/burbank/geomorphology.

Издательство: "John Wiley&Sons Limited"

ISBN: 9781444345032

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  • Geomorphology — (from Greek: γη, ge , earth ; μορφή, morfé , form ; and λόγος, logos , knowledge ) is the study of landforms and the processes that shape them. Geomorphologists seek to understand why landscapes look the way they do: to understand landform… …   Wikipedia

  • Tectonic uplift — Kupe s Sail New Zealand Tectonic uplift is a geological process most often caused by plate tectonics which increases elevation. The opposite of uplift is subsidence, which results in a decrease in elevation. Uplift may be orogenic or isostatic …   Wikipedia

  • geomorphology — geomorphological /jee euh mawr pheuh loj i keuhl/, geomorphologic, adj. geomorphologist, n. /jee euh mawr fol euh jee/, n. the study of the characteristics, origin, and development of landforms. [1890 95; GEO + MORPHOLOGY] * * * Scientific… …   Universalium

  • plate tectonic theory — noun the branch of geology studying the folding and faulting of the earth s crust • Syn: ↑tectonics, ↑plate tectonics • Members of this Topic: ↑Pangaea, ↑Pangea • Hypernyms: ↑morphology, ↑ge …   Useful english dictionary

  • continental landform — ▪ geology Introduction       any conspicuous topographic feature on the largest land areas of the Earth. Familiar examples are mountains (including volcanic (volcanism) cones), plateaus, and valleys. (The term landform also can be applied to… …   Universalium

  • Mountain formation — Thrust and reverse fault movement are an important component of mountain formation. Mountain formation refers to the geological processes that underlie the formation of mountains. These processes are associated with large scale movements of the… …   Wikipedia

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