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Accretionary Prisms and Convergent Margin Tectonics in the Northwest Pacific Basin (Hardcover, 2011 Ed.)
Loot Price: R2,821
Discovery Miles 28 210
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Accretionary Prisms and Convergent Margin Tectonics in the Northwest Pacific Basin (Hardcover, 2011 Ed.)
Series: Modern Approaches in Solid Earth Sciences, 8
Expected to ship within 10 - 15 working days
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Accretionary prisms in convergent margins are natural laboratories
for exploring initial orogenic processes and mountain building
episodes. They are also an important component of continental
growth both vertically and laterally. Accretionary prisms are
seismically highly active and their internal deformation via
megathrusting and out-of-sequence faulting are a big concern for
earthquake and tsunami damage in many coastal cities around the
Pacific Rim. The geometries and structures of modern accretionary
prisms have been well imaged seismically and through deep drilling
projects of the Ocean Drilling Program (and recently IODP) during
the last 15 years. Better understanding of the spatial distribution
and temporal progression of accretionary prism deformation,
structural and hydrologic evolution of the decollement zone
(tectonic interface between the subducting slab and the upper
plate), chemical gradients and fluid flow paths within accretionary
prisms, contrasting stratigraphic and deformational framework
along-strike in accretionary prisms, and the distribution and
ecosystems of biological communities in accretionary prism settings
is most important in interpreting the evolution of ancient complex
sedimentary terrains and orogenic belts in terms of
subduction-related processes. This book is a collection of
interdisciplinary papers documenting the geological, geophysical,
geochemical, and paleontological features of modern accretionay
prisms and trenches in the northwestern Pacific Ocean, based on
many submersible dive cruises, ODP drilling projects, and
geophysical surveys during the last 10 years. It also includes
several papers presenting the results of systematic integrated
studies of recent to ancient on-land accretionary prisms in
comparison to modern analogues. The individual chapters are data
and image rich, providing a major resource of information and
knowledge from these critical components of convergent margins for
researchers, faculty members, and graduate and undergraduate
students. As such, the book will be a major and unique contribution
in the broad fields of global tectonics, geodynamics, marine
geology and geophysics, and structural geology and sedimentology.
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