Author: Timothy M. Kusky
Publisher: Geological Society of London
ISBN: 9781862393035
Category : Science
Languages : en
Pages : 428
Book Description
This volume honours the career of Brian F. Windley, who has been hugely influential in helping to achieve our current understanding of the evolution of the continental crust, and who has inspired many students and scientists to pursue studies on the evolution of the continents. Brian has studied processes of continental formation and evolution on most continents and of all ages, and has educated and inspired two generations of geologists to undertake careers in studies of continental evolution. The volume is organized into six sections, including: oceanic and island arc systems and continental growth; tectonics of accretionary orogens and continental growth; growth and stabilization of continental crust; collisions and intraplate processes; Precambrian tectonics and the birth of continents; and active tectonics and geomorphology of continental collision and growth zones.
The Evolving Continents
Stratigraphic Analysis of Layered Deposits
Author: Ömer Elitok
Publisher: BoD – Books on Demand
ISBN: 9535105787
Category : Science
Languages : en
Pages : 314
Book Description
Stratigraphy, a branch of geology, is the science of describing the vertical and lateral relationships of different rock formations formed through time to understand the earth history. These relationships may be based on lithologic properties (named lithostratigraphy), fossil content (labeled biostratigraphy), magnetic properties (called magnetostratigraphy), chemical features (named chemostratigraphy), reflection seismology (named seismic stratigraphy), age relations (called chronostratigraphy). Also, it refers to archaeological deposits called archaeological stratigraphy. Stratigraphy is built on the concept "the present is the key to the past" which was first outlined by James Hutton in the late 1700s and developed by Charles Lyell in the early 1800s. This book focuses particularly on application of geophysical methods in stratigraphic investigations and stratigraphic analysis of layered basin deposits from different geologic settings and present continental areas extending from Mexico region (north America) through Alpine belt including Italy, Greece, Iraq to Russia (northern Asia).
Publisher: BoD – Books on Demand
ISBN: 9535105787
Category : Science
Languages : en
Pages : 314
Book Description
Stratigraphy, a branch of geology, is the science of describing the vertical and lateral relationships of different rock formations formed through time to understand the earth history. These relationships may be based on lithologic properties (named lithostratigraphy), fossil content (labeled biostratigraphy), magnetic properties (called magnetostratigraphy), chemical features (named chemostratigraphy), reflection seismology (named seismic stratigraphy), age relations (called chronostratigraphy). Also, it refers to archaeological deposits called archaeological stratigraphy. Stratigraphy is built on the concept "the present is the key to the past" which was first outlined by James Hutton in the late 1700s and developed by Charles Lyell in the early 1800s. This book focuses particularly on application of geophysical methods in stratigraphic investigations and stratigraphic analysis of layered basin deposits from different geologic settings and present continental areas extending from Mexico region (north America) through Alpine belt including Italy, Greece, Iraq to Russia (northern Asia).
The Seismogenic Zone of Subduction Thrust Faults
Author: Timothy H. Dixon
Publisher: Columbia University Press
ISBN: 0231512015
Category : Science
Languages : en
Pages : 691
Book Description
Subduction zones, one of the three types of plate boundaries, return Earth's surface to its deep interior. Because subduction zones are gently inclined at shallow depths and depress Earth's temperature gradient, they have the largest seismogenic area of any plate boundary. Consequently, subduction zones generate Earth's largest earthquakes and most destructive tsunamis. As tragically demonstrated by the Sumatra earthquake and tsunami of December 2004, these events often impact densely populated coastal areas and cause large numbers of fatalities. While scientists have a general understanding of the seismogenic zone, many critical details remain obscure. This volume attempts to answer such fundamental concerns as why some interplate subduction earthquakes are relatively modest in rupture length (greater than 100 km) while others, such as the great (M greater than 9) 1960 Chile, 1964 Alaska, and 2004 Sumatra events, rupture along 1000 km or more. Contributors also address why certain subduction zones are fully locked, accumulating elastic strain at essentially the full plate convergence rate, while others appear to be only partially coupled or even freely slipping; whether these locking patterns persist through the seismic cycle; and what is the role of sediments and fluids on the incoming plate. Nineteen papers written by experts in a variety of fields review the most current lab, field, and theoretical research on the origins and mechanics of subduction zone earthquakes and suggest further areas of exploration. They consider the composition of incoming plates, laboratory studies concerning sediment evolution during subduction and fault frictional properties, seismic and geodetic studies, and regional scale deformation. The forces behind subduction zone earthquakes are of increasing environmental and societal importance.
Publisher: Columbia University Press
ISBN: 0231512015
Category : Science
Languages : en
Pages : 691
Book Description
Subduction zones, one of the three types of plate boundaries, return Earth's surface to its deep interior. Because subduction zones are gently inclined at shallow depths and depress Earth's temperature gradient, they have the largest seismogenic area of any plate boundary. Consequently, subduction zones generate Earth's largest earthquakes and most destructive tsunamis. As tragically demonstrated by the Sumatra earthquake and tsunami of December 2004, these events often impact densely populated coastal areas and cause large numbers of fatalities. While scientists have a general understanding of the seismogenic zone, many critical details remain obscure. This volume attempts to answer such fundamental concerns as why some interplate subduction earthquakes are relatively modest in rupture length (greater than 100 km) while others, such as the great (M greater than 9) 1960 Chile, 1964 Alaska, and 2004 Sumatra events, rupture along 1000 km or more. Contributors also address why certain subduction zones are fully locked, accumulating elastic strain at essentially the full plate convergence rate, while others appear to be only partially coupled or even freely slipping; whether these locking patterns persist through the seismic cycle; and what is the role of sediments and fluids on the incoming plate. Nineteen papers written by experts in a variety of fields review the most current lab, field, and theoretical research on the origins and mechanics of subduction zone earthquakes and suggest further areas of exploration. They consider the composition of incoming plates, laboratory studies concerning sediment evolution during subduction and fault frictional properties, seismic and geodetic studies, and regional scale deformation. The forces behind subduction zone earthquakes are of increasing environmental and societal importance.
Geology and Tectonics of Subduction Zones: A Tribute to Gaku Kimura
Author: Timothy Byrne
Publisher: Geological Society of America
ISBN: 0813725348
Category : Science
Languages : en
Pages : 228
Book Description
This volume highlights the career of Dr. Gaku Kimura, professor emeritus of geosciences at the University of Tokyo, by showing the spectrum of research required to understand these dynamic environments and the range of research he has inspired. The first three chapters provide context for the growth of accretionary prisms by examining the thermal structure of the ocean crust, and the sedimentary facies and potential fluid pathways in the Shikoku Basin. Next, two chapters look at the regional-scale structure of the plate boundary and the rheology and hysteresis of the hanging wall of the subduction zone in SW Japan. The following five chapters discuss the progressive deformation and thermal maturation of sediments along accretionary margins from Japan to New Zealand to western North America. The final two chapters look at the deformation processes near the subducting plate interface with the last chapter proposing a link between outcrop-scale observations and seismic slip.
Publisher: Geological Society of America
ISBN: 0813725348
Category : Science
Languages : en
Pages : 228
Book Description
This volume highlights the career of Dr. Gaku Kimura, professor emeritus of geosciences at the University of Tokyo, by showing the spectrum of research required to understand these dynamic environments and the range of research he has inspired. The first three chapters provide context for the growth of accretionary prisms by examining the thermal structure of the ocean crust, and the sedimentary facies and potential fluid pathways in the Shikoku Basin. Next, two chapters look at the regional-scale structure of the plate boundary and the rheology and hysteresis of the hanging wall of the subduction zone in SW Japan. The following five chapters discuss the progressive deformation and thermal maturation of sediments along accretionary margins from Japan to New Zealand to western North America. The final two chapters look at the deformation processes near the subducting plate interface with the last chapter proposing a link between outcrop-scale observations and seismic slip.
The Geology of Japan
Author: T. Moreno
Publisher: Geological Society of London
ISBN: 1862397430
Category : Science
Languages : en
Pages : 529
Book Description
It has been 25 years since publication of the most recent English language summary of the geology of Japan. This book offers an up-to-date comprehensive guide for those interested both in the geology of the Japanese islands and geological processes of island arcs in general. It contains contributions from over 70 different eminent researchers in their fields and is divided into 12 main chapters.
Publisher: Geological Society of London
ISBN: 1862397430
Category : Science
Languages : en
Pages : 529
Book Description
It has been 25 years since publication of the most recent English language summary of the geology of Japan. This book offers an up-to-date comprehensive guide for those interested both in the geology of the Japanese islands and geological processes of island arcs in general. It contains contributions from over 70 different eminent researchers in their fields and is divided into 12 main chapters.
Geology of a Transpressional Orogen Developed During Ridge-trench Interaction Along the North Pacific Margin
Author: Virginia Baker Sisson
Publisher: Geological Society of America
ISBN: 9780813723716
Category : Science
Languages : en
Pages : 392
Book Description
Accompanying CD-ROM contains maps using the comercial drawing program Adobe Illustrator 9.0 for Wintel systems.
Publisher: Geological Society of America
ISBN: 9780813723716
Category : Science
Languages : en
Pages : 392
Book Description
Accompanying CD-ROM contains maps using the comercial drawing program Adobe Illustrator 9.0 for Wintel systems.
Thermal Evolution of the Tertiary Shimanto Belt, Southwest Japan
Author: Michael B. Underwood
Publisher: Geological Society of America
ISBN: 9780813722733
Category : Science
Languages : en
Pages : 188
Book Description
Publisher: Geological Society of America
ISBN: 9780813722733
Category : Science
Languages : en
Pages : 188
Book Description
Earthquake Research and Analysis
Author: Sebastiano D'Amico
Publisher: BoD – Books on Demand
ISBN: 9533079916
Category : Science
Languages : en
Pages : 420
Book Description
This book is devoted to different aspects of earthquake research. Depending on their magnitude and the placement of the hypocenter, earthquakes have the potential to be very destructive. Given that they can cause significant losses and deaths, it is really important to understand the process and the physics of this phenomenon. This book does not focus on a unique problem in earthquake processes, but spans studies on historical earthquakes and seismology in different tectonic environments, to more applied studies on earthquake geology.
Publisher: BoD – Books on Demand
ISBN: 9533079916
Category : Science
Languages : en
Pages : 420
Book Description
This book is devoted to different aspects of earthquake research. Depending on their magnitude and the placement of the hypocenter, earthquakes have the potential to be very destructive. Given that they can cause significant losses and deaths, it is really important to understand the process and the physics of this phenomenon. This book does not focus on a unique problem in earthquake processes, but spans studies on historical earthquakes and seismology in different tectonic environments, to more applied studies on earthquake geology.
Orogenic Processes
Author: Wolfgang Franke (géologue).)
Publisher: Geological Society of London
ISBN: 9781862390737
Category : Science
Languages : en
Pages : 474
Book Description
Publisher: Geological Society of London
ISBN: 9781862390737
Category : Science
Languages : en
Pages : 474
Book Description
Vertical Coupling and Decoupling in the Lithosphere
Author: John Grocott
Publisher: Geological Society of London
ISBN: 9781862391598
Category : Science
Languages : en
Pages : 356
Book Description
" ... developed out of two symposia: 'Deformation at Convergent Margins', convened at the European Union of Geosciences meeting (EUG XI) at Strasbourg in April 2001; and 'Vertical Coupling and Decoupling at Convergent Margins', convened at the AGU Fall meeting in San Francisco in December 2001"--Acknowledgements.
Publisher: Geological Society of London
ISBN: 9781862391598
Category : Science
Languages : en
Pages : 356
Book Description
" ... developed out of two symposia: 'Deformation at Convergent Margins', convened at the European Union of Geosciences meeting (EUG XI) at Strasbourg in April 2001; and 'Vertical Coupling and Decoupling at Convergent Margins', convened at the AGU Fall meeting in San Francisco in December 2001"--Acknowledgements.