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Processes Controlling the Composition of Clastic Sediments

Processes Controlling the Composition of Clastic Sediments PDF Author: Mark J. Johnsson
Publisher: Geological Society of America
ISBN: 0813722845
Category : Science
Languages : en
Pages : 357

Book Description


Processes Controlling the Composition of Clastic Sediments

Processes Controlling the Composition of Clastic Sediments PDF Author: Mark J. Johnsson
Publisher: Geological Society of America
ISBN: 0813722845
Category : Science
Languages : en
Pages : 357

Book Description


Tectonics and Geochemistry of the Northeastern Caribbean

Tectonics and Geochemistry of the Northeastern Caribbean PDF Author: Edward G. Lidiak
Publisher: Geological Society of America
ISBN: 9780813723228
Category : Science
Languages : en
Pages : 226

Book Description


Ages, Geochemistry and Metamorphism of Neoarchean Basement in Shandong Province

Ages, Geochemistry and Metamorphism of Neoarchean Basement in Shandong Province PDF Author: Meiling Wu
Publisher: Springer
ISBN: 3662453436
Category : Science
Languages : en
Pages : 243

Book Description
Focusing on issues of when and how Archean crust in the craton was formed, this PhD thesis book presents major research outcomes of field based metamorphic, geochemical and geochronological investigations on Meso-Neoarchean basement rocks from Shandong Province in the Eastern Block of the North China Craton. Based on major findings and new data, the author proposes that the formation and evolution of Archean crust was governed by mantle plumes, not by plate tectonics. As one of the oldest cratonic blocks in the world containing rocks as old as 3.85 billion years, the formation and evolution of North China Craton is still controversial. Therefore this book will be of value to anyone interested in the evolution of cratonic blocks and Precambrian geology.

Using Geochemical Data

Using Geochemical Data PDF Author: Hugh Rollinson
Publisher: Cambridge University Press
ISBN: 1108803822
Category : Science
Languages : en
Pages : 359

Book Description
This textbook is a complete rewrite, and expansion of Hugh Rollinson's highly successful 1993 book Using Geochemical Data: Evaluation, Presentation, Interpretation. Rollinson and Pease's new book covers the explosion in geochemical thinking over the past three decades, as new instruments and techniques have come online. It provides a comprehensive overview of how modern geochemical data are used in the understanding of geological and petrological processes. It covers major element, trace element, and radiogenic and stable isotope geochemistry. It explains the potential of many geochemical techniques, provides examples of their application, and emphasizes how to interpret the resulting data. Additional topics covered include the critical statistical analysis of geochemical data, current geochemical techniques, effective display of geochemical data, and the application of data in problem solving and identifying petrogenetic processes within a geological context. It will be invaluable for all graduate students, researchers, and professionals using geochemical techniques.

When Did Plate Tectonics Begin on Planet Earth?

When Did Plate Tectonics Begin on Planet Earth? PDF Author: Kent C. Condie
Publisher: Geological Society of America
ISBN: 0813724406
Category : Science
Languages : en
Pages : 306

Book Description
"Inspired by a GSA Penrose Conference held in Lander, Wyoming, June 14-18, 2006, this volume discusses the beginning and evolution of plate tectonics on Earth, and gives readers an introduction to some of the uncertainties and controversies related to the evolution of the planet. In the first three sections of the book, which cover isotopic, geochemical, metamorphic, mineralization, and mantle geodynamic constraints, a variety of papers address the question of when "modern-style" plate tectonics began on planet Earth. The next set of papers focuses on the geodynamic or geophysical constraints for the beginning of plate tectonics. The volume's final section synthesizes a broad range of evidence, from planetary analogues and geodynamic modeling, to Earth's preserved geologic record. This work provides an excellent graduate level text summarizing the current state of knowledge and will be of interest to a wide range of earth and planetary scientists."--Publisher's website.

The Tectonic and Geologic Evolution of Southeast Asian Seas and Islands

The Tectonic and Geologic Evolution of Southeast Asian Seas and Islands PDF Author: Dennis E. Hayes
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 410

Book Description


Continental Tectonics

Continental Tectonics PDF Author: Conall Mac Niocaill
Publisher: Geological Society of London
ISBN: 9781862390515
Category : Science
Languages : en
Pages : 358

Book Description
Brings together a series of papers which explore various aspects of the deformation of continental lithosphere, covering different tectonic settings from the Palaeozoic to the present day. These include terrane accretion and juxtaposition, the exhumation of high-pressure terrains, and mechanisms of crustal extension and rifting.

Plates, Plumes, and Paradigms

Plates, Plumes, and Paradigms PDF Author: Gillian R. Foulger
Publisher: Geological Society of America
ISBN: 0813723884
Category : Science
Languages : en
Pages : 898

Book Description


Dynamics of Plate Tectonics and Mantle Convection

Dynamics of Plate Tectonics and Mantle Convection PDF Author: Joao C. Duarte
Publisher: Elsevier
ISBN: 0323885861
Category : Science
Languages : en
Pages : 610

Book Description
Dynamics of Plate Tectonics and Mantle Convection, written by specialists in the field, gathers state-of-the-art perspectives on the dynamics of plate tectonics and mantle convection. Plate tectonics is a unifying theory of solid Earth sciences. In its initial form, it was a kinematic theory that described how the planet's surface is fragmented into several rigid lithospheric plates that move in relation to each other over the less viscous asthenosphere. Plate tectonics soon evolved to describe the forces that drive and resist plate movements. The Earth sciences community is now developing a new perspective that looks at plate tectonics and mantle convection as part of a single system. Why does our planet have plate tectonics, and how does it work? How does mantle convection drive the supercontinent cycle? How have tectono-convective modes evolved over the Earth's history? How did they shape the planet and impact life? Do other planets have mantle convection and tectonics? These are some of the fascinating questions explored in this book. This book started with a challenge from the editor to the authors to provide perspectives from their vantage point and open the curtain to the endeavors and stories behind the science. - Provides diverse perspectives from different experts around the world in plate tectonics and geodynamics - Includes the most up-to-date knowledge on plate tectonics and mantle convection - Sets the scene for the developments and challenges likely to be faced by researchers in the future of geodynamics

Continent Formation Through Time

Continent Formation Through Time PDF Author: N.M.W. Roberts
Publisher: Geological Society of London
ISBN: 1862393753
Category : Science
Languages : en
Pages : 356

Book Description
The continental crust is our archive of Earth history, and the store of many natural resources; however, many key questions about its formation and evolution remain debated and unresolved: What processed are involved in the formation, differentiation and evolution of continental crust, and how have these changed throughout Earth history?How are plate tectonics, the supercontinent cycle and mantle cooling linked with crustal evolution?What are the rates of generation and destruction of the continental crust through time?How representative is the preserved geological record? A range of approaches are used to address these questions, including field-based studies, petrology and geochemistry, geophysical methods, palaeomagnetism, whole-rock and accessory-phase isotope chemistry and geochronology. Case studies range from the Eoarchaean to Phanerozoic, and cover many different cratons and orogenic belts from across the continents.