Rifted Basins and Aulacogens

Rifted Basins and Aulacogens

Author: S. M. Casshyap

Publisher:

Published: 1993

Total Pages: 332

ISBN-13:

DOWNLOAD EBOOK

Selected papers presented at the Indo-Soviet Symposium on Rifted Basins and Aulacogens: Sedimentation, Crustal Evolution, and Mineralisation, organized by the Dept. of Geology, Aligarh Muslim University and sponsored by the Akademii︠a︡ nauk SSSR and Indian National Science Academy, Jan. 22-30, 1990.


Tectonics of Sedimentary Basins

Tectonics of Sedimentary Basins

Author: Cathy Busby

Publisher: John Wiley & Sons

Published: 2011-12-07

Total Pages: 1034

ISBN-13: 1444347144

DOWNLOAD EBOOK

Investigating the complex interplay between tectonics and sedimentation is a key endeavor in modern earth science. Many of the world's leading researchers in this field have been brought together in this volume to provide concise overviews of the current state of the subject. The plate tectonic revolution of the 1960's provided the framework for detailed models on the structure of orogens and basins, summarized in a 1995 textbook edited by Busby and Ingersoll. Tectonics of Sedimentary Basins: Recent Advances focuses on key topics or areas where the greatest strides forward have been made, while also providing on-line access to the comprehensive 1995 book. Breakthroughs in new techniques are described in Section 1, including detrital zircon geochronology, cosmogenic nuclide dating, magnetostratigraphy, 3-D seismic, and basin modelling. Section 2 presents the new models for rift, post-rift, transtensional and strike slip basin settings. Section 3 addresses the latest ideas in convergent margin tectonics, including the sedimentary record of subduction intiation and subduction, flat-slab subduction, and arc-continent collision; it then moves inboard to forearc basins and intra-arc basins, and ends with a series of papers formed under compessional strain regimes, as well as post-orogenic intramontane basins. Section 4 examines the origin of plate interior basins, and the sedimentary record of supercontinent formation. This book is required reading for any advanced student or professional interested in sedimentology, plate tectonics, or petroleum geoscience. Additional resources for this book can be found at: www.wiley.com/go/busby/sedimentarybasins.


Aulacogens of North America I

Aulacogens of North America I

Author: William a Szary

Publisher:

Published: 2019-11-09

Total Pages: 188

ISBN-13: 9781706966029

DOWNLOAD EBOOK

Aulacogens of North America I is the first of a two book series presenting the aulacogens of the United States that failed to develop during the Proterozoic and Paleozoic Erathems. Chapter 1 provides an introduction to active rift zone development, and defines the aulacogen. The chapter also presents examples of global and U.S. aulacogens, defines basin classification of an intracratonic basin according to the USGS. Chapter 2 begins the detailed descriptions of Proterozoic aulacogens which include the Midcontinental Rift, East Continental and Fort Wayne Rifts, and the New Madrid Seismic Zone (Reelfoot Rift). Chapter 3 presents Paleozoic aulacogens, discussing the Southern Oklahoma Aulacogen including its various components, the Ouachita Rift Zone, the Southern Oklahoma Fault System, the Anardarko Basin, Palo Duro Basin of Texas, the Rome Trough, the New Mexico Aulacogen, and the Delaware Aualcogen of New Mexico.Aulacogens of North American II is the second book of the series which presents the Mesozoic and Cenozoic failed rift systems including the Yellowstone Hotspot Theory and the Columbia River flood basalt conundrum.


Aulacogens of North America II

Aulacogens of North America II

Author: William a Szary

Publisher: Independently Published

Published: 2019-11-09

Total Pages: 172

ISBN-13: 9781707005284

DOWNLOAD EBOOK

Aulacogens of North America II is the second of a two book series presenting the aulacogens of the United States that failed to develop during the Mesozoic and Cenozoic Erathems. Chapter 1 provides an introduction to rift and transtensional basins including intracratonic aulacogens. The chapter presents Cenozoic and Mesozoic Era Basin and Aulacogens identified by the USGS. Chapter 2 begins the detailed descriptions of Mesozoic aulacogens which include the Connecticut River Valley's Hartford Basin, The Newark Basin, Eastern North American Rift System, and the South Georgia Rift. Chapter 3 presents aulacogens, discussing the Great Basin, the Rio Grande Rift which includes the Albuquerque Basin and Quaternary extension of the rift. Chapter 4 presents the Yellowstone Hotspot Theory and its relations to the Columbia River Plateau and the Nevada-Oregon Rift Zone.Aualacogens of North America I is the first book of the series which presents the Proterozoic and Paleozoic failed rift systems .


Geodynamics of Rifting

Geodynamics of Rifting

Author: P.A. Ziegler

Publisher: Elsevier

Published: 2015-12-04

Total Pages: 914

ISBN-13: 1483295087

DOWNLOAD EBOOK

This volume contains papers giving an interdisciplinary review of 12 major rift systems from North and South America, Africa, Europe and Asia. These papers are written by an international group of academic and industrial specialists each of whom is most knowledgeable about the respective rift. The analyzed rifts were selected on the basis of availability of an as-complete-as-possible geological and geophysical data base. Thirteen papers deal with geodynamic processes governing the evolution of rifts. A comprehensive digest of the available stratigraphic, structural, geophysical and petrological data, together with an extensive list of references, is provided for each of the analyzed rift systems. The megatectonic setting and dynamics of evolution of each basin is discussed. Geodynamic models are tested against the record of the analyzed rifts. The question of "active" as against "passive" rifting is addressed. The rifts analyzed range in age from Precambrian to Recent and cover a wide spectrum of megatectonic settings. There is discussion of the evolution of rifts in a plate-tectonic frame. The case histories are followed by discussions addressing the global setting of rifts and geodynamic processes active during the development of rifted basins.


Geology and Hydrocarbon Potential of Neoproterozoic-Cambrian Basins in Asia

Geology and Hydrocarbon Potential of Neoproterozoic-Cambrian Basins in Asia

Author: G. M. Bhat

Publisher: Geological Society of London

Published: 2012

Total Pages: 305

ISBN-13: 186239346X

DOWNLOAD EBOOK

This volume provides a comprehensive overview of the geology and hydrocarbon potential of the major Neoproterozoic Cambrian basins of Asia from Oman, across the Middle East and the Indian Subcontinent, to China and SE Siberia, along with new research on the region.


Proterozoic and Paleozoic Rifts

Proterozoic and Paleozoic Rifts

Author: William a Szary

Publisher:

Published: 2020-09-17

Total Pages: 188

ISBN-13:

DOWNLOAD EBOOK

Proterozoic and Paleozoic Rifts is the first of a two book series presenting the aulacogens of the United States that failed to develop during the Proterozoic and Paleozoic Erathems. Chapter 1 provides an introduction to active rift zone development and defines the aulacogen. The chapter also presents examples of global and U.S. aulacogens, defines the basin classification of an intracratonic basin according to the USGS. Chapter 2 begins the detailed descriptions of Proterozoic aulacogens which include the Midcontinental Rift, East Continental & Fort Wayne Rifts, and the New Madrid Seismic Zone (Reelfoot Rift). Chapter 3 presents Paleozoic aulacogens, discussing the Southern Oklahoma Aulacogen including its various components, the Ouachita Rift Zone, the Southern Oklahoma Fault System, Anardarko Basin, Palo Duro Basin of Texas, the Rome Trough, the New Mexico Aulacogen, and the Delaware Aulacogen of New Mexico.


Global Sedimentology of the Ocean

Global Sedimentology of the Ocean

Author: Christian M. Robert

Publisher: Elsevier

Published: 2008-09-17

Total Pages: 498

ISBN-13: 008093093X

DOWNLOAD EBOOK

A great deal of information has been gained during the past 20 years about the deep ocean. This book synthesizes new information in marine sedimentology, applying concepts to case studies, and integrating the information in a context of plate tectonics, global circulation, and sedimentary processes. The potential of sediment series as archives of past environments is highlighted. * complete update of synthetic information in marine sedimentology.* association of information on the origin and transport of sediment particles, the evolution of sediment series and their role as archives of past environments.


São Francisco Craton, Eastern Brazil

São Francisco Craton, Eastern Brazil

Author: Monica Heilbron

Publisher: Springer

Published: 2016-12-05

Total Pages: 326

ISBN-13: 3319017152

DOWNLOAD EBOOK

The region of the São Francisco river valley in eastern Brazil encompasses two main components of the geologic framework of the South American continent: the São Francisco craton and its marginal orogenic belts. Cratons, as the oldest, differentiated and relatively stable pieces of the continental lithosphere, preserve a substantial part of the Earth's memory. Orogenic belts, on the other hand, record collisional processes that occurred during a limited time span. Because of their topographic relief, mountain belts developed along craton margins provide however access to rock successions not exposed in the low lands of the adjacent cratons. The combination of geologic information obtained in cratonic domains and their marginal orogenic belts thus form the basis for deciphering substantial periods of Earth’s history. Corresponding to the most intensively studied portion of the Precambrian nucleus of the South American plate, the São Francisco craton and its margins host a rock record that spans from the Paleoarchean to the Cenozoic. Precambrian sedimentary successions that witness ancient Earth processes - many of them of global significance - are especially well preserved and exposed in this region. With all these attributes the São Francisco craton together with its fringing orogenic belts can be viewed as a ‘continent within a continent’ or a ‘continent in miniature’.