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Title São Francisco Craton, eastern Brazil : tectonic genealogy of a miniature continent / Monica Heilbron, Umberto G. Cordani, Fernando F. Alkmim, Editors.

Published Cham : Springer International Publishing, [2017]
©2017

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Location Call No. Status
 UniM INTERNET resource    AVAILABLE
Physical description 1 online resource (viii, 331 pages).
Series Regional Geology Reviews
Regional geology reviews.
Springer Earth and Environmental Science eBooks 2017 English+International
Bibliography Includes bibliographical references.
Contents Overview; 1 The São Francisco Craton and Its Margins; Abstract; 1.1 Introduction; 1.2 Geologic Outline of the São Francisco Craton and Its Margins; 1.3 Development of the São Francisco Craton Concept; 1.4 Book Overview; References; 2 Lithospheric Features of the São Francisco Craton; Abstract; 2.1 Introduction; 2.2 Crustal Thickness; 2.3 Gravity Modeling; 2.4 Lithospheric Properties; 2.4.1 Surface-Wave Tomography; 2.4.2 P-Wave Tomography; 2.5 Seismicity and Stresses; 2.6 Discussion; 2.7 Conclusions; Acknowledgments; References; The Craton Basement.
3 Nature and Evolution of the Archean Crust of the São Francisco CratonAbstract; 3.1 Introduction; 3.2 The Archean Record of the São Francisco Craton; 3.3 Archean Assemblages of the Southern Portion of the Craton; 3.3.1 The Mesoarchean Campo Belo Metamorphic Complex; 3.3.2 The Neoarchean Metamorphic Complexes; 3.3.3 Crustal Evolution; 3.4 Archean Assemblages of the Northern Portion of the Craton; 3.4.1 The Gavião and Sobradinho Blocks; 3.4.1.1 Granite-Gneissic Terrains; 3.4.1.2 Greenstone Belts; 3.4.2 The Serrinha Block; 3.4.3 The Jequié Block.
3.4.4 The Basement of the Itabuna-Salvador-Curaçá Belt3.5 Concluding Remarks; Acknowledgments; References; 4 The Paleoproterozoic Eastern Bahia Orogenic Domain; Abstract; 4.1 Introduction; 4.2 Stratigraphy; 4.2.1 Basement; 4.2.2 Paleoproterozoic Units; 4.2.2.1 Supracrustal Assemblages; 4.2.2.2 Granitic Rocks; 4.3 Tectonic Framework and Metamorphism; 4.4 Evolutionary History; 4.5 Final Remarks; Acknowledgments; References; 5 The Paleoproterozoic Mineiro Belt and the Quadrilátero Ferrífero; Abstract; 5.1 Introduction; 5.2 The Mineiro Belt; 5.2.1 Stratigraphy.
5.2.1.1 Paleoproterozoic Granitic Rocks5.2.1.2 Supracrustal Units; 5.2.2 Structure and Metamorphism; 5.3 The Quadrilátero Ferrífero; 5.3.1 Stratigraphy; 5.3.1.1 Basement; 5.3.1.2 Minas Supergroup; 5.3.1.3 Itacolomi Group; 5.3.2 Structure and Metamorphism; 5.4 Tectonic Evolution; 5.5 Regional Correlations; 5.6 Concluding Remarks; Acknowledgments; References; Intracratonic Basins and Precambrian Mafic Dyke Swarms; 6 The Paramirim Aulacogen; Abstract; 6.1 Introduction; 6.2 Stratigraphy; 6.2.1 The Espinhaço Supergroup and Associated Plutonic Rocks; 6.2.1.1 Northern Espinhaço Range Sub-Basin.
Algodão FormationOliveira Dos Brejinhos Group; São Marcos Group; 6.2.1.2 Chapada Diamantina Sub-Basin; Serra da Gameleira Formation; Rio dos Remédios Group and Associated Lagoa Real Plutonic Suite; Paraguaçu Group; Chapada Diamantina Group; 6.2.2 Santo Onofre Group and São Francisco Supergroup; 6.2.2.1 Santo Onofre Group; 6.2.2.2 São Francisco Supergroup; Bebedouro Formation; Salitre Formation; 6.3 Structure; 6.4 Tectonic Evolution; 6.5 Concluding Remarks; Acknowledgments; References; 7 The São Francisco Basin; 7.1 Introduction; 7.2 Definition; 7.3 Stratigraphy; 7.3.1 Basement.
Notes 7.3.2 Paranoá-Upper Espinhaço 1st-Order Sequence.
Summary 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'.
Other author Cordani, Umberto G, editor.
Flecha de Alkmim, Fernando, editor.
Heilbron, Monica, editor.
SpringerLink issuing body.
Subject Geology -- Brazil.
Electronic books.
Electronic book.
ISBN 9783319017150 (electronic bk.)
3319017152 (electronic bk.)
9783319017143
3319017144
Standard Number 10.1007/978-3-319-01715-0