São Francisco Craton, eastern Brazil : tectonic genealogy of a miniature continent

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 l...

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Bibliographic Details
Other Authors: Cordani, Umberto G, (Editor), Flecha de Alkmim, Fernando, (Editor), Heilbron, Monica, (Editor)
Format: eBook
Language: English
Published: Cham : Springer International Publishing, [2017]
Series: Regional geology reviews.
Subjects:
geologie > Brazílie > São Francisco (Brazílie : řeka)
geology > Brasil > São Francisco River (Brazil)
elektronické knihy
sborníky
electronic books
papers of several authors
ISBN: 9783319017150
9783319017143
Physical Description: 1 online resource (viii, 331 pages)

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072 7 |a 55  |x Vědy o Zemi. Geologické vědy  |2 Konspekt  |9 7 
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080 |a (81)  |2 MRF 
080 |a (0.034.2:08)   |2 MRF 
080 |a (082)  |2 MRF 
245 0 0 |a São Francisco Craton, eastern Brazil :  |b tectonic genealogy of a miniature continent /  |c Monica Heilbron, Umberto G. Cordani, Fernando F. Alkmim, Editors. 
264 1 |a Cham :  |b Springer International Publishing,  |c [2017] 
264 4 |c ©2017 
300 |a 1 online resource (viii, 331 pages) 
336 |a text  |b txt  |2 rdacontent 
337 |a počítač  |b c  |2 rdamedia 
338 |a online zdroj  |b cr  |2 rdacarrier 
490 1 |a Regional Geology Reviews 
500 |a 7.3.2 Paranoá-Upper Espinhaço 1st-Order Sequence. 
504 |a Includes bibliographical references. 
506 |a Plný text je dostupný pouze z IP adres počítačů Univerzity Tomáše Bati ve Zlíně nebo vzdáleným přístupem pro zaměstnance a studenty 
520 |a 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'.- Resumé vydavatel 
590 |a SpringerLink  |b Springer Complete eBooks 
650 0 7 |a geologie  |z Brazílie  |z São Francisco (Brazílie : řeka)  |2 czenas  |7 ph114622 
650 0 9 |a geology  |z Brasil  |z São Francisco River (Brazil)  |2 eczenas 
655 7 |a elektronické knihy  |7 fd186907  |2 czenas 
655 7 |a sborníky  |7 fd163935   |2 czenas 
655 9 |a electronic books  |2 eczenas 
655 9 |a papers of several authors  |2 eczenas 
700 1 |a Cordani, Umberto G,  |e editor. 
700 1 |a Flecha de Alkmim, Fernando,  |e editor. 
700 1 |a Heilbron, Monica,  |e editor. 
776 0 8 |i Print version:  |a Heilbron, Monica.  |t São Francisco Craton, Eastern Brazil : Tectonic Genealogy of a Miniature Continent.  |d Cham : Springer International Publishing, ©2016  |z 9783319017143 
830 0 |a Regional geology reviews. 
856 4 0 |u https://proxy.k.utb.cz/login?url=https://link.springer.com/10.1007/978-3-319-01715-0  |y Plný text 
942 |2 udc 
992 |c NTK-SpringerEES 
993 |x NEPOSILAT  |y EIZ 

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