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03602nam a2200505 4500 |
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978-3-030-11190-8 |
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20191026142733.0 |
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190528s2019 gw | s |||| 0|eng d |
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|a 9783030111908
|9 978-3-030-11190-8
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|a 10.1007/978-3-030-11190-8
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|a 551
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|a The Geology of Iberia: A Geodynamic Approach
|h [electronic resource] :
|b Volume 4: Cenozoic Basins /
|c edited by Cecilio Quesada, José Tomás Oliveira.
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| 250 |
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|a 1st ed. 2019.
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| 264 |
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|a Cham :
|b Springer International Publishing :
|b Imprint: Springer,
|c 2019.
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| 300 |
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|a XV, 184 p. 102 illus., 95 illus. in color.
|b online resource.
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| 336 |
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|a text
|b txt
|2 rdacontent
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|a computer
|b c
|2 rdamedia
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|a online resource
|b cr
|2 rdacarrier
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|a text file
|b PDF
|2 rda
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|a Regional Geology Reviews,
|x 2364-6438
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| 505 |
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|a 1. Preface -- 2. Cenozoic basins in Iberia: an introduction -- 3.Alpine foreland basins -- 4.Extension in the West Mediterranean -- 5.Cenozoic basins of western Iberia (Mondego, Lower Tejo and Alvalade basins) -- 6. Late-orogenic intermontane foreland basins in Iberia -- 7. Cenozoic magmatism in Iberia.
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|a Pursuing an innovative, global approach, this unique book provides an updated review of the geology of Iberia and its continental margins from a geodynamic perspective. Owing to its location close to successive plate margins, Iberia has played a pivotal role in the geodynamic evolution of the Gondwanan, Rheic, Pangea, Tethys and Eurasian plates over the last 600 Ma of Earth's history. The geological record starts with the amalgamation of Gondwana in the Neoproterozoic, which was succeeded by the rifting and spreading of the Rheic ocean; its demise, which led to the amalgamation of Pangea in the late Paleozoic; the rifting and spreading of several arms of the Neotethys ocean in the Mesozoic Era and their ongoing closure, which was responsible for the Alpine orogeny. The significant advances in the last 20 years have increasingly attracted international interest in exploring the geology of the Iberian Peninsula. This volume focuses on the Cenozoic basins of the Iberian Geology and consequently the most recent sedimentary features in the Iberian Geology apart of the active ones. In this book, you will find a detailed explanation of the alpine foreland basins, the extension of the west Mediterranean as well as the latest magmatism in Iberia.
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|a Geology.
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|a Geophysics.
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|a Natural disasters.
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|a Geology.
|0 http://scigraph.springernature.com/things/product-market-codes/G17002
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|a Geophysics/Geodesy.
|0 http://scigraph.springernature.com/things/product-market-codes/G18009
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| 650 |
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|a Natural Hazards.
|0 http://scigraph.springernature.com/things/product-market-codes/G32000
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| 700 |
1 |
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|a Quesada, Cecilio.
|e editor.
|4 edt
|4 http://id.loc.gov/vocabulary/relators/edt
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| 700 |
1 |
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|a Oliveira, José Tomás.
|e editor.
|4 edt
|4 http://id.loc.gov/vocabulary/relators/edt
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| 710 |
2 |
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|a SpringerLink (Online service)
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| 773 |
0 |
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|t Springer eBooks
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| 776 |
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|i Printed edition:
|z 9783030111892
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| 776 |
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|i Printed edition:
|z 9783030111915
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| 830 |
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|a Regional Geology Reviews,
|x 2364-6438
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| 856 |
4 |
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|u https://doi.org/10.1007/978-3-030-11190-8
|z Full Text via HEAL-Link
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| 912 |
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|a ZDB-2-EES
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| 950 |
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|a Earth and Environmental Science (Springer-11646)
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