The Geology of Iberia_ A Geodynamic Approach

The Geology of Iberia: A Geodynamic Approach: Volume 4: Cenozoic Basins (Repost)

Cecilio Quesada, José Tomás Oliveira, "The Geology of Iberia: A Geodynamic Approach: Volume 4: Cenozoic Basins"
English | 2019 | ISBN: 303011189X | PDF | pages: 195 | 17.7 mb
The Geology of Iberia: A Geodynamic Approach: Volume 5: Active Processes: Seismicity, Active Faulting and Relief

Cecilio Quesada, "The Geology of Iberia: A Geodynamic Approach: Volume 5: Active Processes: Seismicity, Active Faulting and Relief "
English | ISBN: 3030109305 | 2020 | 126 pages | PDF | 12 MB

The Geology of Iberia: A Geodynamic Approach: Volume 4: Cenozoic Basins  eBooks & eLearning

Posted by roxul at May 28, 2019
The Geology of Iberia: A Geodynamic Approach: Volume 4: Cenozoic Basins

Cecilio Quesada, "The Geology of Iberia: A Geodynamic Approach: Volume 4: Cenozoic Basins "
English | ISBN: 303011189X | 2019 | 184 pages | EPUB, PDF | 137 MB + 18 MB

The Geology of Iberia: A Geodynamic Approach: Volume 3: The Alpine Cycle  eBooks & eLearning

Posted by roxul at June 29, 2019
The Geology of Iberia: A Geodynamic Approach: Volume 3: The Alpine Cycle

Cecilio Quesada, "The Geology of Iberia: A Geodynamic Approach: Volume 3: The Alpine Cycle "
English | ISBN: 3030112942 | 2019 | 568 pages | EPUB, PDF | 386 MB + 61 MB

The Geology of Iberia: A Geodynamic Approach Volume 2: The Variscan Cycle  eBooks & eLearning

Posted by AvaxGenius at Aug. 20, 2019
The Geology of Iberia: A Geodynamic Approach Volume 2: The Variscan Cycle

The Geology of Iberia: A Geodynamic Approach Volume 2: The Variscan Cycle by Cecilio Quesada
English | PDF | 2019 | 560 Pages | ISBN : 3030105180 | 47.39 MB

Taking a new 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 s.l. and Eurasian plates over the last 600 Ma of Earth's history.