[HTML][HTML] Orogenic architecture of the Mediterranean region and kinematic reconstruction of its tectonic evolution since the Triassic
The basins and orogens of the Mediterranean region ultimately result from the opening of
oceans during the early break-up of Pangea since the Triassic, and their subsequent …
oceans during the early break-up of Pangea since the Triassic, and their subsequent …
[图书][B] Paleomagnetism of the Atlantic, Tethys and Iapetus oceans
R Van der Voo - 2005 - ui.adsabs.harvard.edu
This book makes the common techniques of paleomagnetism understandable to students of
geology and explains how paleomagnetism is used to map the movement of major portions …
geology and explains how paleomagnetism is used to map the movement of major portions …
Miocene rotation of Sardinia: New paleomagnetic and geochronological constraints and geodynamic implications
J Gattacceca, A Deino, R Rizzo, DS Jones… - Earth and Planetary …, 2007 - Elsevier
The Miocene rotation of Sardinia (Western Mediterranean) remains poorly constrained
despite a wealth of paleomagnetic data, primarily due to poor chronostratigraphic control …
despite a wealth of paleomagnetic data, primarily due to poor chronostratigraphic control …
Age of the Corsica–Sardinia rotation and Liguro–Provençal Basin spreading: new paleomagnetic and Ar/Ar evidence
The age of spreading of the Liguro–Provençal Basin is still poorly constrained due to the
lack of boreholes penetrating the whole sedimentary sequence above the oceanic crust and …
lack of boreholes penetrating the whole sedimentary sequence above the oceanic crust and …
Paleomagnetic Evidence for Pre‐21 Ma Independent Drift of South Sardinia From North Sardinia‐Corsica:“Greater Iberia” Versus Europe
It is unanimously acknowledged that the Corsica‐Sardinia microplate rotated
counterclockwise (CCW) by 40–50° between 21 and 15 Ma, synchronous with Liguro …
counterclockwise (CCW) by 40–50° between 21 and 15 Ma, synchronous with Liguro …
Eocene rotation of Sardinia, and the paleogeography of the western Mediterranean region
Key to understanding the complex Mediterranean subduction history is the kinematic
reconstruction of its paleogeography after Jurassic extension between Iberia, Eurasia, and …
reconstruction of its paleogeography after Jurassic extension between Iberia, Eurasia, and …
Beginning of the Apennine subduction system in central western Mediterranean: Constraints from Cenozoic “orogenic” magmatic activity of Sardinia, Italy
Major and trace element analyses plus six new 40Ar/39Ar data obtained on feldspar
separates for selected igneous rocks belonging to the Oligo‐Miocene igneous activity of …
separates for selected igneous rocks belonging to the Oligo‐Miocene igneous activity of …
When did Sardinia stop rotating? New palaeomagnetic results
L Vigliotti, VE Langenheim - Terra Nova, 1995 - Wiley Online Library
Previous palaeomagnetic results from Tertiary volcanic rocks of Sardinia suggest that the
island underwent a quick counterclockwise rotation between 20.5 and 19 Ma. In order to test …
island underwent a quick counterclockwise rotation between 20.5 and 19 Ma. In order to test …
Early Permian 90° clockwise rotation of the Maures–Estérel–Corsica–Sardinia block confirmed by new palaeomagnetic data and followed by a Triassic 60° clockwise …
Palaeomagnetic investigations of the Corso-Sardinian block and Maures–Estérel show that
there has been a change in their magnetic orientation during the Late Carboniferous–Early …
there has been a change in their magnetic orientation during the Late Carboniferous–Early …
Alpine plate kinematics revisited: the Adria problem
UG Wortmann, H Weissert, H Funk, J Hauck - Tectonics, 2001 - Wiley Online Library
Tectonic evolution of the Alpine Tethys is controlled by the plate movements of Africa,
Europe, and the Adriatic microplate. It is, however, unclear to which extent and at what times …
Europe, and the Adriatic microplate. It is, however, unclear to which extent and at what times …