Results 31 to 40 of about 27,504 (213)

Rejuvenation of the lithosphere by the Hawaiian plume [PDF]

open access: yesNature, 2004
The volcanism responsible for creating the chain of the Hawaiian islands and seamounts is believed to mark the passage of the oceanic lithosphere over a mantle plume. In this picture hot material rises from great depth within a fixed narrow conduit to the surface, penetrating the moving lithosphere.
Li, X.   +4 more
openaire   +7 more sources

Patol75/Continental-Magmatism-The-Surface-Manifestation-Of-Dynamic-Interactions-Between-Cratonic-Lithosphere: Submission to Geochemistry, Geophysics, Geosystems

open access: yes, 2022
This release includes input files required to reproduce models presented in "Continental Magmatism: The Surface Manifestation Of Dynamic Interactions Between Cratonic Lithosphere, Mantle Plumes And Edge-Driven Convection"
Thomas Duvernay
core   +1 more source

Altered Mantle Fabric Beneath the Mid‐Continent Rift

open access: yesGeochemistry, Geophysics, Geosystems, 2021
We present new, densely sampled shear‐wave splitting results from southern Minnesota and adjacent areas of neighboring states, sampling the southwestern limit of the Archean Superior Province and straddling the Proterozoic Mid‐Continent Rift (MCR).
A. W. Frederiksen   +4 more
doaj   +1 more source

Rifts, orogens, cratons, and global tectonics: Introduction

open access: yesГеодинамика и тектонофизика, 2017
A key role in developing the Earth theory is played by comparative studies of orogens, rifts, and platforms in the equatorial, middle and high latitudes of Asia and the adjacent Arctic regions.
S. V. Rasskazov
doaj   +1 more source

Thermal Structure of Eastern Australia's Upper Mantle and Its Relationship to Cenozoic Volcanic Activity and Dynamic Topography

open access: yesGeochemistry, Geophysics, Geosystems, 2021
Spatio‐temporal changes of upper mantle structure play a significant role in generating and maintaining surface topography. Although geophysical models of upper mantle structure have become increasingly refined, there is a paucity of geologic constraints
P. W. Ball   +4 more
doaj   +1 more source

Geodynamic evolution of a wide plate boundary in the Western Mediterranean, near-field versus far-field interactions

open access: yesBSGF - Earth Sciences Bulletin, 2021
The present-day tectonic setting of the Western Mediterranean region, from the Pyrénées to the Betics and from the Alps to the Atlas, results from a complex 3-D geodynamic evolution involving the interactions between the Africa, Eurasia and Iberia plates
Jolivet Laurent   +11 more
doaj   +1 more source

XXIV ALLRUSSIA YOUTH CONFERENCE ON STRUCTURE OF LITHOSPHERE AND GEODYNAMICS, IRKUTSK, RUSSIA, APRIL 19–24, 2011

open access: yesГеодинамика и тектонофизика, 2015
The information on the XXIV AllRussia youth conference on structure of lithosphere and geodynamics is presented. It was held on April 19–24, 2011 at the Institute of the Earth’s Crust, Irkutsk. The scope of conference is presented.
Victoria A. Khak
doaj   +1 more source

African cratonic lithosphere carved by mantle plumes [PDF]

open access: yes, 2020
How cratons, the ancient cores of continents, evolved since their formation over 2.5 Ga ago is debated. Seismic tomography can map the thick lithosphere of cratons, but its resolution is low in sparsely sampled continents.
Gaina, Carmen   +4 more
core   +1 more source

ANALYSIS OF DEFORMATION PROCESSES IN THE LITHOSPHERE FROM GEODETIC MEASUREMENTS BASED ON THE EXAMPLE OF THE SAN ANDREAS FAULT

open access: yesГеодинамика и тектонофизика, 2015
Analysis of data from permanent GPS observation stations located in tectonically active regions provides for direct observation of deformation processes of the earth's surface which result from elastic interaction of the lithospheric plates and also ...
Yury V. Gabsatarov
doaj   +1 more source

DESTRUCTION OF THE LITHOSPHERE: FAULTBLOCK DIVISIBILITY AND ITS TECTONOPHYSICAL REGULARITIES

open access: yesГеодинамика и тектонофизика, 2015
A new concept is proposed concerning the origin and inception of ‘initial’ faults and formation of large blocks as a result of cooling of the Archaean lithosphere, during which Benard cells had formed (Fig. 5).
Semen I. Sherman
doaj   +1 more source

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