scholarly article | Q13442814 |
P819 | ADS bibcode | 1998Tectp.296...61V |
P356 | DOI | 10.1016/S0040-1951(98)00137-1 |
P50 | author | Andrea Tommasi | Q57246874 |
Alain Vauchez | Q57896503 | ||
Guilhem Barruol | Q57906667 | ||
P2860 | cites work | Heat flow from the Earth's interior: Analysis of the global data set | Q22122451 |
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Partially Molten Middle Crust Beneath Southern Tibet: Synthesis of Project INDEPTH Results | Q34408870 | ||
Did the Atlantic Close and then Re-Open? | Q55878091 | ||
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Development of graben associated with the initial ruptures of the atlantic ocean | Q56136721 | ||
Some remarks on the development of sedimentary basins | Q56523482 | ||
Mantle unrooting in collisional settings | Q57881502 | ||
Magnetotelluric Experiment probes deep physical state of southeastern United States | Q57886042 | ||
SKSsplitting beneath continental rift zones | Q58780078 | ||
Asymmetric upwarp of the asthenosphere beneath the Baikal rift zone, Siberia | Q58780107 | ||
Role of lithospheric strength heterogeneities in the tectonics of Tibet and neighbouring regions | Q59060176 | ||
Seismic evidence for a fossil mantle plume beneath South America and implications for plate driving forces | Q59068772 | ||
Evidence for a 150–200-km thick Archaean lithosphere from diamond inclusion thermobarometry | Q59092650 | ||
Continental rifting at pre-existing lithospheric weaknesses | Q59096582 | ||
Geothermal anomalies along the Rio Grande rift in New Mexico | Q59381714 | ||
Mantle deformation and tectonics: constraints from seismic anisotropy in the western United States | Q59765196 | ||
The role of a heterogeneous inclusion during continental collision | Q59797803 | ||
Numerical modeling of intraplate deformation: Simple mechanical models of continental collision | Q59797806 | ||
Seismic anisotropy beneath the Northern Apennines (Italy) and its tectonic implications | Q59806795 | ||
Electrical resistivity model of the crust and upper mantle from a magnetotelluric survey through the central Pyrenees | Q59876202 | ||
The influence of preexisting structure on the evolution of the Cenozoic Malawi rift (East African rift system) | Q60363235 | ||
Tectonic implications ofS-wave anisotropy beneath SE Brazil | Q60709988 | ||
Lithospheric wedging in the western Alps inferred from the ECORS-CROP traverse | Q60925056 | ||
Termination of a continental-scale strike-slip fault in partially melted crust: The West Pernambuco shear zone, northeast Brazil | Q61660909 | ||
Composition and thickness of the southern Altiplano crust, Bolivia | Q61662492 | ||
Self-indentation of a heterogeneous continental lithosphere | Q61662501 | ||
Imaging a mantle plume beneath the French Massif Central | Q61847997 | ||
Depth extent of cratons as inferred from tomographic studies | Q61906065 | ||
Why do continents break-up parallel to ancient orogenic belts? | Q64029108 | ||
Anisotropy beneath the Pyrenees Range from teleseismic shear wave splitting: Results from a test experiment | Q64029110 | ||
Crustal structure of the Rocky Mountain region | Q64830923 | ||
Uniform-sense normal simple shear of the continental lithosphere | Q65581400 | ||
Mountain building: strike-parallel motion and mantle anisotropy | Q69670330 | ||
Limits on lithospheric stress imposed by laboratory experiments | Q97142243 | ||
Cenozoic extensional tectonics in China | Q97449317 | ||
On the mechanics of the collision between India and Asia | Q97449413 | ||
Intracontinental subduction, crust-mantle décollement and crustal-stacking wedge in the Himalayas and other collision belts | Q97449417 | ||
Present-day stress field changes along the Baikal rift and tectonic implications | Q97449431 | ||
Global patterns of azimuthal anisotropy and deformations in the continental mantle | Q97449480 | ||
On the thermo-mechanical evolution of continental lithosphere | Q97484832 | ||
Rift basin evolution in Africa: the influence of reactivated steep basement shear zones | Q97925124 | ||
Physical changes in the lithosphere associated with thermal relaxation after rifting | Q97999053 | ||
Rio Grande rift: An overview | Q97999055 | ||
Heat flow in the Witwatersrand Basin and environs and its significance for the South African Shield Geotherm and lithosphere thickness | Q97999091 | ||
How preexisting weaknesses control the style of continental breakup | Q97999098 | ||
Continental-scale rheological heterogeneities and complex intraplate tectono-metamorphic patterns: insights from a case-study and numerical models | Q105127432 | ||
Seismic anisotropy in the eastern United States: Deep structure of a complex continental plate | Q105127454 | ||
Transcurrent Shear Zones and Magma Emplacement in Neoproterozoic Belts of Brazil | Q105127472 | ||
Seismic anisotropy in ocean basins: Resistive drag of the sublithospheric mantle? | Q105127477 | ||
Shear zone-controlled magma emplacement or magma-assisted nucleation of shear zones? Insights from northeast Brazil | Q105127488 | ||
Shear-wave splitting in the Appalachians and the Pyrenees: importance of the inherited tectonic fabric of the lithosphere | Q105127497 | ||
The Borborema shear zone system, NE Brazil | Q105127532 | ||
Successive mixing and mingling of magmas in a plutonic complex of Northeast Brazil | Q105127536 | ||
Initiation and propagation of shear zones in a heterogeneous continental lithosphere | Q105127549 | ||
Seismic and electrical anisotropies in the lithosphere across the Grenville Front, Canada | Q107253220 | ||
Interpretation of SKS-waves using samples from the subcontinental lithosphere | Q107275030 | ||
High-temperature creep of olivine single crystals 1. Mechanical results for buffered samples | Q107275406 | ||
P433 | issue | 1-2 | |
P921 | main subject | lithosphere | Q83296 |
rheology | Q271707 | ||
heterogeneity | Q928498 | ||
P304 | page(s) | 61-86 | |
P577 | publication date | 1998-10-01 | |
P1433 | published in | Tectonophysics | Q7692857 |
P1476 | title | Rheological heterogeneity, mechanical anisotropy and deformation of the continental lithosphere | |
P478 | volume | 296 |
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Q61469970 | Finite element model predictions of static deformation from dislocation sources in a subduction zone: Sensitivities to homogeneous, isotropic, Poisson-solid, and half-space assumptions |
Q107421769 | From microscope to mountain belt: 150 years of petrology and its contribution to understanding geodynamics, particularly the tectonics of orogens |
Q47235567 | Laboratory measurements of the viscous anisotropy of olivine aggregates |
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Q102473049 | Structural architecture and displacement accommodation mechanisms at the termination of the Priestley Fault, northern Victoria Land, Antarctica |
Q63387457 | Tectonothermal Evolution of the Broadly Rifted Zone, Ethiopian Rift |
Q59810853 | Three-dimensional laboratory modelling of rifting: application to the Baikal Rift, Russia |
Q64029104 | Upper mantle deformation and seismic anisotropy in continental rifts |
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