Bibliografías temáticas / Lithospheric Deformation

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Literatura académica sobre el tema "Lithospheric Deformation"

Autor: Grafiati
Publicado: 4 de junio de 2021
Última modificación: 14 de febrero de 2022

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Artículos de revistas sobre el tema "Lithospheric Deformation"

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Dérerová, Jana, Miroslav Bielik, Mariana Pašiaková, Igor Kohút y Petra Hlavńová. "Calculation of temperature distribution and rheological properties of the lithosphere along transect II in the Western Carpathian-Pannonian Basin region". Contributions to Geophysics and Geodesy 44, n.º 2 (1 de junio de 2014): 149–60. http://dx.doi.org/10.2478/congeo-2014-0009.

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Abstract The temperature model of the lithosphere along transect II passing through the Western Carpathians and the Pannonian Basin has been calculated using 2D integrated geophysical modelling methodology. Based on the extrapolation of failure criteria, lithology and calculated temperature distribution, we derived the rheology model of the lithosphere in the area. Our results indicate a decrease of the lithospheric strength from the European platform and the Western Carpathians towards the Pannonian Basin. The largest strength can be observed within the upper crust which suggests rigid deformation in this part of the lithosphere. In the lithospheric mantle, strength almost disappears which allows us to assume that the ductile deformation dominates in this part of the lithosphere
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2

Kelly, Sean, Christopher Beaumont y Jared P. Butler. "Inherited terrane properties explain enigmatic post-collisional Himalayan-Tibetan evolution". Geology 48, n.º 1 (28 de octubre de 2019): 8–14. http://dx.doi.org/10.1130/g46701.1.

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Abstract Observations highlight the complex tectonic, magmatic, and geodynamic phases of the Cenozoic post-collisional evolution of the Himalayan-Tibetan orogen and show that these phases migrate erratically among terranes accreted to Asia prior to the Indian collision. This behavior contrasts sharply with the expected evolution of large, hot orogens formed by collision of lithospheres with laterally uniform properties. Motivated by this problem, we use two-dimensional numerical geodynamical model experiments to show that the enigmatic behavior of the Himalayan-Tibetan orogeny can result from crust-mantle decoupling, transport of crust relative to the mantle lithosphere, and diverse styles of lithospheric mantle delamination, which emerge self-consistently as phases in the evolution of the system. These model styles are explained by contrasting inherited mantle lithosphere properties of the Asian upper-plate accreted terranes. Deformation and lithospheric delamination preferentially localize in terranes with the most dense and weak mantle lithosphere, first in the Qiangtang and then in the Lhasa mantle lithospheres. The model results are shown to be consistent with 11 observed complexities in the evolution of the Himalayan-Tibetan orogen. The broad implication is that all large orogens containing previously accreted terranes are expected to have an idiosyncratic evolution determined by the properties of these terranes, and will be shown to deviate from predictions of uniform lithosphere models.
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3

McNutt, Marcia. "Lithospheric stress and deformation". Reviews of Geophysics 25, n.º 6 (1987): 1245. http://dx.doi.org/10.1029/rg025i006p01245.

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Lamarque, Gaelle y Jordi Julià. "Lithospheric and sublithospheric deformation under the Borborema Province of northeastern Brazil from receiver function harmonic stripping". Solid Earth 10, n.º 3 (21 de junio de 2019): 893–905. http://dx.doi.org/10.5194/se-10-893-2019.

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Abstract. The depth-dependent anisotropic structure of the lithosphere under the Borborema Province in northeast Brazil has been investigated via harmonic stripping of receiver functions developed at 39 stations in the region. This method retrieves the first (k=1) and second (k=2) degree harmonics of a receiver function dataset, which characterize seismic anisotropy beneath a seismic station. Anisotropic fabrics are in turn directly related to the deformation of the lithosphere from past and current tectonic processes. Our results reveal the presence of anisotropy within the crust and the lithospheric mantle throughout the entire province. Most stations in the continental interior report consistent anisotropic orientations in the crust and lithospheric mantle, suggesting a dominant northeast–southwest pervasive deformation along lithospheric-scale shear zones developed during the Brasiliano–Pan-African orogeny. Several stations aligned along a northeast–southwest trend located above the (now aborted) Mesozoic Cariri–Potiguar rift display large uncertainties for the fast-axis direction. This non-azimuthal anisotropy may be related to a complex anisotropic fabric resulting from a combination of deformation along the ancient collision between Precambrian blocks, Mesozoic extension and thermomechanical erosion dragging by sublithospheric flow. Finally, several stations along the Atlantic coast reveal depth-dependent anisotropic orientations roughly (sub)perpendicular to the margin. These results suggest a more recent overprint, probably related to the presence of frozen anisotropy in the lithosphere due to stretching and rifting during the opening of the South Atlantic.
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Wilson, Terry J. "Processes of continental Lithospheric Deformation". Geochimica et Cosmochimica Acta 54, n.º 10 (octubre de 1990): 2899–900. http://dx.doi.org/10.1016/0016-7037(90)90030-o.

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Dehler, S. A. y C. E. Keen. "Effects of rifting and subsidence on thermal evolution of sediments in Canada's east coast basins". Canadian Journal of Earth Sciences 30, n.º 9 (1 de septiembre de 1993): 1782–98. http://dx.doi.org/10.1139/e93-158.

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Regional maps of lithospheric deformation and thermal history have been derived for the eastern continental margin of Canada. Subsidence associated with the rifting and cooling stages of rifted margin formation was calculated from gridded maps of sediment thickness and bathymetry along the Labrador, Grand Banks, and Nova Scotian margins. A two-layer lithospheric extension model was used to compute the deformation and thermal evolution of each region. Deformation results show that the crust and lower lithosphere have generally stretched by different amounts, and that either crustal or subcrustal lithospheric stretching dominates beneath the various basins. Thermal modelling results for the older Nova Scotian and Grand Banks margins show a strong correlation between thermal gradient, crustal stretching, and sediment thickness, and the predicted thermal gradient pattern for the younger Labrador margin correlates extremely well with predicted stretching of the still-cooling subcrustal lithosphere. Predictions of sediment maturity (vitrinite reflectance) of basin deposits were obtained from the derived time – temperature histories. Model results have been constrained with observations from individual boreholes and extrapolated away from these well-constrained areas into regions beyond the frontiers of present exploration. Results are presented as maps showing depths to present-day peak thermal maturity zones and the ages at which earliest post-rift sediments reached peak maturity levels. This reconnaissance approach has led to predictions of thermal maturity zones suitable for oil or gas generation in western Orphan Basin and beneath the continental slopes.
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Dérerová, Jana, Miroslav Bielik, Igor Kohút y Dominika Godová. "Calculation of temperature distribution and rheological properties of the lithosphere along transect IV in the Western Carpathian-Pannonian Basin region". Contributions to Geophysics and Geodesy 49, n.º 4 (1 de diciembre de 2019): 497–510. http://dx.doi.org/10.2478/congeo-2019-0026.

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Abstract 2D integrated modelling algorithm was used to calculate the temperature distribution in the lithosphere along the transect IV located in the Western Carpathian-Pannonian Basin area. Based on the determined temperature field and given rheological parameters of the rocks, it was possible to calculate the strength distribution for both compressional and extensional regimes, construct the strength envelopes for chosen columns of the main tectonic units of the model, and thus construct a simple rheological model of the lithosphere along transect IV. The obtained results indicate decrease of the lithospheric strength from the European platform and the Western Carpathians towards the Pannonian Basin. The largest strength (valid for all tectonic units) can be observed within the upper crust with its maxima on the boundary between upper and lower crust, decreasing towards lower crust and disappearing in the lithospheric mantle, suggesting mostly rigid deformation occurring in the upper crust. A local increase in the values of strength can be observed in the eastern segment of the Western Carpathians where crustal thickening accompanies the lithospheric thickening (formation of the lithospheric root), unlike the previous models along transects I and II, that pass through the western segment of the Western Carpathians and their lithosphere-asthenosphere boundary is almost flat and therefore no accompanying crustal thickening is observed and the decrease in strength is slow and steady.
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Singh, Ramesh P., Q. Li y E. Nyland. "Lithospheric deformation beneath the Himalayan region". Physics of the Earth and Planetary Interiors 61, n.º 3-4 (enero de 1990): 291–96. http://dx.doi.org/10.1016/0031-9201(90)90112-b.

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Wu, Fu-Yuan, Jin-Hui Yang, Yi-Gang Xu, Simon A. Wilde y Richard J. Walker. "Destruction of the North China Craton in the Mesozoic". Annual Review of Earth and Planetary Sciences 47, n.º 1 (30 de mayo de 2019): 173–95. http://dx.doi.org/10.1146/annurev-earth-053018-060342.

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The North China Craton (NCC) was originally formed by the amalgamation of the eastern and western blocks along an orogenic belt at ∼1.9 Ga. After cratonization, the NCC was essentially stable until the Mesozoic, when intense felsic magmatism and related mineralization, deformation, pull-apart basins, and exhumation of the deep crust widely occurred, indicative of destruction or decratonization. Accompanying this destruction was significant removal of the cratonic keel and lithospheric transformation, whereby the thick (∼200 km) and refractory Archean lithosphere mantle was replaced by a thin (<80 km) juvenile one. The decratonization of the NCC was driven by flat slab subduction, followed by a rollback of the paleo-Pacific plate during the late Mesozoic. A global synthesis indicates that cratons are mainly destroyed by oceanic subduction, although mantle plumes might also trigger lithospheric thinning through thermal erosion. Widespread crust-derived felsic magmatism and large-scale ductile deformation can be regarded as petrological and structural indicators of craton destruction. ▪ A craton, a kind of ancient continental block on Earth, was formed mostly in the early Precambrian (>1.8 Ga). ▪ A craton is characterized by a rigid lithospheric root, which provides longevity and stability during its evolutionary history. ▪ Some cratons, such as the North China Craton, can be destroyed by losing their stability, manifested by magmatism, deformation, earthquake, etc.
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Dombrádi, Endre, Dimitrios Sokoutis, Gábor Bada, Sierd Cloetingh y Frank Horváth. "Modelling recent deformation of the Pannonian lithosphere: Lithospheric folding and tectonic topography". Tectonophysics 484, n.º 1-4 (marzo de 2010): 103–18. http://dx.doi.org/10.1016/j.tecto.2009.09.014.

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Tesis sobre el tema "Lithospheric Deformation"

1

Beard, Eric P. "Modeling Lithospheric Rheology from Modern Measurements of Bonneville Shoreline Deformation". DigitalCommons@USU, 2012. https://digitalcommons.usu.edu/etd/1362.

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Here I develop a cross-correlation approach to estimating heights of shoreline features, and apply the new method to paleo-shorelines of Pleistocene Lake Bonneville. I calculate 1st-derivative (slope) and 2nd-derivative (curvature) profiles from Digital Elevation Model (DEM) or Global Positioning System Real-Time Kinematic (GPS-RTK) measurements of elevation. I then cross-correlate pairs of profiles that have been shifted by various "lags," or shifts in elevation. The correlation coefficient (a normalized dot-product measure of similarity) is calculated as a function of lag within small (~40 m) windows centered at various elevations. The elevation and lag with the greatest correlation coefficient indicates the shoreline elevation at the reference profile and the change in shoreline height for the profile pair. I evaluate several different algorithms for deriving slope and curvature by examining closure of elevation lags across profile triples. I then model isostatic response to Lake Bonneville loading and unloading. I first model lakeshore uplift response to lake load removal assuming an elastic layer over an inviscid half-space. I obtain a best-fit comparison of predicted to observed shoreline heights for the Bonneville level with an elastic layer thickness, Te, of 25±2 km (at 95% confidence) when using only previously published shoreline elevation estimates. The best-fit for the Bonneville level when using these estimates plus 44 new estimates suggests a Te of 26±2 km. The best-fit model for the Provo level suggests Te of 17±3 km. For the Gilbert level, the response is insensitive to the assumed Te. I next model isostatic response to Bonneville loading and unloading assuming an elastic layer over a viscoelastic halfspace. This approach assumes constant parameters for the entire loading history, and yields a best-fit model with Te =70±5 km and viscosity ç=~2x1018 Pa s with 95% confidence ranging from ~1x1018 to ~5x1019 Pa s when only the previously published data are used. With the newer data added, the best-fit model has Te =58±2 km and ç ranging from ~1x1018 to ~1x1019 Pa s with 95% confidence. The 12-15 m weighted root-mean-square misfit to the best-fitting model is dominated by tectonic signals related to Basin-and-Range tectonics particularly seismic offsets of the Wasatch fault, and closely mimics the geological timescale pattern of basin-subsidence and range-uplift.
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2

Audet, Pascal. "Seismic and mechanical attributes of lithospheric deformation and subduction in western Canada". Thesis, University of British Columbia, 2008. http://hdl.handle.net/2429/2435.

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Convergent continental margins are regions of intense deformation caused by the interaction of oceanic plates with continents. The spatial extent of deformation is broadly commensurate with the specific time scale of the causative phenomenon. For example, subduction-related short-term deformation is limited to <200 km from the margin, whereas long-term plate convergence cause deformation over ∼1000 km landward. Deformation is thus manifested in multiple ways, with attributes depending on the scale of measurement. In this thesis we investigate the use of two geophysical approaches in the study of deformation: 1) The analysis of potential-field anomalies to derive estimates of the elastic thickness (Te) of the lithosphere, and 2) The structural study of past and present subduction systems using seismic observations and modelling. Both approaches involve the development of appropriate methodologies for data analysis and modelling, and their application to the western Canadian landmass. Our findings are summarized as follows: 1) We develop a wavelet-based technique to map variations in Te and its anisotropy; 2) We show how a step-wise transition in Te and its anisotropy from the Cordillera to the Craton is a major factor influencing lithospheric deformation; 3) We implement a waveform modelling tool that includes the effects of structural heterogeneity and anisotropy for teleseismic applications, and use it to model the signature of a fossil subduction zone in a Paleoproterozoic terrane; 4) We use teleseismic recordings to map slab edge morphology in northern Cascadia and show how slab window tectonism and slab stretching led to the creation of the oceanic Explorer plate; 5) We use seismic signals from the subducting oceanic crust to calculate elevated Poisson’s ratio and infer high pore-fluid pressures and a low-permeability plate boundary within the forearc region of northern Cascadia.
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3

Saunders, Paul Nicholas. "The lithospheric structure of western Turkey : crustal deformation in an extending region". Thesis, University of Cambridge, 1996. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.336353.

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4

Moisio, K. (Kari). "Numerical lithospheric modelling: rheology, stress and deformation in the central Fennoscandian Shield". Doctoral thesis, University of Oulu, 2005. http://urn.fi/urn:isbn:9514279514.

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Abstract This thesis deals with the analysis of the rheological structure and tectonic modelling of the Fennoscandian Shield. First, a short introduction to the geology and geophysics of the Fennoscandian Shield is presented followed by a description of rheological concepts. Second, the applied modelling procedures, together with the sources of error are explained. Last a brief summary of each original paper including conclusions is given. Understanding rheological conditions through the entire lithosphere and even deeper is the key for understanding the deformation of the earth's interior. Thus, investigating the rheological structure and possible consequences resulting from tectonic loading are required to some extent when interpreting geophysical data into tectonic models. In this thesis rheological structure is obtained by calculating rheological strength in different locations of the central Fennoscandian Shield. These locations are mainly situated along different deep seismic sounding (DSS) profiles as they provide necessary geophysical information required for model construction. Modelling begins by solving the thermal structure in the lithosphere, as rheological behaviour, mainly ductile flow is strongly controlled by temperature. Results from these calculations show that the rheological structure of the lithosphere depends on the thermal conditions resulting in significant areal variations. Generally, the central Fennoscandian Shield can be considered to be rheologically rather strong. Rheologically weak layers are however usually found in the lower crust. Correlation of the rheological structure with earthquake focal depth data shows that brittle fracture is the relevant mechanism in the earthquake generation and that non-occurrence of deep earthquakes implies low stress or high strength conditions deeper in the crust. Calculated rheological structure is furthermore used as a material parameter in the structural models which are solved next. These results suggest that it is highly unlikely that any considerable ductile deformation in the crust of the central Fennoscandian Shield exists and it seems that the present-day thermal and mechanical conditions in the investigated area do not favour such processes in significant amounts.
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5

Püsök, Adina E. [Verfasser]. "Three-dimensional numerical modelling of subduction/collision and lithospheric deformation / Adina E. Püsök". Mainz : Universitätsbibliothek Mainz, 2016. http://d-nb.info/1105494594/34.

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6

Behn, Mark Dietrich 1974. "The evolution of lithospheric deformation and crustal structure from continental margins to oceanic spreading centers". Thesis, Massachusetts Institute of Technology, 2002. http://hdl.handle.net/1721.1/29061.

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Thesis (Ph. D.)--Joint Program in Oceanography (Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Science; and the Woods Hole Oceanographic Institution), 2002.
Includes bibliographical references (p. 221-243).
This thesis investigates the evolution of lithospheric deformation and crustal structure from continental margins to mid-ocean ridges. The first part (Ch. 2) examines the style of segmentation along the U.S. East Coast Margin and investigates the relationship between incipient margin structure and segmentation at the modem Mid-Atlantic Ridge. The second part (Chs. 3-5) focuses on the mechanics of faulting in extending lithosphere. In Ch. 3, I show that the incorporation of a strain-rate softening rheology in continuum models results in localized zones of high strain rate that are not imposed a priori and develop in response to the rheology and boundary conditions. I then use this approach to quantify the effects of thermal state, crustal thickness, and crustal rheology on the predicted style of extension deformation. The mechanics of fault initiation and propagation along mid-ocean ridge segments is investigated in Ch. 4. Two modes of fault development are identified: Mode C faults that initiate near the center of a segment and Mode E faults that initiate at the segment ends. Numerical results from Ch. 5 predict that over time scales longer than a typical earthquake cycle transform faults behave as zones of significant weakness.
(cont.) Furthermore, these models indicate that Mode E faults formed at the inside-corner of a ridge-transform intersection will experience preferential growth relative to faults formed at the conjugate outside-corner due to their proximity to the weak transform zone. Finally, the last part of this thesis (Ch. 6) presents a new method to quantify the relationship between the seismic velocity and composition of igneous rocks. A direct relationship is derived to relate Vp to major element composition and typical velocity-depth profiles are used to calculate compositional bounds for the lower continental, margin, and oceanic crust.
by Mark Dietrich Behn.
Ph.D.
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7

Cohen, Shaina Marie. "An assessment of heterogeneity within the lithospheric mantle, Marie Byrd Land, West Antarctica". Thesis, Boston College, 2016. http://hdl.handle.net/2345/bc-ir:106873.

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Thesis advisor: Seth C. Kruckenberg
The West Antarctic rift system is one of the most expansive regions of extended continental crust on Earth, but relatively little is known about the structure of the mantle lithosphere in this region. This research aims to examine a suite of ultramafic mantle xenoliths from several volcanic centers located throughout Marie Byrd Land, West Antarctica. Through the use of several complementary analytical methods, the deformational and compositional heterogeneity of the lithospheric mantle in this region is characterized. The Marie Byrd Land xenoliths have equilibration temperatures between 779 and 1198°C, which is a range that corresponds to extraction depths between 39 and 72 km. These samples preserve significant mineralogical and microstructural heterogeneities that document both lateral and vertical heterogeneities within the Marie Byrd Land mantle lithosphere. The modal mineralogy of spinel peridotites varies between 40 – 99% olivine, 0 – 42% diopside, 0 – 45% enstatite and 0 – 5% chromite. Minimum olivine grain sizes range from 60 to 110 µm and maximum olivine grain sizes range from 2.5 to 10.0 mm. The geometric mean grain size of olivine in these samples ranges from 100 µm to 2 mm and has an average of 694 µm. The geometric mean grain size of diopside ranges from 90 to 865 µm and has an average of 325 µm, whereas that of enstatite ranges from 120 µm to 1.2 mm and has an average of 625 µm. Comparatively, the pyroxenites contain 0 – 29% olivine, 29 – 95% diopside, 1 – 36% enstatite and 1 – 11% chromite. Deformation mechanism maps suggest that the olivine within the MBL peridotite xenoliths primarily accommodate strain through the operation of dislocation-accommodated grain-boundary sliding at strain rates between 10-19/s and 10-11/s. This is consistent with microstructural observations of the suite made using optical microscopy (e.g., deformation bands and subgrains in olivine; aligned grain boundaries between contrasting phases). Application of the olivine grain size piezometer indicates that the suite preserves differential stresses ranging from 0.5 MPa to 50 MPa, with mean differential stresses ranging from 4 to 30 MPa. Values of mean differential stress only vary slightly throughout the field area, but generally decrease in magnitude towards the east with maximum values migrating upwards in the lithospheric mantle along this transect. The samples from some volcanic centers are highly homogenous with respect to their microstructural characteristics (e.g., Mount Avers – Bird Bluff), whereas others display heterogeneities on the sub-five-kilometer-scale (e.g., Demas Bluff). Comparatively, mineralogical heterogeneities are more consistent throughout the sample suite with variations generally being observed between the sub-five-kilometer-scale and the sub-ten-kilometer-scale. Most samples within the MBL peridotite suite display axial-[010] or A-type olivine textures. Although less dominant, axial-[100], B-type and random olivine textures are also documented within the suite. Axial-[010] textures have J-indices and M-indices ranging from 1.7 – 4.1 and 0.08 – 0.21, respectively. The average value of the J-index for axial-[010] textures is 2.9, whereas the average M-index of these samples is equal to 0.15. Overall, A-type textures tend to be stronger with J- and M-indices ranging from 1.4 – 9.0 and 0.07 – 0.37, respectively. The olivine crystallographic textures of the MBL xenolith suite are heterogeneous on scales that are smaller than the highest resolution that is attainable using contemporary geophysical methods, which implies that patterns of mantle flow and deformation are far more complex than these studies suggest
Thesis (MS) — Boston College, 2016
Submitted to: Boston College. Graduate School of Arts and Sciences
Discipline: Earth and Environmental Sciences
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8

Frets, Erwin C. "Thermo-mechanical evolution of the subcontinental lithospheric mantle in extensional environment : Insights from the Beni Bousera peridotite massif (Rif belt, Morocco)". Thesis, Montpellier 2, 2012. http://www.theses.fr/2012MON20090/document.

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Les processus de déformation contrôlant l'amincissement de la lithosphère continentale sont encoremal contraints. Nos connaissances sont principalement basées sur la modélisation thermomécaniqued'extension à l'échelle de la lithosphere—utilisant des lois rhéologiques derivées expérimentalement,l'imagerie géophysique et l'analyse de xénolithes provenant de rift continentaux actifs à ce jour, tels quele Rift Est-Africain. L'originalité de ce travail reside dans l'étude des deux plus grands massifs depéridotites sous-continentales ayant enregistrées des conditions primaires du facies à diamant: lesmassifs de Beni Bousera au nord du Maroc et de Ronda au sud de l'Espagne, respectivement. Lesstructures et la zonation petrologique et métamorphique —impliquant une évolution polybarique etpolythermique— préservéees dans ces massifs offrent une opportunité unique pour étudier l'évolutionthermo-mécanique du manteau sous-continental dans un contexte extensif.Dans ce travail, nous avons étudié les mécanismes de déformation des péridotites et despyroxénites afin de contraindre les modes d'exhumation du manteau lithosphérique sous-continental,depuis des conditions du facies des lherzolites à grenat, jusqu'au facies à spinelle et enfin à plagioclase.Nous avons combiné la cartographie des faciès tectono-métamorphiques et des structures ductiles dedéformation, l'analyse des microstructures, la mesure d'orientations préférentielles de réseau (OPR), etla géothermobarométrie conventionelle couplée à la modélisation thermodynamique (PerpleX) afin decontraindre les conditions de pression et température de la déformation. Nous avons montré quel'exhumation précoce du facies à grenat au facies à spinelle était accomodée par une faille transtensiveaffectant le manteau lithosphérique. Dans ce contexte, la zonation tectono-métamorphique et legradient thermique important (ca. 100ºC/km) préservés à Beni Bousera résultent de la juxtapositionmécanique de domaines lithosphériques initialement équilibrés à différentes pressions et températures,fossilisée à une profondeur de ca. 60 km durant l'Oligocène supérieur (ca. 25 Ma). L'exhumation finaledu facies de lherzolite à spinelle au facies à plagioclase et l'emplacement final dans la croûte, mieuxenregistrés dans Ronda, se sont produits par inversion et plissement de la section lithosphériquefortement amincie dans un contexte arrière-arc, probablement lors du retrait vers le sud de lalithosphère subduite et la collision de l'arc avec les paléo-marges maghrébines au Miocène inférieur(21-23 Ma)
The mantle deformation processes that control the thinning and break-up of continentallithosphere remain poorly understood. Our knowledge is restricted to either lithospheric scalethermo-mechanical models —that use experimentally derived flow laws—, geophysicalimaging and/or rare xenoliths from active continental rifts, such as the East African Rift System.The originality of this work relies on the study of the two largest outcrops of diamond faciessubcontinental lithospheric mantle in the world: the Beni Bousera and Ronda peridotite massifsin N Morocco and S Spain, respectively. The structures and petrologic and metamorphic zoningpreserved in these massifs —implying a polybaric and polythermal evolution— provide aunique opportunity to investigate the thermo-mechanical evolution of thick subcontinentallithospheric mantle in extensional settings.In this thesis we studied the deformation mechanisms in both peridotites andpyroxenites to constrain the modes of exhumation of subcontinental lithospheric mantle fromgarnet-, to spinel-, and finally, to plagioclase lherzolite facies conditions. We combined fieldmapping of tectono-metamorphic domains and structural mapping of ductile structures,microstructural analysis, crystal preferred orientations (CPO) measurements and conventionalthermobarometric calculations and thermodynamic modeling (Perple_X) to unravel the pressureand temperature conditions of deformation. We showed that exhumation from garnet- to spinellherzolite facies conditions was accommodated by fast shearing —in thermal disequilibrium—along a lithospheric scale transtensional shear zone. In this context, the petrological zoning andthe large temperature gradient (ca. 100ºC/km) preserved in the Beni Bousera massif representthe mechanical juxtaposition of progressively deeper and hotter lithospheric levels at depths ofca. 60 km in the latest Oligocene (ca. 25 Ma). Final exhumation from spinel- to plagioclasefacies lherzolite and emplacement into the crust is best recorded in the Ronda massif where itoccurred by inversion and lithospheric scale folding of the highly attenuated continentallithosphere in a back-arc region, probably in relation with southward slab rollback andsubsequent collision with the palaeo-Maghrebien passive margin in the early Miocene (21-23Ma)
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Popov, Anton. "Three-dimensional thermo-mechanical modeling of deformation at plate boundaries : case study San Andreas Fault System". Phd thesis, Universität Potsdam, 2008. http://opus.kobv.de/ubp/volltexte/2009/3187/.

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It has always been enigmatic which processes control the accretion of the North American terranes towards the Pacific plate and the landward migration of the San Andreas plate boundary. One of the theories suggests that the Pacific plate first cools and captures the uprising mantle in the slab window, and then it causes the accretion of the continental crustal blocks. The alternative theory attributes the accretion to the capture of Farallon plate fragments (microplates) stalled in the ceased Farallon-North America subduction zone. Quantitative judgement between these two end-member concepts requires a 3D thermomechanical numerical modeling. However, the software tool required for such modeling is not available at present in the geodynamic modeling community. The major aim of the presented work is comprised basically of two interconnected tasks. The first task is the development and testing of the research Finite Element code with sufficiently advanced facilities to perform the three-dimensional geological time scale simulations of lithospheric deformation. The second task consists in the application of the developed tool to the Neogene deformations of the crust and the mantle along the San Andreas Fault System in Central and northern California. The geological time scale modeling of lithospheric deformation poses numerous conceptual and implementation challenges for the software tools. Among them is the necessity to handle the brittle-ductile transition within the single computational domain, adequately represent the rock rheology in a broad range of temperatures and stresses, and resolve the extreme deformations of the free surface and internal boundaries. In the framework of this thesis the new Finite Element code (SLIM3D) has been successfully developed and tested. This code includes a coupled thermo-mechanical treatment of deformation processes and allows for an elasto-visco-plastic rheology with diffusion, dislocation and Peierls creep mechanisms and Mohr-Coulomb plasticity. The code incorporates an Arbitrary Lagrangian Eulerian formulation with free surface and Winkler boundary conditions. The modeling technique developed is used to study the aspects influencing the Neogene lithospheric deformation in central and northern California. The model setup is focused on the interaction between three major tectonic elements in the region: the North America plate, the Pacific plate and the Gorda plate, which join together near the Mendocino Triple Junction. Among the modeled effects is the influence of asthenosphere upwelling in the opening slab window on the overlying North American plate. The models also incorporate the captured microplate remnants in the fossil Farallon subduction zone, simplified subducting Gorda slab, and prominent crustal heterogeneity such as the Salinian block. The results show that heating of the mantle roots beneath the older fault zones and the transpression related to fault stepping, altogether, render cooling in the slab window alone incapable to explain eastward migration of the plate boundary. From the viewpoint of the thermomechanical modeling, the results confirm the geological concept, which assumes that a series of microplate capture events has been the primary reason of the inland migration of the San Andreas plate boundary over the recent 20 Ma. The remnants of the Farallon slab, stalled in the fossil subduction zone, create much stronger heterogeneity in the mantle than the cooling of the uprising asthenosphere, providing the more efficient and direct way for transferring the North American terranes to Pacific plate. The models demonstrate that a high effective friction coefficient on major faults fails to predict the distinct zones of strain localization in the brittle crust. The magnitude of friction coefficient inferred from the modeling is about 0.075, which is far less than typical values 0.6 – 0.8 obtained by variety of borehole stress measurements and laboratory data. Therefore, the model results presented in this thesis provide additional independent constrain which supports the “weak-fault” hypothesis in the long-term ongoing debate over the strength of major faults in the SAFS.
Seit jeher rätselhaft sind die Prozesse, die die Akkretion der Nordamerikanischen Terranen in Richtung der Pazifischen Platte sowie die Wanderung der Plattengrenze der San-Andreas-Verwerfung in Richtung Festland bestimmen. Eine Theorie besagt, dass sich die Pazifische Platte erst abkühlt und den aufsteigenden Mantel im „Slab Window“ fängt und somit die Akkretion der kontinentalen Krustenblöcke bewirkt. Die andere Theorie geht von einer Akkretion durch das Fangen von Teilen der Farallon-Platte (Mikroplatten) aus, die in der inaktiven nordamerikanischen Farallon-Subduktionszone fest stecken. Die quantitative Beurteilung dieser beiden gegensätzlichen Konzepte erfordert eine thermomechanische numerische 3-D-Modellierung. Das dafür benötigte Software Tool steht jedoch der geodynamischen Modellierung derzeit noch nicht zur Verfügung. Das Hauptziel der vorliegenden Arbeit umfasst im Wesentlichen zwei miteinander verbundene Aufgaben. Die erste besteht in der Entwicklung und Erprobung des Finite-Element-Codes, dessen Eigenschaften den hohen Anforderungen an die Ausführung der dreidimensionalen Simulationen lithosphärischer Deformation auf geologischer Zeitskala gerecht werden müssen. Die zweite Aufgabe ist die Anwendung des entwickelten Tools auf die neogenen Deformationen der Kruste und des Mantels entlang der San-Andreas-Verwerfung in Zentral- und Nordkalifornien. Die Modellierung auf geologischer Zeitskala lithosphärischer Deformation bringt für die Software Tools in Bezug auf Konzept und Durchführung zahlreiche Herausforderungen mit sich. Unter anderem gilt es, den Brittle-Ductile-Übergang in einem einzigen Modell sowie die Gesteinsrheologie in einer breiten Spanne unterschiedlicher Temperaturen und Spannungen adäquat darzustellen und die extremen Deformationen der freien Oberfläche und internen Grenzen aufzulösen. Im Rahmen der vorliegenden Arbeit erfolgte die erfolgreiche Entwicklung und Erprobung des neuen Finite-Element-Codes (SLIM3D). Dieser Code beinhaltet eine gekoppelte thermomechanische Behandlung von Deformationsprozessen und ermöglicht eine elasto-visko-plastische Rheologie mit Diffusion, Dislokation, Peierls Kriechmechanismen und Mohr-Coulomb-Plastizität. Der Code verbindet eine Arbitrary Lagrangian-Eulerian kinematische Formulierung mit freien Oberflächen- und Winkler-Randbedingungen. Das entwickelte Modellierungsverfahren wird für die Untersuchung der Aspekte verwendet, die die neogene lithosphärische Deformation in Zentral- und Nordkalifornien beeinflussen. Die Modellanordnung konzentriert sich auf die Interaktion zwischen drei großen tektonischen Elementen in dieser Region: die Nordamerikanische Platte, die Pazifische Platte sowie die Gorda-Platte, die sich in der Mendocino-Triple-Junction treffen. Unter anderem verdeutlicht die Modellierung den Einfluss des Aufsteigens der Asthenosphäre in das sich öffnende „slab window“ der übergelagerten Nordamerikanischen Platte. Die Modelle beziehen auch die angelagerten Überreste der Mikroplatten in der fossilen Farallon-Subduktionszone, die vereinfachte subduzierende Gorda-Platte sowie markante Heterogenitäten der Kruste, wie beispielsweise den „Salinian Block“, mit ein. Die Ergebnisse zeigen, dass die Erwärmung der Mantellithosphäre unter den älteren Störungszonen sowie die Transpression eine Abkühlung im „Slab Window“ als alleinige Begründung für die Ostwärtsbewegung der Plattengrenze nicht zulassen. Aus Sicht der thermomechanischen Modellierung bestätigen die Ergebnisse das geologische Konzept, welches durch das mehrmalige Fangen von Mikroplatten den Hauptgrund für die Wanderung der Plattengrenze der San-Andreas-Verwerfung in Richtung Festland über die letzten 20 Millionen Jahre sieht. Die Überreste der Farallon-Platte, die in der fossilen Subduktionszone gefangen sind, verursachen im Mantel eine wesentlich stärkere Heterogenität als die Abkühlung der Asthenosphäre und stellen somit den effizienteren und direkteren Weg für die Anlagerung der nordamerikanischen Gebiete an die Pazifische Platte dar. Die Modelle demonstrieren, dass ein hoher effektiver Reibungskoeffizient an großen Störungen nicht in der Lage ist, die eindeutigen Zonen der Dehnungslokalisierung in der spröden Kruste vorherzusagen. Die Größe des Reibungskoeffizienten, die sich aus der Modellierung ableitet, beträgt etwa 0,075 und ist damit wesentlich kleiner als die durch unterschiedliche Bohrlochmessungen und Labordaten ermittelten Spannungswerte zwischen 0,6 und 0,8. Daher liefern die in dieser Arbeit präsentierten Ergebnisse der Modelle in der seit langem geführten Debatte über die Stärke von großen Störungen in der San-Andreas-Verwerfung eine zusätzliche unabhängige Begründung der „Weak-Fault“-Hypothese.
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Kourim, Fatna. "Architecture lithosphérique et dynamique du manteau sous le Hoggar : le message des xénolites". Thesis, Montpellier 2, 2013. http://www.theses.fr/2013MON20040.

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Cette étude vise caractériser le manteau lithosphérique du massif du Hoggar (Algérie) et son évolution, grâce à une étude multidisciplinaire (pétrologique, géochimique et pétrophysique) d'enclaves mantelliques échantillonnées par le volcanisme cénozoïque. L'échantillonnage provient de deux districts volcaniques (Tahalagha et Manzaz) situés respectivement en périphérie et au coeur du bombement du Hoggar. Le district de Tahalgha est par ailleurs situé à cheval sur un grand cisaillement pan-africain (le 4°35), séparant deux domaines structuraux majeurs du socle du Hoggar : le Hoggar Central Polycyclique à l'Est (domaine LATEA) et le Hoggar occidental à l'Ouest (bloc d'Iskel). Les xénolites étudiés apportent des informations sur l'évolution du manteau lithosphérique depuis l'orogenèse pan-africaine, au cours de laquelle s'est structuré le socle de cette région (le Bouclier Touareg), jusqu'aux événements cénozoïques responsables du bombement topographique et du volcanisme.L'héritage pan-africain est essentiellement préservé dans les échantillons du district périphérique de Tahalgha, sous la forme de lherzolites équilibrées à basse température (750 - 900°C), à clinopyroxènes appauvris en terres rares légères. Ces échantillons sont considérés comme représentant la lithosphère sous-continentale à l'issue des processus de réjuvénation qui ont marqué les derniers stades de l'orogenèse pan-africaine. Ils montrent des textures de déformation (porphyroclastiques à equigranulaires) bien préservées, attribuées à ces événements et caractérisées par des orientations cristallographiques préférentielles (OPRs) de l'olivine (axiales-[010]) compatibles avec un régime transpressif. Les événements cénozoïques sont marqués par un recuit partiel de ces textures, particulièrement prononcé à Manzaz et dans les échantillons de Tahalgha équilibrés à des températures moyennes à élevées (900-1150°C), et affectés par différents degrés de métasomatisme. Les xénolites de Tahalgha représentent un cas d'étude exemplaire du métasomatisme mantellique, couplant variations texturales, minéralogiques et chimiques le long de gradient locaux de température. Une modification des OPRs d'olivine est observée, qui résulterait à la fois de l'infiltration de liquides métasomatiques et d'une réactivation des accidents pan-africains en cisaillement pur.Des implications importantes de cette étude résident dans l'échelle des variations de premier ordre attribuées aux interactions lithosphère-asthénosphère au Cénozoïque. Celles-ci sont essentiellement à l'échelle du bombement du Hoggar (différences entre Manzaz et Tahalga, c'est-à-dire entre Hoggar central et périphérique) ou à celle de conduits magmatiques et de leurs épontes (variabilité locale des xénolites de Tahalgha). Par contre, les résultats obtenus montrent peu de variations significatives pour les échelles intermédiaires, notamment pour des localités de Tahlagha situées de part et d'autre ou à différentes distances du 4°35. Ceci favorise plutôt, pour l'origine du bombement volcanique du Hoggar, les modèles faisant appel à des structures d'assez grande échelle telle qu'un panache mantellique ou une cellule de convection asthénosphérique de type « Edge Driven Convection », plutôt qu'un processus essentiellement lié à la réactivation des failles lithosphériques pan-africaines
This study aims to characterize the lithospheric mantle of the Hoggar swell (Algeria) and its evolution through time via a multidisciplinary (petrological, geochemical and petrophysical) study of mantle xenoliths sampled by Cenozoic volcanism. The samples were collected in two volcanic districts (Tahalagha and Manzaz) located in the periphery and in the central part of the Hoggar massif, respectively. The Tahalgha sampling also straddles a mega pan-African shear zone (the 4°35 fault) between two major structural domains of the Tuareg Shield basement: the Central Polycyclic Hoggar to the East (LATEA terranes) and the Western Hoggar domain to the West (Iskel block). The studied xenoliths provide information on the evolution of the lithospheric mantle from the Pan-African orogeny – i.e. the period when the Tuareg Shield was structured – to the Cenozoic events responsible for topographic upwelling and volcanism in the Hoggar swell.The Pan-African heritage is found in xenoliths from the peripheral Tahalgha district. These samples are distinguished by low equilibrium temperatures (750-900°C) and LREE-depleted clinopyroxene compositions. They are considered to represent the sub-continental lithosphere after the rejuvenation process that marked the later stages of the Pan-African orogeny. They show well preserved deformation textures (porphyroclastic to equigranular) assigned to these events and characterized by preferential crystallographic orientations (CPOs) of olivine (axial-[010]) consistent with a transpressional regime. The Cenozoic events are marked by partial annealing of these textures, particularly pronounced in the Manzaz samples, as well as in the Tahalgha xenoliths equilibrated at medium to high temperatures (900-1150°C). These samples were affected by different degrees of metasomatism. The Tahalgha xenoliths represent a rather unique case study of mantle metasomatism, where coupled textural, mineralogical and chemical variations occur along local temperature gradients. The Cenozoic events were also responsible for a change in olivine CPOs, resulting from both infiltration of metasomatic fluids and reactivation of Pan-African accidents in a pure-shear regime.Important implications of this study lie in the scale at which the first-order lithosphere modifications ascribed to the Cenozoic event are observed, i.e. either at the scale of the whole Hoggar swell, as shown by the increasing degree of textural annealing and metasomatism from Tahalgha to Manzaz (i.e. from outer to central Hoggar), or at the small scale of magma conduits and their wall rocks, as shown by the local variability registered by the Tahalgha xenoliths. Conversely, our data show little changes at intermediate scales, as might be expected, for instance, among the Tahalgha localities situated on either sides - or at different distances - from the 4°35. As regards the origin of the Hoggar volcanic swell, this result favours the models involving relatively large-scale structures such as a mantle plume or "Edge Driven Convection", rather than a process involving merely the reactivation of pan-African lithospheric faults
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Libros sobre el tema "Lithospheric Deformation"

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Behn, Mark Dietrich. The evolution of lithospheric deformation and crustal structure from continental margins to oceanic spreading centers. Cambridge, Mass: Massachusetts Institute of Technology, 2002.

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Keken, Peter Edwin van. Numerical modelling of thermochemically driven fluid flow with non-Newtonian rheology: Applied to the earth's lithosphere and mantle. [Utrecht: Faculteit Aardwetenschappen der Rijksuniversiteit te Utrecht, 1993.

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Growth and collapse of the Tibetan Plateau. London: Geological Society, 2011.

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Sengör, A. M. Celâl. The large wavelength deformations of the lithosphere: Materials for a history of the evolution of thought from the earliest times to plate tectonics. Boulder, Colo: Geological Society of America, 2003.

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Şengör, A. M. Celâl. The large-wavelength deformations of the lithosphere: Materials for a history of the evolution of thought from the earliest times to plate tectonics. Boulder, CO: Geological Society of America, 2003.

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Şengör, A. M. Celâl. The large wavelength deformations of the lithosphere: Materials for a history of the evolution of thought from the earliest times to plate tectonics. Boulder, CO: Geological Society of America, 2004.

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1929-, Clark Sydney P., Burchfiel B. C. 1934-, Suppe John y Rodgers John 1914-, eds. Processes in continental lithospheric deformation. Boulder, Colo: Geological Society of America, 1988.

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Processes in Continental Lithospheric Deformation. Geological Society of America, 1988. http://dx.doi.org/10.1130/spe218.

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United States. National Aeronautics and Space Administration, ed. Lithospheric structure, seismicity, and contemporary deformation of the United States Cordillera. [Washington, DC: National Aeronautics and Space Administration, 1985.

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United States. National Aeronautics and Space Administration., ed. Lithospheric structure, seismicity, and contemporary deformation of the United States Cordillera. [Washington, DC: National Aeronautics and Space Administration, 1985.

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Capítulos de libros sobre el tema "Lithospheric Deformation"

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Amalvict, Martine y Hilaire Legros. "Lithospheric Deformation and Asthenospheric Pressure". En International Association of Geodesy Symposia, 140–48. New York, NY: Springer New York, 1990. http://dx.doi.org/10.1007/978-1-4615-7109-4_17.

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Pirazzoli, P. A. y D. R. Grant. "Lithospheric Deformation Deduced from Ancient Shorelines". En Recent Plate Movements and Deformation, 67–72. Washington, D. C.: American Geophysical Union, 2013. http://dx.doi.org/10.1029/gd020p0067.

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Aardoom, L. "Current Activities in the Measurement of Lithospheric Plate Motion and Deformation". En Recent Plate Movements and Deformation, 1–3. Washington, D. C.: American Geophysical Union, 2013. http://dx.doi.org/10.1029/gd020p0001.

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Srijayanthi, G. y M. Ravi Kumar. "Seismicity, Lithospheric Structure and Mantle Deformation in the Andaman Nicobar Subduction Zone". En Society of Earth Scientists Series, 107–36. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-39843-9_6.

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Yang, Youqing y Mian Liu. "Algorithms for Optimizing Rheology and Loading Forces in Finite Element Models of Lithospheric Deformation". En Advances in Geocomputing, 119–38. Berlin, Heidelberg: Springer Berlin Heidelberg, 2009. http://dx.doi.org/10.1007/978-3-540-85879-9_4.

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Zoback, M. D. "The Role of Continental Scientific Drilling in Studies of Earthquakes, Crustal Deformation, and Lithospheric Dynamics". En Super-Deep Continental Drilling and Deep Geophysical Sounding, 70–89. Berlin, Heidelberg: Springer Berlin Heidelberg, 1990. http://dx.doi.org/10.1007/978-3-642-50143-2_7.

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Hirth, Greg, Javier EscartíN y Jian Lin. "The Rheology of the Lower Oceanic Crust: Implications for Lithospheric Deformation at Mid-Ocean Ridges". En Faulting and Magmatism at Mid-Ocean Ridges, 291–303. Washington, D. C.: American Geophysical Union, 2013. http://dx.doi.org/10.1029/gm106p0291.

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Braun, Jean y Russell Shaw. "Contrasting styles of lithospheric deformation along the northern margin of the Amadeus Basin, central Australia". En Structure and Evolution of the Australian Continent, 139–56. Washington, D. C.: American Geophysical Union, 1998. http://dx.doi.org/10.1029/gd026p0139.

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Schettino, Antonio. "Seismic Deformation of the Lithosphere". En Quantitative Plate Tectonics, 301–16. Cham: Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-09135-8_11.

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England, P. "Large Rates of Rotation in Continental Lithosphere. Undergoing Distributed Deformation". En Paleomagnetic Rotations and Continental Deformation, 157–64. Dordrecht: Springer Netherlands, 1989. http://dx.doi.org/10.1007/978-94-009-0869-7_11.

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Actas de conferencias sobre el tema "Lithospheric Deformation"

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Demouchy, Sylvie y Patrick Cordier. "Mechanisms of Ductile Deformation in the Lithospheric Mantle (Keynote 3f)". En Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.547.

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Dygert, Nicholas J., Rachel E. Bernard y Whitney M. Behr. "MANTLE XENOLITHS RECORD DEFORMATION ASSOCIATED WITH ACTIVE LITHOSPHERIC DOWNWELLING BENEATH CENTRAL NEVADA". En 67th Annual Southeastern GSA Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018se-312076.

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Sparks, C. Renee y Issac J. Jacques. "GEOLOGIC MAPPING AND LITHOSPHERIC DEFORMATION IN THE STRUCTURALLY COMPLEX REGION OF CENTRAL-WESTERN HONDURAS". En Joint 53rd Annual South-Central/53rd North-Central/71st Rocky Mtn GSA Section Meeting - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019sc-326621.

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Foster, Anna, Fiona Darbyshire y Andrew J. Schaeffer. "THE PHASE-VELOCITY SIGNATURE OF LITHOSPHERIC DEFORMATION IN CENTRAL CANADA AND THE NORTH-CENTRAL UNITED STATES". En 53rd Annual GSA Northeastern Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018ne-311081.

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Kourim, Fatma, Kuo-Lung Wang, Katsuyoshi Michibayanchi y Suzanne Yvette O'Reilly. "Deformation, Metasomatism and Seismic Anisotropy in the Lithospheric Mantle beneath Taiwan Straits, Southeast Asian Margin: Constraints from Mantle Xenoliths". En Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.1364.

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Dilek, Yildirim y Safak Altunkaynak. "CENOZOIC MAGMATISM AND EXTENSIONAL DEFORMATION IN WESTERN ANATOLIA AS A RESULT OF MANTLE RESPONSE TO COLLISION, SLAB BREAK-OFF, AND LITHOSPHERIC TEARING". En GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-341039.

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Weil, Arlo Brandon y Adolph Yonkee. "DEFORMATION PATTERNS ACROSS THE LARAMIDE AND SIERRA PAMPEANAS THICK-SKINNED FORELAND SYSTEMS; RELATIONS TO PLATE DYNAMICS, LITHOSPHERIC STRESS TRANSMISSION, AND CRUSTAL ARCHITECTURE". En GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-316407.

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Lima, Cláudio, Claudio Amaral, Anderson Moraes y Alvaro Maia. "Are The Large Wave-Lenght South American Intraplate Deformation And The Incipient Inversion Of Brazilian Continental Basins Manifestations Of Ongoing Lithospheric/ Crustal Folding?" En 6th International Congress of the Brazilian Geophysical Society. European Association of Geoscientists & Engineers, 1999. http://dx.doi.org/10.3997/2214-4609-pdb.215.sbgf305.

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Shylo, O. M., Ye O. Shylo, A. L. Tserklevych y I. M. Bubniak. "Geometric deformation of the Earth's lithosphere figure and its dynamic interpretation". En 18th International Conference on Geoinformatics - Theoretical and Applied Aspects. European Association of Geoscientists & Engineers, 2019. http://dx.doi.org/10.3997/2214-4609.201902059.

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Hinz, K., M. Block, D. Franke, S. Neben, C. Reichert y H. Roeser. "Deformation of Continental Lithosphere on the Laptev Sea Shelf, Russian Arctic". En 60th EAGE Conference and Exhibition. European Association of Geoscientists & Engineers, 1998. http://dx.doi.org/10.3997/2214-4609.201408467.

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