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Journal articles on the topic 'Lithospheric Deformation'

Author: Grafiati

Published: 4 June 2021

Last updated: 14 February 2022

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1

Dérerová, Jana, Miroslav Bielik, Mariana Pašiaková, Igor Kohút, and 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, no. 2 (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 deform

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2

Kelly, Sean, Christopher Beaumont, and Jared P. Butler. "Inherited terrane properties explain enigmatic post-collisional Himalayan-Tibetan evolution." Geology 48, no. 1 (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

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3

McNutt, Marcia. "Lithospheric stress and deformation." Reviews of Geophysics 25, no. 6 (1987): 1245. http://dx.doi.org/10.1029/rg025i006p01245.

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4

Lamarque, Gaelle, and Jordi Julià. "Lithospheric and sublithospheric deformation under the Borborema Province of northeastern Brazil from receiver function harmonic stripping." Solid Earth 10, no. 3 (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 lith

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5

Wilson, Terry J. "Processes of continental Lithospheric Deformation." Geochimica et Cosmochimica Acta 54, no. 10 (1990): 2899–900. http://dx.doi.org/10.1016/0016-7037(90)90030-o.

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6

Dehler, S. A., and 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, no. 9 (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 subcrusta

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7

Dérerová, Jana, Miroslav Bielik, Igor Kohút, and 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, no. 4 (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 o

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8

Singh, Ramesh P., Q. Li, and E. Nyland. "Lithospheric deformation beneath the Himalayan region." Physics of the Earth and Planetary Interiors 61, no. 3-4 (1990): 291–96. http://dx.doi.org/10.1016/0031-9201(90)90112-b.

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9

Wu, Fu-Yuan, Jin-Hui Yang, Yi-Gang Xu, Simon A. Wilde, and Richard J. Walker. "Destruction of the North China Craton in the Mesozoic." Annual Review of Earth and Planetary Sciences 47, no. 1 (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 (

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10

Dombrádi, Endre, Dimitrios Sokoutis, Gábor Bada, Sierd Cloetingh, and Frank Horváth. "Modelling recent deformation of the Pannonian lithosphere: Lithospheric folding and tectonic topography." Tectonophysics 484, no. 1-4 (2010): 103–18. http://dx.doi.org/10.1016/j.tecto.2009.09.014.

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11

Byrne, Paul K., Richard C. Ghail, A. M. Celâl Şengör, Peter B. James, Christian Klimczak, and Sean C. Solomon. "A globally fragmented and mobile lithosphere on Venus." Proceedings of the National Academy of Sciences 118, no. 26 (2021): e2025919118. http://dx.doi.org/10.1073/pnas.2025919118.

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Venus has been thought to possess a globally continuous lithosphere, in contrast to the mosaic of mobile tectonic plates that characterizes Earth. However, the Venus surface has been extensively deformed, and convection of the underlying mantle, possibly acting in concert with a low-strength lower crust, has been suggested as a source of some surface horizontal strains. The extent of surface mobility on Venus driven by mantle convection, however, and the style and scale of its tectonic expression have been unclear. We report a globally distributed set of crustal blocks in the Venus lowlands th

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12

Larionov, Igor, Evgeny Malkin, and Vladimir Uvarov. "Deformation-Electromagnetic Relations in Lithospheric Activity Manifestations." E3S Web of Conferences 62 (2018): 03002. http://dx.doi.org/10.1051/e3sconf/20186203002.

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It has been shown that dipole radiation of accelerated charges, described by Larmor relation, is the basis of the known mechanic-electromagnetic processes of rock deformation. Comparison of crust deformation acceleration with natural electromagnetic field parameters of ELF-VLF range showed good relation. It manifests in the maxima of occurrence frequency density of synchronous deformation-electromagnetic events on two dimensional histograms. The data of a laser strain-meter and a recorder of natural electromagnetic radiation of ELF-VLF range, recorded in a zone of increased seismic activity (K

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13

Pandey, O. P., and P. K. Agrawal. "Lithospheric Mantle Deformation beneath the Indian Cratons." Journal of Geology 107, no. 6 (1999): 683–92. http://dx.doi.org/10.1086/314373.

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14

Liu, Han-Shou. "Deformation and Instability of Underthrusting Lithospheric Plates." Geophysical Journal of the Royal Astronomical Society 35, no. 1-3 (2009): 185–93. http://dx.doi.org/10.1111/j.1365-246x.1973.tb02421.x.

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15

Dong, Xingpeng, Dinghui Yang, and Hejun Zhu. "Adjoint Tomography of the Lithospheric Structure beneath Northeastern Tibet." Seismological Research Letters 91, no. 6 (2020): 3304–12. http://dx.doi.org/10.1785/0220200135.

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Abstract Northeastern Tibet is still in the primary stage of tectonic deformation and is the key area for studying the lateral expansion of the Tibetan plateau. In particular, the existence of lower crustal flow, southward subduction of the Asian lithosphere, and northward subduction of the Indian lithosphere beneath northeastern Tibet remains controversial. To provide insights into these issues, a high-resolution 3D radially anisotropic model of the lithospheric structure of northeastern Tibet is developed based on adjoint tomography. The Tibetan plateau is characterized as a low S-wave veloc

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16

Clowes, Ron M., Don J. White, and Zoltan Hajnal. "Mantle heterogeneities and their significance: results from Lithoprobe seismic reflection and refraction – wide-angle reflection studiesThis article is one of a series of papers published in this Special Issue on the theme Lithoprobe — parameters, processes, and the evolution of a continent.Lithoprobe Contribution 1486." Canadian Journal of Earth Sciences 47, no. 4 (2010): 409–43. http://dx.doi.org/10.1139/e10-009.

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Within Lithoprobe’s 10 transects, data from more than 20 000 km of multichannel seismic (MCS) reflection profiling and 12 refraction – wide-angle reflection (R/WAR) surveys were acquired. While the main results related to crustal structure, the data also indicated substantial heterogeneity in the lithospheric mantle. Images of fossilized subduction zones from the Eocene to the Neoarchean demonstrate that current plate tectonic processes have been active for more than 2.6 Ga. The Canadian Cordillera has a thin (50–60 km) lithosphere that is likely receiving some dynamic support from the astheno

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17

Tavani, S. "Plate kinematics in the Cantabrian domain of the Pyrenean orogen." Solid Earth 3, no. 2 (2012): 265–92. http://dx.doi.org/10.5194/se-3-265-2012.

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Abstract. The Cantabrian domain represents the western portion of the Pyrenean orogen, in the area where the Iberian continental lithosphere was subducted toward the north underneath the transitional to oceanic lithosphere of the Bay of Biscay. There, the about 100 km of orogenic convergence have been mostly accommodated in the northern portion of the orogen (i.e. the retro wedge) developed in the Bay of Biscay abyssal plain, while only crustal-scale folding with limited internal deformation occurred in the Cantabrian southern wedge (pro-wedge). Integrated meso- and macrostructural analyses an

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18

Osei Tutu, Anthony, Bernhard Steinberger, Stephan V. Sobolev, Irina Rogozhina, and Anton A. Popov. "Effects of upper mantle heterogeneities on the lithospheric stress field and dynamic topography." Solid Earth 9, no. 3 (2018): 649–68. http://dx.doi.org/10.5194/se-9-649-2018.

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Abstract. The orientation and tectonic regime of the observed crustal/lithospheric stress field contribute to our knowledge of different deformation processes occurring within the Earth's crust and lithosphere. In this study, we analyze the influence of the thermal and density structure of the upper mantle on the lithospheric stress field and topography. We use a 3-D lithosphere–asthenosphere numerical model with power-law rheology, coupled to a spectral mantle flow code at 300 km depth. Our results are validated against the World Stress Map 2016 (WSM2016) and the observation-based residual to

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19

Petrescu, Laura, Graham Stuart, Gregory Houseman, and Ian Bastow. "Upper mantle deformation signatures of craton–orogen interaction in the Carpathian–Pannonian region from SKS anisotropy analysis." Geophysical Journal International 220, no. 3 (2020): 2105–18. http://dx.doi.org/10.1093/gji/ggz573.

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SUMMARY Since the Mesozoic, central and eastern European tectonics have been dominated by the closure of the Tethyan Ocean as the African and European plates collided. In the Miocene, the edge of the East European Craton and Moesian Platform were reworked in collision during the Carpathian orogeny and lithospheric extension formed the Pannonian Basin. To investigate the mantle deformation signatures associated with this complex collisional-extensional system, we carry out SKS splitting analysis at 123 broad-band seismic stations in the region. We compare our measurements with estimates of lith

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20

Fernández-Lozano, J., G. Gutiérrez-Alonso, E. Willingshofer, D. Sokoutis, G. de Vicente, and S. Cloetingh. "Shaping of intraplate mountain patterns: The Cantabrian orocline legacy in Alpine Iberia." Lithosphere 11, no. 5 (2019): 708–21. http://dx.doi.org/10.1130/l1079.1.

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Abstract The present-day topography in Iberia is related to geodynamic processes dealing with lithospheric-scale deformation. However, little attention has been paid to the role of inherited crustal- or lithospheric-scale structures involved in the recent observed large-scale topographic patterns. Whereas the analysis of brittle structures focuses on the evolution of Mesozoic sedimentary basins and their subsequent response to tectonic inversion, their contribution to mountain building has been underestimated. Large numbers of structures, from ductile to brittle, which affected the whole litho

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21

Jaquet, Yoann, Thibault Duretz, and Stefan M. Schmalholz. "Dramatic effect of elasticity on thermal softening and strain localization during lithospheric shortening." Geophysical Journal International 204, no. 2 (2015): 780–84. http://dx.doi.org/10.1093/gji/ggv464.

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Abstract We present two-dimensional numerical simulations for shortening a viscoelastoplastic lithosphere to quantify the impact of elasticity on strain localization due to thermal softening. The model conserves energy and mechanical work is converted into heat or stored as elastic strain energy. For a shear modulus G = 1010 Pa, a prominent lithospheric shear zone forms and elastic energy release increases the localization intensity (strain rate amplification). For G = 5 × 1010 Pa shear zones still form but deformation is less localized. For G = 1012 Pa, the lithosphere behaves effectively vis

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22

MacDougall, Malcolm D. J., Alexander Braun, and Georgia Fotopoulos. "Evidence of Lithospheric Boudinage in the Grand Banks of Newfoundland from Geophysical Observations." Geosciences 11, no. 2 (2021): 55. http://dx.doi.org/10.3390/geosciences11020055.

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The evolution of the passive margin off the coast of Eastern Canada has been characterized by a series of rifting episodes which caused widespread extension of the lithosphere and associated structural anomalies, some with the potential to be classified as a result of lithospheric boudinage. Crustal thinning of competent layers is often apparent in seismic sections, and deeper Moho undulations may appear as repeating elongated anomalies in gravity and magnetic surveys. By comparing the similar evolutions of the Grand Banks and the Norwegian Lofoten-Vesterålen passive margins, it is reasonable

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23

Zaporozan, Taras, Andrew W. Frederiksen, Alexey Bryksin, and Fiona Darbyshire. "Surface-wave images of western Canada: lithospheric variations across the Cordillera–craton boundary." Canadian Journal of Earth Sciences 55, no. 8 (2018): 887–96. http://dx.doi.org/10.1139/cjes-2017-0277.

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Two-station surface-wave analysis was used to measure Rayleigh-wave phase velocities between 105 station pairs in western Canada, straddling the boundary between the tectonically active Cordillera and the adjacent stable craton. Major variations in phase velocity are seen across the boundary at periods from 15 to 200 s, periods primarily sensitive to upper mantle structure. Tomographic inversion of these phase velocities was used to generate phase velocity maps at these periods, indicating a sharp contrast between low-velocity Cordilleran upper mantle and high-velocity cratonic lithosphere. De

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24

Jing, Z., F. Bihong, S. Pilong, and G. Qiang. "INVESTIGATION OF LITHOSPHERIC STRUCTURE IN MONGOLIA: INSIGHTS FROM INSAR OBSERVATIONS AND MODELLING." ISPRS - International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences XLII-2/W7 (September 13, 2017): 609–16. http://dx.doi.org/10.5194/isprs-archives-xlii-2-w7-609-2017.

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The western Mongolia is a seismically active intracontinental region, with ongoing tectonic deformation and widespread seismicity related to the far-field effects of India-Eurasia collision. During the 20th century, four earthquakes with the magnitude larger than 8 occurred in the western Mongolia and its surrounding regions, providing a unique opportunity to study the geodynamics of intracontinental tectonic deformations. The 1957 magnitude 8.3 Gobi-Altai earthquake is one of the largest seismic events. The deformation pattern of rupture zone associated with this earthquake is complex, involv

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25

Keep, Myra. "Models of lithospheric-scale deformation during plate collision: effects of indentor shape and lithospheric thickness." Tectonophysics 326, no. 3-4 (2000): 203–16. http://dx.doi.org/10.1016/s0040-1951(00)00123-2.

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26

Larionov, Igor, Yuriy Marapulets, and Mikhail Mishchenko. "Results of atmospheric-lithospheric observations of acoustic radiation in Kamchatka." E3S Web of Conferences 127 (2019): 02023. http://dx.doi.org/10.1051/e3sconf/201912702023.

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Simultaneous atomspheric-lithospheric acoustic observations have been carried out during autumn-spring periods of 2017-2019 in Kamchatka at “Karymshina” observation site located in the zone of different-rank tectonic faults. A laser strainmeter-interferometer, a seismoacoustic receiver and a microbarometer were installed to realize the observations. It was detected that during deformation disturbances, geoacoustic signals are generated in rocks with relative deformations of 10-5 – 10-7 at the place of recording. These signals pass the Earth-atmosphere boundary and are recorded in the air by th

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27

Singh, Harshpal, and Rezene Mahatsente. "Lithospheric Structure of Eastern Tibetan Plateau from Terrestrial and Satellite Gravity Data Modeling: Implication for Asthenospheric Underplating." Lithosphere 2020, no. 1 (2020): 1–19. http://dx.doi.org/10.2113/2020/8897964.

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Abstract The lithosphere of the eastern Tibetan plateau is underlain by a low-velocity zone at shallow depths which is interpreted as asthenospheric material in the upper-most mantle in various seismic tomography studies. The driving mechanism for the presence of asthenospheric material in the upper-most mantle is not well understood, and the spatial extent of the asthenospheric material is not well delineated. We use 2.5D gravity models to assess what drove the asthenospheric flow upwards in the past and determine the lateral extent of the asthenospheric material in the upper-most mantle. The

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28

Sandiford, Mike, John Foden, Shaohua Zhou, and Simon Turner. "Granite genesis and the mechanics of convergent orogenic belts with application to the southern Adelaide Fold Belt." Earth and Environmental Science Transactions of the Royal Society of Edinburgh 83, no. 1-2 (1992): 83–93. http://dx.doi.org/10.1017/s026359330000777x.

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ABSTRACTTwo models for the heating responsible for granite generation during convergent deformation may be distinguished on the basis of the length- and time-scales associated with the thermal perturbation, namely: (1) long-lived, lithospheric-scale heating as a conductive response to the deformation, and (2) transient, localised heating as a response to advective heat sources such as mantle-derived melts. The strong temperature dependence of lithospheric rheology implies that the heat advected within rising granites may affect the distribution and rates of deformation within the developing or

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29

Singh, Sarva Jit, and Sunita Rani. "Lithospheric Deformation Associated with Two-Dimensional Strike-Slip Faulting." Journal of Physics of the Earth 42, no. 3 (1994): 197–220. http://dx.doi.org/10.4294/jpe1952.42.197.

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30

Dayem, Katherine E., Peter Molnar, Marin K. Clark, and Gregory A. Houseman. "Far-field lithospheric deformation in Tibet during continental collision." Tectonics 28, no. 6 (2009): n/a. http://dx.doi.org/10.1029/2008tc002344.

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31

Samae, Vahid, Patrick Cordier, Sylvie Demouchy, et al. "Stress-induced amorphization triggers deformation in the lithospheric mantle." Nature 591, no. 7848 (2021): 82–86. http://dx.doi.org/10.1038/s41586-021-03238-3.

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32

White, Joseph Clancy, and Christopher K. Mawer. "Deep-crustal deformation textures along megathrusts from Newfoundland and Ontario: implications for microstructural preservation, strain rates, and strength of the lithosphere." Canadian Journal of Earth Sciences 29, no. 2 (1992): 328–37. http://dx.doi.org/10.1139/e92-029.

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Lithospheric-scale thrusts from the west Newfoundland ophiolite belt (White Hills Peridotite shear zone) and the south-western Grenville Province (Parry Sound shear zone) involve rocks of lower crustal and (or) upper mantle origin that exhibit intense crystal-plastic deformation of plagioclase, K-feldspar, orthopyroxene, and clinopyroxene, minerals that are commonly viewed as representative of low-ductility phases. The occurrence of this extreme deformation in shear zones that exhibit similar lower crustal syntectonic P–T conditions suggests a phenomenological link between the megathrust envir

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33

Sadeghi-Bagherabadi, Amir, Farhad Sobouti, Abdolreza Ghods, et al. "Upper mantle anisotropy and deformation beneath the major thrust-and-fold belts of Zagros and Alborz and the Iranian Plateau." Geophysical Journal International 214, no. 3 (2018): 1913–18. http://dx.doi.org/10.1093/gji/ggy233.

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SUMMARY We present new SKS splitting measurements obtained from a temporary seismic broad-band network in western Iran across the Arabia–Eurasia collision zone. The average delay time over the entire network was found to be 1.27 ± 0.27 s. In the Zagros where the lithosphere attains its greatest thickness, the fast-axes are predominantly subparallel to the trend of the mountain ranges, suggesting a lithospheric origin of the anisotropy caused by transpressional deformation. In contrast in the Alborz, the fast-axes become subparallel to the absolute plate motion vectors and we propose that aniso

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34

Mussi, Alexandre, Maula Nafi, Sylvie Demouchy, and Patrick Cordier. "On the deformation mechanism of olivine single crystals at lithospheric temperatures: an electron tomography study." European Journal of Mineralogy 27, no. 6 (2015): 707–15. http://dx.doi.org/10.1127/ejm/2015/0027-2481.

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35

Parizot, Oriane, Yves Missenard, Pierre Vergely, et al. "Tectonic Record of Deformation in Intraplate Domains: Case Study of Far-Field Deformation in the Grands Causses Area, France." Geofluids 2020 (July 15, 2020): 1–19. http://dx.doi.org/10.1155/2020/7598137.

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Although tectonic plates are usually considered as rigid blocks, intraplate deformation such as lithospheric buckling or diffuse brittle deformation has been recognized for a long time. However, the origin of these deformations remains puzzling. Indeed, whereas the chronology of deformation at plate boundaries can be constrained by numerous methods (syntectonic sedimentary record, thermochronology, etc.), dating of brittle structures (faults, veins, and joints) in the far-field domains remains challenging, preventing a global interpretation of the system as a whole. In this contribution, we ha

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36

Granet, Michel, Sebastien Judenherc, and Annie Souriau. "Des images du systeme lithosphere-asthenosphere sous la France et leurs implications geodynamiques; l'apport de la tomographie telesismique et de l'anisotropie sismique." Bulletin de la Société Géologique de France 171, no. 2 (2000): 149–67. http://dx.doi.org/10.2113/171.2.149.

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Abstract From seismic tomography and seismic anisotropy, images of the lithosphere-asthenosphere system beneath France for some remarkable tectonic areas have been computed : a continental rift system (the Upper Rhinegraben), an Hercynian structure reactivated by Neogene volcanism (Massif central), a region of a recent continental collision (Pyrenees) and finally a region of an ancient orogeny (Armorican Massif). These images have a horizontal spatial resolution of the order of 10 km and show not only the geometry of the deep geological structures but will also illustrate the link between surf

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37

Telyatnikov, Ilya. "Modeling of deformation processes in lithospheric structures during their static interaction." Thermal Science 23, Suppl. 2 (2019): 591–97. http://dx.doi.org/10.2298/tsci19s2591t.

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We consider a model of lithospheric structures contacting along rectilinear geological faults as a system of composite plates on an elastic foundation. A simplification of the block element method for different-sized blocks is proposed. We also describe an approach that is a modification of the block element method using the method of eigenfunctions. The method is considered on the example of a static interaction problem of extended plates on the surface of an elastic layer for a given surface load. As a result we obtain the representations of solutions describing the surface displacements. Th

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38

Jiménez-Munt, Ivone, Daniel Garcia-Castellanos, and Manel Fernandez. "Thin-sheet modelling of lithospheric deformation and surface mass transport." Tectonophysics 407, no. 3-4 (2005): 239–55. http://dx.doi.org/10.1016/j.tecto.2005.08.015.

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39

Frets, Erwin, Andréa Tommasi, Carlos J. Garrido, José Alberto Padrón-Navarta, Isma Amri, and Kamal Targuisti. "Deformation processes and rheology of pyroxenites under lithospheric mantle conditions." Journal of Structural Geology 39 (June 2012): 138–57. http://dx.doi.org/10.1016/j.jsg.2012.02.019.

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40

YI, Gui-Xi, Hua-Jian YAO, Jie-Shou ZHU, and Robert D. van der Hilst. "Lithospheric Deformation of Continental China from Rayleigh Wave Azimuthal Anisotropy." Chinese Journal of Geophysics 53, no. 1 (2010): 121–35. http://dx.doi.org/10.1002/cjg2.1479.

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41

Deng, Yangfan, and Will Levandowski. "Lithospheric Alteration, Intraplate Crustal Deformation, and Topography in Eastern China." Tectonics 37, no. 11 (2018): 4120–34. http://dx.doi.org/10.1029/2018tc005079.

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42

Goodwillie, Andrew M., and Barry Parsons. "Placing bounds on lithospheric deformation in the central Pacific Ocean." Earth and Planetary Science Letters 111, no. 1 (1992): 123–39. http://dx.doi.org/10.1016/0012-821x(92)90174-t.

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Gordon, Richard G. "Lithospheric Deformation in the equatorial Indian Ocean: Timing and Tibet." Geology 37, no. 3 (2009): 287–88. http://dx.doi.org/10.1130/focus032009.1.

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Bendick, R., and L. Flesch. "Reconciling lithospheric deformation and lower crustal flow beneath central Tibet." Geology 35, no. 10 (2007): 895. http://dx.doi.org/10.1130/g23714a.1.

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Ernst, W. G., Norman H. Sleep, and Tatsuki Tsujimori. "Plate-tectonic evolution of the Earth: bottom-up and top-down mantle circulation." Canadian Journal of Earth Sciences 53, no. 11 (2016): 1103–20. http://dx.doi.org/10.1139/cjes-2015-0126.

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Intense devolatilization and chemical-density differentiation attended accretion of planetesimals on the primordial Earth. These processes gradually abated after cooling and solidification of an early magma ocean. By 4.3 or 4.2 Ga, water oceans were present, so surface temperatures had fallen far below low-pressure solidi of dry peridotite, basalt, and granite, ∼1300, ∼1120, and ∼950 °C, respectively. At less than half their T solidi, rocky materials existed as thin lithospheric slabs in the near-surface Hadean Earth. Stagnant-lid convection may have occurred initially but was at least episodi

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Guillot, Stéphane, and Anne Replumaz. "Importance of continental subductions for the growth of the Tibetan plateau." Bulletin de la Société Géologique de France 184, no. 3 (2013): 199–223. http://dx.doi.org/10.2113/gssgfbull.184.3.199.

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Abstract How and when the Tibetan plateau developed has long been a puzzling question with implications for the current understanding of the behaviour of the continental lithosphere in convergent zones. We present and discuss recent data acquired in geology and geophysics and through igneous and metamorphic petrology and palaeo-altitude estimates. It appears from this research that Tibet initially resulted from the accretion of the Gondwana continental blocks to the southern Asian margin during the Palaeozoic and Mesozoic eras. These successive accretions have potentially favoured the creation

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Liu, Junlai, Mo Ji, Jinlong Ni, et al. "Inhomogeneous thinning of a cratonic lithospheric keel by tectonic extension: The Early Cretaceous Jiaodong Peninsula–Liaodong Peninsula extensional provinces, eastern North China craton." GSA Bulletin 133, no. 1-2 (2020): 159–76. http://dx.doi.org/10.1130/b35470.1.

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Abstract The mechanisms of lithospheric thinning and craton destruction have been hotly debated in the last decades. The Early Cretaceous Jiaodong and Liaodong extensional provinces (JEP and LEP, respectively) of the eastern North China craton are typical areas where the cratonic Archean lithosphere has been intensely extended and thinned. Various extensional structures, e.g., metamorphic core complexes (MCCs), low-angle detachment faults, and extensional basins, characterize the Early Cretaceous crustal deformation of the two provinces. However, profound differences exist in structural develo

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Michibayashi, Katsuyoshi, Makoto Suzuki, and Naoaki Komori. "Progressive deformation partitioning and recrystallization of olivine in the lithospheric mantle." Tectonophysics 587 (March 2013): 79–88. http://dx.doi.org/10.1016/j.tecto.2012.07.008.

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Knoll, Mickaël, Andréa Tommasi, Roland E. Logé, and Javier W. Signorelli. "A multiscale approach to model the anisotropic deformation of lithospheric plates." Geochemistry, Geophysics, Geosystems 10, no. 8 (2009): n/a. http://dx.doi.org/10.1029/2009gc002423.

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Sabadini, R., and L. L. A. Vermeersen. "Influence of lithospheric and mantle stratification on global post-seismic deformation." Geophysical Research Letters 24, no. 16 (1997): 2075–78. http://dx.doi.org/10.1029/97gl01979.

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