Littérature scientifique sur le sujet « Thrust forelimb and backlimb »
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Articles de revues sur le sujet "Thrust forelimb and backlimb":
Wu, Jonny, Ken McClay et Jose de Vera. « Growth of triangle zone fold-thrusts within the NW Borneo deep-water fold belt, offshore Sabah, southern South China Sea ». Geosphere 16, no 1 (19 décembre 2019) : 329–56. http://dx.doi.org/10.1130/ges02106.1.
Pace, Cinnamon M., Richard W. Blob et Mark W. Westneat. « Comparative kinematics of the forelimb during swimming in red-eared slider (Trachemys scripta) and spiny softshell (Apalone spinifera) turtles ». Journal of Experimental Biology 204, no 19 (1 octobre 2001) : 3261–71. http://dx.doi.org/10.1242/jeb.204.19.3261.
Watkins, Hannah, Clare E. Bond, Adam J. Cawood, Mark A. Cooper et Marian J. Warren. « Fracture distribution on the Swift Reservoir Anticline, Montana : Implications for structural and lithological controls on fracture intensity ». Geological Society, London, Special Publications 487, no 1 (16 janvier 2019) : 209–28. http://dx.doi.org/10.1144/sp487.9.
Burberry, C. M., D. L. Cannon, J. W. Cosgrove et T. Engelder. « Fracture patterns associated with the evolution of the Teton anticline, Sawtooth Range, Montana, USA ». Geological Society, London, Special Publications 487, no 1 (31 janvier 2019) : 229–61. http://dx.doi.org/10.1144/sp487.12.
Tavani, Stefano, Pablo Granado, Pau Arbués, Amerigo Corradetti et J. Anton Muñoz. « Syn-thrusting, near-surface flexural-slipping and stress deflection along folded sedimentary layers of the Sant Corneli-Bóixols anticline (Pyrenees, Spain) ». Solid Earth 8, no 2 (4 avril 2017) : 405–19. http://dx.doi.org/10.5194/se-8-405-2017.
Ward, Ayyed Hussein, Thair Mudhir Fahmi et Hasnaa Saleh Khalaf. « Variation of the Anticlines Vergency in the Iraqi Zagros Folds Belt and Its Tectonic Indications ». Tikrit Journal of Pure Science 25, no 2 (17 mars 2020) : 64. http://dx.doi.org/10.25130/j.v25i2.959.
Barrette, Paul D. « Lithostratigraphy and map-scale structure in the western Cape Smith Belt, northern Quebec : a tentative correlation between two tectonic domains ». Canadian Journal of Earth Sciences 31, no 6 (1 juin 1994) : 986–94. http://dx.doi.org/10.1139/e94-087.
Hervouet, Yves, Jose Tomass Castrillo-Delgado et Oscar Odreman. « Interaction entre un chevauchement imbrique et une zone transcurrente ; le flanc nord-ouest de Andes venezueliennes ». Bulletin de la Société Géologique de France 172, no 2 (1 mars 2001) : 159–75. http://dx.doi.org/10.2113/172.2.159.
Stapley, Paul J., Lena H. Ting, Chen Kuifu, Dirk G. Everaert et Jane M. Macpherson. « Bilateral Vestibular Loss Leads to Active Destabilization of Balance During Voluntary Head Turns in the Standing Cat ». Journal of Neurophysiology 95, no 6 (juin 2006) : 3783–97. http://dx.doi.org/10.1152/jn.00034.2006.
ZAMMIT, MARIA, BENJAMIN P. KEAR et RACHEL M. NORRIS. « Locomotory capabilities in the Early Cretaceous ichthyosaur Platypterygius australis based on osteological comparisons with extant marine mammals ». Geological Magazine 151, no 1 (1 novembre 2013) : 87–99. http://dx.doi.org/10.1017/s0016756813000782.
Thèses sur le sujet "Thrust forelimb and backlimb":
Claussmann, Barbara. « Dépôts de transport en masse le long de rides chevauchantes : nouvelles contraintes sur l'évolution tectonostratigraphique des bassins associés à la subduction (Marge Hikurangi, Nouvelle-Zélande) ». Thesis, Amiens, 2021. http://www.theses.fr/2021AMIE0034.
Along active margins, the prevalence of thrust ridges and tectonic processes (e.g., uplift, slope oversteepening) is generally called out as one of the main recurrent reasons for generating slope failures and mass wasting on subduction complexes. The resulting mass-transport deposits (MTDs) are often seen to vary strongly along a single margin and therefore, this research work proposes to investigate their nature, origin and significance in the frame of the tectonostratigraphic evolution of subduction-related sedimentary basins (e.g., trench-slope basins [TSBs]). Here, we present high-resolution outcrop-scale insights on both the characteristics and mechanisms of emplacement of the failed sediments by examining thrust-related MTDs from the Miocene cropping out in the emerged southern portion of the Hikurangi subduction margin (eastern North Island of New Zealand). Regional offshore seismic reflection data are also used to offer a broader overview and understanding of these systems through the study of the larger scale geometries and architectures. Results show the role and importance of the thrust ridges in controlling the TSB infilling. Different styles of MTDs are generated from different structural positions (forelimb and backlimb) and at specific times of thrust-ridge and TSB development. This suggests that MTDs are powerful tectonostratigraphic markers. Here, they help to unravel the evolution of two TSBs and more largely of the Hikurangi Margin at key periods. This study provides new insights on the close interplays between deformation and sedimentation, understandings of which may be key for geohazard, exploration and geodynamic predictions along active margins
Chapitres de livres sur le sujet "Thrust forelimb and backlimb":
Alonso, Juan Luis, et Antonio Teixell. « Forelimb deformation in some natural examples of fault-propagation folds ». Dans Thrust Tectonics, 175–80. Dordrecht : Springer Netherlands, 1992. http://dx.doi.org/10.1007/978-94-011-3066-0_15.
Actes de conférences sur le sujet "Thrust forelimb and backlimb":
Wightman*, Ruth H. « Near-Field Discovery and Optimisation of Complex Forelimb Structures in the Papua New Guinea Fold and Thrust Belt ». Dans International Conference and Exhibition, Melbourne, Australia 13-16 September 2015. Society of Exploration Geophysicists and American Association of Petroleum Geologists, 2015. http://dx.doi.org/10.1190/ice2015-2209771.