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Relevant bibliographies by topics / Thrust forelimb and backlimb

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Journal articles
Dissertations / Theses
Book chapters
Conference papers

Academic literature on the topic 'Thrust forelimb and backlimb'

Author: Grafiati

Published: 17 November 2022

Last updated: 31 December 2022

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Journal articles on the topic "Thrust forelimb and backlimb"

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Wu, Jonny, Ken McClay, and 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 (2019): 329–56. http://dx.doi.org/10.1130/ges02106.1.

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Abstract The NW Borneo deep-water fold-and-thrust belt, offshore Sabah, southern South China Sea, contains a structurally complex region of three to four seafloor ridges outboard of the shelf-slope break. Previous studies have suggested the seafloor ridges formed either above shale diapirs produced by mass movement of overpressured shales (i.e., mobile shale) or above an imbricate fold-and-thrust array. Here, we performed tectonostratigraphic analyses on a petroleum industry three-dimensional (3-D) seismic volume that imaged the full growth stratal record. We show fold growth history, deformat

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Pace, Cinnamon M., Richard W. Blob, and 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 (2001): 3261–71. http://dx.doi.org/10.1242/jeb.204.19.3261.

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SUMMARYSoftshell turtles (Family Trionychidae) possess extensive webbing between the digits of the manus, suggesting that the forelimb may serve as an effective thrust generator during aquatic locomotion. However, the hindlimb has previously been viewed as the dominant propulsive organ in swimming freshwater turtles. To evaluate the potential role of the forelimb in thrust production during swimming in freshwater turtles, we compared the forelimb morphology and three-dimensional forelimb kinematics of a highly aquatic trionychid turtle, the spiny softshell Apalone spinifera, and a morphologica

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Watkins, Hannah, Clare E. Bond, Adam J. Cawood, Mark A. Cooper, and 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 (2019): 209–28. http://dx.doi.org/10.1144/sp487.9.

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AbstractWhere primary porosity and permeability of a rock are unfavourable for hydrocarbon production, fractures can improve reservoir potential by enhancing permeability. Higher fracture intensity may create a better-connected fracture network, improving fractured-reservoir quality. Investigations into the controls on fracture intensity commonly conclude that either structural or lithological factors have the greatest influence on fracture abundance. We use the Swift Reservoir Anticline in northwestern Montana to investigate how fracture intensity varies throughout the structure and determine

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Burberry, C. M., D. L. Cannon, J. W. Cosgrove, and T. Engelder. "Fracture patterns associated with the evolution of the Teton anticline, Sawtooth Range, Montana, USA." Geological Society, London, Special Publications 487, no. 1 (2019): 229–61. http://dx.doi.org/10.1144/sp487.12.

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AbstractThe Teton anticline and adjacent structures, in the Sawtooth Range, Montana, USA, are fractured in such a way that may be taken as a model for fractures propagating during buckle folding. However, advances in understanding both the process of folding in forelands and the evolution of fracture patterns found within these folds suggest that it is time to reinterpret the nexus between fracturing and folding within these classic structures. With the benefit of seismic lines, the Teton anticline is best described as a fault-propagation fold. Joint propagation initiated with the formation of

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Tavani, Stefano, Pablo Granado, Pau Arbués, Amerigo Corradetti, and 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 (2017): 405–19. http://dx.doi.org/10.5194/se-8-405-2017.

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Abstract. In the Spanish Pyrenees, the Sant Corneli-Bóixols thrust-related anticline displays an outstandingly preserved growth strata sequence. These strata lie on top of a major unconformity exposed at the anticline's forelimb that divides and decouples a lower pre-folding unit from an upper syn-folding one. The former consists of steeply dipping to overturned strata with widespread bedding-parallel slip indicative of folding by flexural slip, whereas the syn-folding strata above define a 200 m amplitude fold. In the inner and outer sectors of the forelimb, both pre- and syn-folding strata a

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Ward, Ayyed Hussein, Thair Mudhir Fahmi, and 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 (2020): 64. http://dx.doi.org/10.25130/j.v25i2.959.

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Folds of northern Iraq are considered integral part for the Western Zagros Fold – Thrust Belt. The growth of these folds was due to inversion displacement on inherited listric faults. This research deal with the relationship between the folds vergency and the faults that propagated folds, where that the dip of the back limb (gentle limb) for the fold is parallel to the thrust fault surface that propagated the fold, and the vergency of the fold determined by the forelimb (steep limb) situation. As a results, the folds of the high folded zone and of the western part of the low folded zone showed

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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 (1994): 986–94. http://dx.doi.org/10.1139/e94-087.

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Field investigations in the western part of the Cape Smith Belt outlined four fault-bounded lithological assemblages tectonically overlying foliated to gneissic granitoids of the Archean Superior Province. These assemblages comprise sequences of pillowed volcanic rocks, sedimentary rocks of pelitic and psammitic composition, and volcaniclastic rocks. They are juxtaposed along the Lanyan Lake Fault against a structurally thickened sequence of mafic to ultramafic pillowed volcanic suite belonging to the Chukotat Group. The occurrence of volcaniclastic horizons in the uppermost levels of the Chuk

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Hervouet, Yves, Jose Tomass Castrillo-Delgado, and 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 (2001): 159–75. http://dx.doi.org/10.2113/172.2.159.

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Abstract Geological framework; Geological setting: The Venezuela Andes or Merida Andes (fig. 1) extend from the Colombian border in the SW to Barquisimeto in the NE, and constitute a basement uplift exceeding 5,000 m near Merida (Pico Bolivar). This young chain is bordered to the W by the Maracaibo foredeep basin, and to the E by the Barinas-Apure foreland basin. The Bocono fault divides the Andean Belt in two parts along a NE-SW direction. This shows that the uplift of the Andes is contemporaneous with an oblique translation. In the study area, located on the northwestern flank near Maracaibo

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Stapley, Paul J., Lena H. Ting, Chen Kuifu, Dirk G. Everaert, and 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 (2006): 3783–97. http://dx.doi.org/10.1152/jn.00034.2006.

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The purpose of this study was to determine the source of postural instability in labyrinthectomized cats during lateral head turns. Cats were trained to maintain the head in a forward orientation and then perform a rapid, large-amplitude head turn to left or right in yaw, while standing freely on a force platform. Head turns were biomechanically complex with the primary movement in the yaw plane accompanied by an ipsilateral ear-down roll and nose-down pitch. Cats used a strategy of pushing off by activating extensors of the contralateral forelimb while using all four limbs to produce a rotati

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ZAMMIT, MARIA, BENJAMIN P. KEAR, and 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 (2013): 87–99. http://dx.doi.org/10.1017/s0016756813000782.

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AbstractReconstructing the swimming capabilities of extinct marine tetrapods is critical for unravelling broader questions about their palaeobiology, palaeoecology and palaeobiogeography. Ichthyosaurs have long been the subject of such investigations because, alongside cetaceans, they are one of the few tetrapod lineages to achieve a highly specialized fish-like body plan. The dominant locomotory mode for the majority of derived, post-Triassic ichthyosaurs is hypothesized to have been caudal fin-driven propulsion. Limb-based swimming has however been suggested for some highly autapomorphic for

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Dissertations / Theses on the topic "Thrust forelimb and backlimb"

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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.

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Le long des marges actives, la croissance de rides anticlinales chevauchantes et les processus tectoniques associés sont souvent cités comme étant l'une des causes principales entrainant des déstabilisations de pente et du transport en masse de sédiments au dos des prismes de subduction. Les dépôts associés (MTDs) sont très variés, ne serait-ce que le long d'une même marge, et leur nature, origine et expression peuvent témoigner de l'évolution tectonostratigraphique des bassins sédimentaires liés à la subduction (e.g., bassins perchés). Ce travail présente une analyse haute résolution des cara

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Book chapters on the topic "Thrust forelimb and backlimb"

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Alonso, Juan Luis, and Antonio Teixell. "Forelimb deformation in some natural examples of fault-propagation folds." In Thrust Tectonics. Springer Netherlands, 1992. http://dx.doi.org/10.1007/978-94-011-3066-0_15.

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Conference papers on the topic "Thrust forelimb and backlimb"

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Wightman*, Ruth H. "Near-Field Discovery and Optimisation of Complex Forelimb Structures in the Papua New Guinea Fold and Thrust Belt." In 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.

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