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Готові списки джерел за темами / Trench-Slope basins

Добірка наукової літератури з теми "Trench-Slope basins"

Автор: Grafiati

Опубліковано: 17 листопада 2022

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Статті в журналах з теми "Trench-Slope basins":

1

Okada, Hakuyu. "Anatomy of trench-slope basins: Examples from the Nankai Trough." Palaeogeography, Palaeoclimatology, Palaeoecology 71, no. 1-2 (June 1989): 3–13. http://dx.doi.org/10.1016/0031-0182(89)90026-6.

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2

Narayanaswamy, Bhavani E., and James A. Blake. "A new species of Orbiniella (Polychaeta: Orbiniidae) from deep basins of Antarctica." Journal of the Marine Biological Association of the United Kingdom 85, no. 4 (June 27, 2005): 843–46. http://dx.doi.org/10.1017/s0025315405011793.

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During the 2002 Antarctic Deep-sea Biodiversity (ANDEEP) programme to the Drake Passage, Weddell Sea Basin and South Sandwich Slope and trench, a new deep-water species of orbiniid polychaete was collected: Orbiniella andeepia sp. nov. Orbiniella andeepia appears to be most closely related to O. marionensis but differs in capillary setal structure, the type and number of acicular spines found in each podial lobe. Orbiniella andeepia is only the third deep-water species of Orbiniella to be discovered. It exhibits both a wide depth- and geographic-range within the Antarctic slope and abyssal sediments.

3

Fralick, Philip, Jinhua Wu, and Howard R. Williams. "Trench and slope basin deposits in an Archean metasedimentary belt, Superior Province, Canadian Shield." Canadian Journal of Earth Sciences 29, no. 12 (December 1, 1992): 2551–57. http://dx.doi.org/10.1139/e92-202.

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The identification of a late Archean arc–trench assemblage in northwestern Ontario provides the opportunity to compare depositional systems developed in a Precambrian convergent setting with Cenozoic examples. Two types of sedimentary associations exist in the accretionary complex. Medium- to thick-bedded Bouma A, AB, and ABC felsic turbidites dominate the belt. These are primarily organized into unstructured sequences and reflect deposition in a ramp-like environment with multiple feed points supplying sediment from a forearc basin. Mafic turbidites with possible shallow water reworked intervals form isolated pods within the metasedimentary belt. Erosion of upthrust blocks of sedimentary strata containing ultramafic masses supplied this sediment to elevated slope basins. These types of depositional systems are similar in many respects to those developed in Cenozoic and Holocene arc–trench settings.

4

De Rosa, R., G. G. Zuffa, A. Taira, and J. K. Leggett. "Petrography of trench sands from the Nankai Trough, southwest Japan: implications for long-distance turbidite transportation." Geological Magazine 123, no. 5 (September 1986): 477–86. http://dx.doi.org/10.1017/s0016756800035068.

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AbstractTwenty-three samples of Quaternary sands from Deep Sea Drilling Project (DSDP) Leg 87 Sites 582 (trench axis) and 583 (lowermost terrace of uplifted trench sediments in the accretionary prism) off Shikoku show a 70–80% volcanic component in the terrigenous grain population. This component comprises 30–40% neovolcanic grains, among which basic and intermediate types are present in roughly equal proportions, and 60–70% palaeovolcanic grains, which are predominantly of acidic composition. No volcanic terrane occurs, in the hinterland of the Shikoku portion of the Nankai Trough, and the first such rocks to the east (up the very slight depositional slope of the Nankai Trough axis) are not encountered for more than 500 km. These, occupying the Izu Peninsula and the majority of the Tokai drainage basin to the north, are Neogene and Recent volcanics which are of comparable variability to the volcanic grains in the sands off Shikoku.The minor component of sedimentary, metamorphic and plutonic grains in the Leg 87 sand samples can be matched with the basinal clastic ophiolitic Shimanto and Chichibu terranes and the high-pressure metamorphic Sambagawa terrane which border the Nankai Trough fore-arc along southwest Japan. This detritus also most likely derives from the Tokai drainage basin, where the easternmost outcrops of the above-mentioned terranes occur, because most sediments deriving from Shikoku and the Kii regions are ponded in terraced fore-arc basins or in basins on the lower slope. Only three major submarine canyons debouch into the floor of the Nankai Trough. The easternmost of these, the Suruga Trough, taps the volcanic Izu/Tokai hinterland, and is therefore the conduit for most sand fed to the trench off Shikoku.

5

Patton, J. R., C. Goldfinger, A. E. Morey, C. Romsos, B. Black, and Y. Djadjadihardja. "Seismoturbidite record as preserved at core sites at the Cascadia and Sumatra–Andaman subduction zones." Natural Hazards and Earth System Sciences 13, no. 4 (April 4, 2013): 833–67. http://dx.doi.org/10.5194/nhess-13-833-2013.

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Abstract. Turbidite deposition along slope and trench settings is evaluated for the Cascadia and Sumatra–Andaman subduction zones. Source proximity, basin effects, turbidity current flow path, temporal and spatial earthquake rupture, hydrodynamics, and topography all likely play roles in the deposition of the turbidites as evidenced by the vertical structure of the final deposits. Channel systems tend to promote low-frequency components of the content of the current over longer distances, while more proximal slope basins and base-of-slope apron fan settings result in a turbidite structure that is likely influenced by local physiography and other factors. Cascadia's margin is dominated by glacial cycle constructed pathways which promote turbidity current flows for large distances. Sumatra margin pathways do not inherit these antecedent sedimentary systems, so turbidity currents are more localized.

6

Stevens, Scott H., and Gregory F. Moore. "Deformational and sedimentary processes in trench slope basins of the western Sunda Arc, Indonesia." Marine Geology 69, no. 1-2 (December 1985): 93–112. http://dx.doi.org/10.1016/0025-3227(85)90135-5.

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7

PAL, TAPAN, PARTHA PRATIM CHAKRABORTY, TANAY DUTTA GUPTA, and CHANAM DEBOJIT SINGH. "Geodynamic evolution of the outer-arc–forearc belt in the Andaman Islands, the central part of the Burma–Java subduction complex." Geological Magazine 140, no. 3 (May 2003): 289–307. http://dx.doi.org/10.1017/s0016756803007805.

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The Andaman Islands, the central part of Burma–Java subduction complex, expose tectonostratigraphic units of an accretionary prism in an outer-arc setting and turbidites of a forearc setting. A number of N–S-trending dismembered ophiolite slices of Cretaceous age, occurring at different structural levels with Eocene trench-slope sediments, were uplifted and emplaced by a series of E–dipping thrusts. Subsequently, N–S normal and E–W strike-slip faults resulted in the development of a forearc basin with deposition of Oligocene and Mio-Pliocene sediments. Metapelites and metabasics of greenschist to amphibolite grade occur in a melange zone of ophiolites. The Eocene Mithakhari Group represents pelagic trench sediments and coarser clastics derived from ophiolites. Evidence of frequent facies changes, predominance of mass flow deposits, syn-sedimentary basinal disturbance and wide palaeogeographic variation indicate deposition of Eocene sediments in isolated basins of an immature trench-slope setting. Deposition of the Oligocene Andaman Flysch Group in a forearc setting is indicated by the large-scale persistence of beds, lack of small-scale lithological variation, bimodal provenance, less deformation, a well-defined submarine fan sequence and development predominantly on the eastern part of the outer arc. The Mio-Pliocene Archipelago Group includes alternations of siliciclastic turbidites and subaqueous pyroclastic flow deposits in the lower part and carbonate turbidites in the upper part, suggesting its deposition in the shallower forearc compared to the siliciclastic Oligocene sediments.

8

Malie, Pierre, Julien Bailleul, Frank Chanier, Renaud Toullec, Geoffroy Mahieux, Vincent Caron, Brad Field, Rafael Ferreiro Mählmann, and Sébastien Potel. "Spatial distribution and tectonic framework of fossil tubular concretions as onshore analogues of cold seep plumbing systems, North Island of New Zealand." Bulletin de la Société géologique de France 188, no. 4 (2017): 25. http://dx.doi.org/10.1051/bsgf/2017192.

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Analysis of offshore seismic lines suggests that a strong relationship exists between tectonic structures and fluid migration in accretionary prisms. However, only few field analogues of plumbing systems and their tectonic frameworks have been investigated in detail until now. The uplifted accretionary prism of the Hikurangi Margin (North Island, New Zealand) exposes early to late Miocene mudrocks in coastal cliffs of Cape Turnagain and in the Akitio syncline, south-east of the Pongaroa city. These outcrops display tubular carbonate concretions corresponding to complex subsurface plumbing networks of paleo-seeps within Miocene trench slope basins. We present here, new results on the spatial distribution of these tubular carbonate concretions, with particular attention to their relation to tectonic structures. In the Pongaroa area, tubular carbonate concretions in lower Miocene mudrocks occur along a N-S trend, while in middle Miocene strata they occur along a NNE-SSW direction. The N-S trend parallels a major fault zone (i.e. the Breakdown fault zone), which separates two wide synclines, the Waihoki and the Akitio synclines. During the Early-Middle Miocene, the Breakdown fault zone controlled the evolution of the Akitio trench slope basin constituting its western edge. The NNE-SSW strike parallels the axis of the Akitio syncline and is also parallel to the present-day subduction front. Our results therefore show that tubular concretions are parallel to post-Middle Miocene second order folding and thrusting in the northeastern limb of the Akitio syncline. In the Cape Turnagain area, tubular concretions occur in the western limb of the Cape Turnagain syncline, in the footwall of the major seaward-verging Cape Turnagain fault. This suggests that fluid migrations may occur not only in the crests of anticlines, as observed offshore for present-day plumbing system of cold seeps, but also in the footwalls of thrust faults. All these observations show that the spatial distribution of tubular concretions is controlled by regional tectonic structures with paleo-fluid migrations related to major deformation episodes of the accretionary prism. Thus, we distinguish three episodes events that likely triggered fluid migration leading to the formation of the tubular concretions: (1) In the Early Miocene, shortly after the onset of development of the Akitio trench slope basin, on its inner (western) edge; (2) During the late Middle Miocene, during an extensional deformation episode on the western limb of the Akitio trench slope basin; (3) At the end of the Late Miocene, during a second major shortening period at the footwall of major thrust fault, such as in the Cape Turnagain area.

9

Bailleul, Julien, Frank Chanier, Jacky Ferrière, Cécile Robin, Andrew Nicol, Geoffroy Mahieux, Christian Gorini, and Vincent Caron. "Neogene evolution of lower trench-slope basins and wedge development in the central Hikurangi subduction margin, New Zealand." Tectonophysics 591 (April 2013): 152–74. http://dx.doi.org/10.1016/j.tecto.2013.01.003.

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10

Gambi, Cristina, Nikolaos Lampadariou, and Roberto Danovaro. "Latitudinal, longitudinal and bathymetric patterns of abundance, biomass of metazoan meiofauna: importance of the rare taxa and anomalies in the deep Mediterranean Sea." Advances in Oceanography and Limnology 1, no. 1 (June 1, 2010): 167. http://dx.doi.org/10.4081/aiol.2010.5299.

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Quantitative information on the spatial distribution of meiofaunal abundance, biomass and biodiversity (as richness of higher taxa) is summarised from 476 sites of the deep- Mediterranean Sea, at depths ranging from ca. 200 to 4617 m. Meiofaunal abundance (46531 and 30624 ind 10 cm2 at 200–1000 and 1000–2000m depth intervals) and biomass (12516 and 11920 mgC 10 cm2 at 200–1000 and 1000–2000m depth intervals) in the bathyal sediments of the Mediterranean Sea are similar to those reported in oceans worldwide but at much higher depths (abyssal or hadal). Meiofaunal abundance, biomass and richness of taxa displayed a common decreasing bathymetric pattern, but showed a steeper negative slope than in other oceanic regions. Latitudinal and longitudinal gradients revealed idiosyncratic patterns when different basins (Western, Central and Eastern) and habitats (open slope, canyon, deep basin and trench) were considered. The results of the non parametric multivariate multiple regression analyses revealed that, conversely to what expected, depth is not the key factor in explaining the variance of meiofaunal assemblages living down to 2000m depth. The quality and quantity of food sources explained a larger fraction of the variance of meiofaunal variables (47, 25 and 33% for abundance, biomass and diversity, respectively) and the importance of food sources increased with increasing depth. However, most of the variance remains unexplained suggesting that other factors (such as episodic events, deep currents, other unexplored yet environmental characteristics) can act a key role in driving the observed meiofaunal spatial patterns. The analysis of rare taxa (on a data set of 183 samples), suggested that differences in the meiofaunal community were evident when dominating taxa (nematodes, copepods and polychaetes) were excluded. We report the presence of rare taxa exclusively present in open slope (amphipods) and canyon (cnidarians and decapod larvae) systems, whereas others are exclusively found in one of the two basins (e.g. gastrotrichs in the Western basin and amphipods and gastropods in the Eastern basin). The apparent preference of some rare taxa for a specific habitat or basin could have important implications for the identification of the hot spots of benthic diversity, for identifying the connectivity among systems and for an appropriate management of deep-sea habitats in the Mediterranean Sea.

Більше джерел

Дисертації з теми "Trench-Slope basins":

1

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 caractéristiques et mécanismes de mise en place des sédiments déstabilisés en examinant des MTDs miocènes affleurant dans la partie interne émergée de la marge Sud-Hikurangi (Île du Nord, Nouvelle-Zélande). Des données régionales de sismique réflexion marine ont aussi été utilisées afin d’analyser les géométries et architectures de plus grande échelle. Les résultats témoignent de l'importance des rides structurales dans le contrôle du remplissage sédimentaire des bassins. Différents styles de MTDs sont générés en fonction de leur position structurale (forelimb et backlimb) et à des moments spécifiques du développement des rides et des bassins perchés. Ceci suggère que les MTDs sont de puissants marqueurs tectonostratigraphiques. Ici, ils ont aidé à reconstruire, à des périodes clés, l'évolution de deux bassins et de la marge Hikurangi elle-même. Cette étude offre de nouvelles perspectives sur les interactions entre la déformation et la sédimentation pouvant être essentielles pour la compréhension de l’évolution des marges actives, de leurs risques géologiques et pour leur exploration
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

2

Quinn, Louise Anne. "Foreland and trench slope basin sandstones of the Goose Tickle Group and Lower Head Formation, Western Newfoundland /." 1992. http://collections.mun.ca/u?/theses,96320.

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Частини книг з теми "Trench-Slope basins":

1

Takano, Osamu, Yasuto Itoh, and Shigekazu Kusumoto. "Variation in Forearc Basin Configuration and Basin-filling Depositional Systems as a Function of Trench Slope Break Development and Strike-Slip Movement: Examples from the Cenozoic Ishikari–Sanriku-Oki and Tokai-Oki–Kumano-Nada Forearc Basins, Japan." In Mechanism of Sedimentary Basin Formation - Multidisciplinary Approach on Active Plate Margins. InTech, 2013. http://dx.doi.org/10.5772/56751.

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2

Kudrass, Herman R., and Dennis A. Ardus. "Geological Techniques." In Continental Shelf Limits. Oxford University Press, 2000. http://dx.doi.org/10.1093/oso/9780195117820.003.0019.

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In the previous chapters, the use of geophysical data for delineating the continental shelf has been discussed in some detail. But the determination of the case for any extension of the legal continental shelf beyond 200 nautical miles (M) from the territorial sea baseline may in some circumstances require a geological survey to confirm that a topographic or geophysical feature comprising what appears to be a natural prolongation of land territory is of continental or oceanic origin. A geological survey may also be necessary to determine the occurrence, thickness, and extent of sediments beyond the foot of the slope. Continental margins represent regions of transition from the landmass to the ocean basin and may be present-day areas of sediment erosion or deposition. Sediment supply to the continental shelf and slope, or the extent of erosion on the continental shelf and upper slope, is influenced by tectonic activity, sea-level fluctuations, climate change, variation in the wave or current regime, and various other processes. Bottom currents or gravity transport (turbidity) processes combine to varying degrees with pelagic sedimentation (the accumulation of the remains of marine organisms) to extend the supply of sediment well beyond the shelf and slope to the continental rise, ocean trench, or abyssal plain (Evans et al., 1998). In order to understand the geology of such areas, it is necessary to determine the structural setting, the tectonic and sedimentary evolution, the chrono-and lithostratigraphy, and the volcanic history. Understanding the ocean floor is a prerequisite for the determination of the extent of the continental shelf under UNCLOS. It is also highly relevant to the identification and delineation of mineral and energy resources, for determining the waste disposal potential of parts of the seafloor, and for undertaking an assessment of the risk of slope failure. None of these are directly relevant to establishing the new limits of the continental shelf, but they are highly relevant to its long-term exploitation. In order to achieve the necessary level of knowledge, the seafloor morphology and seabed character derived from bathymetric and sonar surveys (described in chapters 9 and 10) and the three-dimensional geology determined by geophysical surveys using seismic profiling, magnetometer, and gravity meter (discussed in chapters 12 and 13) need to be calibrated or "ground truthed" by sampling and coring (figure 14.1; Stoker et al., 1994).

3

Strand, K. "SEM Microstructural Analysis of a Volcanogenic Sediment Component in a Trench-Slope Basin of the Chile Margin." In Proceedings of the Ocean Drilling Program, 141 Scientific Results. Ocean Drilling Program, 1995. http://dx.doi.org/10.2973/odp.proc.sr.141.007.1995.

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Тези доповідей конференцій з теми "Trench-Slope basins":

1

Keaton, Jeffrey R., Luther H. Boudra, and Eleanor L. Huggins. "Enhancing Pipeline Project Management With Refined Rock Excavation Forecasting." In 2016 11th International Pipeline Conference. American Society of Mechanical Engineers, 2016. http://dx.doi.org/10.1115/ipc2016-64306.

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Accurate rock-excavation forecasting is one of the geotechnical risk factors that challenge successful management of cross-country pipeline projects. Pipeline construction personnel with local experience typically estimate rock excavation requirements for economic feasibility, permitting, and contracts. Where the excavation is paid on a “classified” basis, construction bid and contract documents typically call for excavation of “ditch” rock to be paid per lineal foot, whereas “area” or right-of-way (ROW) grading rock is paid per cubic yard. This paper briefly reviews the desktop procedure for estimating rock excavation quantities presented at IPC2012 and describes refinements to the procedure that expand its utility for pipeline project managers and planners. Input for the desktop study consists of digital GIS files of topography, geology, soil survey, pipeline alignment, and construction ROW layout and width. Publically available topographic data commonly has a horizontal resolution of 10-m; therefore, the pipeline centerline is subdivided into 10-m-long segments, the endpoints of which are used to summarize the data and perform calculations. Profiles of elevation, maximum ground slope, apparent ground slope across the ROW perpendicular to segment alignment (sidehill slope), and the relative sidehill slope direction are plotted for visual reference. A virtual geologic field reconnaissance along the alignment is performed using Google Earth Pro to supplement digital geology and soil survey data. Bedrock type is interpreted for general ease of excavation (granite versus shale) and soil survey map units are used to identify shallow cemented zones or bedrock that form the basis for an overall rock excavation index factor, which is expressed in terms of estimated mean and standard deviation of depth to rock and rock-like material. Rock factors vary based on the range of pipe size and ground conditions for a particular pipeline project or segment. Rock Factor 0 on a recent project corresponded to a mean-minus-one standard deviation (−1σ) depth to rock that was below pipeline depth, whereas Rock Factor 3 corresponded to a −1σ rock depth that was above pipeline depth. Refined rock excavation calculations consider equipment parameters (boom reach, track offset), trench configuration parameters (working pad width, bench offset, two-tone geometry), centerline distance to adjacent pipelines, and direction of lay, as well as pipe diameter and minimum cover depth. Desktop rock excavation results can be further refined by field examination and seismic refraction surveys to check depth to blast rock in trench excavations which is interpreted to be seismic velocities >1,220 to 1,370 m/s. Construction records of actual blasting details are needed to further improve the rock excavation model.

2

Wang, Genhou, Xiao Liang, Jinhan Gao, and Guoli Yuan. "Middle–Late Triassic trench-slope basin in Central Qiangtang, Tibet: Records of subduction-accretion process of the Paleo-Tethys Ocean." In 15th International Congress of the Brazilian Geophysical Society & EXPOGEF, Rio de Janeiro, Brazil, 31 July-3 August 2017. Brazilian Geophysical Society, 2017. http://dx.doi.org/10.1190/sbgf2017-323.

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3

Hildebrand, Robert, Janok P. Bhattacharya, and Joseph B. Whalen. "TYING SEDIMENTATION IN THE WESTERN INTERIOR BASIN TO THE MID-CRETACEOUS PENINSULAR RANGES OROGENY USING STARVED OUTER-SLOPE TRENCH DEPOSITS AND POST-COLLISIONAL MOLASSE." In GSA Connects 2021 in Portland, Oregon. Geological Society of America, 2021. http://dx.doi.org/10.1130/abs/2021am-368845.

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