eltanin fracture zone

2006). 4065 km S of Avarua, Cook Islands / pop: 13,373 / local time: 16:34:59.2 2016-05-02 You can help Wikipedia by expanding it. Earth Extremities I cover many earth extremities ranging from Earthquakes, Quake Swarms, Volcanic Activity/Eruptions, CME's - Coronal Mass Ejections, Solar Flares, Geomagnetic Storms, Magnetosphere Pressure plus other solar related radiation pulses, Asteroid/Meteorite Threats, Solar . [6] P. Earthquakes of Mw 6.2-6.4 occur along each transform but larger events are confined to the eastern half of the Heezen, two parts of the Tharp and segments of the Hollister. . The data since 1969 and those of Stewart & Okal (1983) for events back to 1920 indicate that earthquakes of Mw > 7 have not ruptured very long segments of any of the transforms. The transverse ridge separates the present trench from an 800km (500mi)-long aseismic valley where the Romanche transform was located until about 108 Ma. Strike-slip faulting with moment magnitudes Mw up to 6.4 characterizes most of these events. Where is and what is Eltanin Transform Fault and Fracture Zone? A geometric technique for relocating hotspots and refining absolute 3) to indicate stationarity of well-coupled and poorly coupled behaviour along transform segments since at least 1969. The central part of the Tharp transform near -350 km in Fig. [5], The hydrothermal vents of the MAR support many life forms. Dziewonski VanDeMark (2006) analysed the relative locations of earthquakes of moderate magnitude along oceanic transform faults with a double-difference method using Rayleigh waves of periods between 30 and 80 s. He used 92 events along the Eltanin transform faults from 1980 to early 2006, about half of the number we analysed. Several of those well-coupled segments ruptured quasi-periodically in earthquakes of Mw~5.5-6 and with repeat times shorter than 10 yr. We choose the Eltanin transform faults as another good place to search for these phenomena. That may account for the variety of Mws along it. Wolfe et al. LOUISVILLE RIDGE AND ELTANIN FRACTURE ZONE 3053 west to isolated peaks superimposed on ridge segments in the southeast. The point source depth of 10.4 km places the 2007 earthquake 6-7 km below the ocean floor. The morphology of the Atlantis Fracture Zone is typical of that of slow-slipping transforms. The average repeat time for the eight events of Mw > 5.9 is 4.0 1.0 (1 SD) yr. C.G. They are the scars on the seafloor basalt that are created by offsets in the mid-ocean ridge. It is that region where three of the four normal faulting earthquakes in Fig. This transform migration was preceded by a process 2517 Ma during which the Miocene shallow-water platform mentioned above reached sea level as the transverse ridge was first uplifted, then deformed, and finally buried under the sea. Cumulative seismic moment release 1971 to 2010 along two segments of Tharp transform as indicated in Fig. (1993) attribute it to one of those small spreading centres. If we assume that all of the true depths of these earthquakes are shallow, what size error or bias should we expect in estimates of Mo? Instead, we have chosen not to use models of the depth of seismic faulting in estimating coupling but to calculate downdip width from a segments length along strike, moment release rate and relative plate rate assuming' full seismic coupling. How are fracture zones like the Eltanin created? If those segments are not fully coupled, our calculations of downdip width, of course, are minimum estimates. H.W. For the larger and more complex 2001 earthquake the rupture initiation depth is 8.9 km, and the centroid depth, taking into account the propagation of the point source in the direction of the directivity vector, is approximately 11 km, about 7 km below the ocean floor. (2009). A break in the smooth trend of the ridge at latitude 37.5S has been recognized in both bathymetric and altimetric data. Wolfe et al. Log of cumulative number of earthquakes per 20 yr larger than a given Mw as a function of Mw. . He found that interevent times for those pairs was tightly clustered around 5 yr with a COV ~ 0.2. If the anomalous trend is real, having one group of events (east or west) off the primary transform then almost becomes a necessary interpretation. The absence of known earthquakes on the three transforms beyond their bounding ridge crests and the spacing of magnetic anomalies, however, indicate that the Pacific and Antarctic plates are intact today beyond the active parts of those transforms and that the lengths of the transforms are not continuing to grow. This is in accord with the findings of Stewart & Okal (1983) that the Eltanin system has not broken in great events since 1920 and is unlikely to do so. Cumulative seismic moment release from 1976 to 2010 along a 42-km section of Heezen transform indicated in Fig. www.science.gov These are very small, typically 3-15 km for the earliest events and 1-2 km for earthquakes since 2000. Those estimates are smaller than those for oceanic transforms at much slower moving plate boundaries, which is in accord with the notion, which we accept, that temperatures are higher at a given depth for fast moving plate boundaries. J.T. The shaded area is the "Hollister region" whose seismicity is detailed in Fig. . The horizontal axis is parallel to computed transform directions; the vertical is perpendicular to it. This yielded 110 earthquakes for that period. Solid line indicates Mw=mb. The continuity in smooth trend of the ridge and the Eltanin Fracture Zone suggests some relationship between them. Data for the reanalysis were collected from all the main global digital networks that have operated since 1976. Origin of the Louisville ridge and its relationship to the Eltanin R.A. Bivalve communities have been reported around vents further south. 3). 2. Lonsdale The Polar and Subantarctic Fronts are observed to pass along the Udinstev Fracture Zone 3 as the jets in the flow are steered by the topography (e.g., Moore et al. https://session.masteringgeology.com/problemAsset/3004355/4/MGEO_3004355_PartD.jpg. Eltanin | Article about Eltanin by The Free Dictionary G. We show in detail, however, that some segments of the three transforms are aseismic at the Mw > 5.4 level whereas others are more strongly coupled. What is the labour of cable stayed bridges? As it flows north, it is constrained by numerous obstacles on the seafloor. The earthquakes were analysed using the standard Global CMT (GCMT) algorithm as described in Dziewonski et al. Chain and romanche fracture zones - ScienceDirect We refer to the magnitudes derived from those moment tensors as either new or recomputed Mws. We propose that the remainder of the plate motion . Aseismic parts of the Heezen and Tharp fracture zones can be traced far to the northwest and southeast. The remarkable quasi-repeatability of events of Mw > 5.9 may be attributed to the isolation of an asperity, that is, a single resisting fault segment that ruptures mainly or solely in earthquakes. The Eltanin Fault System (Eltanin Fracture Zone) is a series of six or seven dextral transform faults that offset the Pacific-Antarctic Ridge, a spreading zone between the Pacific Plate and the Antarctic Plate.The affected zone of the Pacific-Antarctic Ridge is about 800 km long, between 56 S, 145 W and 54.5 S, 118.5 W, southwest of Easter Island, and about as far as one can get from . The 'Ar-39Ar dating of rocks dredged either side of the break suggest that it is analogous to the bend in the Hawaiian-Emperor seamount chain. One exception to this general observation is the earthquake on 2000 October 4. Bathymetric Features 67%. FRACTURE ZONE. Smith 7, many of the smaller events are either aftershocks or foreshocks and are considered to be noise for the purposes of assessing the repeat times of the largest earthquakes. Phipps Morgan & Forsyth (1988), Shen & Forsyth (1992), Behn (2007), Gregg et al. The new result is well constrained by the surface wave data, which were not included in the original analysis. Somewhat smaller estimates of W are obtained using a value of appropriate to the uppermost mantle. Woodward Given the uncertainty of its CMT location, we think it is reasonably associated with a previous rupture of the same asperity as in Figs 4 and 7. The presence of large events just to its west and the variety of Mws, however, suggest that it does not always rupture as a single asperity. Previously, some epicentral locations in that area were uncertain by as much as 500 km. 4. The 40Ar39Ar dating of rocks dredged . Of the 84 earthquakes from 1976 to 1989, we rejected seven CMT solutions. SmartFigure: The Eltanin Fracture Zone Flashcards | Quizlet Exploring Data Coaching Activity: Longshore C, SmartFigure: Geostrophic current and western. DeMets The Eltanin Fault System (Eltanin Fracture Zone) is a series of six or seven dextral transform faults that offset the Pacific-Antarctic Ridge, a spreading zone between the Pacific Plate and the Antarctic Plate.The affected zone of the Pacific-Antarctic Ridge is about 800 km long, between 56 S, 145 W and 54.5 S, 118.5 W, southwest of Easter Island, and about as far as one can get from . It bisects the Mid-Atlantic Ridge (MAR) just north of the equator at the narrowest part of the Atlantic between Brazil and West Africa, extending from 2N to 2S and from 16W to 20W. Understanding the Regional Variability of Eddy Diffusivity in the Origin of the Louisville Ridge and its relationship to the Eltanin Correct Option: O They are the scars on the seafloor basalt that are created by offsets in the mid-ocean ridge. 1997, 2005). J. . Since the length along strike, L, was not determined for individual earthquakes, for the calculations later we took a length of 105 km for the entire eastern end of the Heezen transform, which includes several segments that have ruptured in large shocks (Fig. Seismic properties of the Eltanin Transform System, South Pacific The seismic history of the Eltanin Fracture Zone on the Pacific-Antarctic Ridge for the years 1920-1981 shows that the seismic slip accumulated during this recording interval accounts for only a small fraction (less than 10%) of the amount of slip predicted by kinematic models of plate motion. Subsequent locations of earthquakes and mapping of bathymetry and magnetic anomalies showed that the Eltanin zone consisted of three en echelon transforms (Molnar et al. The segment of the Tharp transform between -210 and -241 km has a T of 8 yr, Mw 6.08-6.3 and five events. Sedimentary rocks consist of particles derived from Depths modelled by Wolfe et al. 7. Only the Heezen transform has been surveyed by swath mapping (Lonsdale 1994). . Listen to the audio pronunciation of Eltanin Fracture Zone on pronouncekiwi 1975; Lonsdale 1994), which were named for M. Tharp, B. Heezen and C. Hollister (Fig. The boat was returning to France after spending a few months on a scientific mission near Cape Horn as part of the first International Polar Year. What is error code E01-5 on Toyota forklift. Hence, we cannot distinguish between those two models. Small amounts of normal faulting occurring off transform is in accord with the idea that the Euler pole has moved relatively recently in time to place each of the three transform zones under a small component of extension. Four segments of the Tharp transform (Fig. (2007) and others modelled temperatures in the vicinity of oceanic transform faults at fast moving plate boundaries that differ from those for the earlier simple plate cooling models. Which letter is pointing to a transform fault? 5 and the bathymetric expression of it in Fig. Centroid moment tensor solutions are recomputed for 190 earthquakes from 1976 to 2010 along the Heezen, Tharp and Hollister transform faults of the Eltanin system using a 3-D seismic velocity model. Also, there was no discontinuous change in the calculated Mo when the CMT was evaluated above the Moho (which in PREM is at 24.4 km) or below it. Maternovskaya R.G. Elevation map for localities Click for legend, zoom in for elevation lines Routing error m , | Map style: OpenTopoMap ( CC-BY-SA) Age- and sex-specific incidence of femoral neck and - PubMed The segment between -575 and -580 km was the site of only two large earthquakes, Mw 6.22 and 6.24. Thermal models with constant and variable mineral physics properties are formally analyzed for fits against recently filtered databases for heat flow and topography. Altimetry-drived Antarctic Circumpolar Current fronts - SEANOE Formed around Antarctica, the AABW is cold, has low salinity, and high silicate concentration. Distances along the transform are calculated from an arbitrary origin of coordinates at 55.4 S, 125.0 W. Structural geomorphology of the eltanin fault system and adjacent In the basin on the eastern side of the MAR the Walvis Ridge blocks the northward passage. The western part of the transverse ridge consists of fragments of uplifted oceanic crust and upper mantle. T.F. . 5 contains only two earthquakes of Mw 5.45 and 5.50. McGuire 11 for Mw > 6. The Eltanin Fault System (Eltanin Fracture Zone) is a series of six or seven dextral transform faults that offset the Pacific-Antarctic Ridge, a spreading zone between the Pacific Plate and the Antarctic Plate. M.S. 2006-01-01. D.W. 4. Wolfe The Udintsev Fracture Zone is a suitable site for a long-term monitoring of the Antarctic Circumpolar Current 1 Introduction The Antarctic Circumpolar Current (ACC) forms a continuous near-zonal band of eastward flow. We determined a CMT solution for it using seven digital stations and obtained a Mw of 6.1, a strike-slip mechanism and a location (red triangle) about 20 km west of the group indicated in Fig. PDF Transform Plate Boundaries And Fracture Zones By Joao C Duarte 7 for events of Mw > 5.55 (blue) and Mw > 5.9 (red). In contrast, VanDeMark (2006) used few events, a double-difference methodology and a uniform velocity model for Rayleigh waves in calculating revised earthquake locations along the Eltanin transforms. Since the number and azimuthal distribution of the global long-period stations used in computing the CMT solutions increased dramatically since 1976, especially in the 1990s, we choose to use digital data from as many stations as possible in our analyses rather than from merely the few that recorded most of the events. J.K. a generally flat zone extending from the shore to the shelf break continental margin shallow-water areas close to continent abyssal plain flat depositional surfaces that cover extensive portions of the deep-ocean basins The method that used most frequently to investigate sediment and rock layers of the sea floor is: Our calculations of moment magnitude Mw are compared with determinations of the short-period magnitude mb in Fig. The smooth trend of the ridge is NNW-SSE with a trend break at about 37.8S. Lat: [2] However, the total offset is about 1600km. Observations of the Antarctic Circumpolar Current Over the Udintsev trench to the Eltanin Fracture Zone. . Their poorly determined repeat times range from 13 to 24 yr. . Most prominent is an asymmetric transverse ridge, at which abyssal hills adjacent to the fault zone have been . We show events characterized by a predominance of strike-slip faulting that we located since 1976 in red along with the few earthquakes in blue that involved a predominance of normal faulting. His relocations are shown in Figs 4-6 in green. Series of faults that offset the Pacific-Antarctic Ridge, "Seismicity and Aseismic Slip Along the Eltanin Fracture Zone", "The Pacififi c-Antarctic Ridge between 4115'S and 5245'S: Survey and sampling during the PACANTARCTIC 2 cruise", "Earthquakes along Eltanin transform system, SE Pacific Ocean: fault segments characterized by strong and poor seismic coupling and implications for long-term earthquake prediction", https://en.wikipedia.org/w/index.php?title=Eltanin_Fault_System&oldid=1068451688, Creative Commons Attribution-ShareAlike License 3.0, This page was last edited on 28 January 2022, at 13:46. Moment release in earthquakes of Mw= 6.08 is about 60 per cent of that for Mw > 5.55. Extending the work of Stewart & Okal (1983), they again emphasized the dominance of aseismic slip. Note exaggerated scale in transform-perpendicular direction. 1975; Lonsdale 1994), which were named for M. Tharp, B. Heezen and C. Hollister . We find or confirm two anomalous characteristics: the . Fig. Eltanin fracture zone Scope Notes: SE Pacific. One 30-42-km-long segment of the Heezen transform that appears to be an isolated well-coupled asperity has ruptured in eight earthquakes of Mw 5.9-6.1 quasi-periodically with a coefficient of variation of 0.26 every 4.0 1.0 yr. Other well-coupled fault segments, which were sites with earthquakes up to Mw 6.39 and fewer events since 1976, have average repeat times of about 7-24 yr. The four estimates of W in Table 1 range from 3.9 to 6.0 km. Aseismic parts of the Heezen and Tharp fracture zones can be traced far to the northwest and . The ridge segments and transform faults of the East Pacific Rise and Pacific-Antarctic ridge are the sites of the fastest rates of the seafloor spreading and relative plate motion in the world. P. Since the 40-km section of the Tharp (Fig. The combined three Eltanin transform faults are much more active at the Mw~ 6 level than a comparable length of either the San Andreas Fault in California or other transform systems on land. 2 shows the areal distribution of strike-slip earthquakes Mw > 5.5 as a function of their recomputed magnitude, Mw, in red along the three transform faults of the Eltanin system. Eltanin is an island located in the South Pacific Ocean, following the contours of the Eltanin Fracture Zone. Menke They also calculated Mw for three earthquakes in 1969, 1971 and 1973; they and Molnar et al. 7; several were the sites of two or three earthquakes of Mw > 6.15. It is the only example of a very short time interval between large shocks along segments of the Eltanin transforms. This experiment addresses one component of the potential bias that may be present in CMT seismic moments. Molnar The Eltanin Transform Fault and Fracture Zone is a series of six or seven dextral transform faults along ~800 km of the. If those short spreading centres are very young, they may not have had enough time to become oriented perpendicular to the transform. Thesaurus Terms | GeoScienceWorld Nearby ocean bottom seismometers are needed to detect them. Map view of CMT locations of earthquakes along Tharp transform from 1976 to 2010. Tectonic and magmatic ridges in the eltanin fault system - SpringerLink 1988). Lonsdale (1994) concludes that a zone of extension north of the Heezen transform developed following a Pliocene change in relative plate motion. . The flow of NADW through the Romanche and Chain Fracture Zones may serve as a conduit for larval transport from the western North Atlantic to the eastern South Atlantic. Nakata , and M is in kg. Their surface wave magnitudes, Ms, are plotted. Added to Thesaurus in 1989. To address part of this question, we performed the following experiment. The steep slope of about -2.9 for Mw > 6 is unusual. G. We report the unique occurren 4. Cumulative moment release is shown in Fig. Undersea Features Fishing & Outdoor Fracture Zone Maps - MyFishMaps.com Bohnenstiehl et al. 2. Red and green symbols denote strike-slip faulting. Red triangle indicates CMT solution for shock of 1975 April 19. They find that aftershock zones of nearby pairs of moderate-size earthquakes along fast-moving transforms were separated by small spreading centres. The segment between -210 and -241 km consists of a large number of events of Mw > 5.55, one of Mw 6.08, three of 6.15 =Mw= 6.17 and one of Mw 6.3 (Stewart & Okal 1983) on 1973 September 18. S. Carbotte (written communication, 2011 July 22) notes, however, that some of the shocks along the eastern end of the Tharp transform might fall within a zone of deformed/rotated seafloor south of the transform that looks quite similar to the zone of deformation north of the Heezen transform described by Lonsdale (1994) and seen in Fig. Cumulative moment release along that segment is displayed in Fig. The data for Mw > 5.9 are fit remarkably well by the slip predictable model of Shimazaki & Nakata (1980) whereby the size of the next earthquake is proportional to the time since the previous event. Most of the earlier earthquakes analysed here are larger than Mw= 5.5, since smaller earthquakes appear to have gone largely undetected until the 1990s. where is and what is eltanin transform fault and fracture. Kent They were generally too small to generate stable CMT results. Fracture Zone. Lamont-Doherty Earth Observatory Contribution 7505. Argus This term has multiple hierarchies. The fault segment between -665 and -680 km (green symbols in Fig. Their average repeat time is 7.1 yr and their COV is 0.28. Okal The surface wave catalogue (Ekstram 2006) starts in 1990, and the magnitude that is associated with events in that catalogue is usually very close to the Mw obtained in a CMT analysis. In that simple model, earthquakes should extend to greater depths and presumably be larger near the centres of transforms, which is clearly not the case for the Heezen and Tharp faults. Fox Cumulative seismic moment release for shocks of Mw > 5.55 from 1969 to 2010 along three additional segments of Heezen transform fault as indicated in Fig. As in Fig. Solutions for new earthquakes of Mw > 5.5 were not found after early 2002. We determined a few CMT mechanisms for which PDE or ISC did not compute hypocentres, for which we relied on detections and locations based on intermediate-period surface waves (Ekstram 2006). The coefficient of variation (COV), the standard deviation, SD, divided by the average repeat time, is 0.26. This attests to the very thin lithosphere at fast spreading ridges. The segment of the Heezen from 179 to 200 km has the next smallest T, 7.1 yr, Mw 5.89-6.5 and six events. Abercrombie . This technique has the potential to rigorously assess hotspot fixity and to locate extinct hotspots. Tromp Okal The 2004 Parkfield earthquake of Mw 6.0 had a rupture length of 20-25 km (Johanson et al. In this method, the moment tensor and source centroid are estimated by matching observed long-period three-component seismograms to synthetic waveforms calculated using normal-mode summation. The repeat times of those largest events are longer but uncertain since they are based on few earthquakes. The affected zone of the Pacific-Antarctic Ridge is about 800kmlong, between 56 S, 145 W and 54.5 S, 118.5 W,[1] southwest of Easter Island, and about as far as one can get from land on planet Earth (4852.6S 12323.6W). 4706 km S of Papeete, French Polynesia / pop: 26,400 / local time: 01:42:15.1 2017-06-15 Eltanin Fracture Zone System: IHO-IOC GEBCO Gazetteer of Undersea Feature Names : English: Eltanin Fracture Zone: US BGN Advisory Committee on Undersea Features (ACUF) PlaceType: Fracture Zone : Latitude: 54 8' 16.8" S (-54.137999) Longitude: 127 32' 7.3" W (-127.53537) Min. (2010) that describes the relative motion of the Pacific and Antarctic plates. D.R. Solomon [1], It was named after the French navy ship La Romanche, commanded by captain Louis-Ferdinand Martial which on 11 October 1883 made soundings that revealed the trench. The series includes two events of 6.17 and 6.18 and one of less certain Mw of 6.5 (Stewart & Okal 1983) on 1971 April 4 that are much larger than the other three. We also used the same 3-D velocity model for our new CMT solutions. Ryan and M. Tolstoy for helpful discussions. Symbols, axes and origin of coordinates same as Fig. Topographic Map of Eltanin Fracture Zone. We assume that earthquakes along a given segment of a transform occur on single faults although the distribution of CMT solutions scatters about 15 km perpendicular to the transforms. [8], Coordinates: .mw-parser-output .geo-default,.mw-parser-output .geo-dms,.mw-parser-output .geo-dec{display:inline}.mw-parser-output .geo-nondefault,.mw-parser-output .geo-multi-punct{display:none}.mw-parser-output .longitude,.mw-parser-output .latitude{white-space:nowrap}000N 1800W / 0.000N 18.000W / 0.000; -18.000, "Dolomite formation in pelagic limestone and diatomite, Romanche Fracture Zone, Equatorial Atlantic", 10.1175/1520-0485(1998)028<1929:MITRFZ>2.0.CO;2, "Lower Cretaceous to Eocene sedimentary transverse ridge at the Romanche Fracture Zone and the opening of the equatorial Atlantic", "Hydrothermal activity on the southern Mid-Atlantic Ridge: Tectonically- and volcanically-controlled venting at 45S", "Transport of Bottom Water in the Romanche Fracture Zone and the Chain Fracture Zone", 10.1175/1520-0485(1998)028<0779:TOBWIT>2.0.CO;2, "Biodiversity and biogeography of hydrothermal vent species: thirty years of discovery and investigations", https://en.wikipedia.org/w/index.php?title=Romanche_Trench&oldid=1090955796, This page was last edited on 1 June 2022, at 10:32. For LNADW and AABW, the Romanche and Chain Fracture Zones (just south of the equator) are the only deep passages in the MAR where interbasin exchange is possible. What kind of fault is represented by the eltanin and romanche fracture zones? Enter the email address you signed up with and we'll email you a reset link. Clearly, a gradient in the maximum size of earthquakes and seismic coupling occurs between the eastern and western ends of the Heezen transform. Distances: 4585 km SE of Wellington, New Zealand / pop: 382,000 / local time: 23:42:15.1 2017-06-15 . The Atlantis Fracture Zone (30 N) is one of the smallest transform faults along the Mid-Atlantic Ridge with a spatial offset of 70 km and an age offset of ~ 6 Ma. 3457km (2148mi) S of Adamstown, Pitcairn. Moment magnitudes are given below each solution. "zone of fracture" in Chinese : , ; ; ,; ; "amsterdam fracture zone" in Chinese : "aseismic fracture zone" in Chinese : The average displacement per earthquake is 0.32 m assuming full coupling and an average repeat time of 4 yr. Figs 8-10 show cumulative moment release throughout 2010 for seven additional segments of the three Eltanin faults. Similarly, earthquake recurrence is more difficult to examine for other long oceanic transform faults, such as those in the equatorial Atlantic, that have considerably smaller long-term slip rates.

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