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Journal articles on the topic 'Mid-ocean ridges'

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Published: 4 June 2021
Last updated: 21 February 2023

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1

Delaney, John. "Mid‐ocean ridges." Eos, Transactions American Geophysical Union 72, no. 8 (February 19, 1991): 90. http://dx.doi.org/10.1029/eo072i008p00090-03.

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2

McClintock, Peter V. E. "Mid-Ocean Ridges." Contemporary Physics 57, no. 1 (December 11, 2015): 143. http://dx.doi.org/10.1080/00107514.2015.1111414.

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3

Collier, Jenny. "Review of ‘Mid-Ocean Ridges’." Geophysical Journal International 197, no. 3 (April 9, 2014): 1884. http://dx.doi.org/10.1093/gji/ggu041.

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4

Schouten, Hans, Kim D. Klitgord, and John A. Whitehead. "Segmentation of mid-ocean ridges." Nature 317, no. 6034 (September 1985): 225–29. http://dx.doi.org/10.1038/317225a0.

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5

Langmuir, Charles, and Donald Forsyth. "Mantle Melting Beneath Mid-Ocean Ridges." Oceanography 20, no. 1 (March 1, 2007): 78–89. http://dx.doi.org/10.5670/oceanog.2007.82.

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6

Cann, Joe. "Subtle minds and mid-ocean ridges." Nature 393, no. 6686 (June 1998): 625–27. http://dx.doi.org/10.1038/31347.

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7

Ghods, A., and J. Arkani-Hamed. "Melt migration beneath mid-ocean ridges." Geophysical Journal International 140, no. 3 (March 1, 2000): 687–97. http://dx.doi.org/10.1046/j.1365-246x.2000.00032.x.

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8

Humphris, Susan E. "Hydrothermal processes at mid-ocean ridges." Reviews of Geophysics 33 (1995): 71. http://dx.doi.org/10.1029/95rg00296.

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9

Solomon, S. C., and D. R. Toomey. "The Structure of Mid-Ocean Ridges." Annual Review of Earth and Planetary Sciences 20, no. 1 (May 1992): 329–66. http://dx.doi.org/10.1146/annurev.ea.20.050192.001553.

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10

Cronin, Vincent S. "Instantaneous velocity of mid-ocean ridges." Tectonophysics 230, no. 3-4 (February 1994): 151–59. http://dx.doi.org/10.1016/0040-1951(94)90132-5.

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11

Alt, Jeffrey C. "Hydrothermal fluxes at mid-ocean ridges and on ridge flanks." Comptes Rendus Geoscience 335, no. 10-11 (September 2003): 853–64. http://dx.doi.org/10.1016/j.crte.2003.02.001.

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12

Lissenberg, C. Johan, Christopher J. MacLeod, and Emma N. Bennett. "Consequences of a crystal mush-dominated magma plumbing system: a mid-ocean ridge perspective." Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences 377, no. 2139 (January 7, 2019): 20180014. http://dx.doi.org/10.1098/rsta.2018.0014.

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Crystal mush is rapidly emerging as a new paradigm for the evolution of igneous systems. Mid-ocean ridges provide a unique opportunity to study mush processes: geophysical data indicate that, even at the most magmatically robust fast-spreading ridges, the magma plumbing system typically comprises crystal mush. In this paper, we describe some of the consequences of crystal mush for the evolution of the mid-ocean ridge magmatic system. One of these is that melt migration by porous flow plays an important role, in addition to rapid, channelized flow. Facilitated by both buoyancy and (deformation-enhanced) compaction, porous flow leads to reactions between the mush and migrating melts. Reactions between melt and the surrounding crystal framework are also likely to occur upon emplacement of primitive melts into the mush. Furthermore, replenishment facilitates mixing between the replenishing melt and interstitial melts of the mush. Hence, crystal mushes facilitate reaction and mixing, which leads to significant homogenization, and which may account for the geochemical systematics of mid-ocean ridge basalt (MORB). A second consequence is cryptic fractionation. At mid-ocean ridges, a plagioclase framework may already have formed when clinopyroxene saturates. As a result, clinopyroxene phenocrysts are rare, despite the fact that the vast majority of MORB records clinopyroxene fractionation. Hence, melts extracted from crystal mush may show a cryptic fractionation signature. Another consequence of a mush-dominated plumbing system is that channelized flow of melts through the crystal mush leads to the occurrence of vertical magmatic fabrics in oceanic gabbros, as well as the entrainment of diverse populations of phenocrysts. Overall, we conclude that the occurrence of crystal mush has a number of fundamental implications for the behaviour and evolution of magmatic systems, and that mid-ocean ridges can serve as a useful template for trans-crustal mush columns elsewhere. This article is part of the Theo Murphy meeting issue ‘Magma reservoir architecture and dynamics'.
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13

TOH, Hiroaki. "Asymmetric Electrical Structures Beneath Mid-Ocean Ridges." Journal of Geography (Chigaku Zasshi) 112, no. 5 (2003): 684–91. http://dx.doi.org/10.5026/jgeography.112.5_684.

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14

Roger Buck, W., Suzanne M. Carbotte, and Carolyn Mutter. "Controls on extrusion at mid-ocean ridges." Geology 25, no. 10 (1997): 935. http://dx.doi.org/10.1130/0091-7613(1997)025<0935:coeamo>2.3.co;2.

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15

Ribe, Neil M. "On the dynamics of mid-ocean ridges." Journal of Geophysical Research: Solid Earth 93, B1 (January 10, 1988): 429–36. http://dx.doi.org/10.1029/jb093ib01p00429.

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16

Cyril Patrick Masalu, Desiderius. "Global Mid-Ocean Ridges Mantle Tomography Profiles." Earth Sciences 4, no. 2 (2015): 80. http://dx.doi.org/10.11648/j.earth.20150402.13.

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17

Cordery, Matthew J., and Jason Phipps Morgan. "Convection and melting at mid-ocean ridges." Journal of Geophysical Research: Solid Earth 98, B11 (November 10, 1993): 19477–503. http://dx.doi.org/10.1029/93jb01831.

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18

Sempere, Jean-Christophe, and Ken C. MacDonald. "Marine tectonics: Processes at mid-ocean ridges." Reviews of Geophysics 25, no. 6 (1987): 1313. http://dx.doi.org/10.1029/rg025i006p01313.

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19

Buck, W. Roger, Luc L. Lavier, and Alexei N. B. Poliakov. "Modes of faulting at mid-ocean ridges." Nature 434, no. 7034 (April 2005): 719–23. http://dx.doi.org/10.1038/nature03358.

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20

Tirone, M., G. Sen, and J. P. Morgan. "Petrological geodynamic modeling of mid-ocean ridges." Physics of the Earth and Planetary Interiors 190-191 (January 2012): 51–70. http://dx.doi.org/10.1016/j.pepi.2011.10.008.

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21

Schwarzenbach, Esther M., and Matthew Steele-MacInnis. "Fluids in Submarine Mid-Ocean Ridge Hydrothermal Settings." Elements 16, no. 6 (December 1, 2020): 389–94. http://dx.doi.org/10.2138/gselements.16.6.389.

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Seawater interaction with the oceanic lithosphere crucially impacts on global geochemical cycles, controls ocean chemistry over geologic time, changes the petrophysical properties of the oceanic lithosphere, and regulates the global heat budget. Extensive seawater circulation is expressed near oceanic ridges by the venting of hydrothermal fluids through chimney structures. These vent fluids vary greatly in chemistry, from the metal-rich, acidic fluids that emanate from “black smokers” at temperatures up to 400 °C to the metal-poor, highly alkaline and reducing fluids that issue from the carbonate–brucite chimneys of ultramafic-hosted systems at temperatures below 110 °C. Mid-ocean ridge hydrothermal systems not only generate signifi-cant metal resources but also host unique life forms that may be similar to those of early Earth.
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22

Dalton, Colleen A., Charles H. Langmuir, and Allison Gale. "Geophysical and Geochemical Evidence for Deep Temperature Variations Beneath Mid-Ocean Ridges." Science 344, no. 6179 (April 3, 2014): 80–83. http://dx.doi.org/10.1126/science.1249466.

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The temperature and composition of Earth’s mantle control fundamental planetary properties, including the vigor of mantle convection and the depths of the ocean basins. Seismic wave velocities, ocean ridge depths, and the composition of mid-ocean ridge basalts can all be used to determine variations in mantle temperature and composition, yet are typically considered in isolation. We show that correlations among these three data sets are consistent with 250°C variation extending to depths >400 kilometers and are inconsistent with variations in mantle composition at constant temperature. Anomalously hot ridge segments are located near hot spots, confirming a deep mantle-plume origin for hot spot volcanism. Chemical heterogeneity may contribute to scatter about the global trend. The coherent temperature signal provides a thermal calibration scale for interpreting seismic velocities located distant from ridges.
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23

Wang, Liping, and Chester J. Koblinsky. "Influence of mid-ocean ridges on Rossby waves." Journal of Geophysical Research 99, no. C12 (1994): 25143. http://dx.doi.org/10.1029/94jc02374.

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24

Rabinowicz, M., S. Rouzo, J. C. Sempere, and C. Rosemberg. "Three-dimensional mantle flow beneath mid-ocean ridges." Journal of Geophysical Research: Solid Earth 98, B5 (May 10, 1993): 7851–69. http://dx.doi.org/10.1029/92jb02740.

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25

Faul, Ulrich H. "Melt retention and segregation beneath mid-ocean ridges." Nature 410, no. 6831 (April 2001): 920–23. http://dx.doi.org/10.1038/35073556.

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26

Mitchell, N., J. Escartin, and S. Allerton. "Detachment faults at mid-ocean ridges garner interest." Eos, Transactions American Geophysical Union 79, no. 10 (1998): 127. http://dx.doi.org/10.1029/98eo00095.

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27

Batiza, Rodey. "Magmatic segmentation of mid-ocean ridges: a review." Geological Society, London, Special Publications 118, no. 1 (1996): 103–30. http://dx.doi.org/10.1144/gsl.sp.1996.118.01.06.

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28

Lin, Jian, and E. M. Parmentier. "Mechanisms of lithospheric extension at mid-ocean ridges." Geophysical Journal International 96, no. 1 (January 1989): 1–22. http://dx.doi.org/10.1111/j.1365-246x.1989.tb05246.x.

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29

Sorokhtin, N. O., L. I. Lobkovsky, G. V. Novikov, N. E. Kozlov, O. Yu Bogdanova, and S. L. Nikiforov. "Regularities of ore formation in mid-ocean ridges." Doklady Earth Sciences 465, no. 2 (December 2015): 1215–17. http://dx.doi.org/10.1134/s1028334x15120156.

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30

Albers, Michael, and Ulrich R. Christensen. "Channeling of plume flow beneath mid-ocean ridges." Earth and Planetary Science Letters 187, no. 1-2 (April 2001): 207–20. http://dx.doi.org/10.1016/s0012-821x(01)00276-x.

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31

Arai, Shoji, and Makoto Miura. "Podiform chromitites do form beneath mid-ocean ridges." Lithos 232 (September 2015): 143–49. http://dx.doi.org/10.1016/j.lithos.2015.06.015.

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32

Roberts, D. G. "The mid-ocean ridges: Mountains below sea level." Marine and Petroleum Geology 13, no. 3 (May 1996): 349. http://dx.doi.org/10.1016/0264-8172(96)90008-2.

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33

MACDONALD, K. C., D. S. SCHEIRER, and S. M. CARBOTTE. "Mid-Ocean Ridges: Discontinuities, Segments and Giant Cracks." Science 253, no. 5023 (August 30, 1991): 986–94. http://dx.doi.org/10.1126/science.253.5023.986.

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34

Nowacki, Andy, J. Michael Kendall, and James Wookey. "Mantle anisotropy beneath the Earth's mid-ocean ridges." Earth and Planetary Science Letters 317-318 (February 2012): 56–67. http://dx.doi.org/10.1016/j.epsl.2011.11.044.

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35

Mével, Catherine. "Serpentinization of abyssal peridotites at mid-ocean ridges." Comptes Rendus Geoscience 335, no. 10-11 (September 2003): 825–52. http://dx.doi.org/10.1016/j.crte.2003.08.006.

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36

Antonovskaya, Galina N., Irina M. Basakina, Natalya V. Vaganova, Natalia K. Kapustian, Yana V. Konechnaya, and Alexey N. Morozov. "Spatiotemporal Relationship between Arctic Mid-Ocean Ridge System and Intraplate Seismicity of the European Arctic." Seismological Research Letters 92, no. 5 (June 16, 2021): 2876–90. http://dx.doi.org/10.1785/0220210024.

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Abstract In this article, we investigate the influence of the Arctic mid-ocean ridge system (AMORS), including the Gakkel and Mohns ridges, and the Knipovich ridge–Lena trough (KL) segment, on seismicity of the Novaya Zemlya archipelago area (NZ) and the northernmost margin of the East-European Platform (EEP) for 1980–2019. For each individual area, the annual seismic energy was obtained by adding the energies of all earthquakes. To do this, we have converted various types of magnitude by different seismic networks into moment magnitude Mw. We compiled the updated catalog for the NZ, the northern EEP, and the northern part of the Ural fold belt (UFB). As a result, we constructed time distributions of annual seismic energy releases for each composing ridges of AMORS, NZ, and EEP combined with UFB. A model based on the Elsasser’s one describing the transfer of lithospheric stress disturbances in the horizontal direction was built, and quantitative calculations of the disturbance propagations from AMORS were performed. Results are in good agreement with the annual seismic energy time lags between rifts and NZ and EEP together with the UFB. We calculated correlation coefficients between the seismic energy releases over the time for the structures, enabling identification of the characteristic excitation cycles and estimation of the interval of disturbance transfer from AMORS. As a result, disturbances from the Gakkel ridge appear 3 yr later in NZ, from the KL segment in 4 yr, and from the Mona ridge in 8 yr. For the EEP + UBF combined area, we found the following disturbances spreading lags as 7 yr for the Mona ridge, 4 yr for the KL segment, and 5 yr for the Gakkel ridge. The obtained damping amplitudes of the disturbance spreading from the arctic ridges are sufficient to affect the intraplate seismic activity.
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37

Grevemeyer, Ingo, Nicholas W. Hayman, Dietrich Lange, Christine Peirce, Cord Papenberg, Harm J. A. Van Avendonk, Florian Schmid, Laura Gómez de La Peña, and Anke Dannowski. "Constraining the maximum depth of brittle deformation at slow- and ultraslow-spreading ridges using microseismicity." Geology 47, no. 11 (September 23, 2019): 1069–73. http://dx.doi.org/10.1130/g46577.1.

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Abstract The depth of earthquakes along mid-ocean ridges is restricted by the relatively thin brittle lithosphere that overlies a hot, upwelling mantle. With decreasing spreading rate, earthquakes may occur deeper in the lithosphere, accommodating strain within a thicker brittle layer. New data from the ultraslow-spreading Mid-Cayman Spreading Center (MCSC) in the Caribbean Sea illustrate that earthquakes occur to 10 km depth below seafloor and, hence, occur deeper than along most other slow-spreading ridges. The MCSC spreads at 15 mm/yr full rate, while a similarly well-studied obliquely opening portion of the Southwest Indian Ridge (SWIR) spreads at an even slower rate of ∼8 mm/yr if the obliquity of spreading is considered. The SWIR has previously been proposed to have earthquakes occurring as deep as 32 km, but no shallower than 5 km. These characteristics have been attributed to the combined effect of stable deformation of serpentinized mantle and an extremely deep thermal boundary layer. In the context of our MCSC results, we reanalyze the SWIR data and find a maximum depth of seismicity of 17 km, consistent with compilations of spreading-rate dependence derived from slow- and ultraslow-spreading ridges. Together, the new MCSC data and SWIR reanalysis presented here support the hypothesis that depth-seismicity relationships at mid-ocean ridges are a function of their thermal-mechanical structure as reflected in their spreading rate.
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38

Gordienko, V. V., and L. Ya Gordienko. "P-velocity of the upper mantle." Geofizicheskiy Zhurnal 43, no. 2 (June 3, 2021): 152–65. http://dx.doi.org/10.24028/gzh.v43i2.230194.

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The authors have constructed models featuring seismic P-wave velocity distribution in the upper mantle beneath oceanic, continental and transition regions, such as mid-ocean ridges, basins, trenches, island arcs, and back-arc troughs, Atlantic transitional zones, flanking plateaus of mid-ocean ridges, platforms, geosynclines, rifts, recent activation zones. The models are in agreement with the deep-seated processes in the tectonosphere as predicted in terms of the advection-polymorphism hypothesis. The models for areas of island arcs and coastal ridges are similar to those for alpine geosynclines disturbed by recent activation. The models for areas of mid-ocean ridges and back-arc troughs are identical. They fit the pattern of recent heat-and-mass transfer in the case of rifting, which, given the basic crust with continental thickness, leads to oceanization. The model for the basin reflects the effect of thermal anomalies smoothing beneath mid-ocean ridges or back-arc troughs about 60 million years later. The model for the trench and flanking plateau reflects the result of lateral heating of the mantle’s upper layers beneath the quiescent block from the direction of the island arc and basin (trench) and mid-ocean ridge and basin (flanking plateau). A detailed bibliography on regions covered by studies was presented in the authors’ earlier publications over past eight years. There are quite significant differences between models for regions of the same type that are described in publications of other authors. This is largely due to the fact that individual authors adopt a priori concepts on the velocity structure of the upper mantle. High variability of seismic P-wave velocities within the subsurface depth interval has been detected as a result of all sufficiently detailed studies. This variability is responsible for the sharp increase in the scatter of arrival times of waves from earthquakes at small angular distances. The corresponding segments of travel-time graphs were simply ignored, and the graphs started from about 3° after which the scatter of arrival time acquired a stable character. Accordingly, velocity profiles were constructed, as a rule, starting from depths of about 50 km. The constructed velocity profiles vary little from region to region with the same type of endogenous regimes. This enables us to maintain that the models represent standard (typical) VP distributions in the mantle beneath the regions, just as presumed in terms of the theory.
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39

LEE, DAPHNE E., MURRAY R. GREGORY, CARSTEN LÜTER, OLGA N. ZEZINA, JEFFREY H. ROBINSON, and DAVID M. CHRISTIE. "Melvicalathis, a new brachiopod genus (Terebratulida: Chlidonophoridae) fromdeep sea volcanic substrates, and the biogeographic significance of the mid-oceanridge system." Zootaxa 1866, no. 1 (September 3, 2008): 136. http://dx.doi.org/10.11646/zootaxa.1866.1.6.

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Brachiopods form a small but significant component of the deep-sea benthos in all oceans. Almost half of the 40 brachiopod species so far described from depths greater than 2000 m are small, short-looped terebratulides assigned to two superfamilies, Terebratuloidea and Cancellothyridoidea. In this study we describe Melvicalathis, a new genus of cancellothyridoid brachiopod (Family Chlidonophoridae; Subfamily Eucalathinae) from ocean ridge localities in the south and southeast Pacific Ocean, and cryptic habitats within lava caves in glassy basalt dredged from the Southeast Indian Ridge, Indian Ocean. These small, punctate, strongly-ribbed, highly spiculate brachiopods occur at depths between 2009 m and 4900 m, and appear to be primary colonisers on the inhospitable volcanic rock substrate. The ecology and life-history of Melvicalathis and related deep-sea brachiopods are discussed. Brachiopods are rarely reported from the much-studied but localised hydrothermal vent faunas of the mid ocean ridge systems. They are, however, widespread members of a poorly known deep-sea benthos of attached, suspension-feeding epibionts that live along the rarely sampled basalt substrates associated with mid-ocean ridge systems. We suggest that these basalt rocks of the mid-ocean ridge system act as deep-sea “superhighways” for certain groups of deep-sea animals, including brachiopods, along which they may migrate and disperse. Although the mid-ocean ridges form the most extensive, continuous, essentially uniform habitat on Earth, their biogeographic significance may not have been fully appreciated.
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40

Ozerova, N. A., G. A. Cherkashov, S. I. Andreev, A. Yu Lein, M. P. Davydov, T. V. Stepanova, and M. A. Gruzdeva. "Mercury in Mid-Ocean ridges (on the example of Mid-Atlantic ridge and East Pacific rise)." Journal de Physique IV (Proceedings) 107 (May 2003): 1001–4. http://dx.doi.org/10.1051/jp4:20030467.

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41

Qiu, Yan, Yingmin Wang, Wenkai Huang, Weiguo Li, Haiteng Zhuo, Wenbo Du, and Chenglin Gong. "Jump event of mid-ocean ridge during the eastern subbasin evolution of the South China Sea." Interpretation 4, no. 3 (August 1, 2016): SP67—SP77. http://dx.doi.org/10.1190/int-2015-0154.1.

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The South China Sea is one of the largest marginal seas in the Western Pacific region, and it has been widely accepted that the evolution of the basin and the development of its oceanic crusts is closely linked to seafloor spreading. A great controversy, however, is around whether or not there was a jump of mid-ocean ridges during seafloor spreading, particularly in the eastern South China Sea subbasin. A tectonostratigraphic interpretation using high-resolution seismic data demonstrated that: (1) a southward jump event of the mid-ocean ridge took place in the eastern subbasin during the seafloor spreading; (2) the orientation of the mid-ocean ridge had dramatically changed after the event resulting in that the abandoned mid-ocean ridge is along an east–west direction, whereas the younger one is generally east–northeast/west–southwest oriented; (3) the corresponding surface caused by the jump tectonic event and the pre-event sequence can be traced throughout the earlier formed oceanic crust; and (4) paleo-magnetic data showed that the event occurred at approximately 25–23.8 Ma. The results of this study could be used to better understand the evolution and filling of the South China Sea and other associated marginal basins.
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42

Su, Wusi, and W. Roger Buck. "Buoyancy effects on mantle flow under Mid-Ocean Ridges." Journal of Geophysical Research: Solid Earth 98, B7 (July 10, 1993): 12191–205. http://dx.doi.org/10.1029/93jb00994.

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43

Cowie, Patience A., Christopher H. Scholz, Margo Edwards, and Alberto Malinverno. "Fault strain and seismic coupling on mid-ocean ridges." Journal of Geophysical Research: Solid Earth 98, B10 (October 10, 1993): 17911–20. http://dx.doi.org/10.1029/93jb01567.

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44

Gerya, T. "Dynamical Instability Produces Transform Faults at Mid-Ocean Ridges." Science 329, no. 5995 (August 26, 2010): 1047–50. http://dx.doi.org/10.1126/science.1191349.

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45

Collier, Martin L., and Peter B. Kelemen. "The Case for Reactive Crystallization at Mid-Ocean Ridges." Journal of Petrology 51, no. 9 (August 18, 2010): 1913–40. http://dx.doi.org/10.1093/petrology/egq043.

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46

Katz, Richard F. "Porosity-driven convection and asymmetry beneath mid-ocean ridges." Geochemistry, Geophysics, Geosystems 11, no. 11 (November 2010): n/a. http://dx.doi.org/10.1029/2010gc003282.

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47

Brandl, Philipp A., Marcel Regelous, Christoph Beier, Hugh St C. O'Neill, Oliver Nebel, and Karsten M. Haase. "The timescales of magma evolution at mid-ocean ridges." Lithos 240-243 (January 2016): 49–68. http://dx.doi.org/10.1016/j.lithos.2015.10.020.

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48

Marty, Bernard, and Igor N. Tolstikhin. "CO2 fluxes from mid-ocean ridges, arcs and plumes." Chemical Geology 145, no. 3-4 (April 1998): 233–48. http://dx.doi.org/10.1016/s0009-2541(97)00145-9.

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49

Wang, Shuya, Anzhou Cao, Xu Chen, Qiang Li, and Jinbao Song. "On the resonant triad interaction over mid-ocean ridges." Ocean Modelling 158 (February 2021): 101734. http://dx.doi.org/10.1016/j.ocemod.2020.101734.

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50

Tretkoff, Ernie. "Research Spotlight: Buoyancy explains asymmetry along mid‐ocean ridges." Eos, Transactions American Geophysical Union 92, no. 8 (February 22, 2011): 72. http://dx.doi.org/10.1029/2011eo080021.

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