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1

Rondot, Jehan. "Modèles d'astroblèmes d'après le déplacement des masses rocheuses : Charlevoix et le Ries." Canadian Journal of Earth Sciences 44, no. 5 (2007): 607–17. http://dx.doi.org/10.1139/e06-115.

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One can determine the movement of rock masses in the formation of an astrobleme by ascertaining the displacements of stratigraphic reference levels before and during the impact. A discontinuity in the zone of shock metamorphism in the Charlevoix (Quebec, Canada) structure corresponds with a major fault separating an irregularly uplifted crown area from a depressed inner zone. The displacement along this circular fault is inverse to the normal displacement of the layers of this structure, that is to say, a broad collapsed area of terraces and grabens on the outside, and a gradual central build-up in the inner zone. This phenomenon can be explained as a consequence of the formation of a crater of excavation through impact, where a force of expansion tends to raise the edges of the crater, as insertion continues to the bottom of the crater. An essentially similar model for small and large craters is inferred in the first phase of formation. The readjustment that follows depends on the size of the crater and the material impacted. Started by decompression, the readjustment tends to continue until balance occurs along the fracture slip surfaces that initially formed on impact. The fractures are filled by impact fault breccias, particularly by mylolisthenites. This readjustment also depends on the speed of the meteorite at impact, as suggested by the central prominences found in the Charlevoix and the bassin form for the Ries (Germany).
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2

Doppler, Gerhard, Ulrich Haas, and Martin Herz. "Tertiary Molasse south of the Ries Crater." Jahresberichte und Mitteilungen des Oberrheinischen Geologischen Vereins 102 (April 2, 2020): 193–220. http://dx.doi.org/10.1127/jmogv/102/0010.

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3

BUCHNER, E. "An approach towards the projectile trajectory during the oblique Steinheim meteorite impact by the interpretation of structural crater features and the distribution of shatter cones." Geological Magazine 155, no. 1 (2017): 193–202. http://dx.doi.org/10.1017/s0016756817000711.

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AbstractThe distinct alignment of the Steinheim Basin and the Nördlinger Ries impact structures in SW Germany and the Central European tektite strewn field suggest ENE-directed trajectories of the Ries and Steinheim impacting bodies. From impact experiments, the asymmetry of the Steinheim crater and the arrangement of structural features therein are in good agreement with features produced during an oblique impact at 30° from the horizontal. The restriction of shatter cones to the eastern segment of the Steinheim Basin crater also suggests a west–east-directed trend of the impact direction, and supports previous models that favoured such impactor trajectory.
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4

Pösges, Gisela. "The Ries Crater Museum in Nördlingen, Bavaria, Germany." Meteoritics & Planetary Science 40, no. 9-10 (2005): 1555–57. http://dx.doi.org/10.1111/j.1945-5100.2005.tb00417.x.

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5

Arp, Gernot. "Sedimentary and chemical evolution of the Ries crater lake." Jahresberichte und Mitteilungen des Oberrheinischen Geologischen Vereins 102 (April 2, 2020): 55–94. http://dx.doi.org/10.1127/jmogv/102/0004.

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6

KÖLBL-EBERT, MARTINA. "A GENTLE GRADUALIST IN A CATASTROPHISTS’ WORLD: REINHOLD SEEMANN’S TECTONIC THEORY OF RIES IMPACT CRATER (GERMANY)." Earth Sciences History 41, no. 1 (2022): 161–85. http://dx.doi.org/10.17704/1944-6187-41.1.161.

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ABSTRACT The German geologist Reinhold Seemann (1888–1975), curator at the Wurttemberg natural history collections in Stuttgart, focussed most of his scientific work on the younger Tertiary north of the Alps. After 1936 he became especially interested in the Nordlinger Ries, an enigmatic geological structure in Southern Germany, which at that time was considered by most geologists to have originated through a volcanic catastrophe, but in the 1960s was to be reinterpreted as an impact crater. Seemann, however, adhered to a gradualist theory of Ries Basin genesis throughout his life, regarding the abundant broken and fragmented debris at Ries Basin as tectonic breccias, crushed by a hypothetical subterranean ‘wedge’ of rock slowly moving north, pushed by pressure built-up during alpine orogenesis and surfacing at the Ries area. As his correspondence with his younger colleague Helmut Holder shows, Seemann’s tectonic alternative was motivated strongly by his philosophical attitude preferring even wildly speculative and complex processes—as long as they acted gently and gradually—over any violent, catastrophic explanations however well-founded. His philosophy may have been influenced by his personal experience with two world wars, leading to his preference and campaigning for a gentle view of geological processes.
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7

Jung, Dietmar. "New drillings in the autochthonous surroundings of the Ries crater." Jahresberichte und Mitteilungen des Oberrheinischen Geologischen Vereins 103 (April 11, 2021): 177–88. http://dx.doi.org/10.1127/jmogv/103/0004.

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8

Horn, P., D. Müller-Sohnius, H. Köhler, and G. Graup. "RbSr systematics of rocks related to the Ries Crater, Germany." Earth and Planetary Science Letters 75, no. 4 (1985): 384–92. http://dx.doi.org/10.1016/0012-821x(85)90181-5.

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9

Sturm, Sebastian, Gerwin Wulf, Dietmar Jung, and Thomas Kenkmann. "The Ries impact, a double-layer rampart crater on Earth." Geology 41, no. 5 (2013): 531–34. http://dx.doi.org/10.1130/g33934.1.

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10

GRAUP, Günther. "Carbonate-silicate liquid immiscibility upon impact melting: Ries Crater, Germany." Meteoritics & Planetary Science 34, no. 3 (1999): 425–38. http://dx.doi.org/10.1111/j.1945-5100.1999.tb01351.x.

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11

Artemieva, N. A., K. Wünnemann, F. Krien, W. U. Reimold, and D. Stöffler. "Ries crater and suevite revisited-Observations and modeling Part II: Modeling." Meteoritics & Planetary Science 48, no. 4 (2013): 590–627. http://dx.doi.org/10.1111/maps.12085.

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12

Stöffler, Dieter, Natalia A. Artemieva, Kai Wünnemann, et al. "Ries crater and suevite revisited-Observations and modeling Part I: Observations." Meteoritics & Planetary Science 48, no. 4 (2013): 515–89. http://dx.doi.org/10.1111/maps.12086.

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13

Frank, Ota, Jan Jehlička, Věra Hamplová, and Aleš Svatoš. "The search for fullerenes in rocks from the Ries impact crater." Meteoritics & Planetary Science 40, no. 2 (2005): 307–14. http://dx.doi.org/10.1111/j.1945-5100.2005.tb00382.x.

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14

Leroux, Hugues. "Weathering features in shocked quartz from the Ries impact crater, Germany." Meteoritics & Planetary Science 40, no. 9-10 (2005): 1347–52. http://dx.doi.org/10.1111/j.1945-5100.2005.tb00405.x.

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15

Morlok, Andreas, Aleksandra Stojic, Isabelle Dittmar, et al. "Mid-infrared spectroscopy of impactites from the Nördlinger Ries impact crater." Icarus 264 (January 2016): 352–68. http://dx.doi.org/10.1016/j.icarus.2015.10.003.

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16

Kölbl-Ebert, Martina. "From volcano to impact crater: a history of the impact hypothesis at Ries Crater and Steinheim Basin from 1900 to 1970." Neues Jahrbuch für Geologie und Paläontologie - Monatshefte 2003, no. 10 (2003): 591–602. http://dx.doi.org/10.1127/njgpm/2003/2003/591.

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17

Markgraf, Kristina, Kurt Kroepelin, Stefan Hölzl, Dietmar Jung, and Gernot Arp. "Lacustrine clays associated with mud cracks and bituminous shales of the central Ries crater fill margin (Miocene, Nördlinger Ries)." Jahresberichte und Mitteilungen des Oberrheinischen Geologischen Vereins 102 (April 2, 2020): 313–24. http://dx.doi.org/10.1127/jmogv/102/0016.

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18

Koch, Stephan A., Stuart A. Gilder, Jean Pohl, and Claudia Trepmann. "Geomagnetic field intensity recorded after impact in the Ries meteorite crater, Germany." Geophysical Journal International 189, no. 1 (2012): 383–90. http://dx.doi.org/10.1111/j.1365-246x.2012.05399.x.

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19

Hough, R. M., I. Gilmour, C. T. Pillinger, et al. "Diamond and silicon carbide in impact melt rock from the Ries impact crater." Nature 378, no. 6552 (1995): 41–44. http://dx.doi.org/10.1038/378041a0.

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20

Vennemann, Torsten W., Andreas Morlok, Wolf von Engelhardt, and Kurt Kyser. "Stable isotope composition of impact glasses from the Nördlinger Ries impact crater, Germany." Geochimica et Cosmochimica Acta 65, no. 8 (2001): 1325–36. http://dx.doi.org/10.1016/s0016-7037(00)00600-1.

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21

Jung, Dietmar, and Kurt Kroepelin. "Geology of the eastern and northeastern Ries crater margin and the “Vorries”-zone." Jahresberichte und Mitteilungen des Oberrheinischen Geologischen Vereins 102 (April 2, 2020): 117–32. http://dx.doi.org/10.1127/jmogv/102/0006.

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22

Goresy, A. E. "An Ultradense Polymorph of Rutile with Seven-Coordinated Titanium from the Ries Crater." Science 293, no. 5534 (2001): 1467–70. http://dx.doi.org/10.1126/science.1062342.

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23

Arp, Gernot, Sebastian Schultz, Volker Karius, and James W. Head. "Ries impact crater sedimentary conglomerates: Sedimentary particle 'impact pre-processing', transport distances and provenance, and implications for Gale crater conglomerates, Mars." Icarus 321 (March 2019): 531–49. http://dx.doi.org/10.1016/j.icarus.2018.12.003.

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24

Wimmer, Karl, Günter Schweigert, Dietmar Jung, and Theo Simon. "First Description of Limestone Shatter Cones in the Middle Keuper of the Ries Crater." Jahresberichte und Mitteilungen des Oberrheinischen Geologischen Vereins 104 (May 31, 2022): 91–106. http://dx.doi.org/10.1127/jmogv/104/0002.

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25

Schwarz, Winfried H., Michael Hanel, and Mario Trieloff. "U‐Pb dating of zircons from an impact melt of the Nördlinger Ries crater." Meteoritics & Planetary Science 55, no. 2 (2020): 312–25. http://dx.doi.org/10.1111/maps.13437.

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26

Gucsik, Arnold, Tasuku Okumura, Masahiro Kayama, Hirotsugu Nishido, and Kiyotaka Ninagawa. "Planar Deformation Features in Quartz from the Ries Impact Crater: Advanced by Micro-Raman Spectroscopy." Spectroscopy Letters 44, no. 7-8 (2011): 469–73. http://dx.doi.org/10.1080/00387010.2011.610402.

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27

Jung, Dietmar, Ulrich Haas, Gerhard Doppler, and Martin Herz. "Distribution and thickness of the ejecta blanket south of the Ries crater (Miocene, South Germany)." Jahresberichte und Mitteilungen des Oberrheinischen Geologischen Vereins 102 (April 2, 2020): 267–82. http://dx.doi.org/10.1127/jmogv/102/0013.

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28

Engelhardt, W. V., J. Arndt, B. Fecker, and H. G. Pankau. "Suevite breccia from the Ries crater, Germany: Origin, cooling history and devitrification of impact glasses." Meteoritics 30, no. 3 (1995): 279–93. http://dx.doi.org/10.1111/j.1945-5100.1995.tb01126.x.

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29

Madden, Megan E. Elwood, David A. Kring, and Robert J. Bodnar. "Shock re-equilibration of fluid inclusions in crystalline basement rocks from the Ries crater, Germany." Meteoritics & Planetary Science 41, no. 2 (2006): 247–62. http://dx.doi.org/10.1111/j.1945-5100.2006.tb00208.x.

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30

MUTTIK, Nele, Kalle KIRSIMÄE, Peeter Somelar, and Gordon R. Osinski. "Post-impact alteration of surficial suevites in Ries crater, Germany: Hydrothermal modification or weathering processes?" Meteoritics & Planetary Science 43, no. 11 (2008): 1827–40. http://dx.doi.org/10.1111/j.1945-5100.2008.tb00646.x.

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31

BUCHNER, Elmar, and Martin SCHMIEDER. "Multiple fluvial reworking of impact ejecta-A case study from the Ries crater, southern Germany." Meteoritics & Planetary Science 44, no. 7 (2009): 1051–60. http://dx.doi.org/10.1111/j.1945-5100.2009.tb00787.x.

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32

Bogard, Donald, Friedrich Hörz, and Dieter Stöffler. "Loss of radiogenic argon from shocked granitic clasts in suevite deposits from the Ries Crater." Geochimica et Cosmochimica Acta 52, no. 11 (1988): 2639–49. http://dx.doi.org/10.1016/0016-7037(88)90032-4.

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33

Arp, Gernot. "Lacustrine bioherms, spring mounds, and marginal carbonates of the Ries-impact-crater (Miocene, Southern Germany)." Facies 33, no. 1 (1995): 35–89. http://dx.doi.org/10.1007/bf02537444.

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34

Buchner, Elmar, and Martin Schmieder. "Possible traces of the impactor on fracture surfaces of shattered belemnites from the Nördlinger Ries crater (Southern Germany) and potential consequences for the classification of the Ries impactor." Zeitschrift der Deutschen Gesellschaft für Geowissenschaften 168, no. 2 (2017): 245–62. http://dx.doi.org/10.1127/zdgg/2017/0090.

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35

Sturm, Sebastian, Thomas Kenkmann, Malte Willmes, Gisela Pösges, and Harald Hiesinger. "The distribution of megablocks in the Ries crater, Germany: Remote sensing, field investigation, and statistical analyses." Meteoritics & Planetary Science 50, no. 1 (2014): 141–71. http://dx.doi.org/10.1111/maps.12408.

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36

Von Engelhardt, Wolf. "Distribution, petrography and shock metamorphism of the ejecta of the Ries crater in Germany—a review." Tectonophysics 171, no. 1-4 (1990): 259–73. http://dx.doi.org/10.1016/0040-1951(90)90104-g.

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37

Meyer, C., M. Jebrak, D. Stoffler, and U. Riller. "Lateral transport of suevite inferred from 3D shape-fabric analysis: Evidence from the Ries impact crater, Germany." Geological Society of America Bulletin 123, no. 11-12 (2011): 2312–19. http://dx.doi.org/10.1130/b30393.1.

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38

Pernicka, Ernst, Peter Horn, and Jean Pohl. "Chemical record of the projectile in the graded fall-back sedimentary unit from the Ries Crater, Germany." Earth and Planetary Science Letters 86, no. 1 (1987): 113–21. http://dx.doi.org/10.1016/0012-821x(87)90194-4.

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39

Goresy, Ahmed El, Philippe Gillet, Ming Chen, Friedel Künstler, Günther Graup, and Volker Stähle. "In situ discovery of shock-induced graphite-diamond phase transition in gneisses from the Ries Crater, Germany." American Mineralogist 86, no. 5-6 (2001): 611–21. http://dx.doi.org/10.2138/am-2001-5-603.

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40

ENGELHARDT, Wolf. "Suevite breccia of the Ries impact crater, Germany: Petrography, chemistry and shock metamorphism of crystalline rock clasts." Meteoritics & Planetary Science 32, no. 4 (1997): 545–54. http://dx.doi.org/10.1111/j.1945-5100.1997.tb01299.x.

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41

Tartèse, Romain, Stanley Endley, and Katherine H. Joy. "U‐Pb dating of zircon and monazite from the uplifted Variscan crystalline basement of the Ries impact crater." Meteoritics & Planetary Science 57, no. 4 (2022): 830–49. http://dx.doi.org/10.1111/maps.13798.

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42

Newsom, Horton E., Günther Graup, Terry Sewards, and Klaus Keil. "Fluidization and hydrothermal alteration of the Suevite deposit at the Ries Crater, West Germany, and implications for Mars." Journal of Geophysical Research 91, B13 (1986): E239. http://dx.doi.org/10.1029/jb091ib13p0e239.

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43

Jung, Dietmar, and Kurt Kroepelin. "Thrust faulting and block rotation at the eastern Ries crater margin – Geological investigations at the Eireiner quarry (Wemding)." Jahresberichte und Mitteilungen des Oberrheinischen Geologischen Vereins 102 (April 2, 2020): 283–92. http://dx.doi.org/10.1127/jmogv/102/0014.

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44

St�hle, Volker, Rainer Altherr, Mario Koch, and Lutz Nasdala. "Shock-induced formation of kyanite (Al2SiO5) from sillimanite within a dense metamorphic rock from the Ries crater (Germany)." Contributions to Mineralogy and Petrology 148, no. 2 (2004): 150–59. http://dx.doi.org/10.1007/s00410-004-0599-6.

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45

Muttik, Nele, Kalle Kirsimäe, and Torsten W. Vennemann. "Stable isotope composition of smectite in suevites at the Ries crater, Germany: Implications for hydrous alteration of impactites." Earth and Planetary Science Letters 299, no. 1-2 (2010): 190–95. http://dx.doi.org/10.1016/j.epsl.2010.08.034.

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46

Stüeken, Eva E., Christopher Tino, Gernot Arp, Dietmar Jung, and Timothy W. Lyons. "Nitrogen isotope ratios trace high-pH conditions in a terrestrial Mars analog site." Science Advances 6, no. 9 (2020): eaay3440. http://dx.doi.org/10.1126/sciadv.aay3440.

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High-pH alkaline lakes are among the most productive ecosystems on Earth and prime targets in the search for life on Mars; however, a robust proxy for such settings does not yet exist. Nitrogen isotope fractionation resulting from NH3 volatilization at high pH has the potential to fill this gap. To validate this idea, we analyzed samples from the Nördlinger Ries, a Miocene impact crater lake that displayed pH values up to 9.8 as inferred from mineralogy and aqueous modeling. Our data show a peak in δ15N of +17‰ in the most alkaline facies, followed by a gradual decline to around +5‰, concurrent with the proposed decline in pH, highlighting the utility of nitrogen isotopes as a proxy for high-pH conditions. In combination with independent mineralogical indicators for high alkalinity, nitrogen isotopes can provide much-needed quantitative constraints on ancient atmospheric Pco2 (partial pressure of CO2) and thus climatic controls on early Earth and Mars.
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47

Montano, Damaris, Marta Gasparrini, Axel Gerdes, Giovanna Della Porta, and Richard Albert. "In-situ U-Pb dating of Ries Crater lacustrine carbonates (Miocene, South-West Germany): Implications for continental carbonate chronostratigraphy." Earth and Planetary Science Letters 568 (August 2021): 117011. http://dx.doi.org/10.1016/j.epsl.2021.117011.

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48

Hofmann, P., D. Leythaeuser, and L. Schwark. "Organic matter from the Bunte Breccia of the Ries Crater, southern Germany: investigating possible thermal effects of the impact." Planetary and Space Science 49, no. 8 (2001): 845–51. http://dx.doi.org/10.1016/s0032-0633(01)00034-4.

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49

Heap, Michael J., H. Albert Gilg, Paul K. Byrne, Fabian B. Wadsworth, and Thierry Reuschlé. "Petrophysical properties, mechanical behaviour, and failure modes of impact melt-bearing breccia (suevite) from the Ries impact crater (Germany)." Icarus 349 (October 2020): 113873. http://dx.doi.org/10.1016/j.icarus.2020.113873.

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50

Arp, Gernot, Andreas Reimer, Klaus Simon, et al. "The Erbisberg drilling 2011: Implications for the structure and postimpact evolution of the inner ring of the Ries impact crater." Meteoritics & Planetary Science 54, no. 10 (2019): 2448–82. http://dx.doi.org/10.1111/maps.13293.

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