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Cited by 38Cryospheric studies and observationsHigh-pressure geophysics and materialsGeological and Tectonic Studies in Latin America

Lithospheric Erosion in the Patagonian Slab Window, and Implications for Glacial Isostasy

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Mark, Hannah F., Wiens, Douglas A., Ivins, Erik R., Richter, Andreas, Ben Mansour, Walid, Magnani, M. Beatrice, Marderwald, Eric, Adaros, Rodrigo +1 more·2022·Geophysical Research Letters
DOI 10.1029/2021gl096863

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Abstract

The Patagonian slab window has been proposed to enhance the solid Earth response to ice mass load changes in the overlying Northern and Southern Patagonian Icefields (NPI and SPI, respectively). Here, we present the first regional seismic velocity model covering the entire north‐south extent of the slab window. A slow velocity anomaly in the uppermost mantle indicates warm mantle temperature, low viscosity, and possibly partial melt. Low velocities just below the Moho suggest that the lithospheric mantle has been thermally eroded over the youngest part of the slab window. The slowest part of the anomaly is north of 49°S, implying that the NPI and the northern SPI overlie lower viscosity mantle than the southern SPI. This comprehensive seismic mapping of the slab window provides key evidence supporting the previously hypothesized connection between post‐Little Ice Age anthropogenic ice mass loss and rapid geodetically observed glacial isostatic uplift (≥4 cm/yr).

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  • The asthenosphere viscosity from the models when TA > 100 °C is <10^19 Pa s, with the lowest viscosity value of 10^16 Pa s imposed where partial melting occurs.

    “the asthenosphere viscosity from our models when TA > 100 °C is < 10 19 Pa s, with the lowest viscosity value of 10 16 Pa s imposed where partial melting, supported by the regional Holocene volcanism (Stern and Kilian, 1996) and by geophysical data (e.g.shear wave velocity data by Mark et al., 2022), occurs.”

    From Fast uplift in the southern Patagonian Andes due to long- and short-term deglaciation and the asthenospheric window underneath (2024) · cites this paper as Mark et al., 2022

    Section 3.1 reports anomalously low shear-wave velocities in the Patagonian slab window, so Mark et al. provide the geophysical data cited. Section 3.2 says thermal erosion likely requires melt or fluids and that melt may be supplied by upwelling mantle; it does not establish that partial melting occurs at the specific locations where the citing authors impose their lowest viscosity. The viscosity values are attributed to the citing authors’ own models, not to Mark et al. (LLM, conf=0.84)

    Experimental — accuracy not yet measured

  • Increased asthenospheric temperatures beneath southern Patagonia are highly supported by geophysical data.

    “increased asthenospheric temperatures beneath southern Patagonia are highly supported by the geophysical data”

    From Fast uplift in the southern Patagonian Andes due to long- and short-term deglaciation and the asthenospheric window underneath (2024) · cites this paper as Mark et al., 2022

  • The thermo-mechanical visco-elastoplastic forward modelling approach helps to constrain the increase in temperature in geodynamic asthenospheric upwelling contexts, such as in southern Patagonia.

    “Our thermo-mechanical visco-elastoplastic forward modelling approach thus helps to constrain the increase in temperature in geodynamic asthenospheric upwelling contexts, such as in southern Patagonia”

    From Fast uplift in the southern Patagonian Andes due to long- and short-term deglaciation and the asthenospheric window underneath (2024) · cites this paper as Mark et al., 2022

  • Lithospheric thinning due to the asthenospheric window underneath southern Patagonia affects the regional uplift rates.

    “Lithospheric thinning due to the asthenospheric window underneath southern Patagonia thus affects the regional uplift rates as previously suggested”

    From Fast uplift in the southern Patagonian Andes due to long- and short-term deglaciation and the asthenospheric window underneath (2024) · cites this paper as Mark et al., 2022

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References 74 · Cited by 38

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  1. Agurto-Detzel, H., Rietbrock, A., Bataille, K., Miller, M., Iwamori, H., & Priestley, K. (2014). Seismicity distribution in the vicinity of the Chile Triple Junction, Aysén Region, southern Chile. Journal of South American Earth Sciences, 51, 1-11. https://doi.org/10.1016/j. jsames.2013.12.011 · DOI
  2. Barmin, M. P., Ritzwoller, M. H., & Levshin, A. L. (2001). A fast and reliable method for surface wave tomography. Pure and Applied Geophys- ics, 158(8), 1351-1375. https://doi.org/10.1007/pl00001225 · DOI
  3. Bensen, G. D., Ritzwoller, M. H., Barmin, M. P., Levshin, A. L., Lin, F., Moschetti, M. P., et al. (2007). Processing seismic ambient noise data to obtain reliable broad-band surface wave dispersion measurements. Geophysical Journal International, 169(3), 1239-1260. https://doi. org/10.1111/j.1365-246X.2007.03374.x · DOI
  4. Bianchi, I., Park, J., Piana Agostinetti, N., & Levin, V. (2010). Mapping seismic anisotropy using harmonic decomposition of receiver functions: An application to Northern Apennines, Italy. Journal of Geophysical Research, 115(B12), B12317. https://doi.org/10.1029/2009JB007061 · DOI
  5. Bourgois, J., Lagabrielle, Y., Martin, H., Dyment, J., Frutos, J., & Cisternas, M. E. (2016). A review on forearc ophiolite obduction, adakite-like generation, and slab window development at the Chile Triple Junction area: Uniformitarian framework for spreading-ridge subduction. Pure and Applied Geophysics, 173(10-11), 3217-3246. https://doi.org/10.1007/s00024-016-1317-9 · DOI
  6. Boutonnet, E., Arnaud, N., Guivel, C., Lagabrielle, Y., Scalabrino, B., & Espinoza, F. (2010). Subduction of the south Chile active spreading ridge: A 17Ma to 3Ma magmatic record in central Patagonia (western edge of Meseta del Lago Buenos Aires, Argentina). Journal of Volcan- ology and Geothermal Research, 189(3-4), 319-339. https://doi.org/10.1016/j.jvolgeores.2009.11.022 · DOI
  7. Breitsprecher, K., & Thorkelson, D. J. (2009). Neogene kinematic history of Nazca-Antarctic-Phoenix slab windows beneath Patagonia and the Antarctic Peninsula. Tectonophysics, 464(1-4), 10-20. https://doi.org/10.1016/j.tecto.2008.02.013 · DOI
  8. Cande, S. C., Leslie, R. B., Parra, J. C., & Hobart, M. (1987). Interaction between the Chile ridge and Chile trench: Geophysical and geothermal evidence. Journal of Geophysical Research, 92(B1), 495. https://doi.org/10.1029/JB092iB01p00495 · DOI
  9. Cuitiño, J. I., Varela, A. N., Ghiglione, M. C., Richiano, S., & Poiré, D. G. (2019). The Austral-Magallanes Basin (southern Patagonia): A synthe- sis of its stratigraphy and evolution. Latin American Journal of Sedimentology and Basin Analysis, 26(2), 155-166.
  10. DeLong, S. E., Schwarz, W. M., & Anderson, R. N. (1979). Thermal effects of ridge subduction. Earth and Planetary Science Letters, 44(2), 239-246. https://doi.org/10.1016/0012-821X(79)90172-9 · DOI
  11. Dickinson, W. R. (1981). Plate tectonics of the continental margin of California. In W. G. Ernst (Ed.), The geotectonic development of California (Rubey) (Vol. 1, pp. 1-28). Prentice Hall.
  12. Dietrich, R., Ivins, E. R., Casassa, G., Lange, H., Wendt, J., & Fritsche, M. (2010). Rapid crustal uplift in Patagonia due to enhanced ice loss. Earth and Planetary Science Letters, 289(1-2), 22-29. https://doi.org/10.1016/j.epsl.2009.10.021 · DOI
  13. Forsythe, R. D., Nelson, E. P., Carr, M. J., Kaeding, M. E., Herve, M., Mpodozis, C., et al. (1986). Pliocene near-trench magmatism in southern Chile: A possible manifestation of ridge collision. Geology, 14(1), 23-27. https://doi.org/10.1130/0091-7613(1986)14<23:pnmisc>2.0.co;2 · DOI
  14. Furlong, K. P., & Govers, R. (1999). Ephemeral crustal thickening at a triple junction: The Mendocino crustal conveyor. Geology, 27(2), 127-130. https://doi.org/10.1130/0091-7613(1999)027<0127:ectaat>2.3.co;2 · DOI · Paper page
  15. Gallego, A., Russo, R. M., Comte, D., Mocanu, V. I., Murdie, R. E., & Vandecar, J. C. (2010). Seismic noise tomography in the Chile ridge sub- duction region. Geophysical Journal International, 182(3), 1478-1492. https://doi.org/10.1111/j.1365-246X.2010.04691.x · DOI
  16. Georgieva, V., Melnick, D., Schildgen, T. F., Ehlers, T. A., Lagabrielle, Y., Enkelmann, E., & Strecker, M. R. (2016). Tectonic control on rock uplift, exhumation, and topography above an oceanic ridge collision: Southern Patagonian Andes (47°S), Chile: Neotectonics and Topography in Patagonia. Tectonics, 35(6), 1317-1341. https://doi.org/10.1002/2016TC004120 · DOI
  17. Gorring, M. L., Kay, S. M., Zeitler, P. K., Ramos, V. A., Rubiolo, D., Fernandez, M. I., & Panza, J. L. (1997). Neogene Patagonian plateau lavas: Continental magmas associated with ridge collision at the Chile Triple Junction. Tectonics, 16(1), 1-17. https://doi.org/10.1029/96TC03368 · DOI
  18. Groome, W. G., & Thorkelson, D. J. (2009). The three-dimensional thermo-mechanical signature of ridge subduction and slab window migration. Tectonophysics, 464(1-4), 70-83. https://doi.org/10.1016/j.tecto.2008.07.003 · DOI
  19. Guillaume, B., Martinod, J., Husson, L., Roddaz, M., & Riquelme, R. (2009). Neogene uplift of central eastern Patagonia: Dynamic response to active spreading ridge subduction? Tectonics, 28(2). https://doi.org/10.1029/2008TC002324 · DOI
  20. Guivel, C., Lagabrielle, Y., Bourgois, J., Martin, H., Arnaud, N., Fourcade, S., et al. (2003). Very shallow melting of oceanic crust during spread- ing ridge subduction: Origin of near-trench Quaternary volcanism at the Chile Triple Junction. Journal of Geophysical Research, 108(B7). https://doi.org/10.1029/2002JB002119 · DOI
  21. Helffrich, G. (2006). Extended-time multitaper frequency domain cross-correlation receiver-function estimation. Bulletin of the Seismological Society of America, 96(1), 344-347. https://doi.org/10.1785/0120050098 · DOI
  22. Hirth, G., & Kohlstedt, D. (2003). Rheology of the upper mantle and the mantle wedge: A view from the experimentalists. In J. Eiler (Ed.), Inside the subduction factory (pp. 83-105). American Geophysical Union. https://doi.org/10.1029/138GM06 · DOI
  23. Ivins, E. R., & James, T. S. (2004). Bedrock response to Llanquihue Holocene and present-day glaciation in southernmost South America. Geo- physical Research Letters, 31(24), L24613. https://doi.org/10.1029/2004GL021500 · DOI · Paper page
  24. Ivins, E. R., James, T. S., Wahr, J., Schrama, J. O., Landerer, F. W., & Simon, K. M. (2013). Antarctic contribution to sea level rise observed by GRACE with improved GIA correction. Journal of Geophysical Research: Solid Earth, 118(6), 3126-3141. https://doi.org/10.1002/jgrb.50208 · DOI
  25. Ivins, E. R., Wal van der, W., Wiens, D. A., Lloyd, A. J., & Caron, L. (2021). Antarctic upper mantle rheology. Geological Society, London, Memoirs, 56. https://doi.org/10.1144/M56-2020-19 · DOI
  26. Ivins, E. R., Watkins, M. M., Yuan, D.-N., Dietrich, R., Casassa, G., & Rülke, A. (2011). On-land ice loss and glacial isostatic adjustment at the Drake Passage: 2003-2009. Journal of Geophysical Research, 116(B2), B02403. https://doi.org/10.1029/2010JB007607 · DOI
  27. Jacob, T., Wahr, J., Pfeffer, W. T., & Swenson, S. (2012). Recent contributions of glaciers and ice caps to sea level rise. Nature, 482(7386), 514-518. https://doi.org/10.1038/nature10847 · DOI
  28. Jin, G., & Gaherty, J. B. (2015). Surface wave phase-velocity tomography based on multichannel cross-correlation. Geophysical Journal Interna- tional, 201(3), 1383-1398. https://doi.org/10.1093/gji/ggv079 · DOI
  29. Karato, S. (2008). Deformation of earth materials. An introduction to the rheology of solid Earth (p. 463). Cambridge University Press.
  30. Kennett, B. L. N., & Engdahl, E. R. (1991). Traveltimes for global earthquake location and phase identification. Geophysical Journal Internation- al, 105(2), 429-465. https://doi.org/10.1111/j.1365-246X.1991.tb06724.x · DOI
  31. Kennett, B. L. N., Engdahl, E. R., & Buland, R. (1995). Constraints on seismic velocities in the Earth from traveltimes. Geophysical Journal International, 122(1), 108-124. https://doi.org/10.1111/j.1365-246x.1995.tb03540.x · DOI
  32. Klemann, V., Ivins, E. R., Martinec, Z., & Wolf, D. (2007). Models of active glacial isostasy roofing warm subduction: Case of the South Pata- gonian Ice Field. Journal of Geophysical Research, 112(B9), B09405. https://doi.org/10.1029/2006JB004818 · DOI · Paper page
  33. Kustowski, B., Ekström, G., & Dziewoński, A. M. (2008). Anisotropic shear-wave velocity structure of the Earth's mantle: A global model. Journal of Geophysical Research, 113(B6), B06306. https://doi.org/10.1029/2007JB005169 · DOI
  34. Lange, H., Casassa, G., Ivins, E. R., Schröder, L., Fritsche, M., Richter, A., et al. (2014). Observed crustal uplift near the Southern Patagonian Icefield constrains improved viscoelastic Earth models. Geophysical Research Letters, 41(3), 805-812. https://doi.org/10.1002/2013GL058419 · DOI · Paper page
  35. Lin, F.-C., & Ritzwoller, M. H. (2011). Helmholtz surface wave tomography for isotropic and azimuthally anisotropic structure. Geophysical Journal International, 186(3), 1104-1120. https://doi.org/10.1111/j.1365-246X.2011.05070.x · DOI
  36. Lin, F.-C., Ritzwoller, M. H., & Snieder, R. (2009). Eikonal tomography: Surface wave tomography by phase front tracking across a regional broad-band seismic array. Geophysical Journal International, 177(3), 1091-1110. https://doi.org/10.1111/j.1365-246X.2009.04105.x · DOI
  37. Lin, S. (2014). Three-dimensional mantle circulations and lateral slab deformation in the southern Chilean subduction zone. Journal of Geophys- ical Research: Solid Earth, 119(4), 3879-3896. https://doi.org/10.1002/2013JB010864 . · DOI
  38. Lloyd, A. J., Wiens, D. A., Zhu, H., Tromp, J., Nyblade, A. A., Aster, R. C., et al. (2020). Seismic structure of the Antarctic upper mantle imaged with adjoint tomography. Journal of Geophysical Research: Solid Earth, 125(3), 2019JB017823. https://doi.org/10.1029/2019JB017823 · DOI
  39. Marshak, R. S., & Karig, D. E. (1977). Triple junctions as a cause for anomalously near-trench igneous activity between the trench and volcanic arc. Geology, 5(4), 233-236. https://doi.org/10.1130/0091-7613(1977)5<233:TJAACF>2.0.CO;2 · DOI
  40. McCrory, P. A., Wilson, D. S., & Stanley, R. G. (2009). Continuing evolution of the Pacific-Juan de Fuca-North America slab window sys- tem-A trench-ridge-transform example from the Pacific Rim. Tectonophysics, 464(1-4), 30-42. https://doi.org/10.1016/j.tecto.2008.01.018 · DOI
  41. Murdie, R. E., & Russo, R. M. (1999). Seismic anisotropy in the region of the Chile margin triple junction. Journal of South American Earth Sciences, 12(3), 261-270. https://doi.org/10.1016/S0895-9811(99)00018-8 · DOI
  42. Oerlemans, J. (2005). Extracting a climate signal from 169 glacier records. Science, 308(5722), 675-677. https://doi.org/10.1126/science.1107046 · DOI
  43. Park, J., & Levin, V. (2000). Receiver functions from multiple-taper spectral correlation estimates. Bulletin of the Seismological Society of Amer- ica, 90(6), 1507-1520. https://doi.org/10.1785/0119990122 · DOI
  44. Park, J., Lindberg, C. R., & Vernon, F. L. (1987). Multitaper spectral analysis of high-frequency seismograms. Journal of Geophysical Research, 92(B12), 12675-12684. https://doi.org/10.1029/JB092iB12p12675 · DOI
  45. Pedregosa, F., Varoquaux, G., Gramfort, A., Michel, V., Thirion, B., Grisel, O., et al. (2011). Scikit-learn: Machine learning in Python. Journal of Machine Learning Research, 12, 2825-2830.
  46. Radić, V., & Hock, R. (2011). Regionally differentiated contribution of mountain glaciers and ice caps to future sea-level rise. Nature Geoscience, 4(2), 91-94. https://doi.org/10.1038/ngeo1052 · DOI
  47. Ramos, V. A., & Ghiglione, M. C. (2008). Tectonic evolution of the Patagonian Andes. Developments in Quaternary Sciences, 11, 57-71. https://doi.org/10.1016/S1571-0866(07)10004-X · DOI
  48. Richter, A., Groh, A., Horwath, M., Ivins, E. R., Marderwald, E., Hormaechea, J. L., et al. (2019). The rapid and steady mass loss of the Patago- nian Icefields throughout the GRACE era: 2002-2017. Remote Sensing, 11(8), 909. https://doi.org/10.3390/rs11080909 · DOI
  49. Richter, A., Ivins, E. R., Lange, H., Mendoza, L., Schröder, L., Hormaechea, J. L., et al. (2016). Crustal deformation across the southern Patago- nian icefield observed by GNSS. Earth and Planetary Science Letters, 452, 206-215. https://doi.org/10.1016/j.epsl.2016.07.042 · DOI
  50. Robertson Maurice, S. D., Wiens, D. A., Koper, K. D., & Vera, E. (2003). Crustal and upper mantle structure of southernmost South America inferred from regional waveform inversion. Journal of Geophysical Research: Solid Earth, 108(B1). https://doi.org/10.1029/2002JB001828 · DOI
  51. Rodriguez, E. E., & Russo, R. M. (2020). Southern Chile crustal structure from teleseismic receiver functions: Responses to ridge subduction and terrane assembly of Patagonia. Geosphere, 16(1), 378-391. https://doi.org/10.1130/GES01692. · DOI
  52. Russo, R. M., Gallego, A., Comte, D., Mocanu, V. I., Murdie, R. E., & VanDecar, J. C. (2010). Source-side shear wave splitting and upper mantle flow in the Chile Ridge subduction region. Geology, 38(8), 707-710. https://doi.org/10.1130/G30920. · DOI · Paper page
  53. Russo, R. M., Luo, H., Wang, K., Ambrosius, B., Mocanu, V., He, J., et al. (2022). Lateral variation in slab window viscosity inferred from global navigation satellite system (GNSS)-observed uplift due to recent mass loss at Patagonia Ice fields. Geology, 50(1), 111-115. https:// doi.org/10.1130/G49388. · DOI
  54. Russo, R. M., VanDecar, J. C., Comte, D., Mocanu, V. I., Gallego, A., & Murdie, R. E. (2010). Subduction of the Chile Ridge: Upper mantle structure and flow. GSA Today, 20(9), 4-10. https://doi.org/10.1130/GSATG61A. · DOI
  55. Ryan, W. B. F., Carbotte, S. M., Coplan, J. O., O'Hara, S., Melkonian, A., Arko, R., et al. (2009). Global multi-resolution topography synthesis. Geochemistry, Geophysics, Geosystems, 10(3), Q03014. https://doi.org/10.1029/2008GC002332 · DOI
  56. Sandvol, E., Seber, D., Calvert, A., & Barazangi, M. (1998). Grid search modeling of receiver functions: Implications for crustal structure in the Middle East and North Africa. Journal of Geophysical Research: Solid Earth, 103(B11), 26899-26917. https://doi.org/10.1029/98JB02238 · DOI
  57. Schilling, M. E., Carlson, R. W., Tassara, A., Conceição, R. V., Bertotto, G. W., Vásquez, M., et al. (2017). The origin of Patagonia revealed by Re-Os systematics of mantle xenoliths. Precambrian Research, 294, 15-32. https://doi.org/10.1016/j.precamres.2017.03.008 · DOI
  58. Schimmel, M., & Gallart, J. (2007). Frequency-dependent phase coherence for noise suppression in seismic array data. Journal of Geophysical Research: Solid Earth, 112(B4). https://doi.org/10.1029/2006JB004680 · DOI
  59. Schimmel, M., Stutzmann, E., & Gallart, J. (2011). Using instantaneous phase coherence for signal extraction from ambient noise data at a local to a global scale: Ambient noise signal extraction. Geophysical Journal International, 184(1), 494-506. https://doi. org/10.1111/j.1365-246X.2010.04861.x · DOI
  60. Shen, W., Ritzwoller, M. H., Kang, D., Kim, Y., Lin, F.-C., Ning, J., et al. (2016). A seismic reference model for the crust and uppermost mantle beneath China from surface wave dispersion. Geophysical Journal International, 206(2), 954-979. https://doi.org/10.1093/gji/ggw175 · DOI
  61. Shen, W., Ritzwoller, M. H., Schulte-Pelkum, V., & Lin, F.-C. (2013). Joint inversion of surface wave dispersion and receiver functions: A Bayes- ian Monte-Carlo approach. Geophysical Journal International, 192(2), 807-836. https://doi.org/10.1093/gji/ggs050 · DOI
  62. Shibutani, T., Ueno, T., & Hirahara, K. (2008). Improvement in the extended-time multitaper receiver function estimation technique. Bulletin of the Seismological Society of America, 98(2), 812-816. https://doi.org/10.1785/0120070226 · DOI
  63. Stacey, F. D., & Davis, P. M. (2008). Physics of the Earth. Cambridge University Press.
  64. Stern, C. R., & Kilian, R. (1996). Role of the subducted slab, mantle wedge and continental crust in the generation of adakites from the Andean Austral Volcanic Zone. Contributions to Mineralogy and Petrology, 123(3), 263-281. https://doi.org/10.1007/s004100050155 · DOI · Paper page
  65. Thorkelson, D. J. (1996). Subduction of diverging plates and the principles of slab window formation. Tectonophysics, 255(1-2), 47-63. https:// doi.org/10.1016/0040-1951(95)00106-9 · DOI
  66. Thorkelson, D. J., & Breitsprecher, K. (2005). Partial melting of slab window margins: Genesis of adakitic and non-adakitic magmas. Lithos, 79(1-2), 25-41. https://doi.org/10.1016/j.lithos.2004.04.049 · DOI
  67. Wiens, D. A., Mansour, W. B., Mark, H. F., Shore, P., Richter, A., & Barrientos, S. (2021). Geodynamics of the Patagonian slab window con- strained by shear wave splitting and seismic imaging. Paper presented at the AGU Fall Meeting, Earth and Space Science Open Archive, New Orleans, LA and virtual. https://doi.org/10.1002/essoar.10509443. · DOI
  68. Wiens, D. A., Robertson, S., Smith, G. P., Shore, P., Vera, E., Barrientos, S., et al. (1998). Seismic experiment in Patagonia and Antarctica (SEPA). IRIS Newsletter, 17(1), 9-11.
  69. Withers, M., Aster, R., Young, C., Beiriger, J., Harris, M., Moore, S., & Trujillo, J. (1998). A comparison of select trigger algorithms for automated global seismic phase and event detection. Bulletin of the Seismological Society of America, 88(1), 12. https://doi.org/10.1785/ bssa0880010095 · DOI
  70. Wu, P., Wang, H., & Steffen, H. (2013). The role of thermal effect on mantle seismic anomalies under Laurentia and Fennoscandia from observa- tions of glacial isostatic adjustment. Geophysical Journal International, 192(1), 7-17. https://doi.org/10.1093/gji/ggs009 · DOI
  71. Zhu, L., & Kanamori, H. (2000). Moho depth variation in southern California from teleseismic receiver functions. Journal of Geophysical Re- search: Solid Earth, 105(B2), 2969-2980. https://doi.org/10.1029/ · DOI

Authors
Mark, H. F., Wiens, D. A., Ivins, E. R., Richter, A., Ben Mansour, W., Magnani, M. B., Marderwald, E., Adaros, R., & Barrientos, S.
Affiliations
  • Washington University in St. Louis (US)
  • Jet Propulsion Laboratory (US)
  • Consejo Nacional de Investigaciones Científicas y Técnicas (AR)
  • Department of Earth and Planetary Sciences Washington University in St. Louis St. Louis MO USA
  • Southern Methodist University (US)
  • Empresa Nacional del Petróleo Magallanes Chile
  • Centro Sismológico Nacional (CL)
Corresponding author
Mark, Hannah F.
ORCID
Venue
Geophysical Research Letters
Publisher
American Geophysical Union (AGU)
Published
2022-01-25
Volume
49
Issue
2
ISSN
  • 0094-8276 (ISSN-L)
  • 1944-8007
DOI
10.1029/2021gl096863
OpenAlex
W4226389690
Cited by
38
References
74
Citations by year
2026: 7 · 2025: 11 · 2024: 8 · 2023: 11 · 2022: 1
FWCI
2.96
Type
journal article
Language
en
Open access
Licence
onlinelibrary.wiley.com/termsAndConditions#vor (vor)
Locations
  • Geophysical Research Letters (publishedVersion)
  • Open Access Server of the Woods Hole Scientific Community (Woods Hole Scientific Community) (submittedVersion)
Funders
  • National Science Foundation (EAR‐1714154, EAR‐1714662)
  • Jet Propulsion Laboratory (NNH19ZDA001N‐GRACEFO)
Topics
  • Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Cryospheric studies and observations
  • Physical Sciences › Earth and Planetary Sciences › Geophysics › High-pressure geophysics and materials
  • Physical Sciences › Earth and Planetary Sciences › Geophysics › Geological and Tectonic Studies in Latin America
Keywords
glacial isostasy, glacial isostatic adjustment, Northern Patagonian Icefield, Southern Patagonian Icefield, seismic velocity model, mantle viscosity, partial melt, Little Ice Age

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Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.

Statistics and arithmetic are recomputed, not judged.

Confidence bands are shown only for fields calibrated on our annotated test set. None is calibrated yet, so no band is shown.

What counts as a claim ›How we measure confidence ›How we check this ›

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