Magnitude and duration of surface uplift above the Socorro magma body

Geology

Volumn 37, Issue 3, 2009, Pages 231-234

  Finnegan, Noah J ^a,b   Pritchard, Matthew E ^a  

^a Institute for the Study of the Continents   (United States)

^b UNIVERSITY OF CALIFORNIA   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

INTERFEROMETRIC SYNTHETIC APERTURE RADARS; MAGMA BODIES; NEW MEXICO; PLEISTOCENE; RIO GRANDE;

GEODETIC SATELLITES; IMAGING SYSTEMS; SOIL CONSERVATION; SYNTHETIC APERTURE RADAR;

SYNTHETIC APERTURES;

MAGMA; PLEISTOCENE; SUBSIDENCE; SYNTHETIC APERTURE RADAR; TECTONIC STRUCTURE; UPLIFT;

NEW MEXICO; NORTH AMERICA; SOCORRO [NEW MEXICO]; UNITED STATES;

CAPSICUM PUBESCENS;

EID: 69649087109     PISSN: 00917613     EISSN: 00917613     Source Type: Journal    
DOI: 10.1130/G25132A.1     Document Type: Article

References (17)

1. Ake, J.P., and Sanford, A.R., 1988, New evidence for the existence and internal structure of a thin layer of magma at mid-crustal depths near Socorro, New Mexico: Seismological Society of America Bulletin, v. 78, p. 1335-1359.
2. Bachman, G.O., and Mehnert, H.H., 1978, New K-Ar dates and the late Pliocene to Holocene geomorphic history of the central Rio Grande region, New Mexico: Geological Society of America Bulletin, v. 89, p. 283-292, doi: 10.1130/0016-7606 (1978)89<283:NKDATL>2.0.CO;2.
3. Balch, R.S., Hartse, H.E., Sanford, A.R., and Lin, K., 1997, A new map of the geographic extent of the Socorro magma body: Seismological Society of America Bulletin, v. 87, p. 174-182.
4. Connell, S.D., Love, D.W., Maldonado, F., Jackson, P.B., McIntosh, W.C., and Eppes, M.C., 2000, Is the top of the Santa Fe Group diachronous in the Albuquerque Basin? [abs.], in Cole, J.C., ed., U.S. Geological Survey Middle Rio Grande Basin Study - Proceedings of the Fourth Annual Workshop, Albuquerque, New Mexico, February 15-16, 2000: U.S. Geological Survey Open-File Report 00-488.
5. Connell, S.D., Love, D.W., and Dunbar, N.W., 2007, Geomorphology and stratigraphy of inset fluvial deposits along the Rio Grande valley in the central Albuquerque basin, New Mexico: New Mexico Geology, v. 29, p. 13-31.
6. Ferguson, R.I., Cudden, J.R., Hoey, T.B., and Rice, S.P., 2006, River system discontinuities due to lateral inputs: Generic styles and controls: Earth Surface Processes and Landforms, v. 31, p. 1149-1166, doi: 10.1002/esp.1309.
7. Fialko, Y., and Simons, M., 2001, Evidence for on-going inflation of the Socorro magma body, New Mexico, from interferometric synthetic aperture radar imaging: Geophysical Research Letters, v. 28, p. 3549-3552, doi: 10.1029/2001GL013318.
8. Fialko, Y., Khazan, Y., and Simons, M., 2001, Deforma tion due to a pressurized horizontal circular crack in an elastic half-space, with applications to volcano geodesy: Geophysical Journal International, v. 146, p. 181-190, doi: 10.1046/j.1365-246X.2001.00452.x.
9. Gellis, A.C., Pavich, M.J., Bierman, P.R., Clapp, E.M., Ellevein, A., and Aby, S., 2004, Modern sediment yield compared to geologic rates of sediment production in a semi-arid basin, New Mexico: Assessing the human impact: Earth Surface Processes and Landforms, v. 29, p. 1359-1372.
10. Happ, S.C., 1948, Sedimentation in the middle Rio Grande Valley, New Mexico: Geological Society of America Bulletin, v. 59, p. 1191-1216, doi: 10.1130/0016-7606(1948)59[1191:SITMRG] 2.0.CO;2.
11. Larsen, S.R., Reilinger, R., and Brown, L., 1986, Evidence of ongoing crustal deformation related to magmatic activity near Socorro, New Mexico: Journal of Geophysical Research, v. 91, p. 6283-6293, doi: 10.1029/JB091iB06p06283.
12. Mackin, J.H., 1948, Concept of the graded river: Geological Society of America Bulletin, v. 59, p. 463-512, doi: 10.1130/0016-7606(1948)59 [463:COTGR]2.0.CO;2.
13. Ouchi, S., 1985, Response of alluvial rivers to slow active tectonic movement: Geological Society of America Bulletin, v. 96, p. 504-515, doi: 10.1130/0016-7606(1985)96<504:ROARTS> 2.0.CO;2.
14. Pierce, K.L., Cannon, K.P., Meyer, G.A., Trehesch, M.J., and Watts, R.D., 2002, Post-glacial infl ation-deflation cycles, tilting, and faulting in the Yellowstone Caldera based on Yellowstone Lake shorelines: U.S. Geological Survey Open-File Report 02-0142.
15. Sanford, A.R., Mott, R.P., Shuleski, P.J., Rinehart, E.J., Caravella, F.J., Ward, R.M., and Wallace, T.C., 1977, Geophysical evidence for a magma body in the vicinity of Socorro, New Mexico, in Heacock, J.G., ed., The Earth's crust: Its nature and physical properties: American Geophysical Union Geophysical Monograph 20, p. 385-404.
16. Smith, R.L., and Bailey, R.A., 1966, The Bandelier Tuff: A study of ash-flow eruption cycles from zoned magma chambers: Bulletin of Volcanology, v. 29, p. 8031-8051.
17. U.S. Geological Survey and New Mexico Bureau of Mines and Mineral Resources, 2006, Quaternary fault and fold database for the United States: http//earthquake.usgs.gov/regional/qfaults/(February 2008).