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M.B. Underwood
M.B. Underwood
Verified email at missouri.edu
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Cited by
Year
New insights into deformation and fluid flow processes in the Nankai Trough accretionary prism: Results of Ocean Drilling Program Leg 190
GF Moore, A Taira, A Klaus, L Becker, B Boeckel, BA Cragg, A Dean, ...
Geochemistry, Geophysics, Geosystems 2 (10), 2001
2142001
Initial reports
E Davis, AT Fisher, JV Firth, EM Andersson, K Aoike, K Becker, KA Brown, ...
Proceedings of the Ocean Drilling Program 139, 1992
2031992
Origin and evolution of a splay fault in the Nankai accretionary wedge
M Strasser, GF Moore, G Kimura, Y Kitamura, AJ Kopf, S Lallemant, ...
Nature Geoscience 2 (9), 648-652, 2009
1982009
Compositional and fluid pressure controls on the state of stress on the Nankai subduction thrust: A weak plate boundary
KM Brown, A Kopf, MB Underwood, JL Weinberger
Earth and Planetary Science Letters 214 (3-4), 589-603, 2003
1902003
Sediment deformation and hydrogeology of the Nankai Trough accretionary prism: Synthesis of shipboard results of ODP Leg 131
A Taira, I Hill, J Firth, U Berner, W Brückmann, T Byrne, T Chabernaud, ...
Earth and Planetary Science Letters 109 (3-4), 431-450, 1992
1701992
Abnormal fluid pressures and fault-zone dilation in the Barbados accretionary prism: Evidence from logging while drilling
JC Moore, TH Shipley, D Goldberg, Y Ogawa, F Filice, A Fisher, ...
Geology 23 (7), 605-608, 1995
1471995
Sedimentary facies associations within subduction complexes
MB Underwood, SB Bachman
Geological Society, London, Special Publications 10 (1), 537-550, 1982
1371982
Slumping and mass transport deposition in the Nankai fore arc: Evidence from IODP drilling and 3‐D reflection seismic data
M Strasser, GF Moore, G Kimura, AJ Kopf, MB Underwood, J Guo, ...
Geochemistry, Geophysics, Geosystems 12 (5), 2011
1212011
3. Sediment Inputs to Subduction Zones
MB Underwood
The seismogenic zone of subduction thrust faults, 42-85, 2007
1142007
Diagenesis, sediment strength, and pore collapse in sediment approaching the Nankai Trough subduction zone
GA Spinelli, PS Mozley, HJ Tobin, MB Underwood, NW Hoffman, ...
Geological Society of America Bulletin 119 (3-4), 377-390, 2007
1052007
Initial report Leg 131
A Taira, I Hill, J Firth, U Berner, W Brückmann, T Byrne, T Chabernaud, ...
Proc. Ocean Drilling Program, 1991
1021991
Trenches and trench-slope basins
MB Underwood, GF Moore, CJ Busby, RV Ingersoll
Tectonics of sedimentary basins, 179-219, 1995
931995
Evaluation of factors controlling smectite transformation and fluid production in subduction zones: Application to the Nankai Trough
DM Saffer, MB Underwood, AW McKiernan
Island Arc 17 (2), 208-230, 2008
912008
Upslope flow of turbidity currents: A comparison among field observations, theory, and laboratory models
MT Muck, MB Underwood
Geology 18 (1), 54-57, 1990
891990
Sediment geochemistry, clay mineralogy, and diagenesis: a synthesis of data from Leg 131, Nankai Trough
MB Underwood
Proceedings of the Ocean Drilling Program, Scientific Results, College …, 1993
831993
Clay mineralogy of mudstones from the Nankai Trough reference Sites 1173 and 1177 and frontal accretionary prism Site 1174
JF Steurer, MB Underwood, H Mikada, GF Moore
Proc. ODP, Sci. Results 190 (196), 1-37, 2003
812003
A comparison among organic and inorganic indicators of diagenesis and low-temperature metamorphism, Tertiary Shimanto Belt, Shikoku, Japan
MB Underwood, MM Laughland, SM Kang
SPECIAL PAPERS-GEOLOGICAL SOCIETY OF AMERICA, 45-45, 1993
791993
Character of sediments entering the Costa Rica subduction zone: Implications for partitioning of water along the plate interface
GA Spinelli, MB Underwood
Island Arc 13 (3), 432-451, 2004
772004
Evolution of tectono-sedimentary systems in the Kumano Basin, Nankai Trough forearc
GF Moore, BB Boston, M Strasser, MB Underwood, RA Ratliff
Marine and Petroleum Geology 67, 604-616, 2015
752015
Hydrogeologic responses to three‐dimensional temperature variability, Costa Rica subduction margin
GA Spinelli, DM Saffer, MB Underwood
Journal of Geophysical Research: Solid Earth 111 (B4), 2006
732006
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