SUBGLACIAL TILL - A PHYSICAL FRAMEWORK FOR ITS PROPERTIES AND PROCESSES

[1] DEFORMATION OF TILL BENEATH ICE STREAM-B, WEST ANTARCTICA [J]. NATURE, 1986, 322 (6074) : 57 - 59

[2] Andrade E. da C, 1949, P PHYS SOC LOND B, V62, P483, DOI [10.1088/0370-1301/62/8/303, DOI 10.1088/0370-1301/62/8/303]

[3] ATKINSON JH, 1978, MECHANICS SOILS INTR

[4] Bear J, 1972, DYNAMICS FLUIDS PORO

[5] CONTINUUM THEORY OF FLUID SATURATED POROUS MEDIA [J]. JOURNAL OF APPLIED MECHANICS, 1971, 38 (01): : 1 - &

[6] General theory of three-dimensional consolidation [J]. JOURNAL OF APPLIED PHYSICS, 1941, 12 (02) : 155 - 164

[7] SEISMIC MEASUREMENTS REVEAL A SATURATED POROUS LAYER BENEATH AN ACTIVE ANTARCTIC ICE STREAM [J]. NATURE, 1986, 322 (6074) : 54 - 57

[8] Boulton, 1979, J GLACIOL, V23, P15, DOI 10.3189/S0022143000029713

[9] Boulton G. S., 1979, J GLACIOL, V24, P29, DOI DOI 10.3198/1979J0G24-90-29-43

[10] Boulton G.S., 1974, GEOGR ANN A, V56, P121, DOI [DOI 10.2307/520702, 10.1080/04353676.1974.11879894]

[1] DEFORMATION OF TILL BENEATH ICE STREAM-B, WEST ANTARCTICA [J]. NATURE, 1986, 322 (6074) : 57 - 59

[2] Andrade E. da C, 1949, P PHYS SOC LOND B, V62, P483, DOI [10.1088/0370-1301/62/8/303, DOI 10.1088/0370-1301/62/8/303]

[3] ATKINSON JH, 1978, MECHANICS SOILS INTR

[4] Bear J, 1972, DYNAMICS FLUIDS PORO

[5] CONTINUUM THEORY OF FLUID SATURATED POROUS MEDIA [J]. JOURNAL OF APPLIED MECHANICS, 1971, 38 (01): : 1 - &

[6] General theory of three-dimensional consolidation [J]. JOURNAL OF APPLIED PHYSICS, 1941, 12 (02) : 155 - 164

[7] SEISMIC MEASUREMENTS REVEAL A SATURATED POROUS LAYER BENEATH AN ACTIVE ANTARCTIC ICE STREAM [J]. NATURE, 1986, 322 (6074) : 54 - 57

[8] Boulton, 1979, J GLACIOL, V23, P15, DOI 10.3189/S0022143000029713

[9] Boulton G. S., 1979, J GLACIOL, V24, P29, DOI DOI 10.3198/1979J0G24-90-29-43

[10] Boulton G.S., 1974, GEOGR ANN A, V56, P121, DOI [DOI 10.2307/520702, 10.1080/04353676.1974.11879894]