DEFORMATIONAL MODELS OF RIFTING AND FOLDING ON VENUS

[11] FORMATION OF SEDIMENTARY BASINS OF GRABEN TYPE BY EXTENSION OF CONTINENTAL CRUST [J]. TECTONOPHYSICS, 1976, 36 (1-3) : 77 - 86

[12] MECHANISM OF GRABEN FORMATION - THE WEDGE SUBSIDENCE HYPOTHESIS [J]. TECTONOPHYSICS, 1983, 94 (1-4) : 11 - 22

[13] LIMITS ON LITHOSPHERIC STRESS IMPOSED BY LABORATORY EXPERIMENTS [J]. JOURNAL OF GEOPHYSICAL RESEARCH, 1980, 85 (NB11): : 6248 - 6252

[14] FRICTION OF ROCKS [J]. PURE AND APPLIED GEOPHYSICS, 1978, 116 (4-5) : 615 - 626

[15] VENUS - VOLCANISM AND RIFT FORMATION IN BETA REGIO [J]. SCIENCE, 1984, 226 (4671) : 167 - 170

[16] VENUS - FURTHER EVIDENCE OF IMPACT CRATERING AND TECTONIC ACTIVITY FROM RADAR OBSERVATIONS [J]. SCIENCE, 1979, 204 (4400) : 1424 - 1427

[17] CAMPBELL DB, 1983, SCIENCE, V221, P664

[18] THE TRANSITION FROM HIGH-TEMPERATURE CREEP TO FRACTURE IN MARYLAND DIABASE [J]. JOURNAL OF GEOPHYSICAL RESEARCH, 1982, 87 (NB8): : 6781 - 6790

[19] CRUMPLER LS, 1986, GEOLOGY, V14, P1031, DOI 10.1130/0091-7613(1986)14<1031:OBOV>2.0.CO

[20] 2

[11] FORMATION OF SEDIMENTARY BASINS OF GRABEN TYPE BY EXTENSION OF CONTINENTAL CRUST [J]. TECTONOPHYSICS, 1976, 36 (1-3) : 77 - 86

[12] MECHANISM OF GRABEN FORMATION - THE WEDGE SUBSIDENCE HYPOTHESIS [J]. TECTONOPHYSICS, 1983, 94 (1-4) : 11 - 22

[13] LIMITS ON LITHOSPHERIC STRESS IMPOSED BY LABORATORY EXPERIMENTS [J]. JOURNAL OF GEOPHYSICAL RESEARCH, 1980, 85 (NB11): : 6248 - 6252

[14] FRICTION OF ROCKS [J]. PURE AND APPLIED GEOPHYSICS, 1978, 116 (4-5) : 615 - 626

[15] VENUS - VOLCANISM AND RIFT FORMATION IN BETA REGIO [J]. SCIENCE, 1984, 226 (4671) : 167 - 170

[16] VENUS - FURTHER EVIDENCE OF IMPACT CRATERING AND TECTONIC ACTIVITY FROM RADAR OBSERVATIONS [J]. SCIENCE, 1979, 204 (4400) : 1424 - 1427

[17] CAMPBELL DB, 1983, SCIENCE, V221, P664

[18] THE TRANSITION FROM HIGH-TEMPERATURE CREEP TO FRACTURE IN MARYLAND DIABASE [J]. JOURNAL OF GEOPHYSICAL RESEARCH, 1982, 87 (NB8): : 6781 - 6790

[19] CRUMPLER LS, 1986, GEOLOGY, V14, P1031, DOI 10.1130/0091-7613(1986)14<1031:OBOV>2.0.CO

[20] 2