Nested-scale investigation of tectonic windows into super-fast spread crust exposed at the Pito Deep Rift. InterRidge Newsletter. 2005;14:5-8.
Chemistry of Deep (3500-5600m) Pacific MORB- Why is the Pacific anomalous? Geophysical Research Letters. 1995;22:3067-70.
Tectonics of an incipient oceanic rift. Marine Geophysical Researches. 1988;9:147-63.
Geological mapping of the East Pacific Rise axis (10 [degrees] 19' -11 [degrees] 53'N) using the Argo and Angus imaging systems. Canadian Mineralogist. 1988;26:467-86.
Offset spreading centers near 12 [degrees] 53 N on East Pacific Rise: Submersible observations and composition of the volcanics. Marine Geophysical Researches. 1985;7:359-77.
Submersible observations at the axis of the ultra-fast-spreading East Pacific Rise (17-30 to 21-30 S). Earth and Planetary Science Letters. 1985;75:339-53.
Geological setting of hydrothermal activity at 12 [degrees] 50'N on the East Pacific Rise; A submersible study. Earth and Planetary Science Letters. 1984;69:176-86.
Geological processes of the mid-ocean ridge and their relationship to sulfide deposition. In: Rona PA, Bostroem K, Laubier L, Smith KL, editors. Hydrothermal processes at seafloor spreading centers. New York, N.Y.: Plenum Press; 1983. p. 47-62. (NATO conference series. IV, Marine sciences).
Intense hydrothermal activity at the axis of the East Pacific Pise near 13 [degrees] N: Submersible witnesses the growth of sulfide chimney. Marine Geophysical Researches. 1983;6:1-14.
The East Pacific Rise near 21 [degrees] N, 13 [degrees] N and 20 [degrees] S: Inferences for along-strike variability of axial processes of the Mid-Ocean Ridge. Earth and Planetary Science Letters. 1983;64:93-116.