Past and Future Evolution of Marine Geology
Helpful to educators and students.
Emery, K.O. and D.A. Ross
SEPM Special Volume, pp. 11-14, 1991 WHOI-R-91-006
An attempt is made to understand some of the ways that marine geology developed during the past 50 years, essentially the working lifespan of an active but venerable scientist. This interpretation is aided by comparing marine geology with the development of land geology during a longer period, and by attempting to understand the relative roles of science and technology in the field of marine geology. Excursions from simple straight-line advance for all geology (and also for other fields) are provided by the unexpected appearances of broad generalizations, or paradigms, that commonly are developed by a few scientists and opposed by many, at least for a time. These sudden advances await the accumulation of critical masses of knowledge that, in turn, depend upon exceptional opportunities, partly in the form of adequate funding and partly by transfer of technology. These unusual circumstances make accurate prediction of future advances in marine geology (and in other scientific and technical fields) unreliable but still worthy of thought.
Diffuse Flow from Hydrothermal Vents
Only available on loan from the National Sea Grant Library
Trivett, D.A.
Ph.D. Thesis, Massachusetts Institute of Technology/Woods Hole Oceanographic Institution Joint Program Dissertation for Sc. D. in Ocean Engineering, 216 pp., 1991 WHOI-X-91-001
The effluent from a collection of diffuse hydrothermal vents was modelled to determine the fate of this source of flow under typical environmental conditions at seafloor spreading centers. A laboratory simulation was conducted to test an analytic model of diffuse plume rise. The results showed that diffuse plumes are likely to remain near the seafloor, with their maximum rise height scaled with the diameter of the source of diffuse flow. The entrainment of ambient seawater into these plumes is limited by the proximity to the seafloor, thus slowing the rate of dilution. The model of diffuse plume behaviour was used to guide the design and implementation of a scheme for monitoring the flow from diffuse hydrothermal vents in the ocean. A deployment of an array at the Southern Juan de Fuca Ridge yielded measurements of a variety of diffuse plume properties, including total heat output.
The Sound Field Near Hydrothermal Vents on Axial Seamount, Juan De Fuca Ridge
Little, S.A., K.D. Stolzenbach, and G.M. Purdy
Journal of Geophysical Research, Vol. 95, No. B8, pp. 12927-12945, 1990 WHOI-R-90-009
The Geologic Enigma of the Red Sea Rift
Uchupi, E. and D.A. Ross
In: Ittekkot, V., S. Kempe, and W. Michaelis (eds.), Facets of Modern Biogeochemistry, Springer Verlag, pp. 52-61, 1990 WHOI-R-90-011
Tectonic Development of the Western Branch of the East African Rift System
Ebinger, C.J.
Geological Society of America Bulletin, Vol. 1, pp. 885-903, 1989 WHOI-R-89-009
Geometric and Kinematic Development of Border Faults and Accommodation Zones, Kivu-rusizi Rift, Africa
Ebinger, C.J.
Tectonics, Vol. 8, No. 1, pp. 117-133, 1989 WHOI-R-89-005
Chronology of Volcanism and Rift Basin Propagation: Rungwe Volcanic Province, East Africa
Ebinger, C.J., A. Deino, R. Drake, and A. Tesha
Journal of Geophysical Research, Vol. 94, pp. 15785-15803, 1989 WHOI-R-89-022
Thermal and Mechanical Development of the East African Rift System
Only available on loan from the National Sea Grant Library
Ebinger, C.J.
Ph.D. Thesis, Massachusetts Institute of Technology/Woods Hole Oceanographic Institution Joint Program in Oceanography and Oceanographic Engineering, 180 pp., 1988 WHOI-X-88-002
Fluid Flow and Sound Generation at Hydrothermal Vent Fields
Only available on loan from the National Sea Grant Library
Little, S.A.
Ph.D. Thesis, Massachusetts Institute of Technology/Woods Hole Oceanographic Institution Joint Program in Oceanography and Oceanographic Engineering, 152 pp., 1988 WHOI-X-88-001
Several experiments are presented in this thesis which examine methods to measure and monitor fluid flow from hydrothermal vent fields. Simultaneous velocity, temperature, and conductivity data were collected in the convective flow emanating from a hydrothermal vent field located on the East Pacific rise. The horizontal profiles obtained indicate that the flow field approaches an ideal plume in the temperature and velocity distribution. Such parameters as total heat flow and maximum plume height can be estimated using either the velocity or the temperature information. The results of these independent calculations are in close agreement. The nonlinear effects of large temperature variations on heat capacity and volume changes slightly alter the calculations applied to obtain these values.
Post-miocene Rifting and Diapirism in the Northern Red Sea
Mart, Y. and D.A. Ross
Marine Geology, Vol. 74, pp. 173-190, 1987 WHOI-R-87-003
The Geology of the Persian Gulf: Gulf of Oman Region: A Synthesis
Ross, D.A., E. Uchupi, and R.S. White
Review of Geophysics, Vol. 24, No. 3, pp. 537-556, 1986 WHOI-R-86-003
The Tectonic Style of the Northern Red Sea
Uchupi, E. and D.A. Ross
Geo-Marine Letters, Vol. 5, pp. 203-209, 1986 WHOI-R-86-015
Multichannel seismic reflection profiles recorded in the northern Red Sea show structures that are interpreted to be the result of the intrusion of uppermost Miocene salt. The authors believe that the evaporites are underlaid by attenuated continental crust and the flow of salt is due to renewed faulting of basement in the Pliocene when sea floor spreading began between latitudes 21:N and 15:30'N.
Continental-oceanic Crustal Transition off Southwest Africa
Austin, J.A. and E. Uchupi
The American Association of Petroleum Geologists Bulletin, Vol. 66, No. 9, pp. 1328-1347, 1982 WHOI-R-82-027
Salt Diapirism and Associated Faulting Beneath the Eastern End of Georges Bank
Uchupi, E., J.A. Austin Jr., and D.H. Gever
Northeastern Geology, Vol. 4, No. 1, pp. 20-22, 1982 WHOI-R-82-006
Mesozoic-cenozoic Regressions and the Development of the Margin off Northeastern North America
Uchupi, E., J.P. Ellis, J.A. Austin Jr., G.H. Keller, and R.D. Ballard In: Scrutton, R.A. and M. Taiwani (eds.), The Ocean Floor, John Wiley & Sons, Ltd., Chichester, pp. 81-95, 1982 WHOI-R-82-023
Mesozoic Lithofacies Development and Economic Potential of the Georges Bank Basin off Southern New England
Austin, J.A. and E. Uchupi
Northeastern Geology, Vol. 2, No. 2, pp. 55-61, 1980 WHOI-R-80-016
Geology of New England Passive Margin
Austin, J.A., E. Uchupi, D.R. Shaughnessy, and R.D. Ballard
The American Association of Petroleum Geologists Bulletin, Vol. 64, No. 4, pp. 501-526, 1980 WHOI-R-80-009
The Use of the Coastal Oceans in the 80's: Opportunities for Marine Geology
Only available on loan from the National Sea Grant Library
Ross, D.A. and D.G. Aubrey
Woods Hole Oceanographic Institution Technical Report WHOI-80-19, 63 pp., 1980 WHOI-T-80-004
Continental Margin Subsidence and Heat Flow: Important Parameters in Formation of Petroleum Hydrocarbons
Royden, L., J.G. Sclater, and R.P. Von Herzen
The American Association of Petroleum Geologists Bulletin, Vol. 64, No. 2, pp. 173-187, 1980 WHOI-R-80-007
Geology of the Passive Margin off New England
Only available on loan from the National Sea Grant Library
Austin, J.A.
1979 WHOI-Y1-79-002
Particulate Calcium Carbonate in New England Shelf Waters: Result of Shell Degradation and Resuspension
Only available on loan from the National Sea Grant Library
Fitzgerald, M.G., C.M. Parmenter, and J.D. Milliman
1979 WHOI-R-79-018
The Geologic History of the Passive Margin off New England and the Canadian Maritime Provinces
Uchupi, E. and J.A. Austin Jr.
1979 WHOI-R-79-007
Last updated: January 9, 2013 | 
