Active and relict sea-floor hydrothermal mineralization at the TAG hydrothermal field, Mid-Atlantic Ridge
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C. V. Raman | M. Hannington | S. Petersen | S. Humphris | M. Tivey | P. Rona | C. Lalou | G. Thompson
[1] M. Hannington,et al. Gold-rich polymetallic sulfides from the Lau back arc and implications for the geochemistry of gold in sea-floor hydrothermal systems of the Southwest Pacific , 1993 .
[2] P. Gente,et al. Tectonic setting and mineralogical and geochemical zonation in the Snake Pit sulfide deposit (Mid-Atlantic Ridge at 23 degrees N) , 1993 .
[3] M. Hannington,et al. Relict hydrothermal zones in the TAG Hydrothermal Field, Mid‐Atlantic Ridge 26°N, 45°W , 1993 .
[4] H. Elderfield,et al. A dual origin for the hydrothermal component in a metalliferous sediment core from the Mid-Atlantic Ridge , 1993 .
[5] Y. Fouquet,et al. New age data for Mid‐Atlantic Ridge hydrothermal sites: TAG and Snakepit chronology revisited , 1993 .
[6] M. Tivey,et al. Reduced crustal magnetization beneath the active sulfide mound, TAG hydrothermal field, Mid-Atlantic Ridge at 26°N , 1993 .
[7] M. Tivey,et al. Magnetic modeling near selected areas of hydrothermal activity on the Mid‐Atlantic and Gorda Ridges , 1992 .
[8] M. D. Rudnicki,et al. Theory applied to the Mid-Atlantic ridge hydrothermal plumes: the finite-difference approach , 1992 .
[9] P. Rona,et al. Discrete and diffuse heat transfer atashes vent field, Axial Volcano, Juan de Fuca Ridge , 1992 .
[10] S. Solomon,et al. Microearthquake Characteristics of a Mid‐Ocean Ridge along‐axis high , 1992 .
[11] M. Hannington,et al. Comparative mineralogy and geochemistry of gold-bearing sulfide deposits on the mid-ocean ridges , 1991 .
[12] Evan B. Forde,et al. The structure, mass and interactions of the hydrothermal plumes at 26°N on the Mid-Atlantic Ridge , 1991 .
[13] J. Karson,et al. Block-tilting, transfer faults, and structural control of magmatic and hydrothermal processesin the TAG area, Mid-Atlantic Ridge 26°N , 1990 .
[14] J. Sempere,et al. Bathymetry of the mid-atlantic ridge, 24°-31°N: A map series , 1990 .
[15] P. Rona,et al. Magnetic properties and opaque mineralogy of rocks from selected seafloor hydrothermal sites at oceanic ridges , 1990 .
[16] J. Sempere,et al. Evidence from gravity data for focused magmatic accretion along the Mid-Atlantic Ridge , 1990, Nature.
[17] P. Rona,et al. Geochronology of TAG and Snakepit hydrothermal fields, Mid-Atlantic Ridge: witness to a long and complex hydrothermal history , 1990 .
[18] L. Zonenshain,et al. Tectonics of the Mid-Atlantic rift valley between the TAG and MARK areas (26 24°N): Evidence for vertical tectonism , 1989 .
[19] A. C. Campbell,et al. Chemistry of hot springs on the Mid-Atlantic Ridge , 1988, Nature.
[20] D. Forsyth,et al. Gravity anomalies of the ridge-transform system in the South Atlantic between 31 and 34.5° S: Upwelling centers and variations in crustal thickness , 1988 .
[21] M. Tivey,et al. Submersible investigation of an extinct hydrothermal system on the Galapagos Ridge; sulfide mounds, stockwork zone, and differentiated lavas , 1988 .
[22] S. Humphris,et al. Active vents and massive sulfides at 26 degrees N (TAG) and 23 degrees N (Snakepit) on the Mid-Atlantic Ridge , 1988 .
[23] P. Rona,et al. Geologic controls of hydrothermal activity in the Mid-Atlantic Ridge rift valley: Tectonics and volcanics , 1988 .
[24] M. Hannington,et al. Gold and native copper in supergene sulphides from the Mid-Atlantic Ridge , 1988, Nature.
[25] Richard A. Feely,et al. Composition and dissolution of black smoker particulates from active vents on the Juan de Fuca Ridge , 1987 .
[26] K. Stolzenbach,et al. Measurements of plume flow from a hydrothermal vent field , 1987 .
[27] M. Hannington,et al. Gold in sea-floor polymetallic sulfide deposits , 1986 .
[28] P. Rona,et al. Manganese geochemistry near high-temperature vents in the Mid-Atlantic Ridge rift valley , 1986 .
[29] P. Rona,et al. Chronology of selected hydrothermal Mn oxide deposits from the transatlantic geotraverse , 1986 .
[30] P. Rona,et al. Black smokers, massive sulphides and vent biota at the Mid-Atlantic Ridge , 1986, Nature.
[31] M. Mottl,et al. Geologic form and setting of a hydrothermal vent field at lat 10°56′N, East Pacific Rise: A detailed study using Angus and Alvin , 1986 .
[32] J. Cann,et al. A simple magma-driven thermal balance model for the formation of volcanogenic massive sulphides , 1985 .
[33] R. Lowell,et al. Hydrothermal models for the generation of massive sulfide ore deposits , 1985 .
[34] H. Schouten,et al. Segmentation of mid-ocean ridges , 1985, Nature.
[35] M. Mottl,et al. Morphology, mineralogy and chemistry of hydrothermal deposits from the TAG area, 26°N Mid-Atlantic Ridge☆ , 1985 .
[36] P. Rona,et al. Hydrothermal manganese plumes in the Mid-Atlantic Ridge rift valley , 1985, Nature.
[37] M. Mottl,et al. Hydrothermal activity at the Trans‐Atlantic Geotraverse Hydrothermal Field, Mid‐Atlantic Ridge crest at 26°N , 1984 .
[38] T. McDougall,et al. A note on fluid dynamic processes which can influence the deposition of massive sulfides , 1984 .
[39] J. Edmond,et al. Flow rates in the axial hot springs of the East Pacific Rise (21°N): Implications for the heat budget and the formation of massive sulfide deposits , 1984 .
[40] Robert D. Ballard,et al. The East Pacific Rise near 21°N, 13°N and 20°S: inferences for along-strike variability of axial processes of the Mid-Ocean Ridge , 1983 .
[41] P. Rona,et al. Geochemistry of sediments from the TAG Hydrothermal Field, M.A.R. at latitude 26° N , 1983 .
[42] L. Merlivat,et al. East Pacific Rise Near 13�N: Geology of New Hydrothermal Fields , 1983, Science.
[43] P. Rona,et al. Structural behavior of fracture zones symmetric and asymmetric about a spreading axis: Mid-Atlantic Ridge (latitude 23°N to 27°N) , 1980 .
[44] D. G. Temple,et al. Geology of a submarine hydrothermal field, Mid-Atlantic Ridge, 26°n latitude , 1979 .
[45] J. Morse,et al. Metal-enriched sediments from the TAG Hydrothermal Field , 1978, Nature.
[46] B. Parsons,et al. An analysis of the variation of ocean floor bathymetry and heat flow with age , 1977 .
[47] J. Lavelle,et al. Magnetic anomaly patterns on Mid‐Atlantic Ridge crest at 26°N , 1977 .
[48] R. Lowell,et al. On the interpretation of near-bottom water temperature anomalies , 1976 .
[49] P. Rona,et al. Anomalous water temperatures over Mid-Atlantic Ridge crest at 26° North latitude , 1975 .
[50] P. Rona,et al. Crest of the Mid‐Atlantic Ridge at 26°N , 1975 .
[51] H. Koide,et al. Formation of fractures around magmatic intrusions and their role in ore localization , 1975 .
[52] P. Rona,et al. Rapidly accumulating manganese deposit from the Median Valley of the Mid‐Atlantic Ridge , 1974 .
[53] P. Rona,et al. The TAG hydrothermal field , 1974, Nature.
[54] Roger N. Anderson,et al. Implications of Heat Flow and Bottom Water Temperature in the Eastern Equatorial Pacific , 1972 .
[55] E. Ratcliffe. The thermal conductivities of ocean sediments , 1960 .
[56] A. E. Maxwell,et al. The measurement of thermal conductivity of deep‐sea sediments by a needle‐probe method , 1959 .
[57] Geoffrey Ingram Taylor,et al. Turbulent gravitational convection from maintained and instantaneous sources , 1956, Proceedings of the Royal Society of London. Series A. Mathematical and Physical Sciences.
[58] N. P. Fofonoff,et al. Algorithms for Computation of Fundamental Properties of Seawater. Endorsed by Unesco/SCOR/ICES/IAPSO Joint Panel on Oceanographic Tables and Standards and SCOR Working Group 51. Unesco Technical Papers in Marine Science, No. 44. , 1983 .
[59] P. Rona. New evidence for seabed resources from global tectonics , 1973 .
[60] J. Turner,et al. Buoyant Plumes and Thermals , 1969 .