The Trans-Atlantic Geotraverse hydrothermal field: A hydrothermal system on an active detachment fault
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Maurice A. Tivey | Margaret K. Tivey | Susan E. Humphris | S. Humphris | M. Tivey | M. Tivey | Margaret K. Tivey | Maurice A. Tivey
[1] M. Mottl,et al. Morphology, mineralogy and chemistry of hydrothermal deposits from the TAG area, 26°N Mid-Atlantic Ridge☆ , 1985 .
[2] D. Bohnenstiehl,et al. Faulting and fault scaling on the median valley floor of the trans‐Atlantic geotraverse (TAG) segment, ∼26°N on the Mid‐Atlantic Ridge , 1999 .
[3] J. Sempere,et al. Bathymetry of the mid-atlantic ridge, 24°-31°N: A map series , 1990 .
[4] S. J. Reynolds,et al. Structural aspects of fluid-rock interactions in detachment zones , 1987 .
[5] R. Sohn. Stochastic analysis of exit fluid temperature records from the active TAG hydrothermal mound (Mid‐Atlantic Ridge, 26°N): 1. Modes of variability and implications for subsurface flow , 2007 .
[6] A. Schultz,et al. Conductive heat flow at the TAG Active Hydrothermal Mound: Results from 1993-1995 submersible surveys , 1996 .
[7] P. Rona,et al. Rapidly accumulating manganese deposit from the Median Valley of the Mid‐Atlantic Ridge , 1974 .
[8] G. Cherkashev,et al. Mineralogy, chemical composition and structure of the MIR Mound, TAG Hydrothermal Field , 1996 .
[9] M. Hannington,et al. Heat flow and mineralogy of TAG Relict High‐Temperature Hydrothermal Zones: Mid‐Atlantic Ridge 26°N, 45°W , 1996 .
[10] M. Hannington,et al. Comparison of the TAG mound and stockwork complex with Cyprus-type massive sulfide deposits , 1998 .
[11] Deborah K. Smith,et al. Fault rotation and core complex formation: Significant processes in seafloor formation at slow‐spreading mid‐ocean ridges (Mid‐Atlantic Ridge, 13°–15°N) , 2008 .
[12] P. Herzig,et al. Proceedings of the Ocean Drilling Program, 158 Scientific Results , 1998 .
[13] S. N. White,et al. New Observations on the Distribution of Past and Present Hydrothermal Activity in the TAG Area of the Mid-Atlantic Ridge (26°08′ N) , 1998 .
[14] P. Rona,et al. Geochronology of TAG and Snakepit hydrothermal fields, Mid-Atlantic Ridge: witness to a long and complex hydrothermal history , 1990 .
[15] S. Humphris,et al. A synthesis of geological and geochemical investigations of the TAG hydrothermal field: Insights into fluid-flow and mixing processes in a hydrothermal system , 2000 .
[16] M. Mottl,et al. Hydrothermal activity at the Trans‐Atlantic Geotraverse Hydrothermal Field, Mid‐Atlantic Ridge crest at 26°N , 1984 .
[17] M. C. Kleinrock,et al. Megamullions and mullion structure defining oceanic metamorphic core complexes on the Mid-Atlantic Ridge , 1998 .
[18] Y. Fouquet,et al. New age data for Mid‐Atlantic Ridge hydrothermal sites: TAG and Snakepit chronology revisited , 1993 .
[19] A. C. Campbell,et al. Time series studies of vent fluids from the TAG and MARK sites (1986, 1990) Mid-Atlantic Ridge: a new solution chemistry model and a mechanism for Cu/Zn zonation in massive sulphide orebodies , 1995, Geological Society, London, Special Publications.
[20] S. Petersen,et al. The geological setting of the ultramafic-hosted Logatchev hydrothermal field (14°45′N, Mid-Atlantic Ridge) and its influence on massive sulfide formation , 2009 .
[21] M. Tivey,et al. FLUID MIXING AND ANHYDRITE PRECIPITATION WITHIN THE TAG MOUND , 1997 .
[22] 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 .
[23] M. Tivey,et al. 10. FLUID MIXING AND ANHYDRITE PRECIPITATION WITHIN THE TAG MOUND 1 , 1998 .
[24] V. Preedy,et al. Time Series Studies , 2010 .
[25] S. Humphris,et al. 19. GEOCHEMICAL CHANGES DURING HYDROTHERMAL ALTERATION OF BASEMENT IN THE STOCKWORK BENEATH THE ACTIVE TAG HYDROTHERMAL MOUND 1 , 1998 .
[26] H. Edmonds,et al. Chemical characteristics of hydrothermal fluids from the TAG Mound of the Mid‐Atlantic Ridge in August 1994: Implications for spatial and temporal variability of hydrothermal activity , 1996 .
[27] J. Reyss,et al. 9. AGE OF SUB-BOTTOM SULFIDE SAMPLES AT THE TAG ACTIVE MOUND 1 , 1998 .
[28] Kentaro Nakamura,et al. Serpentinized troctolites exposed near the Kairei Hydrothermal Field, Central Indian Ridge: Insights into the origin of the Kairei hydrothermal fluid supporting a unique microbial ecosystem , 2009 .
[29] M. Hannington,et al. Gold-rich sea-floor gossans in the Troodos Ophiolite and on the Mid-Atlantic Ridge , 1991 .
[30] G. Beaudoin,et al. Silver-lead-zinc veins, metamorphic core complexes, and hydrologic regimes during crustal extension , 1991 .
[31] P. Rona,et al. Crest of the Mid‐Atlantic Ridge at 26°N , 1975 .
[32] M. Tivey,et al. Reduced crustal magnetization beneath Relict Hydrothermal Mounds: TAG Hydrothermal Field, Mid‐Atlantic Ridge, 26°N , 1996 .
[33] M. Tivey,et al. 14. TEMPERATURE AND SALINITY OF FLUID INCLUSIONS IN ANHYDRITE AS INDICATORS OF SEAWATER ENTRAINMENT AND HEATING IN THE TAG ACTIVE MOUND 1 , 1998 .
[34] Klas Lackschewitz,et al. Proceedings of the Ocean Drilling Program , 2002 .
[35] S. Humphris,et al. Structural control on sea-floor hydrothermal activity at the TAG active mound , 1996, Nature.
[36] Brian M. Smith,et al. K-metasomatism and detachment-related mineralization, Harcuvar Mountains, Arizona , 1988 .
[37] P. Rona,et al. The TAG hydrothermal field , 1974, Nature.
[38] Deborah K. Smith,et al. Tectonic versus magmatic extension in the presence of core complexes at slow-spreading ridges from a visualization of faulted seafloor topography , 2010 .
[39] J. Trefry,et al. History and geochemistry of a metalliferous sediment core from the Mid-Atlantic Ridge at 26°N , 1988 .
[40] R. Sohn. Stochastic analysis of exit fluid temperature records from the active TAG hydrothermal mound (Mid‐Atlantic Ridge, 26°N): 2. Hidden Markov models of flow episodes , 2007 .
[41] Yufeng Yao,et al. Anhydrite precipitation and the extent of hydrothermal recharge zones at ocean ridge crests , 2002 .
[42] J. Charlou,et al. Gases and helium isotopes in high temperature solutions sampled before and after ODP Leg 158 Drilling at TAG Hydrothermal Field (26°N, MAR) , 1996 .
[43] M. Hannington,et al. Fluid inclusion studies as a guide to the temperature regime within the TAG hydrothermal mound, 26°N, Mid-Atlantic Ridge , 1998 .
[44] S. Humphris,et al. On the Sr isotope and REE compositions of anhydrites from the TAG seafloor hydrothermal system , 2005 .
[45] W. Buck,et al. Role of melt supply in oceanic detachment faulting and formation of megamullions , 2008 .
[46] J. Sempere,et al. Segmentation of the Mid-Atlantic Ridge between 24° N and 30°40' N , 1990, Nature.
[47] S. Humphris,et al. Feeding biology of the shrimp Rimicaris exoculata at hydrothermal vents on the Mid-Atlantic Ridge , 1988 .
[48] R. Sohn,et al. Microearthquake evidence for reaction‐driven cracking within the Trans‐Atlantic Geotraverse active hydrothermal deposit , 2014 .
[49] C. V. Raman,et al. Active and relict sea-floor hydrothermal mineralization at the TAG hydrothermal field, Mid-Atlantic Ridge , 1993 .
[50] 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 .
[51] P. Rona,et al. Anomalous water temperatures over Mid-Atlantic Ridge crest at 26° North latitude , 1975 .
[52] Maurice A. Tivey,et al. A near‐bottom magnetic survey of the Mid‐Atlantic Ridge axis at 26°N: Implications for the tectonic evolution of the TAG segment , 2003 .
[53] R. Evans. A seafloor gravity profile across the TAG Hydrothermal Mound , 1996 .
[54] P. Rona,et al. Chronology of selected hydrothermal Mn oxide deposits from the transatlantic geotraverse , 1986 .
[55] K. Fujioka,et al. Chemistry of hydrothermal fluids at the TAG Active Mound, MAR 26°N, in 1998 , 2001 .
[56] Deborah K. Smith,et al. Central role of detachment faults in accretion of slow-spreading oceanic lithosphere , 2008, Nature.
[57] 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 .
[58] Jian Lin,et al. A geological model for the structure of ridge segments in slow spreading ocean crust , 1994 .
[59] R. Koski. Sulphide mineralization and wall-rock alteration in ophiolites and modern oceanic spreading centres , 1983 .
[60] Chiba Hitoshi,et al. Stable isotope study of anhydrite and sulfide minerals at the TAG hydrothermal mound, Mid-Atlantic Ridge, 26 degrees N , 1998 .
[61] P. Tyler,et al. Subannual Temporal Variation in Faunal Distributions at the TAG Hydrothermal Mound (26° N, Mid‐Atlantic Ridge) , 1999 .
[62] A. Glazner,et al. Hydrothermal systems and Tertiary low-angle normal faulting in the southwestern United States , 1985 .
[63] C. German,et al. Continuation of the hydrothermal fluid chemistry time series at TAG, and the effects of ODP drilling , 1996 .
[64] M. Tivey,et al. Reduced crustal magnetization beneath the active sulfide mound, TAG hydrothermal field, Mid-Atlantic Ridge at 26°N , 1993 .
[65] Hanumant Singh,et al. A Self‐Consistent Bathymetric Mapping Algorithm , 2007, J. Field Robotics.
[66] M. Cannat,et al. Geological context and vents morphology of the ultramafic‐hosted Ashadze hydrothermal areas (Mid‐Atlantic Ridge 13°N) , 2012 .
[67] C. You,et al. Evolution of an active sea-floor massive sulphide deposit , 1998, Nature.
[68] M. Hannington,et al. The internal structure of an active sea-floor massive sulphide deposit , 1995, Nature.
[69] A. C. Campbell,et al. Chemistry of hot springs on the Mid-Atlantic Ridge , 1988, Nature.
[70] M. Kinoshita,et al. Tidally-driven effluent detected by long-term temperature monitoring at the TAG hydrothermal mound, Mid-Atlantic Ridge , 1998 .
[71] M. Hannington,et al. Deducing patterns of fluid flow and mixing within the TAG active hydrothermal mound using mineralogical and geochemical data , 1995 .
[72] R. Sohn,et al. Crustal structure of the Trans‐Atlantic Geotraverse (TAG) segment (Mid‐Atlantic Ridge, 26°10′N): Implications for the nature of hydrothermal circulation and detachment faulting at slow spreading ridges , 2007 .
[73] W. Wilcock,et al. Modeling the effects of tidal loading on mid‐ocean ridge hydrothermal systems , 2005 .
[74] P. Rona,et al. Black smokers, massive sulphides and vent biota at the Mid-Atlantic Ridge , 1986, Nature.
[75] Brian M. Smith,et al. Deep-seated fluid involvement in ductile-brittle deformation and mineralization, South Mountains metamorphic core complex, Arizona , 1991 .
[76] Mark D. Hannington,et al. Hydrothermal sulfide accumulation along the Endeavour Segment, Juan de Fuca Ridge , 2014 .
[77] J. Escartín,et al. Oceanic detachment faults focus very large volumes of black smoker fluids , 2007 .
[78] G. Früh-Green,et al. Detachment Fault Control on Hydrothermal Circulation Systems: Interpreting the Subsurface Beneath The Tag Hydrothermal Field Using The Isotopic and Geological Evolution of Oceanic Core Complexes in The Atlantic , 2013 .
[79] John F. Casey,et al. Life cycle of oceanic core complexes , 2009 .
[80] J. Reyss,et al. Hydrothermal activity on a 105‐year scale at a slow‐spreading ridge, TAG hydrothermal field, Mid‐Atlantic Ridge 26°N , 1995 .
[81] S. Humphris,et al. Constraints on the energy and chemical balances of the modern TAG and ancient Cyprus seafloor sulfide deposits , 2000 .
[82] S. Solomon,et al. Microearthquake Characteristics of a Mid‐Ocean Ridge along‐axis high , 1992 .
[83] S. Humphris,et al. Detailed morphology of the TAG Active Hydrothermal Mound: Insights into its formation and growth , 1996 .
[84] M. Hannington,et al. Relict hydrothermal zones in the TAG Hydrothermal Field, Mid‐Atlantic Ridge 26°N, 45°W , 1993 .
[85] R. Sohn,et al. Three‐dimensional seismic structure of a Mid‐Atlantic Ridge segment characterized by active detachment faulting (Trans‐Atlantic Geotraverse, 25°55′N‐26°20′N) , 2012 .
[86] J. Spencer,et al. Possible controls of base- and precious-metal mineralization associated with Tertiary detachment faults in the lower Colorado River trough, Arizona and California , 1986 .
[87] J. Lavelle,et al. Magnetic anomaly patterns on Mid‐Atlantic Ridge crest at 26°N , 1977 .
[88] M. Hannington,et al. Volcanic Associated Massive Sulfide Deposits: Processes and Examples in Modern and Ancient Settings , 1997 .
[89] S. Humphris,et al. Kinematics and geometry of active detachment faulting beneath the Trans-Atlantic Geotraverse (TAG) hydrothermal field on the Mid-Atlantic Ridge , 2007 .
[90] A. Schultz,et al. A poroelastic model for the tidal modulation of seafloor hydrothermal systems , 2004 .
[91] A. Schultz,et al. Estimate of heat flux and its temporal variation at the TAG hydrothermal mound, Mid-Atlantic Ridge 26°N , 2003 .
[92] Deborah K. Smith,et al. Widespread active detachment faulting and core complex formation near 13° N on the Mid-Atlantic Ridge , 2006, Nature.