Evidence from Sardinian basalt geochemistry for recycling of plume heads into the Earth's mantle

[1]  A. Sobolev,et al.  Recycled oceanic crust observed in ‘ghost plagioclase’ within the source of Mauna Loa lavas , 2000, Nature.

[2]  F. Albarède,et al.  Hf isotope evidence for pelagic sediments in the source of hawaiian basalts , 1999, Science.

[3]  F. Albarède,et al.  Relationships between Lu–Hf and Sm–Nd isotopic systems in the global sedimentary system , 1999 .

[4]  R. Hilst,et al.  Compositional stratification in the deep mantle , 1999, Science.

[5]  E. Hauri,et al.  Osmium-isotope variations in Hawaiian lavas: evidence for recycled oceanic lithosphere in the Hawaiian plume , 1998 .

[6]  F. Albarède,et al.  A Hf‐Nd isotopic correlation in ferromanganese nodules , 1998 .

[7]  S. Philander,et al.  The role of ocean-atmosphere interactions in tropical cooling during the last glacial maximum , 1998, Science.

[8]  E. R. Engdahl,et al.  Evidence for deep mantle circulation from global tomography , 1997, Nature.

[9]  V. Morra,et al.  High-Mg subduction-related Tertiary basalts in Sardinia, Italy , 1997 .

[10]  J. Beck,et al.  Abrupt changes in early Holocene tropical sea surface temperature derived from coral records , 1997, Nature.

[11]  K. Sims,et al.  INFERENCES ABOUT MANTLE MAGMA SOURCES FROM INCOMPATIBLE ELEMENT CONCENTRATION RATIOS IN OCEANIC BASALTS , 1997 .

[12]  A. Hofmann,et al.  Mantle geochemistry: the message from oceanic volcanism , 1997, Nature.

[13]  W. Broecker Glacial Climate in the Tropics , 1996, Science.

[14]  B. Hanan,et al.  Lead and Helium Isotope Evidence from Oceanic Basalts for a Common Deep Source of Mantle Plumes , 1996, Science.

[15]  A. Hofmann,et al.  Source characteristics derived from very incompatible trace elements in Mauna Loa and Mauna Kea basalts, Hawaii Scientific Drilling Project , 1996 .

[16]  E. Mosley‐Thompson,et al.  Late Glacial Stage and Holocene Tropical Ice Core Records from Huascar�n, Peru , 1995, Science.

[17]  T. Crowley Pleistocene temperature changes , 1994, Nature.

[18]  W. White 238U/204Pb in MORB and open system evolution of the depleted mantle , 1993 .

[19]  A. Hofmann,et al.  himu-em: The French Polynesian connection , 1992 .

[20]  S. Hart,et al.  Mantle Plumes and Entrainment: Isotopic Evidence , 1992, Science.

[21]  L. François,et al.  Modelling the Phanerozoic carbon cycle and climate: constraints from the 87Sr/86Sr isotopic ratio of seawater. , 1992, American journal of science.

[22]  B. Weaver The origin of ocean island basalt end-member compositions: trace element and isotopic constraints , 1991 .

[23]  E. Grossman,et al.  Oxygen isotopes in meteoric calcite cements as indicators of continental paleoclimate , 1991 .

[24]  F. Albarède,et al.  A major 2.1 Ga event of mafic magmatism in west Africa: An Early stage of crustal accretion , 1990 .

[25]  L. Railsback Influence of changing deep ocean circulation on the Phanerozoic oxygen isotopic record , 1990 .

[26]  M. McCulloch,et al.  Ancient seafloor signals in Pitcairn Island lavas and evidence for large amplitude, small length-scale mantle heterogeneities , 1989 .

[27]  C. Langmuir,et al.  Global correlations of ocean ridge basalt chemistry with axial depth and crustal thickness , 1987 .

[28]  H. Newsom,et al.  Siderophile and chalcophile element abundances in oceanic basalts, Pb isotope evolution and growth of the Earth's core , 1986 .

[29]  R. Nance,et al.  Tectonic cycles and the history of the Earth's biogeochemical and paleoceanographic record , 1986 .

[30]  A. Hofmann,et al.  Nb and Pb in oceanic basalts: new constraints on mantle evolution , 1986 .

[31]  D. Rind,et al.  Terrestrial Conditions at the Last Glacial Maximum and CLIMAP Sea-Surface Temperature Estimates: Are They Consistent? , 1985, Quaternary Research.

[32]  Claude J. Allègre,et al.  Basalt genesis and mantle structure studied through Th-isotopic geochemistry , 1982, Nature.

[33]  Stephen H. Richardson,et al.  Correlated Nd, Sr and Pb isotope variation in Walvis Ridge basalts and implications for the evolution of their mantle source , 1982 .

[34]  A. Nur,et al.  Continental accretion: from oceanic plateaus to allochthonous terranes. , 1981, Science.

[35]  S. Savin The History of the Earth's Surface Temperature During the Past 100 Million Years , 1977 .

[36]  A. Hall Composition and Petrology of the Earth's Mantle , 1977, Mineralogical Magazine.

[37]  J. D. Hays,et al.  Variations in the Earth ' s Orbit : Pacemaker of the Ice Ages Author ( s ) : , 2022 .

[38]  S. Epstein,et al.  Hydrogen and oxygen isotope ratios in nodular and bedded cherts , 1976 .

[39]  J. Steiner,et al.  Possible Galactic Causes for Periodic and Episodic Glaciations , 1973 .

[40]  M. Tester,et al.  THE CARBON CYCLE AND CO2 OVER PHANEROZOIC TIME : THE ROLE OF LAND PLANTS , 1998 .

[41]  R. Berner,et al.  GEOCARB III : A REVISED MODEL OF ATMOSPHERIC CO 2 OVER PHANEROZOIC TIME , 2001 .

[42]  F. Innocenti,et al.  Geochemistry and mineralogy of volcanic rocks from ODP sites 650, 651, 655 and 654 in the Tyrrhenian sea , 1988 .

[43]  P. Vogt,et al.  Subduction of Aseismic Oceanic Ridges: Effects on Shape, Seismicity, and Other Characteristics of Consuming Plate Boundaries , 1976 .

[44]  A. Ringwood Composition and petrology of the earth's mantle , 1975 .