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Lamont-Doherty Geological Observatory of Columbia University, Palisades, NY 10964 USA
Lamont-Doherty Geological Observatory of Columbia University, Palisades, N.Y. 10964 USA
Lamont-Doherty Earth Observatory, Palisades, NY; CNR, Ist. Geologica Marina, Bologna, Italy
Universite Lille, Villeneuve d'Ascq, France
Lamont-Doherty Geological Observatory, Columbia University, Palisades, NY 10964 USA
Istituto di Scienze Marine, Geologia Marina, CNR, Via Gobetti 101, 40129, Bologna, Italy; Lamont Doherty Earth Observatory, Columbia University, Palisades, New York 10964, USA
Institute of Marine and Atmospheric Sciences, University of Miami
Lamont-Doherty Geological Observatory, Columbia University, Palisades, N.Y. 10964 USA
Lamont-Doherty Earth Observatory of Columbia University, Palisades, New York 10964, USA; Dipartimento di Scienze della Terra, Università "La Sapienza", P.le Aldo Moro 5, 00187, Rome, Italy
CNR, Istituto di Geologia Marina, Bologna ,Italy; Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY 10964, USA
CNR-ISMAR, Sezione Istituto Geologia Marina, Bologna Via Gobetti, 101, 40129 Bologna, Italy; Lamont Doherty Earth Observatory, Columbia University, New York, USA
Lamont-Doherty Earth Observatory, Earth Institute at Columbia University, Palisades, New York, USA
26 million years of mantle upwelling below a segment of the Mid Atlantic Ridge: The Vema Lithospheric Section revisited
A cold suboceanic mantle belt at the Earth's equator
Anomalous opening of the Equatorial Atlantic due to an equatorial mantle thermal minimum
Aragonite from deep sea ultramafic rocks
Dust in the Caribbean atmosphere traced to an African dust storm
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