Citation: N. Fagel et al., CHANGES IN THE WESTERN BOUNDARY UNDERCURRENT OUTFLOW SINCE THE LAST GLACIAL MAXIMUM, FROM SMECTITE ILLITE RATIOS IN DEEP LABRADOR SEA SEDIMENTS/, Paleoceanography, 12(1), 1997, pp. 79-96
Citation: N. Fagel et al., MULTIPLE SEAWATER-DERIVED GEOCHEMICAL SIGNATURES IN INDIAN OCEANIC PELAGIC CLAYS, Geochimica et cosmochimica acta, 61(5), 1997, pp. 989-1008
Authors:
INNOCENT C
FAGEL N
STEVENSON RK
HILLAIREMARCEL C
Citation: C. Innocent et al., SM-ND SIGNATURE OF MODERN AND LATE QUATERNARY SEDIMENTS FROM THE NORTHWEST NORTH-ATLANTIC - IMPLICATIONS FOR DEEP CURRENT CHANGES SINCE THELAST GLACIAL MAXIMUM, Earth and planetary science letters, 146(3-4), 1997, pp. 607-625
Citation: N. Fagel et al., CLAY SUPPLIES IN THE CENTRAL INDIAN BASIN SINCE THE LATE MIOCENE - CLIMATIC OR TECTONIC CONTROL, Marine geology, 122(1-2), 1994, pp. 151-172
Authors:
DEBRABANT P
FAGEL N
CHAMLEY H
BOUT V
CAULET JP
Citation: P. Debrabant et al., NEOGENE TO QUATERNARY CLAY MINERAL FLUXES IN THE CENTRAL INDIAN BASIN, Palaeogeography, palaeoclimatology, palaeoecology, 103(3-4), 1993, pp. 117-131