FN Archimer Export Format
PT J
TI Variation des sources de sediments dans le detroit de Makassar (Indonesie) au quaternaire recent: Role des facteurs morphostructuraux et eustatiques
OT Sediment sources in the Makassar Strait (Indonesia) during the Late Quaternary
BT 
AF FAUGERES, J-C
   GAYET, J
   GONTHIER, E
   LATOUCHE, C
   MAILLET, N
AS 1:;2:;3:;4:;5:;
FF 1:;2:;3:;4:;5:;
IF 0.662
TC 0
UR https://archimer.ifremer.fr/doc/00268/37924/36005.pdf
LA French
DT Article
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   MISEDOR
BO Coriolis
   Jean Charcot
AB Mineralogical analyses of sediments from the Makassar Strait, collected during the Corindon and Misedor cruises (dredges, piston and box cores) show the existing differences between sediments supplied from Kalimantan in the West and sediments supplied from Sulawesi in the East. The Kalimantan source is characterized by quartzitic sand, with rare feldspars, heavy minerals consisting mainly of pyroxene (hypersthene) and amphibole and predominant illite-kaolinite in the clay mineral assemblage. In contrast, the Sulawesi source differs by a great abundance of feldspars, lithoclasts and micas with predominant amphibole and pyroxene (augite) and major illite-chlorite clay minerals.
PY 1990
SO Oceanologica Acta, Special issue
SN 0399-1784
PU Gauthier-Villars
ID 37924
ER

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