FN Archimer Export Format
PT J
TI Impact de la trangression holocene sur la sedimentation dans le detroit de Makassar (Indonesie)
OT Impact of the Holocene transgression on the Quaternary sedimentation in the Makassar Strait (Indonesia)
BT 
AF GAYET, J
   CARBONEL, P
   DUPRAT, J
   LABEYRIE, L
   FAUGERES, J-C
   GONTHIER, E
   MOYES, J
AS 1:;2:;3:;4:;5:;6:;7:;
FF 1:;2:;3:;4:;5:;6:;7:;
IF 0.662
TC 0
UR https://archimer.ifremer.fr/doc/00268/37898/35979.pdf
LA French
DT Article
AB Biomarker data associated with isotopic curve partial differential super(18)O served to establish a stratigraphic scale and thereby a chronology of fluctuations in the circulation and sedimentation of the Kalimantan continental rise throughout the last climatic cycle. During the glacial maximum, period of low sea-level sediments were deposited by turbidity currents originating from Kalimantan. During deglaciation, during rise of the sea-level and more particularly in the Holocene, material issued from Kalimantan either contributed to the building of the Mahakam delta or was dispersed over the shelf. Sulawesi inputs, less abundant and mineralogically different from Kalimantan material, were observed onto the Kalimantan rise. During this same period, circulation in the Makassar strait slowed down progressively while stratification became more marked and practically permanent in the Holocene.
PY 1990
SO Oceanologica Acta, Special issue
SN 0399-1784
PU Gauthier-Villars
ID 37898
ER

EF