FN Archimer Export Format
PT J
TI Volcanics from the Sierra Leone Rise
BT 
AF HEKINIAN, Roger
   BONTE, P.
   DUPLEY, P.L.
   BLANC, P.L.
   JEHANO, C.
   LABEYRIE, L.
   DUPLEYSSIS, J.C.
AS 1:;2:;3:;4:;5:;6:;7:;
FF 1:;2:;3:;4:;5:;6:;7:;
TC 0
UR https://archimer.ifremer.fr/doc/1979/publication-5259.pdf
LA English
DT Article
DE ;Histoire Ifremer
AB THE Sierra Leone Rise, located in the east equatorial Atlantic, forms a discontinuous chain of seamounts as shallow as 2 km extending with a general NE-SW trend from near the Sierra Leone Coast of Africa, to the St Paul fracture zone near the Mid-Atlantic Ridge (Fig. 1). The origin of this feature has remained a topic of discussion. Sheridan et al.  have hypothesised that the Sierra Leone Rise is a volcanic structure formed at the beginning of the opening of the Atlantic in the early Cretaceous period. [NOT CONTROLLED OCR]
PY 1979
PD DEC
SO Nature
PU Macmillan Journals
VL 257
IS 5680
BP 536
EP 538
ID 5259
ER

EF