FN Archimer Export Format
PT J
TI Volcanics from the walvis ridge
BT 
AF HEKINIAN, Roger
AS 1:;
FF 1:;
TC 0
UR https://archimer.ifremer.fr/doc/1972/publication-5124.pdf
LA English
DT Article
DE ;Histoire Ifremer
AB THE Walvis Ridge is a non-continuous aseismic feature  in the south-eastern Atlantic Ocean with a general trend north-east/ south-west.  Close to the principal interruptions of the ridge is a north-south topographiç lineation shown on Simpson's map  (Fig. 1).  The ridge appears to be attached at its northeast end to the shelf of Angola and South-west Africa and at its south-west end to the east flank of the Mid-Atlantic Ridge through two volcanic islands,  Tristan da Cunha and Gough (Fig. 1). These two islands are made up of recent alkalibasalt-trachyte suite². . The geology of the Walvis Ridge has remained relatively unknown. [NOT CONTROLLED OCR]
PY 1972
SO Nature Physical Science
PU Macmillan Journals
ID 5124
ER

EF