Ab. Watts et al., A SEISMIC STUDY OF LITHOSPHERIC FLEXURE IN THE VICINITY OF TENERIFE, CANARY-ISLANDS, Earth and planetary science letters, 146(3-4), 1997, pp. 431-447
Seismic data have been used to determine the crustal and upper mantle
structure of Tenerife, Canary Islands, a volcanic island of Tertiary a
ge located on >140 Ma oceanic crust. Reflection data show that oceanic
basement dips gently towards the island, forming a flexural moat whic
h is infilled by 2-3 km of well stratified material. The moat is chara
cterised by a major angular unconformity, which we attribute to volcan
ic loading of pre-existing oceanic crust and overlying sediments and t
he subsequent infilling of the flexure by material that was derived, a
t least in part, from the islands. Refraction data show that the flexe
d oceanic crust has a mean thickness of 6.41 +/- 0.42 km and upper and
lower crustal velocities of 4.8-5.3 km s(-1) and 6.7-7.3 km s(-1) res
pectively. The flexure, which has been verified by gravity modelling,
can be explained by a model in which Tenerife and adjacent islands hav
e loaded a lithosphere with a long-term (>10(6) yr) elastic thickness
of approximately 20 km. Seismic and gravity data suggest that up to 1.
5 x 10(5) km(3) of magmatic material has been added to the surface of
the flexed oceanic crust which, assuming an age of 6-16 Ma for the shi
eld building stage on Tenerife, implies a magma generation rate of abo
ut 0.006 to 0.02 km(3) a(-1). This rate is similar to estimates from o
ther African oceanic islands (e.g., Reunion and Cape Verdes), but is s
ignificantly less than that which has been calculated at Hawaii. There
is no evidence in either the seismic or gravity data that any signifi
cant amount of magmatic material has ''underplated'' the flexed oceani
c crust. The crustal and upper mantle structure at Tenerife therefore
differs from other oceanic islands such as Hawaii and Marquesas where
>4 km of underplated material have been reported.