Ja. Goff et Jr. Cochran, THE BAUER SCARP RIDGE JUMP - A COMPLEX TECTONIC SEQUENCE REVEALED IN SATELLITE ALTIMETRY, Earth and planetary science letters, 141(1-4), 1996, pp. 21-33
We investigate here the ridge jump that led to abandonment of the Gala
pagos Rise and formation of the Bauer scarp during the initiation of t
he present day configuration of the East Pacific Rise since the lower
Miocene. We use recently available high resolution satellite-derived g
ravity data to investigate in detail the tectonic structure of the eas
tern Pacific from the Equator to 20 degrees S. With this data, we iden
tify fracture zones, abandoned spreading ridges, scarps, and other sea
floor features that provide evidence for discerning tectonic history.
Based on our structural interpretation of the satellite-derived gravit
y field, we make the following conclusions: (1) The Galapagos Rise spr
eading center appears to have originated by opening of the Marquesas/M
endana transform complex as a result of the change in spreading direct
ion following breakup of the Farallon Plate. (2) The Galapagos Rise wa
s not the sole locus of spreading following plate reorganization at si
milar to 20 Ma through to the initiation of the Bauer scarp at similar
to 8 Ma, as had been previously hypothesized. Rather, it and a second
western spreading axis were likely active concurrently, forming a cou
nterclockwise-rotating Bauer Microplate at a much earlier stage than t
hought previously. (3) The Bauer scarps are pseudofaults associated wi
th northward rift propagation. Propagation proceeded in several stages
. A first propagator emanating from the Garrett transform complex stal
led at the future location of the Wilkes transform creating an area of
complex morphology near its northern tip. A second propagator, also e
manating from the Garrett complex followed in the first's wake and bro
ke through the complex region. At this point the propagation proceeded
very rapidly to the northern end of the Bauer Microplate (the Gallego
fracture zone, later to become the Yaquina transform fault). Ridge pr
opagation continued north in two more stages, creating the Gofar and Q
uebrada transforms at the terminus of each stage.