The portion of the East Pacific Rise (EPR) between 5° and 12°S
can be subdivided into three areas by fracture zones that offset the
rise axis at about 6.5°S and 9°S. In all three regions, the spreading
axis of the EPR is defined by a topographic block 300 to 350 m high
and about 15 km wide. The axial block commonly has subordinate
peaks or shoulders on each flank that vary up to 5 km wide.
Analysis of linear magnetic anomalies in the southern of the
three areas suggests that sea-floor spreading has been occurring at
rates of 80 mm/y to the west and 77 mm/y to the east during the
last 1.7 million years (my). The rise axis is offset in two places
about 10 km. These displacements are interpreted to be the result of
discrete jumps of the site of spreading activity. Reconnaissance data
from the east flank of the EPR indicate that spreading activity on this
portion of the rise began just over 8 my ago when the site of crustal
accretion jumped westward from the now dormant Galapagos Rise. About 4.6 my ago the section of rise crest between approximately
10.5°S and the 9°S fracture zone jumped westward a distance of at
least 10 km, isolating the pre-existing axial block. By 1.7 my ago,
this axial offset no longer existed, implying a relatively westward
migration of the rise axis south of 10.5° during the period from 4.6
to 1.7 my ago. The two offsets of the present axis occurred between
1.6 and 0.9 my ago and 0.7 my ago and the present in the north and
south, respectively.
The formation of the axial block, its associated shoulders and
the abyssal topography, apparently consisting of tilted fault blocks
with steep sides facing the axis, can be explained by an empirical
model. This model combines extrusion of basalt along the spreading
axis to form the axial block and rotational faulting to form the
shoulders of the block and then lower the shoulders to merge with the
abyssal topography of the uppermost rise flanks.
In the region north of the 6.5°S fracture zone, seismic activity
on the rise crest, combined with topographic information, suggests
that the EPR axis is unstable here and that it is in the process of reorienting
to a more stable regional trend. Identification and mapping
of magnetic anomalies in the vicinity of 6°S reveal a spreading rate
of about 77 mm/y, an episode of oblique spreading that occurred 1.7
my ago, and a 10 km westward jump of the axis which occurred since
0.7 my ago. The fracture zone at 6.5°S offsets the EPR axis 55 km right laterally. Both the bathymetric and magnetic expression of
this fracture zone are markedly reduced a few tens of kilometers
away from its active portion, implying that some change in the processes
forming the fracture zone occurred about 0.3 my ago.
Between the fracture zones at 6.5° and 9°S, two deactivated
segments of the rise axis, each about 40 km long, occur 90 and 65
km west of the currently active axis. These inactive axial segments
were isolated by eastward jumps of the spreading center. The more
northerly jump, along 6.5°S, occurred 0.3 my ago and spanned 68
km. The other, along 7°S, covered a similar distance and is either
just completed or still going on. Reconnaissance data from this part
of the EPR suggests that sea-floor spreading began here about 6.5
my ago and has been continuing at a rate of approximately 78 mm/y. / Graduation date: 1975
| Identifer | oai:union.ndltd.org:ORGSU/oai:ir.library.oregonstate.edu:1957/28562 |
| Date | 03 June 1974 |
| Creators | Rea, David K. |
| Contributors | van Andel, T. H., Kulm, LaVerne D. |
| Source Sets | Oregon State University |
| Language | en_US |
| Detected Language | English |
| Type | Thesis/Dissertation |
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