Abstract
The Pito Rift area is the site of actively deforming oceanic lithosphere that has been primarily under extension for at least the past million years, based on kinematic reconstructions. The major morphologic features, Pito Deep and Pito Seamount, are aligned toward the Euler pole for relative motion between the Easter and Nazca plates. SeaMARC II side-scan and bathymetry data indicate that there are two general modes of faulting currently active in the Pito Rift area. One is associated with incipient rifting of old (∼3 Ma) Nazca lithosphere by large NW-SE normal faults, and the other is associated with a broad area of right-lateral transform shear between the Nazca and Easter plates. This transform shear is distributed over a broad region because of the northward growth of the East Rift and parallel tectonic rifting within the Pito Rift area. The majority of the Pito Rift area is composed of preexisting blocks of Nazca plate that are back-tilted away from Pito Deep and strike perpendicular to present and previous relative plate motions. This observation suggests that block-faulting and back-tilting are the primary mechanisms responsible for the distributed lithospheric extension, in agreement with gravity and magnetic analyses (Martinez et al., this issue).
The only recent volcanic flows observed in side-scan data are from the Pito Seamount area and to the outside of the outer pseudofault of the East Rift. The significance of the young flows near the outer pseudofault is not understood. We interpret the flows extending northwest from the Pito Seamount as representing a newly formed seafloor spreading axis within the Pito Rift area. Gravity and magnetic analyses (Martinez et al., this issue) together with SeaMARC II bathymetry and side-scan data support this interpretation.
Based on the tectonic evolution of the Easter microplate, we propose an evolutionary model for the formation of the Pito Rift area, where new ‘tectonic’ grabens form immediately west of the previous graben and with slightly more counterclockwise orientation. The duration and history of tectonic activity for each graben are not well constrained.
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References
Anderson-FontanaS., EngelnJ. F., LundgrenP., LarsonR. L., and SteinS., 1986, Tectonics and Evolution of the Juan Fernandez Microplate at the Pacific-Nazca-Antarctic Triple Junction, J. Geophys. Res. 91, 2005–2018.
BlackintonJ. G., HussongD. M., and KosalosJ. G., 1983, First Results from a Combination Side-Scan Sonar and Sea-Floor Mapping System (SeaMARC II), Offshore Technology Conference 4478, 307–311.
BuckW. R., 1986, Small-Scale Convection Induced by Passive Rifting: the Cause for Uplift of Rift Shoulders, Earth Planet. Sci. Lett 77, 362–372.
ChristieD. M. and SintonJ. M., 1981, Evolution of Abyssal Lavas along Propagating Segments of the Galapagos Spreading Center, Earth Planet. Sci. Lett. 56, 321–335.
CroughS. T., 1978, Thermal Origin of Mid-Plate Hotspot Swells, Geophys. J. R. Astr. Soc. 55, 451–469.
EngelnJ. F. and SteinS., 1984, Tectonics of the Easter Plate, Earth Planet. Sci. Lett 68, 259–270.
EngelnJ. F., SteinS., WernerJ., and GordonR. G., 1988, Microplate and Shear Zone Models for Oceanic Spreading Center Reorganizations, J. Geophys. Res. 93, 2839–2856.
FrancheteauJ., PatriatP., SegoufinJ., ArmijoR., DoucoureM., Yelles-ChaoucheA., ZukinJ., CalmantS., NaarD. F., and SearleR. C., 1988, Pito and Orongo Fracture Zones: the Northern and Southern boundaries of the Easter Microplate (Southeast Pacific), Earth Planet. Sci. Lett. 89, 363–374.
FrancheteauJ., ArmijoR., CheineeJ-L., HekinianR., LonsdaleP. F., and BlumN., 1990, 1 Ma East Pacific Rise Oceanic Crust and Uppermost Mantle Exposed by Rifting in Hess Deep (Equatorial Pacific Ocean), Earth Planet. Sci. Lett. 101, 281–295.
HagenR. A., BakerN. A., NaarD. F., and HeyR. N., 1990, A SeaMARC II Survey of Recent Submarine Volcanism near Easter Island, Mar. Geophys. Res. 12, 297–315.
HandschumacherD. W., PilgerR. H., ForemanJ. A., and CampbellJ. R., 1981, Structure and Evolution of the Easter Plate, Geol. Soc. Am. Mem. 154, 63–76.
HaxbyW. F. and WeisselJ. K., 1986, Evidence for Small-Scale Mantle Convection from Seasat Altimetry Data, J. Geophys. Res. 91, 3507–3520.
HeyR. N., 1977, A New Class of Pseudofaults and their Bearing on Plate Tectonics: a Propagating Rift Model, Earth Planet. Sci. Lett. 37, 321–325.
Hey, R. N. and Naar, D. F., 1987, Cruise Report, R/V Moana Wave, Leg 8711, Hawaii Institute of Geophysics, University of Hawaii, 1–23.
HeyR. N., DuennebierF. K., and MorganW. J., 1980, Propagating Rifts on Mid-Ocean Ridges, J. Geophys. Res. 85, 3647–3658.
HeyR. N., NaarD. F., KleinrockM. C., Phipps MorganW. J., MoralesE., and SchillingJ-G., 1985, Microplate Tectonics along a Superfast Seafloor Spreading System near Easter Island, Nature 317, 320–325.
HeyR. N., KleinrockM. C., MillerS. P., AtwaterT. M., and SearleR. C., 1986, Sea Beam/Deep-Tow Investigation of an Oceanic Propagating Rift System, J. Geophys. Res. 91, 3369–3393.
HeyR. N., KlausA., IcayW., and NaarD. F., 1988, SeaMARC II Survey of the Propagating Limb of a Large Non-Transform Offset along the Fastest Spreading EPR Segment, Eos Trans. AGU 69, 1429.
HeyR. N., SintonJ. M., and DuennebierF. K., 1989, Propagating Rifts and Spreading Centers, in WintererE. L., HussongD. M., and DeckerR. W., (eds.), The Eastern Pacific Ocean and Hawaii, Boulder, Colorado, Geol. Soc. Am., The Geology of North America, v. N, 161–176.
HussongD. M. and FryerP., 1983, Back-Arc Seamounts and the SeaMARC II Seafloor Mapping System, Eos Trans. AGU 64, 627–632.
KlausA., IcayW., NaarD. F., and HeyR. N., 1991, SeaMARC II Survey of a Propagating Limb of a Large Non-Transform Offset along the Fastest Spreading East Pacific Rise Segment, J. Geophys. Res. 96, 9985–9998.
KleinrockM. C. and HeyR. N., 1989a, Detailed Tectonics near the Tip of the Galapagos 95.5° W Propagator: How the Lithosphere Tears and a Spreading Axis Develops, J. Geophys. Res. 94, 13801–13838.
KleinrockM. C. and HeyR. N., 1989b, Migrating Transform Zone and Lithospheric Transfer at the Galapagos 95.5° W Propagator, J. Geophys. Res. 94, 13859–13878.
LarsonR. L., SchoutenH., KleinrockM., and BirdR., 1988, The Juan Fernandez Microplate: an Example of Second Order Plate Motion and Ball Bearing Tectonics, Eos Trans. AGU 69, 1423.
LonsdaleP., 1983, Laccoliths and Small Volcanoes on the Flank of the East Pacific Rise, Geology 11, 706–709.
MacdonaldK. C., MillerS. P., HeustisS. P., and SpiessF. N., 1980, Three-Dimensional Modelling of a Magnetic Reversal Boundary from Inversion of Deep-Tow Measurements, J. Geophys. Res. 85, 3670–3680.
MammerickxJ. and SandwellD., 1986, Rifting of Old Oceanic Lithosphere, J. Geophys. Res. 91, 1975–1988.
MammerickxJ. and SharmanG. F., 1988, Tectonic Evolution of the North Pacific During the Cretaceous Quiet Period, J. Geophys. Res. 85, 3009–3024.
MammerickxJ., NaarD. F., and TyceR. L., 1988, The Mathematician Paleoplate, J. Geophys. Res. 93, 3025–3040.
MartinezF., NaarD. F., ReedT. B., and HeyR. N., 1991, Three-Dimensional SeaMARC II, Gravity, and Magnetics Study of Large-Offset Rift Propagation at the Pito Rift, Easter Microplate, Mar. Geophys. Res. 13, 255–285 (this issue).
MorganW. J., 1972, Plate Motions and Deep Mantle Convection, Mem. Geol. Soc. Am. 132, 7–22.
Naar, D. F., 1990, Large-Scale Plate Boundary Reorganization at the Easter Microplate, Ph.D. dissertation, Scripps Institution of Oceanography, University of California, 214 pp.
NaarD. F. and HeyR. N., 1986, Fast Rift Propagation along the East Pacific Rise near Easter Island, J. Geophys. Res. 91, 3425–3438.
Naar, D. F. and Hey, R. N., 1989, Recent Pacific-Easter-Nazca Plate Motions, in Evolution of Mid Ocean Ridges, IUGG Symposium 8, AGU Geophysical Monograph 57, 9–30.
NaarD. F. and HeyR. N., 1991, Tectonic Evolution of the Easter Microplate, J. Geophys. Res. 96, 7961–7993.
RusbyR. I., SearleR. C., EngelnJ., HeyR. N., NaarD., and ZukinJ., 1988, GLORIA and Other Surveys of the Easter and Juan Fernandez Microplates, Eos Trans. AGU 69, 1428.
SchillingJ-G., SigurdssonH., DavisA. N., and HeyR. N., 1985, Easter Microplate Evolution, Nature 317, 325–331.
SchoutenH., KlitgordK. D., and GalloD. G., 1988, Microplate Kinematics of the Second Order, Eos Trans. AGU 69, 488.
Schouten, H., Klitgord, K. D., and Gallo, D. G., 1991, Microplate Kinematics of the Second Order, J. Geophys. Res. (in press).
SearleR. C., RusbyR. I., EngelnJ., HeyR. N., ZukinJ., HunterP. M., LeBasT. P., HoffmanH-J., and LivermoreR., 1989, Comprehensive Sonar Imaging of the Easter Microplate, Nature 341, 701–705.
SempereJ-C., MeshkovA., ThommeretM., and MacdonaldK., 1988, Magnetic Properties of Some Young Basalts from the East Pacific Rise, Mar. Geophys. Res. 9, 131–146.
SempereJ-C., GeeJ., NaarD. F., and HeyR. N., 1989, Three-Dimensional Inversion of the Magnetic Field over the Easter-Nazca Propagating Rift near 25° S, 112° 25′W, J. Geophys. Res. 94, 17409–17420.
SenderK. L., ShorA., and HagenR., 1989, SeaMARC II Side-Scan Processing Techniques, Eos Trans. AGU 70, 11304.
SintonJ. M., WilsonD. S., ChristieD. M., HeyR. N., and DelaneyJ. R., 1983, Petrological consequences of Rift Propagation on Oceanic Spreading Ridges, Earth Planet. Sci. Lett. 62, 193–207.
SmithW. H. F., and WesselP., 1990, Gridding with Continuous Curvature Splines in Tension, Geophys. 55, 293–305.
Stewart, W. K., 1988, Multisensor Modeling Underwater with Uncertain Information, Ph.D. Dissertation, Woods Hole Oceanographic Institution.
WeisselJ. K. and KarnerG. D., 1989, Flexural Uplift of Rift Flanks Due to Mechanical Unloading of the Lithosphere During Extension, J. Geophys. Res. 94, 13919–13950.
WesselP. and SmithW. H. F., 1988, The GMT-SYSTEM: Version 1.0. Technical Reference and Cookbook, Internal Report, Lamont-Doherty Geological Observatory, Columbia University, New York.
ZukinJ. and FrancheteauJ., 1990, A Tectonic Test of Instantaneous Kinematics of the Easter Microplate, Oceanologica Acta, vol. Spec. 10, 183–198.
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Naar, D.F., Martinez, F., Hey, R.N. et al. Pito Rift: How a large-offset rift propagates. Marine Geophysical Researches 13, 287–309 (1991). https://doi.org/10.1007/BF00366280
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DOI: https://doi.org/10.1007/BF00366280