Redefinition of the Terminus of the Middle America Trench

Abstract

The terminus of the Middle America Trench has been traditionally represented as an arc, concave towards the continent. Tres Marías Islands are located at the terminus of the Middle America Trench in western Mexico, and their location is not only intriguing but also a key to the re-construction of the position of Baja California peninsula before separation from the North America plate. Previous re-constructions suggested various places around the location of Tres Marías Islands for the position of the tip of the peninsula, and several converge to a position that invades the area occupied by the islands, offering no explanation for the overlap. Before peninsular separation from North America, the Guadalupe trench followed a smooth curve; recreating the position of this paleo-trench yields a baseline for fixing the position of the peninsula, as well as the original position of the Tres Marías Islands fragment. A new tectonic view of the structure of the Middle America Trench terminus is proposed, replacing the traditional arc representation with a series of en echelon blocks, the northernmost terminates at the Tres Marías Escarpment. The long sides of the blocks correspond to previously identified geological faults in the Bahía de Banderas region, while their offshore continuation is supported by topographic observations. As a test of this model I show the corresponding re-construction of the position of Baja California prior to separation from the North America plate and the positional evolution of the peninsula and the Tres Marías fragment from Chron 4n.2 (7.90 Ma) to Chron 3n.4 (5.12 Ma).

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R. Alvarez, "Redefinition of the Terminus of the Middle America Trench," International Journal of Geosciences, Vol. 4 No. 4, 2013, pp. 766-776. doi: 10.4236/ijg.2013.44070.

Conflicts of Interest

The authors declare no conflicts of interest.

References

[1] D. Karig and W. Jensky. “The Proto-Gulf of California,” Earth and Planetary Science Letters, Vol. 17, No. 2, 1972, pp. 169-174. doi:10.1016/0012-821X(72)90272-5
[2] L. Ferrari, E. Pasquaré, S. Venegas, D. Castillo and F. Romero, “Regional Tectonics of Western Mexico and Its Implications for the Northern Boundary of the Jalisco Block,” Geofísica Internacional, Vol. 33, No. 1, 1994, pp. 139-151.
[3] D. G. Moore and J. R. Curray, “Geologic and Tectonic History of the Gulf of California,” In: J. R.Curray, D. G. Moore, et al., Eds., Initial Reports of the Deep Sea Drilling Project, US Government Printing Office, Washington DC, 1982, pp. 1279-1294.
[4] J. M. Stock and K. V. Hodges, “Pre-Pliocene Extension around the Gulf of California and the Transfer of Baja California to the Pacific Plate,” Tectonics, Vol. 8, No. 1, 1989, pp. 99-115. doi:10.1029/TC008i001p00099
[5] M. Lyle and G. E. Ness, “The Opening of the Southern Gulf of California,” In: J. P. Dauphin and B. R. T. Simoneit, Eds., The Gulf and Peninsular Province of the Californias, Memoir 47, AAPG, 1991, pp. 403-423.
[6] R. L. Fisher, “Middle America Trench: Topography, and Structure,” Geological Society of America Bulletin, Vol. 72, 1961, pp. 703-720. doi:10.1130/0016-7606(1961)72[703:MATTAS]2.0.CO;2
[7] G. E. Ness and M. W. Lyle, “A Seismo-Tectonic Map of the Gulf and Peninsular Province of the Californias,” In: J. P. Dauphin and B. R. T. Simoneit, Eds., The Gulf and Peninsular Province of the Californias, Memoir 47, AAPG, 1991, pp. 71-78.
[8] K. D. Klitgord and J. Mammerickx, “North East Pacific Rise: Magnetic Anomaly and Bathymetric Framework,” Journal of Geophysical Research, Vol. 87, No. B8, 1982, pp. 6725-6750. doi:10.1029/JB087iB08p06725
[9] P. B. Gans, “Large-Magnitude Oligo-Miocene Extension in Southern Sonora: Implications for the Tectonic Evolution of Northwest Mexico,” Tectonics, Vol. 16, No. 3, 1997, pp. 388-408. doi:10.1029/97TC00496
[10] P. J. Umhoefer, “Why Did the Southern Gulf of California Rupture so Rapidly?—Oblique Divergence across Hot, Weak Lithosphere along a Tectonically Active Margin,” GSA Today, Vol. 21, No. 11, 2011.
[11] R. Larson, H. Menard and S. Smith, “Gulf of California: A Result of Ocean-Floor Spreading and Transform Faulting,” Science, Vol. 161, No. 3843, 1968, pp. 781-784. doi:10.1126/science.161.3843.781
[12] R. G. Gastil, G. Morgan and D. Krumenacher, “The Tectonic History of Peninsular California and Adjacent Mexico,” In: W. G. Ernst, Ed., The Geotectonic Development of California, Englewood Cliffs, 1981, pp. 285-306.
[13] J. C. Crowell, “Juncture of San Andreas Transform System and Gulf of California Rift,” Oceanologica Acta, Supplement, Vol. 4, 1981, pp. 137-141.
[14] R. S. Yeats and B. U. Haq, “Deep-Sea Drilling off the Californias: Implications of Leg 63,” In: R. S. Yeats, B. U. Haq, et al., Eds., Initial Reports of the Deep Sea Drilling Project, US Printing Office, Washington DC, 1981, pp. 949-963.
[15] W. R. Dickinson, “OVERVIEW: Tectonic Implications of Cenozoic Volcanism in Coastal California,” Geological Society of America Bulletin, Vol. 109, No. 8, 1997, pp. 936-954. doi:10.1130/0016-7606(1997)109<0936:OTIOCV>2.3.CO;2
[16] G. A. Rusnak, R. L. Fisher and F. P. Shepard, “Bathymetry and Faults of Gulf of California,” In: T. H. van Andel and G. C. Shor Jr., Eds., Marine Geology of the Gulf of California, American Association Petroleum Geologists, Tulsa, 1964, pp. 59-75.
[17] T. Atwater and J. Stock, “Pacific-North America Plate Tectonics of the Neogene Southwestern United States: An update,” In: C. A. Hall, C. A. Nelson and W. G. Ernst, Eds., Integrated Earth and Environmental Evolution of the Southwest: The Clarence A. Hall, Jr. Volume, Geological Society of America, 1998, pp. 393-420.
[18] M. Pardo and G. Suárez, “Shape of the Subducted Rivera and Cocos Plates in Southern Mexico: Seismic and Tectonic Implications,” Journal of Geophysical Research, Vol. 100, No. B7, 1995, pp. 12357-12373. doi:10.1029/95JB00919
[19] J. E. Spencer and W. R. Normark, “Tosco-Abreojos Fault Zone: A Neogene Transform Plate Boundary within the Pacific Margin of Southern Baja California, Mexico,” Geology, Vol. 7, 1979, pp. 554-557. doi:10.1130/0091-7613(1979)7<554:TFZANT>2.0.CO;2
[20] C. DeMets and S. Traylen, “Motion of the Rivera Plate Since 10 Ma Relative to the Pacific and North American Plates and the Mantle,” Tectonophysics, Vol. 318, No. 1-4, 2000, pp. 119-159. doi:10.1016/S0040-1951(99)00309-1
[21] J. R. Curray, D. G. Moore, D. Kelts and G. Einsele, “Tectonics and Geological History of the Passive Continental Margin at the Tip of Baja California,” In: R. S. Yeats, B. U. Haq, et al., Eds., Initial Reports of the Deep Sea Drilling Project, US Printing Office, Washington DC, 1981, pp. 1089-1116.
[22] J. Arzate, R. Alvarez, V. Yutsis, J. Pacheco and H. López-Loera, “Geophysical Modeling of Valle de Banderas Graben and Its Structural Relation to Bahía de Banderas, Mexico,” Revista Mexicana de Ciencias Geológicas, Vol. 23, No. 2, 2006, pp. 184-198.
[23] R. Alvarez, “Submarine Topography and Faulting in Bahía de Banderas, Mexico,” Geofísica Internacional, Vol. 46, No. 2, 2007, pp. 93-116.
[24] P. Lonsdale, “Structural Patterns of the Pacific Floor Offshore of Peninsular California,” In: J. P. Dauphin and B. R. T. Simoneit, Eds., The Gulf and Peninsular Province of the Californias, Memoir 47, AAPG, 1991, pp. 87-125.
[25] J. M. Fletcher, M. Grove, D. Kimbrough, O. Lovera and G. E. Gehrels, “Ridge-Trench Interactions and the Neogene Tectonic Evolution of the Magdalena Shelf and Southern Gulf of California: Insights from Detrital Zircon U-Pb Ages From the Magdalena Fan and Adjacent Areas,” GSA Bulletin, Vol. 119, No. 11-12, 2007, pp. 1313-1336. doi:10.1130/B26067.1
[26] K. M. Marsaglia, “Sandstone Detrital Modes Support Magdalena Fan Displacement from the Mouth of the Gulf of California,” Geology, Vol. 32, No. 1, 2004, pp. 45-48. doi:10.1130/G20099.1
[27] J. Mammerickx and K. D. Klitgord, “North East Pacific Rise: Evolution From 25 my B:P. to the Present,” Journal of Geophysical Research, Vol. 87, 1982, pp. 6751-6759. doi:10.1029/JB087iB08p06751
[28] P. Lonsdale, “Segmentation and Disruption of the East Pacific Rise in the Mouth of the Gulf of California,” Marine Geophysical Researches, Vol. 17, No. 4, 1995, pp. 323-359. doi:10.1007/BF01227039
[29] R. Alvarez, “Banderas Rift Zone: A Plausible NW Limit of the Jalisco Block,” Geophysical Research Letters, Vol. 29, No. 20, 2002, pp. 1994-1997. doi:10.1029/2002GL016089
[30] R. Alvarez, H. López-Loera and J. Arzate, “Modeling the Marine Magnetic Field of Bahia de Banderas, Mexico, Confirms the Half-Graben Structure of the Bay,” Tectonophysics, Vol. 489, No. 1-4, 2010, pp. 14-28. doi:10.1016/j.tecto.2010.03.012
[31] R. Reyes-Flores, “Exploración Petrolera en la Plataforma Continental del Pacífico (Edos. Nayarit-Sinaloa),” Ingeniería Petrolera, 1983, pp. 5-20.
[32] R. M. Prol-Ledesma, et al., “Heat Flow Variations along the Middle America Trench,” Marine Geophysical Researches, Vol. 11, No. 1, 1989, pp. 69-76. doi:10.1007/BF00286248
[33] D. Lizarralde, et al., “Variations in Styles of Rifting in the Gulf of California,” Nature, Vol. 448, 2007, pp. 467-469. doi:10.1038/nature06035
[34] R. P. Von Herzen, “Geothermal Heat Flow in the Gulfs of California and Aden,” Science, Vol. 140, No. 3572, 1963, pp. 1207-1208. doi:10.1126/science.140.3572.1207
[35] S. H. Jaramillo and G. Suárez, “The 4 December 1948 Earthquake (MW 6.4): Evidence of Reverse Faulting beneath the Tres Marías Escarpment and Its Implications for the Rivera-North American Relative Plate Motion,” Geofísica Internacional, Vol. 50, No. 3, 2011, pp. 313-317.

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