Bandy W.L., Michaud François, Gutierrez C.A.M., Dyment J., Bourgois J., Royer J.Y., Calmus T., Sosson M., Ortega-Ramirez J.
Source
Pure and Applied Geophysics, 2011,
168 (8-9), p. 1391-1413 ISSN 0033-4553
To better define the morphotectonic elements and tectonic development of the Mid-Rivera-Transform Discordance, multibeam bathymetric, seafloor backscatter, multichannel seismic reflection and total field marine magnetic data were collected along the entire Rivera Transform west of 107A degrees W during the BART and FAMEX campaigns of the N.O. L'Atalante conducted in 2002. These data show that, although the transform tectonized zone of the Rivera Transform west of 107A degrees 30'W is a single continuous morphologic basin, this basin consists of two distinct morphotectonic domains: an eastern domain which morphologically is a deep rhombochasm within which organized seafloor spreading has occurred, and a western 'leaky transform' domain. These new data, in conjunction with the results of previous studies, support the idea that the Rivera-Pacific Euler pole is migrating southward towards the eastern half of the Rivera Transform, and further indicate a recent (< 0.14 Ma), and most likely ongoing, clockwise reorganization of the principle transform displacement zones of the Rivera Transform west of 108A degrees W. We propose that the Mid-Rivera-Transform Discordance owes its origin to this eastward progressing, clockwise reorganization of the transform segments that is occurring in response to recent changes in Rivera-Pacific relative plate motion.
