Changes in the tectonic regime above a subduction zone of Andean Type: The Andes of Peru and Bolivia during the Pliocene‐Pleistocene

Abstract

This paper adresses the changes in the tectonic regime in the Peruvian and Bolivian Andes that have occurred since the upper Miocene when the present‐day elevation of the Cordillera above sea level has been almost reached. The stress patterns are deduced essentially from a field study of fault kinematics and a numerical inversion of the slip vector data measured on the fault planes. The Cuzco fault system in southern Peru is chosen as an example to illustrate the methodology used. In this region, striations on both active and Holocene faults are in agreement with a N‐S extension. But faults affecting early Pleistocene deposits exhibit two families of striations. The younger results from the previous N‐S extension: the older, involving reverse motions, results from either an E‐W or a N‐S compression. Faults affecting Pliocene formations often show an oldest family of striations resulting from a NE‐SW or an E‐W trending extension. Thus three tectonic regimes are demonstrated which are also supported by regional unconformities and sedimentological data: (1) a Pliocene extensional regime, (2) a lower Pleistocene compressional regime, and (3) a mid‐Pleistocene‐present‐day extensional regime. Similar analyses conducted in the Pacific and sub‐Andean lowlands allow sketching of the successive Pliocene‐Pleistocene stress patterns in the Central Andes. The Quaternary and present‐day stress pattern is characterized by a N‐S extension in the High Andes and in the Pacific lowlands and by an E‐W compression in the sub‐Andean lowlands and at the contact between the Nazca and South American plates. This stress pattern is interpreted at a large wavelength (>100 km) as an effect of compensated topography. This model supposes that the vertical lithospheric stress, σzz, increases with the topography, the crustal thickness, and the low‐density mantle beneath and that the lithospheric maximum (compressional) horizontal stress σHmax, trending E‐W roughly parallel to the convergence, is fairly constant. On both edges of the Andes, the tectonics being compressional, σzz is σ3 and σHmax is σ1. In the High Andes, σzz becomes σ1, then the E‐W trending σHmax is σ2 and σHmin trending N‐S is σ3, allowing extension to occur in this direction. The Pliocene stress pattern was characterized by a NE‐SW or an E‐W trending extension in the High Andes, in the Pacific lowlands, and possibly in the sub‐Andean lowlands. This stress pattern was clearly different from the present‐day one because the E‐W trending stress was σHmin. This required a weak push or, eventually, tractional boundary forces acting on the South American lithosphere. It is suggested that this might result from a strong slab pull due to a long, steeply dipping slab which decreased the value of the σxx stress transmitted to the overriding plate. The early Pleistocene state of stress was compressional. Since the elevation of the Andes had not markedly decreased during this period, this required an increase of the E‐W trending stress value. This resulted from a strong coupling between the...

Magma evolution of Quaternary minor volcanic centres in southern Peru, Central Andes

“…The present day stress regime in southern Peru is controlled by: (1) north-south stretching, related to the extensional regime of the high Andean Cordillera and to the slow motion of the convergent plates, and; (2) east-west compression associated with the N80-trending convergent oceanic Nazca plate (Sébrier and Soler 1991;Mercier et al 1992). Moreover, data obtained with SPOT and SAR ERS-1 satellite images (Mering et al 1996) indicate that the tectonic regime in southern Peru close to Arequipa (Fig.…”

Slope instabilities at an active continental margin: large-scale polyphase submarine slides along the northern Peruvian margin, between 5 °S and 6 °S

“…Mercier et al (1992) suggested that weakening of the crust occurred for successive periods, probably extensional, during which the slab progressively lengthened and increased in depth, therefore favouring a seaward migration of the slab flexure. Thickening of the crust occurred during the compressional events (Sebrier and Soler, 1991), resulting from the rupture of a long, high-angle dipping slab under its own weight (Mercier et al, 1992). …”

Explosive volcanism (VEI 6) without caldera formation: insight from Huaynaputina volcano, southern Peru

“…While the former two systems are associated with the Rio Tambo graben, the third system is minor and the last one consists of a series of sinistral, en echelon strike slip faults which are parallel to the Central Volcanic Zone (Lavallée et al unpublished). A study of fault kinematics by Mercier et al (1992) suggested that the mid-Pleistocene to present-day tectonic regime of the High Andes is characterized by a vertical maximum stress induced by the high elevation (>4,000 m), a secondary E-W compression caused by collision of the Pacific and South America plates, and a resulting N-S extension in the direction of σ3 (Fig. 1).…”

“…This ancestral volcano consists of 500 m of andesite porphyry of the Pastillo volcanic complex (James Lavallée, 2003). The current stress vectors of the High Andes are indicated in the inset (Mercier et al 1992). The location of earthquakes that occurred in the area since 1471 are indicated by a circle, which includes the depth estimate (Ceresis, 1985 Tosdal et al 1981;INGEMMET 2000a).…”