Geología y estructura del Cerro Guanaquero, Río Diamante, Mendoza

Abstract

This study presents new data on a poorly known sector of the Cordillera Principal of Mendoza, in the headwaters of the Diamante river basin in Cerro Guanaquero and surrounding areas. The exposed units are divided in four main groups: marine and continental sedimentary Mesozoic sequences intensively folded and thrust, intermediate intrusives and volcanic rocks of Neogene age, Pliocene to Recent volcanic rocks of intermediate to basic composition, and unconsolidated Quaternary deposits. The Cerro Guanaquero, a Quaternary stratovolcano intensively eroded by Pleistocene glaciers, with its 4,841 meters is the most prominent orographic feature of the region. It is constituted essentially by pyroxene to biotite-bearing gray porphyritic andesites. Pyroclastic deposits, volcanic agglomerates, ignimbrites, and basalts are interbedded with the andesitic flows. The K-Ar date by whole-rock method of an andesite yielded an age of 1.4 ± 0.1 Ma. The Andean deformation begins as a thin-skinned fold and thrust belt, with detachment folds in the western areas that advanced to the east as propagation folds. The compression ended west of the 69º47´W with the inversion of the Mesozoic rift normal faults. Along this meridian the most important fault of the region is found, which has been correlated with the Malargüe fault, well developed south of the study area. This fault bounds the thin-skinned Aconcagua fold and trust belt, and the thick-skinned Malargüe fold and thrust belt, controlled by tectonic inversion. The volcanism was very intense in the Pliocene and Quaternary, associated with a steepening of the subducted oceanic slab, at the time that the region was passively uplifted. The resistance of the volcanic rocks to the erosion compared with the Mesozoic sedimentary rocks, plus the high erosive efficiency of the Pleistocene´s glaciers, gave place to the inversion of the relief. The erosion rate was exceptional, reaching at least 7 cm/100 years during the Quaternary.

This study presents new data on a poorly known sector of the Cordillera Principal of Mendoza, in the headwaters of the Diamante river basin in Cerro Guanaquero and surrounding areas. The exposed units are divided in four main groups: marine and continental sedimentary Mesozoic sequences intensively folded and thrust, intermediate intrusives and volcanic rocks of Neogene age, Pliocene to Recent volcanic rocks of intermediate to basic composition, and unconsolidated Quaternary deposits. The Cerro Guanaquero, a Quaternary stratovolcano intensively eroded by Pleistocene glaciers, with its 4,841 meters is the most prominent orographic feature of the region. It is constituted essentially by pyroxene to biotite-bearing gray porphyritic andesites. Pyroclastic deposits, volcanic agglomerates, ignimbrites, and basalts are interbedded with the andesitic flows. The K-Ar date by whole-rock method of an andesite yielded an age of 1.4 ± 0.1 Ma. The Andean deformation begins as a thin-skinned fold and thrust belt, with detachment folds in the western areas that advanced to the east as propagation folds. The compression ended west of the 69º47´W with the inversion of the Mesozoic rift normal faults. Along this meridian the most important fault of the region is found, which has been correlated with the Malargüe fault, well developed south of the study area. This fault bounds the thin-skinned Aconcagua fold and trust belt, and the thick-skinned Malargüe fold and trust belt, controlled by tectonic inversion. The volcanism was very intense in the Pliocene and Quaternary, associated with a steepening of the subducted oceanic slab, at the time that the region was passively uplifted. The resistance of the volcanic rocks to the erosion compared with the Mesozoic sedimentary rocks, plus the high erosive efficiency of the Pleistocene's glaciers, gave place to the inversion of the relief. The erosion rate was exceptional, reaching at least 7 cm/100 years during the Quaternary.