Abstract
Abstract. We present the results of a series of physical models aiming to reproduce rapid subsidence (at least 25 m in 30 years) observed in the sediments of a maar crater caused by extraction of groundwater in the interconnected adjacent aquifer. The model considered plausible variations in the geometry of the crater basement and the measured rate of groundwater extraction (1 m per year in the time interval from 2005 to 2011) in 15 wells located around the structure. The experiments were built within a rigid plastic bowl in which the sediments and rocks of the maar sequence were modeled using different materials: (a) plasticine for the rigid country rock, (b) gravel for the fractured country rock forming the diatreme fill and, (c) water saturated hollow glass microbeads for the lacustrine sedimentary fill of the crater. Water table was maintained initially at the surface of the sediments and then was allowed to flow through a hole made at the base of the rigid bowl. Water extraction provoked a sequence of gentle deformation, fracturing, and faulting of the surface in all the experiments. Vertical as well as lateral displacements were observed in the surface of the experiments. We discuss the results of 2 representative models. The model results reproduced the main geometry of the ring faults affecting the crater sediments and helps to explain the diversity of structures observed in relation with the diatreme geometry. The surface of the models was monitored continuously with an optical interferometric technique called structured light projection. Images collected at nearly constant time intervals were analyzed using the ZEBRA software and the obtained interferometric pairs permitted to analyze the full field subsidence in the model (submilimetric vertical displacements). The experiments were conducted at a continuous flow rate extraction and show a also a linear subsidence rate. Comparison among the results of the physical models and the fault system associated to subsidence in the maar show that fault geometry in the sedimentary sequence imitates closely the geometry of the volcanic basement.
Highlights
Rincón de Parangueo is a Quaternary volcanic maar, a crater formed by a phreatomagmatic eruption, located in the northern portion of the Michoacán-Guanajuato volcanic field in the central sector of the Trans Mexican Volcanic Belt (Fig. 1, location of the maar: 20◦25.839 N, −101◦14.917 W)
Subsidence in the experiments formed patterns directly related to the geometry of the rigid country rock modeled below the sedimentary cover
Varying systematically the geometry of the diatreme and analyzing the results give important insights on the evolution of deformational features associated with land subsidence
Summary
Rincón de Parangueo is a Quaternary volcanic maar, a crater formed by a phreatomagmatic eruption, located in the northern portion of the Michoacán-Guanajuato volcanic field in the central sector of the Trans Mexican Volcanic Belt (Fig. 1, location of the maar: 20◦25.839 N, −101◦14.917 W). Sinking at the bottom of the crater produced a ring-fault system which is exposed near the former coast of the lake, on a pair of parallel 15 m high topographic scarps. Normal faults exposed at the topographic scarp produced in some areas deformation domains that are consistent with the presence of listric detachment structures, which produced rollover anticlines with axes located near the former coast of the lake. Water withdrawal in the aquifer system adjacent to the volcanic field has been pointed out as the cause for deformation and desiccation of the lake since the 1980’s decade (Escolero-Fuentes and Alcocer-Duran, 2004; Aranda-Gómez et al, 2013; and references therein). The maar may be divided into two significant hydrogeological units, a deforming lacustrine sedimentary unit, acting as an aquitard and, the high fractured diatreme hydraulically connected with the regional aquifer system. In this work we aim at reproducing the subsidence observed in the Rincón de Parangueo maar by constructing a series of scaled physical models
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