Three-dimensional magnetotelluric inversion for the characterization of the Sol de Manana high-enthalpy geothermal field, Bolivia

被引:4
作者
Quiroga, Bruno Pereyra [1 ,2 ,3 ]
Rioseco, Ernesto Meneses [1 ,4 ]
Kapinos, Gerhard [5 ]
Brasse, Heinrich [6 ]
机构
[1] Leibniz Inst Appl Geophys LIAG, Dept Geotherm & Informat Syst, Stilleweg 2, D-30655 Hannover, Germany
[2] Tech Univ Clausthal, Inst Surface Energy Syst, Agricolastr 10, D-38678 Clausthal Zellerfeld, Germany
[3] Empresa Nacl Electricidad SA ENDE, Calle Colombia 0-0655, Cochabamba, Bolivia
[4] Georg August Univ Gottingen, Geosci Ctr, Dept Appl Geol, Goldschmidtstr 3, D-37077 Gottingen, Germany
[5] Fed Inst Geosci & Nat Resources BGR, Berlin Off, Wilhelmstr 25-30, D-13593 Berlin, Germany
[6] Free Univ Berlin, Inst Geol Sci, Geophys Sect, Malteserstr 74-100, D-12249 Berlin, Germany
关键词
High-enthalpy geothermal reservoir; Exploration geophysics; Magnetotelluric method; 3-D MT inversion; Laguna Colorada geothermal project; Bolivia; PUNA VOLCANIC COMPLEX; CENTRAL ANDES; ALTIPLANO; EVOLUTION; BENEATH; IGNIMBRITES; PLATEAU; SMOOTH; MODEL; STRATIGRAPHY;
D O I
10.1016/j.geothermics.2023.102748
中图分类号
TE [石油、天然气工业]; TK [能源与动力工程];
学科分类号
0807 ; 0820 ;
摘要
We describe the three-dimensional magnetotelluric modeling results of Laguna Colorada -Sol de Man & SIM;ana geothermal field in SW Bolivia. It is located near Laguna Colorada in the foothills of the Western Cordillera of the Andes and at the margin of the Altiplano-Puna Magma Body (APMB), which is characterized by a vast electrical conductivity anomaly and corresponding seismic anomalies in the mid and deep crust. The magnetotelluric (MT) data comprising 70 stations were modeled by a 3-D inversion. The final model shows a broad conductor at a few hundred meters in depth, which we interpret as the confining cap layer. Beneath, equally widespread, a layer of intermediate resistivity marks the high-temperature hydrothermal reservoir. Detailed interpretation of MT data with information from existing wells suggests a potential for a high-enthalpy geothermal field.
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页数:21
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