Overview of part of the Farallón Negro Volcanic Complex, looking ESE from the Agua Tapada area. Apparent are the volcanic rocks and the strongly sericitized Agua Tapada intrusion in the front. Sediments at the base of the Cerro Durazno volcanics (the prominent escarpment in the background) are exposed as a result of uplift along a reverse NNW–SSE-trending fault (see Fig. )
2004 a) shows that the complex consists of the remnants of a 20-km-wide stratocone, intruded by numerous subvolcanic stocks (Fig. 2 ).
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