Abstract
Two drillings carried out at Cerro Prieto (Province of Málaga), together with additional geophysical data, revealed the existence of an igneous body formed of rock-types previously unknown in the Subbetic zone. The recovered rocks, emplaced under hypoabyssal conditions, are predominantly porphyric, containing olivine, diopside and TiO
Original language | English |
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Pages (from-to) | 111-130 |
Number of pages | 22 |
Journal | Geologica Acta |
Volume | 8 |
Issue number | 2 |
DOIs | |
Publication status | Published - Jun 2010 |