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Tectonothermal analysis of a major unit of the Cantabrian Zone: the Ponga unit (Variscan belt, NW Spain).
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- International Journal of Earth Sciences, 2018, v. 107, n. 8, p. 2727, doi. 10.1007/s00531-018-1623-9
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Tectonothermal evolution of the northeastern Cantabrian zone (Spain).
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- International Journal of Earth Sciences, 2017, v. 106, n. 5, p. 1539, doi. 10.1007/s00531-016-1365-5
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Tectonothermal evolution in the core of an arcuate fold and thrust belt: the south-eastern sector of the Cantabrian Zone (Variscan belt, north-western Spain).
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- Solid Earth, 2016, v. 7, n. 4, p. 1003, doi. 10.5194/se-7-1003-2016
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Tectonothermal evolution of a foreland fold and thrust belt: the Cantabrian Zone (Iberian Variscan belt, NW Spain).
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- Terra Nova, 2007, v. 19, n. 6, p. 469, doi. 10.1111/j.1365-3121.2007.00773.x
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SERPUKHOVIAN CONODONTS FROM NORTHERN SPAIN AND THEIR BIOSTRATIGRAPHIC APPLICATION.
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- Palaeontology, 2007, v. 50, n. 4, p. 883, doi. 10.1111/j.1475-4983.2007.00684.x
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Geothermal palaeogradients and metamorphic zonation from the conodont colour alteration index (CAI).
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- Terra Nova, 2001, v. 13, n. 2, p. 79, doi. 10.1046/j.1365-3121.2001.00328.x
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Conodont colour alteration indices (CAI) of Upper Ordovician limestones from the Iberian Peninsula.
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- Netherlands Journal of Geosciences / Geologie en Mijnbouw, 1998, v. 77, n. 1, p. 77, doi. 10.1023/A:1003510915479
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