# name
Mineralogy and geochemistry of Fe-Ti oxide ores from the Don Dieguito massif type anorthosite suite, Sierra Nevada de Santa Marta, Colombia

# metadata.dc.description.abstract[].value
Fe-Ti oxide ores are commonly associated with Proterozoic massif-type anorthosite bodies emplaced during the Grenville orogeny (~1.2-1.0 Ga). Some of these anorthositic bodies occur in the northernmost part of the Santa Marta Massif, Colombia. They locally contain crosscutting Fe-Ti(-V) ore bodies between the El Hierro creek and the Don Dieguito river. We have distinguished two types of Fe-Ti(-V) ores: i) oxide-apatite norite (fine grained ilmenite and magnetite disseminated in an assemblage of apatite, amphibole, chlorite, rutile and sericitized plagioclase) and ii) banded nelsonite (coarser grained ilmenite, magnetite and apatite distributed in bands, with minor baddeleyite, srilankite and högbomite).

# metadata.dc.publisher[].value
Universidad Nacional Autónoma de México (UNAM)

# metadata.dc.relation.ispartof[].value
Boletín de la Sociedad Geológica Mexicana, 2020, vol. 72, num. 3, p. A200720

# metadata.dc.rights[].value
cc-by-nc-nd (c) Betancur, Sebastián et al., 2020

# metadata.dc.source[].value
Articles publicats en revistes (Mineralogia, Petrologia i Geologia Aplicada)

# metadata.dc.title[].value
Mineralogy and geochemistry of Fe-Ti oxide ores from the Don Dieguito massif type anorthosite suite, Sierra Nevada de Santa Marta, Colombia