Medri, Alessia
(2022)
Mineralogy and Geochemistry of Phosporite Deposits from Tropic Seamount (NE Tropical Atlantic Ocean).
[Laurea magistrale], Università di Bologna, Corso di Studio in
Geologia e territorio [LM-DM270], Documento full-text non disponibile
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Abstract
Marine phosphorite deposits can form in a variety of environments, and despite of similar P contents, their mineralogy can change substantially. Seamount phosphorites are increasingly recognized for their P resources and are known to concentrate rare earth elements (REEs) and yttrium (Y) during early diagenetic formation, much more than continental-margin phosphorite deposits. Their importance is increasing in terms of economic potential but have always been studied for paleoenvironmental reconstruction purposes. The Canary Island Seamount Province (CISP) has been extensively studied for its Fe-Mn crusts and nodules deposits, but to date there has not been any systematic study on the phosphorite substrate rocks. This study aims at characterizing the mineralogy and geochemistry of the Tropic seamount phosphorites and offer insights into their mechanisms of formation. The Tropic seamount is a guyot that presents a variety of depositional environments. Two types of phosphorite slabs were identified: (1) a massive facies with oxic enrichments of Mn, Cr, Co, Ni and Cu located on the summit edges and flanks, and (2) a complex facies with suboxic-to-anoxic enrichments of U and V observed on the phosphorites located on the summit of the guyot. Both phosphorite types experienced advanced phosphatization (P2O5 between 24 and 31 wt.%, 3-4 wt.% of F). Differences in uptake of rare earth elements + yttrium (REY) and variations in mineralogy (e.g., presence of foraminifera vs. rounded glauconite grains, carbonate fragments or bioclasts) between the two types, allow phosphorites that formed in upwelling, nutrient-rich and oxic-suboxic environments to be distinguished from those which formed in suboxic-anoxic organic-poor environments. A potential combined ore deposit (Fe-Mn crusts + phosphorites) with high REY contents, like the seamount phosphorites analyzed in this study (ΣREY=870 μg/g on average), could help supply the resources needed for green-tech and high-tech applications.
Abstract
Marine phosphorite deposits can form in a variety of environments, and despite of similar P contents, their mineralogy can change substantially. Seamount phosphorites are increasingly recognized for their P resources and are known to concentrate rare earth elements (REEs) and yttrium (Y) during early diagenetic formation, much more than continental-margin phosphorite deposits. Their importance is increasing in terms of economic potential but have always been studied for paleoenvironmental reconstruction purposes. The Canary Island Seamount Province (CISP) has been extensively studied for its Fe-Mn crusts and nodules deposits, but to date there has not been any systematic study on the phosphorite substrate rocks. This study aims at characterizing the mineralogy and geochemistry of the Tropic seamount phosphorites and offer insights into their mechanisms of formation. The Tropic seamount is a guyot that presents a variety of depositional environments. Two types of phosphorite slabs were identified: (1) a massive facies with oxic enrichments of Mn, Cr, Co, Ni and Cu located on the summit edges and flanks, and (2) a complex facies with suboxic-to-anoxic enrichments of U and V observed on the phosphorites located on the summit of the guyot. Both phosphorite types experienced advanced phosphatization (P2O5 between 24 and 31 wt.%, 3-4 wt.% of F). Differences in uptake of rare earth elements + yttrium (REY) and variations in mineralogy (e.g., presence of foraminifera vs. rounded glauconite grains, carbonate fragments or bioclasts) between the two types, allow phosphorites that formed in upwelling, nutrient-rich and oxic-suboxic environments to be distinguished from those which formed in suboxic-anoxic organic-poor environments. A potential combined ore deposit (Fe-Mn crusts + phosphorites) with high REY contents, like the seamount phosphorites analyzed in this study (ΣREY=870 μg/g on average), could help supply the resources needed for green-tech and high-tech applications.
Tipologia del documento
Tesi di laurea
(Laurea magistrale)
Autore della tesi
Medri, Alessia
Relatore della tesi
Correlatore della tesi
Scuola
Corso di studio
Indirizzo
CURRICULUM C: RAW MATERIALS EXPLORATION AND SUSTAINABILITY
Ordinamento Cds
DM270
Parole chiave
marine phosphorite deposits,seamount phosphorites,rare earth elements,yttrium,resources,Tropic seamount,CISP
Data di discussione della Tesi
21 Luglio 2022
URI
Altri metadati
Tipologia del documento
Tesi di laurea
(NON SPECIFICATO)
Autore della tesi
Medri, Alessia
Relatore della tesi
Correlatore della tesi
Scuola
Corso di studio
Indirizzo
CURRICULUM C: RAW MATERIALS EXPLORATION AND SUSTAINABILITY
Ordinamento Cds
DM270
Parole chiave
marine phosphorite deposits,seamount phosphorites,rare earth elements,yttrium,resources,Tropic seamount,CISP
Data di discussione della Tesi
21 Luglio 2022
URI
Gestione del documento: