Academic Journal

High-Resolution Analysis of Critical Minerals and Elements in Fe–Mn Crusts from the Canary Island Seamount Province (Atlantic Ocean)

التفاصيل البيبلوغرافية
العنوان: High-Resolution Analysis of Critical Minerals and Elements in Fe–Mn Crusts from the Canary Island Seamount Province (Atlantic Ocean)
المؤلفون: Marino, Egidio, González, Francisco Javier, Lunar Hernández, Rosario, Reyes, Jesús, Medialdea, Teresa, Castillo Carrión, Mercedes, Bellido, Eva, Somoza Losada, Luis
بيانات النشر: MDPI
سنة النشر: 2018
المجموعة: Universidad Complutense de Madrid (UCM): E-Prints Complutense
مصطلحات موضوعية: 553.3, 553.43, ferromanganese crusts, high-resolution analysis, critical elements, co-chronometer, diagenesis, hydrogenesis, phosphatization, Geoquímica, Mineralogía (Geología), Petrología, 2503 Geoquímica, 2506.11 Mineralogía
الوصف: Two Fe–Mn crusts among 35 samples, from six seamounts in the Canary Island Seamount Province, were selected as representatives of the endpoint members of two distinct types of genetic processes, i.e., mixed diagenetic/hydrogenetic and purely hydrogenetic. High-resolution analyses pursued the main aim of distinguishing the critical elements and their association with mineral phases and genetic processes forming a long-lived Fe–Mn crust. The Fe–Mn crust collected on the Tropic Seamount is composed of dense laminations of Fe-vernadite (>90%) and goethite group minerals, reflecting the predominance of the hydrogenetic process during their formation. Based on high-resolution age calculation, this purely hydrogenetic crust yielded an age of 99 Ma. The Fe–Mn crust collected on the Paps Seamount shows a typical botryoidal surface yielding an age of 30 Ma. electron probe microanalyzer (EPMA) spot analyses show two main types of manganese oxides, indicating their origin: (i) hydrogenetic Fe-vernadite, the main Mn oxide, and (ii) laminations of interlayered buserite and asbolane. Additionally, the occurrence of calcite, authigenic carbonate fluor-apatite (CFA) and palygorskite suggests early diagenesis and pervasive phosphatization events. Sequential leaching analysis indicated that Co, Ni, Cu, Ba and Ce are linked to Mn minerals. Therefore, Mn-oxides are enriched in Ni and Cu by diagenetic processes or in Co and Ce by hydrogenetic processes. On the other hand, Fe-oxides concentrate V, Zn, As and Pb. Moreover, the evidence of HREE enrichment related to Fe-hydroxides is confirmed in the mixed hydrogenetic/diagenetic crust. ; Depto. de Mineralogía y Petrología ; Fac. de Ciencias Geológicas ; TRUE ; Unión Europea. H2020 ; Ministerio de Economía y Competitividad (MINECO) ; Instituto Geológico y Minero de España (IGME) ; pub
نوع الوثيقة: article in journal/newspaper
وصف الملف: application/pdf
اللغة: English
تدمد: 2075-163X
Relation: REMIMARES (IGME-2571); (EXPLOSEA (CTM2016-75947-R); SUBVENT (CGL2012-39524-C02); CTM2010-09496-E); GeoERA-MINDeSEA (731166); EMODnet-Geology (EASME/EMFF/2016/1.31.2-Lot 1/SI2.750862); FPU014/06774; https://www.mdpi.com/2075-163X/8/7/285; https://hdl.handle.net/20.500.14352/13100
DOI: 10.3390/min8070285
الاتاحة: https://hdl.handle.net/20.500.14352/13100
https://doi.org/10.3390/min8070285
https://www.mdpi.com/2075-163X/8/7/285
Rights: Atribución 3.0 España ; open access ; https://creativecommons.org/licenses/by/3.0/es/
رقم الانضمام: edsbas.ADE16CCA
قاعدة البيانات: BASE
الوصف
تدمد:2075163X
DOI:10.3390/min8070285