FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2223021372> ?p ?o ?g. }

• W2223021372 abstract "Metallogeny aims to reconstruct the genesis and distribution of ore deposits, focusing on their relationships in space and time. For decades, Europe is highly dependent on imports of mineral resources. Characterizing and quantifying the petrological, mineralogical and chemical contents of the ores outside Europe enable to recognize their economic potential. Manganese is a little-known element occurring in natural environments in the form of silicate (Braunite; Mn 7 SiO 12), carbonate (Rhodocrosite; MnCO 3) or oxide (Pyrolusite; MnO 2). It is the 12 th abundant element in the earth crust and the 4 th produced element worldwide in 2011 (International Manganese Institute). It holds a major role in the world market due to its use as alloys in steelmaking processes (90% of the Mn uses). The large amounts of Mn-oxides occurring along the WSW-ENE 30 kilometers ore belt give to the Imini district a key role on manganese production in Morocco with raw concentrations reaching more than 72-88 wt. %. The three stratabound layers of approximately 1 meter-thick, trapped in a 14 meters-thick dolostone of Cenomanian-Turonian in age (100.5 to 89.8 million years old – hereafter noted Ma), show mainly pyrolusite (MnO 2) and small amounts of hollandite group minerals [(Ba,K,Pb)Mn 8 O 16 ], romanechite [(H 2 O,Ba) 2 Mn 5 O 10 ] and lithiophorite [(Al,Li)MnO 2 (OH) 2 ]. These minerals are responsible of the high grade of the deposits without any major contamination such as of Fe, Si, P, S … By coupling field observations, microscope analyses and X-ray diffraction we can provide some evidences about the ore formation. Deposition and concentration of manganese oxides follow a two steps mineralizing sequence with (1) a replacement of the host rock dolostone followed by (2) the formation of banded concretions in an open system enhanced by fluid circulation. These mineralogical observations coupled with geochemical and chronological data indicate a multistage formation in a high oxygenized karstic environment. After dolostone formation (100.5-89.8 Ma), the mineralized layers were formed in several stages according to Ar-Ar and K-Ar ages of ~70 Ma, ~50-45 Ma and ~20-14 Ma. The manganese oxide minerals of the Imini district may occur coevally to two tectonic phases in the Atlas Mountain of Morocco. Although the source of Mn is still debated, the WSW-ENE orientation of the ore belt may indicate a tectonic link to the mineralization. This structural relationship and the more permeable character of the host rock dolostone compared to surrounding rocks explain the location of manganese oxides in the Imini area." @default.
• W2223021372 created "2016-06-24" @default.
• W2223021372 creator A5020370423 @default.
• W2223021372 creator A5020646283 @default.
• W2223021372 creator A5033727965 @default.
• W2223021372 creator A5041305433 @default.
• W2223021372 creator A5043515651 @default.
• W2223021372 creator A5046514907 @default.
• W2223021372 creator A5060040805 @default.
• W2223021372 creator A5062709678 @default.
• W2223021372 creator A5073012090 @default.
• W2223021372 date "2014-01-01" @default.
• W2223021372 modified "2023-09-23" @default.
• W2223021372 title "Genesis of Manganese Ore Deposits of the Imini District (Morocco)" @default.
• W2223021372 hasPublicationYear "2014" @default.
• W2223021372 type Work @default.
• W2223021372 sameAs 2223021372 @default.
• W2223021372 citedByCount "0" @default.
• W2223021372 crossrefType "journal-article" @default.
• W2223021372 hasAuthorship W2223021372A5020370423 @default.
• W2223021372 hasAuthorship W2223021372A5020646283 @default.
• W2223021372 hasAuthorship W2223021372A5033727965 @default.
• W2223021372 hasAuthorship W2223021372A5041305433 @default.
• W2223021372 hasAuthorship W2223021372A5043515651 @default.
• W2223021372 hasAuthorship W2223021372A5046514907 @default.
• W2223021372 hasAuthorship W2223021372A5060040805 @default.
• W2223021372 hasAuthorship W2223021372A5062709678 @default.
• W2223021372 hasAuthorship W2223021372A5073012090 @default.
• W2223021372 hasConcept C119127063 @default.
• W2223021372 hasConcept C121332964 @default.
• W2223021372 hasConcept C127313418 @default.
• W2223021372 hasConcept C17409809 @default.
• W2223021372 hasConcept C178790620 @default.
• W2223021372 hasConcept C185592680 @default.
• W2223021372 hasConcept C191897082 @default.
• W2223021372 hasConcept C192562407 @default.
• W2223021372 hasConcept C199289684 @default.
• W2223021372 hasConcept C26148502 @default.
• W2223021372 hasConcept C2776062231 @default.
• W2223021372 hasConcept C2776268066 @default.
• W2223021372 hasConcept C2776277684 @default.
• W2223021372 hasConcept C2776432453 @default.
• W2223021372 hasConcept C2777335606 @default.
• W2223021372 hasConcept C2778410265 @default.
• W2223021372 hasConcept C2778818709 @default.
• W2223021372 hasConcept C2779002002 @default.
• W2223021372 hasConcept C2779642852 @default.
• W2223021372 hasConcept C2780181037 @default.
• W2223021372 hasConcept C2780659211 @default.
• W2223021372 hasConcept C2993225395 @default.
• W2223021372 hasConcept C37914503 @default.
• W2223021372 hasConcept C528890316 @default.
• W2223021372 hasConcept C542268612 @default.
• W2223021372 hasConceptScore W2223021372C119127063 @default.
• W2223021372 hasConceptScore W2223021372C121332964 @default.
• W2223021372 hasConceptScore W2223021372C127313418 @default.
• W2223021372 hasConceptScore W2223021372C17409809 @default.
• W2223021372 hasConceptScore W2223021372C178790620 @default.
• W2223021372 hasConceptScore W2223021372C185592680 @default.
• W2223021372 hasConceptScore W2223021372C191897082 @default.
• W2223021372 hasConceptScore W2223021372C192562407 @default.
• W2223021372 hasConceptScore W2223021372C199289684 @default.
• W2223021372 hasConceptScore W2223021372C26148502 @default.
• W2223021372 hasConceptScore W2223021372C2776062231 @default.
• W2223021372 hasConceptScore W2223021372C2776268066 @default.
• W2223021372 hasConceptScore W2223021372C2776277684 @default.
• W2223021372 hasConceptScore W2223021372C2776432453 @default.
• W2223021372 hasConceptScore W2223021372C2777335606 @default.
• W2223021372 hasConceptScore W2223021372C2778410265 @default.
• W2223021372 hasConceptScore W2223021372C2778818709 @default.
• W2223021372 hasConceptScore W2223021372C2779002002 @default.
• W2223021372 hasConceptScore W2223021372C2779642852 @default.
• W2223021372 hasConceptScore W2223021372C2780181037 @default.
• W2223021372 hasConceptScore W2223021372C2780659211 @default.
• W2223021372 hasConceptScore W2223021372C2993225395 @default.
• W2223021372 hasConceptScore W2223021372C37914503 @default.
• W2223021372 hasConceptScore W2223021372C528890316 @default.
• W2223021372 hasConceptScore W2223021372C542268612 @default.
• W2223021372 hasOpenAccess W2223021372 @default.
• W2223021372 hasRelatedWork W2015671727 @default.
• W2223021372 hasRelatedWork W2017344213 @default.
• W2223021372 hasRelatedWork W2036173815 @default.
• W2223021372 hasRelatedWork W2042069658 @default.
• W2223021372 hasRelatedWork W2297672059 @default.
• W2223021372 hasRelatedWork W2316585823 @default.
• W2223021372 hasRelatedWork W2319525270 @default.
• W2223021372 hasRelatedWork W2323848254 @default.
• W2223021372 hasRelatedWork W2370795607 @default.
• W2223021372 hasRelatedWork W2743321551 @default.
• W2223021372 hasRelatedWork W2811510947 @default.
• W2223021372 hasRelatedWork W2892207910 @default.
• W2223021372 hasRelatedWork W2954836989 @default.
• W2223021372 hasRelatedWork W2954999101 @default.
• W2223021372 hasRelatedWork W2955347357 @default.
• W2223021372 hasRelatedWork W3003863698 @default.
• W2223021372 hasRelatedWork W3022030047 @default.
• W2223021372 hasRelatedWork W3164148012 @default.
• W2223021372 hasRelatedWork W2002981688 @default.
• W2223021372 hasRelatedWork W2961244470 @default.
• W2223021372 isParatext "false" @default.

• next