Molybdenum-uranium-vanadium geochemistry in the lower Paleozoic Alum Shale of Scandinavia: Implications for vanadium exploration

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Standard

Molybdenum-uranium-vanadium geochemistry in the lower Paleozoic Alum Shale of Scandinavia : Implications for vanadium exploration. / Bian, Leibo; Schovsbo, Niels H.; Chappaz, Anthony; Zheng, Xiaowei; Nielsen, Arne Thorshoj; Ulrich, Thomas; Wang, Xibo; Dai, Shifeng; Galloway, Jennifer M.; Malachowska, Aleksandra; Xu, Xuhui; Sanei, Hamed.

I: International Journal of Coal Geology, Bind 239, 103730, 2021.

Publikation: Bidrag til tidsskrift › Tidsskriftartikel › Forskning › fagfællebedømt

Harvard

Bian, L, Schovsbo, NH, Chappaz, A, Zheng, X, Nielsen, AT, Ulrich, T, Wang, X, Dai, S, Galloway, JM, Malachowska, A, Xu, X & Sanei, H 2021, 'Molybdenum-uranium-vanadium geochemistry in the lower Paleozoic Alum Shale of Scandinavia: Implications for vanadium exploration', International Journal of Coal Geology, bind 239, 103730. https://doi.org/10.1016/j.coal.2021.103730

APA

Bian, L., Schovsbo, N. H., Chappaz, A., Zheng, X., Nielsen, A. T., Ulrich, T., Wang, X., Dai, S., Galloway, J. M., Malachowska, A., Xu, X., & Sanei, H. (2021). Molybdenum-uranium-vanadium geochemistry in the lower Paleozoic Alum Shale of Scandinavia: Implications for vanadium exploration. International Journal of Coal Geology, 239, [103730]. https://doi.org/10.1016/j.coal.2021.103730

Vancouver

Bian L, Schovsbo NH, Chappaz A, Zheng X, Nielsen AT, Ulrich T o.a. Molybdenum-uranium-vanadium geochemistry in the lower Paleozoic Alum Shale of Scandinavia: Implications for vanadium exploration. International Journal of Coal Geology. 2021;239. 103730. https://doi.org/10.1016/j.coal.2021.103730

Author

Bian, Leibo ; Schovsbo, Niels H. ; Chappaz, Anthony ; Zheng, Xiaowei ; Nielsen, Arne Thorshoj ; Ulrich, Thomas ; Wang, Xibo ; Dai, Shifeng ; Galloway, Jennifer M. ; Malachowska, Aleksandra ; Xu, Xuhui ; Sanei, Hamed. / Molybdenum-uranium-vanadium geochemistry in the lower Paleozoic Alum Shale of Scandinavia : Implications for vanadium exploration. I: International Journal of Coal Geology. 2021 ; Bind 239.

Bibtex

@article{a578f65defd74abf9e91ef10593d5fbc,
title = "Molybdenum-uranium-vanadium geochemistry in the lower Paleozoic Alum Shale of Scandinavia: Implications for vanadium exploration",
abstract = "This paper investigates the hyper-enrichments of molybdenum (Mo), uranium (U), and vanadium (V) in the lower Paleozoic, Alum Shale of Denmark, Sweden, Norway, and Estonia. Molybdenum and U are mainly associated with organic matter and the highest contents are found in the Furongian part of the Alum Shale. This Furongian hyper-enrichment of Mo and U commenced with the Steptoean Positive Carbon Isotope Excursion (SPICE) event. The temporal distribution of V content increases moderately from the Miaolingian to the Furongian, followed by a significant increase in the Early Ordovician. In addition, the vanadium content generally increases towards the offshore, distal part of the Alum Shale basin. The geochemical affinity of V seems to change from organic matter in the Cambrian to minerals in the Early Ordovician. The hyper-enrichment of V in the Lower Ordovician succession appears to result from upwelling of deep oceanic water. The spatial distribution of V in the Alum Shale indicates that the highest concentrations are located in Scania, southernmost Sweden.",
keywords = "Molybdenum (Mo), Uranium (U), Vanadium (V), Alum Shale, Scandinavia, Cambrian, Ordovician",
author = "Leibo Bian and Schovsbo, {Niels H.} and Anthony Chappaz and Xiaowei Zheng and Nielsen, {Arne Thorshoj} and Thomas Ulrich and Xibo Wang and Shifeng Dai and Galloway, {Jennifer M.} and Aleksandra Malachowska and Xuhui Xu and Hamed Sanei",
year = "2021",
doi = "10.1016/j.coal.2021.103730",
language = "English",
volume = "239",
journal = "International Journal of Coal Geology",
issn = "0166-5162",
publisher = "Elsevier",

}

RIS

TY - JOUR

T1 - Molybdenum-uranium-vanadium geochemistry in the lower Paleozoic Alum Shale of Scandinavia

T2 - Implications for vanadium exploration

AU - Bian, Leibo

AU - Schovsbo, Niels H.

AU - Chappaz, Anthony

AU - Zheng, Xiaowei

AU - Nielsen, Arne Thorshoj

AU - Ulrich, Thomas

AU - Wang, Xibo

AU - Dai, Shifeng

AU - Galloway, Jennifer M.

AU - Malachowska, Aleksandra

AU - Xu, Xuhui

AU - Sanei, Hamed

PY - 2021

Y1 - 2021

N2 - This paper investigates the hyper-enrichments of molybdenum (Mo), uranium (U), and vanadium (V) in the lower Paleozoic, Alum Shale of Denmark, Sweden, Norway, and Estonia. Molybdenum and U are mainly associated with organic matter and the highest contents are found in the Furongian part of the Alum Shale. This Furongian hyper-enrichment of Mo and U commenced with the Steptoean Positive Carbon Isotope Excursion (SPICE) event. The temporal distribution of V content increases moderately from the Miaolingian to the Furongian, followed by a significant increase in the Early Ordovician. In addition, the vanadium content generally increases towards the offshore, distal part of the Alum Shale basin. The geochemical affinity of V seems to change from organic matter in the Cambrian to minerals in the Early Ordovician. The hyper-enrichment of V in the Lower Ordovician succession appears to result from upwelling of deep oceanic water. The spatial distribution of V in the Alum Shale indicates that the highest concentrations are located in Scania, southernmost Sweden.

AB - This paper investigates the hyper-enrichments of molybdenum (Mo), uranium (U), and vanadium (V) in the lower Paleozoic, Alum Shale of Denmark, Sweden, Norway, and Estonia. Molybdenum and U are mainly associated with organic matter and the highest contents are found in the Furongian part of the Alum Shale. This Furongian hyper-enrichment of Mo and U commenced with the Steptoean Positive Carbon Isotope Excursion (SPICE) event. The temporal distribution of V content increases moderately from the Miaolingian to the Furongian, followed by a significant increase in the Early Ordovician. In addition, the vanadium content generally increases towards the offshore, distal part of the Alum Shale basin. The geochemical affinity of V seems to change from organic matter in the Cambrian to minerals in the Early Ordovician. The hyper-enrichment of V in the Lower Ordovician succession appears to result from upwelling of deep oceanic water. The spatial distribution of V in the Alum Shale indicates that the highest concentrations are located in Scania, southernmost Sweden.

KW - Molybdenum (Mo)

KW - Uranium (U)

KW - Vanadium (V)

KW - Alum Shale

KW - Scandinavia

KW - Cambrian

KW - Ordovician

U2 - 10.1016/j.coal.2021.103730

DO - 10.1016/j.coal.2021.103730

M3 - Journal article

VL - 239

JO - International Journal of Coal Geology

JF - International Journal of Coal Geology

SN - 0166-5162

M1 - 103730

ER -

ID: 261271358