Article (Scientific journals)
In-situ trace element and Sr isotope signature of apatite: A new key to unravelling the genesis of polymetallic mineralisation in black shales of the Early Cambrian Niutitang Formation, Southern China
Decrée, Sophie; Pašava, Jan; Baele, Jean-Marc et al.
2022In Ore Geology Reviews, 150, p. 105130
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Keywords :
Hydrothermal brines; Mafic affinity; Ni-Mo-PGE sulphide ore; Phosphorite; Rare Earth Elements; Black shales; Early cambrians; Hydrothermal brine; Ni-mo-PGE sulphide ore; Southern China; Sr isotopes; Sulphide ores; Traces elements; Geology; Geochemistry and Petrology; Economic Geology
Abstract :
[en] The Early Cambrian Mo-Ni-PGE sulphidic black shale in the Niutitang Formation on the margin of the Yangtze Craton (Southern China) is known for its extremely high metal concentrations. It is also very rich in phosphate that formed contemporaneously with the sulphides. Detailed petrological as well as in-situ trace element and Sr isotope analyses of authigenic apatite revealed new information on the metallogenesis of this enigmatic rock unit. In the ore bed, apatite forms nodules or is found in phosphatic (phoslithoclasts) and sulphide clasts. In the latter, the replacement of organic matter and sulphides by apatite microspherules suggests a microbially mediated phosphogenesis. Enrichment in middle rare earth elements emphasizes the role played by Fe-oxyhydroxides and organic matter in element scavenging. Moderately reducing conditions are supported by a lack of Ce and Eu anomalies. The trace element signature of apatite and its initial 87Sr/86Sr (0.7032–0.7190), which is - for a group of analyses - well below the signature of Lower Cambrian seawater, points to some contribution from mafic rock-sourced hydrothermal brines. This effectively explains the exceptional enrichment of Ni and PGE in the sulphides. Seawater remains, however, the preferred source for other elements such as P and Mo.
Disciplines :
Earth sciences & physical geography
Author, co-author :
Decrée, Sophie;  Royal Belgian Institute of Natural Sciences-Geological Survey of Belgium, Brussels, Belgium
Pašava, Jan;  Czech Geological Survey, Prague, Czech Republic
Baele, Jean-Marc  ;  Université de Mons - UMONS
Mercadier, Julien;  Université de Lorraine, CNRS, CREGU, GeoRessources Lab, Vandoeuvre-lès-Nancy, France
Rösel, Delia;  Department of Earth Sciences, University of Göteborg, Göteborg, Sweden
Frimmel, Hartwig;  Bavarian Georesources Centre, Dept. of Geodynamics and Geomaterials Research, Institute of Geography and Geology, University of Würzburg, Germany
Language :
English
Title :
In-situ trace element and Sr isotope signature of apatite: A new key to unravelling the genesis of polymetallic mineralisation in black shales of the Early Cambrian Niutitang Formation, Southern China
Publication date :
November 2022
Journal title :
Ore Geology Reviews
ISSN :
0169-1368
eISSN :
1872-7360
Publisher :
Elsevier B.V.
Volume :
150
Pages :
105130
Peer reviewed :
Peer Reviewed verified by ORBi
Research unit :
F401 - Géologie fondamentale et appliquée
Research institute :
R400 - Institut de Recherche en Science et Ingénierie des Matériaux
Funders :
Julius-Maximilians-Universität Würzburg
Agence Nationale de la Recherche
Česká geologická služba
Belgian Federal Science Policy Office
CNRS
Funding text :
The authors would like to express their gratitude to Ulrich Schüssler and Stefan Höhn for their assistance in acquiring electron microprobe analyses at the University of Würzburg. Chantal Peiffert is warmly thanked for help in acquiring LA-ICP-MS analyses. The authors thank Thomas Goovaerts for helping to improve the English of the manuscript. The research was partly funded by the Belgian Federal Science Policy Office (BELSPO) - BRAIN program (DESIRED projects). The LA-ICP-MS laboratory from GeoRessources was partly funded by the French National Research Agency through the national program “Investissements d'avenir” of the Labex Ressources21 with the reference ANR-10-LABX-21-RESSOURCES21. This is also a contribution to the Strategic Research Plan of the Czech Geological Survey (DKRVO 2018-2022). The authors also warmly thank Franco Pirajno (Editor), and two anonymous reviewers, for helpful remarks on the manuscript. Their comments have contributed to improve substantially the quality of this paper.The authors would like to express their gratitude to Ulrich Schüssler and Stefan Höhn for their assistance in acquiring electron microprobe analyses at the University of Würzburg. Chantal Peiffert is warmly thanked for help in acquiring LA-ICP-MS analyses. The authors thank Thomas Goovaerts for helping to improve the English of the manuscript. The research was partly funded by the Belgian Federal Science Policy Office (BELSPO) - BRAIN program (DESIRED projects). The LA-ICP-MS laboratory from GeoRessources was partly funded by the French National Research Agency through the national program “Investissements d’avenir” of the Labex Ressources21 with the reference ANR-10-LABX-21-RESSOURCES21. This is also a contribution to the Strategic Research Plan of the Czech Geological Survey (DKRVO 2018-2022). The authors also warmly thank Franco Pirajno (Editor), and two anonymous reviewers, for helpful remarks on the manuscript. Their comments have contributed to improve substantially the quality of this paper.
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