Origin of unusual HREE-Mo-rich carbonatites in the Qinling orogen, China
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F62156489%3A43210%2F16%3A43909884" target="_blank" >RIV/62156489:43210/16:43909884 - isvavai.cz</a>
Result on the web
<a href="http://dx.doi.org/10.1038/srep37377" target="_blank" >http://dx.doi.org/10.1038/srep37377</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1038/srep37377" target="_blank" >10.1038/srep37377</a>
Alternative languages
Result language
angličtina
Original language name
Origin of unusual HREE-Mo-rich carbonatites in the Qinling orogen, China
Original language description
Carbonatites, usually occurring within intra-continental rift-related settings, have strong light rare earth element (LREE) enrichment; they rarely contain economic heavy REE (HREE). Here, we report the identification of Late Triassic HREE-Mo-rich carbonatites in the northernmost Qinling orogen. The rocks contain abundant primary HREE minerals and molybdenite. Calcite-hosted fluid inclusions, inferred to represent a magmatic-derived aqueous fluid phase, contain significant concentrations of Mo (~17 ppm), reinforcing the inference that these carbonatitic magmas had high Mo concentrations. By contrast, Late Triassic carbonatites in southernmost Qinling have economic LREE concentrations, but are depleted in HREE and Mo. Both of these carbonatite types have low δ26Mg values (-1.89 to - 1.07%o), similar to sedimentary carbonates, suggesting a recycled sediment contribution for REE enrichment in their mantle sources. We propose that the carbonatites in the Qinling orogen were formed, at least in part, by the melting of a subducted carbonate-bearing slab, and that 10 Ma younger carbonatite magmas in the northernmost Qinling metasomatized the thickened eclogitic lower crust to produce high levels of HREE and Mo.
Czech name
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Czech description
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Classification
Type
J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database
CEP classification
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OECD FORD branch
10505 - Geology
Result continuities
Project
<a href="/en/project/LQ1601" target="_blank" >LQ1601: CEITEC 2020</a><br>
Continuities
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)
Others
Publication year
2016
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
Scientific Reports
ISSN
2045-2322
e-ISSN
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Volume of the periodical
6
Issue of the periodical within the volume
18 November
Country of publishing house
GB - UNITED KINGDOM
Number of pages
10
Pages from-to
"Nestrankovano"
UT code for WoS article
000388256300001
EID of the result in the Scopus database
2-s2.0-84995948863