Petrogenetic significance of ocellar camptonite dykes in the Ditrau Alkaline Massif, Romania

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Batki, Aniko (author)

Petrogenetic significance of ocellar camptonite dykes in the Ditrau Alkaline Massif, Romania

Article/chapterEnglish2014

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Elsevier BV,2014
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LIBRIS-ID:oai:DiVA.org:su-106587
https://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-106587URI
https://doi.org/10.1016/j.lithos.2014.04.022DOI

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Language:English
Summary in:English

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Subject category:ref swepub-contenttype
Subject category:art swepub-publicationtype

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AuthorCount:4;
Camptonite dykes intrude the rift-related Mesozoic igneous body of the Ditrau Alkaline Massif, Eastern Carpathians, Romania. We present and discuss mineral chemical data, major and trace elements, and the Nd isotopic compositions of the dykes in order to define their nature and origin. The dykes are classified as the clinopyroxene-bearing (camptonite-I) and clinopyroxene-free (camptonite-II) varieties. Camptonite-I consists of aluminian-ferroan diopside phenocrysts accompanied by kaersutite, subordinate Ti-rich annite, albite to oligoclase and abundant calcite-albite ocelli. Camptonite-II comprises K-rich hastingsite to magnesiohastingsite, Ti-rich annite, albite to andesine, abundant accessory titanite and apatite, and silicate ocelli filled mainly with plagioclase (An(4-34)). Age-corrected Nd-143/Nd-144 ratios vary from 0.51258 to 0.51269. The high epsilon(Nd) values of +4.0 to +6.1 which are consistent with intra-plate composition, together with light rare earth element (LREE), large ion lithophile element (LIE) and high field strength element (HFSE) enrichment in the camptonites is ascribed to the formation of small melt batches of a metasomatised sub-lithospheric mantle source. The presence of an asthenospheric 'high mu' ocean island basalt (HIMU-OIB)-type mantle component in the source region has also been revealed. A 1-4% degree of partial melting of an enriched garnet Iherzolite mantle source containing pargasitic amphibole followed by fractionation is inferred to have been involved in the generation of the camptonites. They are deduced to be parental melts to the Ditrau Alkaline Massif.

Subject headings and genre

NATURVETENSKAP Geovetenskap och miljövetenskap Geologi hsv//swe
NATURAL SCIENCES Earth and Related Environmental Sciences Geology hsv//eng
Camptonite
Ocelli
Metasomatised sub-lithosphere
HIMU-OIB mantle component
Intra-plate magmatism
Ditrau Alkaline Massif

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Pal-Molnar, Elemer (author)
Dobosi, Gabor (author)
Skelton, AlasdairStockholms universitet,Institutionen för geologiska vetenskaper(Swepub:su)skelt (author)
Stockholms universitetInstitutionen för geologiska vetenskaper (creator_code:org_t)

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In:Lithos: Elsevier BV200, s. 181-1960024-49371872-6143

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NATURAL SCIENCES: NATURAL SCIENCES; and Earth and Relate ...; and Geology

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