Repozytorium Uniwersytetu Jagiellońskiego

Source rocks for heavy minerals in lower part of Menilite formation of Skole Nappe (Polish Flysch Carpathians), based on study of detrital garnet and tourmaline

Source rocks for heavy minerals in lower part of ...

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dc.contributor.author Salata, Dorota [SAP11018120] pl
dc.date.accessioned 2015-04-22T06:34:47Z
dc.date.available 2015-04-22T06:34:47Z
dc.date.issued 2013 pl
dc.identifier.issn 0208-9068 pl
dc.identifier.uri http://ruj.uj.edu.pl/xmlui/handle/item/5422
dc.language eng pl
dc.rights Dodaję tylko opis bibliograficzny *
dc.rights.uri *
dc.title Source rocks for heavy minerals in lower part of Menilite formation of Skole Nappe (Polish Flysch Carpathians), based on study of detrital garnet and tourmaline pl
dc.type JournalArticle pl
dc.description.physical 1-17 pl
dc.identifier.weblink http://www.asgp.pl/83_1_001_017 pl
dc.abstract.en The study focused on the chemistry of detrital garnet and tourmaline from sediments of the Boryslav and Kliva Sandstone types in the Oligocene part of the Menilite Formation of the Skole Nappe (Western Outer Carpathians, Poland), with regard to provenance. Almandine and almandine-pyrope compositional varieties are the most common garnets, with minor almandine-pyrope-grossular garnet. Scarce garnet grains, with grossular and spessartine as the dominant end-members, are also present. The tourmaline belongs to the alkali tourmaline principal group and represents the schörl-dravite series. The detrital garnet and tourmaline display strong, compositional similarities to minerals, occurring in igneous and metamorphic rocks of the Bohemian Massif, as well as to detrital grains, deposited within the internal basins of the massif. This suggests that the primary rocks for the garnet and tourmaline may be crystalline complexes of the Bohemian Massif. However, other uplifted areas, similar to the complexes of the Bohemian Massif, cannot be ruled out. Such hypothetical areas could be located in the northern foreland of the Carpathian basins. Euhedral tourmaline and other minerals, occurring in the heavy- mineral assemblages studied, most probably were derived from eroded and presently not exposed, crystalline complexes, originally situated in the Skole Basin foreland or within the basin. pl
dc.subject.en detrital tourmaline pl
dc.subject.en detrital garnet pl
dc.subject.en provenance pl
dc.subject.en flysch pl
dc.subject.en Menilite formation pl
dc.subject.en Oligocene pl
dc.subject.en Skole Nappe pl
dc.description.volume 83 pl
dc.description.number 1 pl
dc.title.journal Annales Societatis Geologorum Poloniae pl
dc.language.container eng pl
dc.date.accession 2015-03-11 pl
dc.affiliation Wydział Biologii i Nauk o Ziemi : Instytut Nauk Geologicznych pl
dc.subtype Article pl
dc.rights.original OTHER; otwarte czasopismo; ostateczna wersja wydawcy; w momencie opublikowania; 0; pl
.pointsMNiSW [2013 A]: 20


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