Anagram & Information om | Engelska ordet PELITES

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• 93 Ga, unconformably and in places structurally overlain by a supracrustal sequence of shallow water quartzites and pelites, the Muva Supergroup, in which sparse volcanic tuffs have given ages of between 1.
• Ackermann (1950) for a folded supracrustal shallow water succession of quartzites and pelites in the Irumide Belt of Zambia.
• The lower volcanic section is covered by garnet and diopside bearing calc–silicate layers and finely layered metasediments composed of coarse-grained actinolite, hornblende and biotite followed by pelites and semi-pelites that are intruded by separate sills.
• It consists of Proterozoic orthogneisses and early Paleozoic volcanic (amphibolites with MORB-protoliths and tuffs) and sedimentary (pelites, calcareous schists and marbles) rocks that were metamorphosed at high grade during the Hercynian orogeny (up to amphibolite facies).
• The zone consists of Proterozoic orthogneisses and early Paleozoic volcanic (amphibolites with MORB-protoliths and tuffs) and sedimentary (pelites, calcareous schists and marbles) rocks that were metamorphosed at high grade during the Hercynian orogeny (up to amphibolite facies).
• This flysch sequence consisted of monotonous, rhythmically interbedded clayey (pelites) and sandy (greywackes) deposits reaching the astonishing thickness of 15 kilometers in places.
• The western belt is dark-gray slate/phyllite with minor interbedding of pelites of quartz-carbonate granulite.
• They are a complex mix of psammites, phyllites, pelites, semipelites, quartzites and meta-limestones and other lithologies originally laid down as marine sand, mud, silt etc.
• The area of the Cañadón Calcáreo also includes lacustrine and palustrine rocks, including shales, pelites, psammites and coarse clastics.
• The group consists of a mixture of psammites, semi-pelites and pelites, which are deformed and no sedimentological analysis has been carried out, nor have the group been sampled for detrital zircons.

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