An Ovoid K-feldspar mantled by Na-feldspar is called rapakivi. Rapakivi may form either by (1) decompression during ascent of felsic magma through the crust to a shallow magma chamber or by (2) mixing of mafic- and felsic-magma within a magma chamber. We
Kaiser, Jason F.
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The diverse mesoscopic structures in rapakivi granites of Southeastern Finland : episyenites and related processes [PDF]
Peralkaline syenites and granites form a small yet significant group of rocks within the A-type granite association worldwide. Although the Mid-Proterozoic Finnish rapakivi (A-type) granite complexes are voluminous in southern Finland, they only host ...
Suikkanen, Einari
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Microorganisms in Superficial Deposits on the Stone Monuments in Saint Petersburg. [PDF]
Sazanova KV +5 more
europepmc +1 more source
Radiological Hazard Evaluation of Some Egyptian Magmatic Rocks Used as Ornamental Stone: Petrography and Natural Radioactivity. [PDF]
Lasheen ESR +5 more
europepmc +1 more source
Active anaerobic methane oxidation and sulfur disproportionation in the deep terrestrial subsurface. [PDF]
Bell E +7 more
europepmc +1 more source
Rio Branco rapakivi batholith magmatism, Southwestern of Amazonian Craton - MT
Rio Branco Rapakivi Batholith is located on the southwestern portion of the Amazonian Craton in Mato Grosso and belongs to the Cachoeirinha Tectonic Domain, part of the Rio Negro-Juruena Geochronological Province, Central Brasil.
de Araújo, Larissa Marques Barbosa +1 more
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The Margaree pluton extends for >40 km along the axis of the Ganderian Aspy terrane of northern Cape Breton Island, Nova Scotia. The pluton consists mainly of coarse-grained megacrystic syenogranite, intruded by small bodies of medium-grained ...
White, Chris E +3 more
core +1 more source
Mesoproterozoic Strike-Slip Faulting within the Åland Rapakivi Batholith, Southwestern Finland
Paleostress inversion analysis of outcrop data from brittle fault structures within the Mesoproterozoic 1.58 Ga Åland rapakivi granite, southwestern Finland, revealed two separate strike-slip faulting stages. Stage 1 is dominated by dextral slip along E–
Nicklas Nordbäck +5 more
doaj +1 more source
The Vehmaa rapakivi granite batholith - An assemblage of successive intrusions indicating a piston-type collapsing centre [PDF]
O. Selonen +3 more
doaj +1 more source
Long-lived Paleoproterozoic eclogitic lower crust. [PDF]
Buntin S +7 more
europepmc +1 more source

