Results 21 to 30 of about 147 (81)
Metalogenia de las carbonatitas en dominios plutónicos, subvolcánicos y volcánicos: Tchivira, Bonga y Catanda, Angola [PDF]
[spa] Se han seleccionado tres carbonatitas de la estructura tectónica de Lucapa en Angola representativas de diferentes niveles de emplazamiento de los magmas: plutónico (Tchivira), subvolcánico (Bonga) y volcánico (Catanda).
Bambi, Aurora Cuaiela Joao Mateus
core +7 more sources
Archetypal kimberlite from the Maniitsoq region, southern West Greenland and analogy to South Africa [PDF]
Ultramafic dyke rocks with kimberlitic megacrysts and mantle nodules have been known for decades from the northern part of the Archaean block and adjacent Proterozoic terranes in southern West Greenland (Fig.
Jebens, Martin +3 more
core +1 more source
Olivine from the deep mantle-derived rocks, such as ultramafic lamprophyres, carries important information about the composition of the mantle source, the processes of mantle metasomatism, the origin of specific silicate-carbonate melts, as well as the ...
Ilya Prokopyev +4 more
core +1 more source
The once-contiguous North Atlantic craton (NAC) is crosscut by the Labrador Sea that opened during the Early Cenozoic after extensive Mesozoic continental rifting and removal of cratonic mantle.
Foley, Stephen F. +6 more
core +1 more source
© 2020 To provide new insights into the origin and evolution of ultramafic lamprophyres (UMLs) and their mantle source, we examined two UML (aillikite and damtjernite) occurrences of different ages in the western portion of the Siberian Craton (Ilbokich ...
Batalin G.A. +10 more
core
Late Cretaceous ultramafic lamprophyres and carbonatites from the Delitzsch Complex, Germany
The Delitzsch Complex consists of late Cretaceous ultramafic lamprophyres and carbonatitic rocks. They form dikes and diatremes, emplaced into Palaeozoic to lower Permian volcanic and sedimentary rocks, and are covered by up to 120 m thick sequences of ...
Kämpf, H., Romer, R.L., Krüger, J.C.
core +1 more source
Late Jurassic ultramafic lamprophyre (UML) sills and dikes occur as 3 km-long intrusions within the allochthonous Whara Formation of the Batain nappes, eastern Oman.
S. Nasir (1385112)
core +1 more source
Petrogenesis of juvenile pelletal lapilli in ultramafic lamprophyres. [PDF]
Prokopyev I +5 more
europepmc +1 more source
Perturbation of the deep-Earth carbon cycle in response to the Cambrian Explosion. [PDF]
Giuliani A +9 more
europepmc +1 more source
Remnants of early Earth differentiation in the deepest mantle-derived lavas. [PDF]
Giuliani A +3 more
europepmc +1 more source

