From mantle roots to surface eruptions: Cenozoic and Mesozoic continental basaltic magmatism

0448855 - GFÚ 2016 DE eng J - Článek v odborném periodiku
Kämpf, H. - Németh, K. - Puziewicz, J. - Mrlina, Jan - Geissler, W.H.
From mantle roots to surface eruptions: Cenozoic and Mesozoic continental basaltic magmatism.
International Journal of Earth Sciences. Roč. 104, č. 8 (2015), s. 1909-1912. ISSN 1437-3254. E-ISSN 1437-3262
Institucionální podpora: RVO:67985530
Klíčová slova: continental basaltic volcanism * BASALT 2013 conference * Cenozoic * Mesozoic
Kód oboru RIV: DC - Seismologie, vulkanologie a struktura Země
Impakt faktor: 2.133, rok: 2015

Basaltic volcanism is an important process in shaping large areas of the Earth’s surface, not only in continental extensional environments and at the ocean floor. This special issue contains a collection of fifteen papers that are dedicated to recent researches on various aspects of continental basaltic magmatism from its mantle roots via the ascent paths of the melt to the surface where different styles of volcanism take place erupting lavas or through explosive volcanism depositing various types of pyroclasts. Two of the fifteen were published earlier. Continental basaltic volcanism also contributes to the total terrestrial sedimentary budget not only by its primary pyroclastic deposits but also their reworked varieties. Most of the papers result from presentations at the BASALT 2013 conference, which took place from April 18–24, 2013, in Görlitz.
Trvalý link: http://hdl.handle.net/11104/0250458