APHA Szerző - Cronin S. J.4

P23536

 Hyaloclastites, peperites and soft-sediment deformation textures of a shallow subaqueous Miocene rhyolitic dome-cryptodome complex, Pálháza, Hungary.

Authors Németh K.,  Pécskay Z.,  Martin U.,  Gméling K.,  Molnár F.,  Cronin S. J.
Megjelenés helye Geological Society, London, Special Publications 302 (2008) 63
Character Scientific paper, proceedings
Topics Earth, Cosmic and Environm. Res.
Linkek Hivatkozások (7)

P19860

 Peperites and soft sediment deformation textures of a shallow subaqueous Miocene rhyolitic cryptodome and dyke complex, Pálháza, Hungary.

Authors Németh K.,  Pécskay Z.,  Martin U.,  Gméling K.,  Molnár F.,  Cronin S. J.
Megjelenés helye Physical Geology of Subvolcanic Systems: Laccoliths, Sills and Dykes. LASI II. Isle of Skye, UK. 1-3 April, 2006. Proceedings. The Geological Society 0 (2006) 36
Character Scientific paper, proceedings
Topics Earth, Cosmic and Environm. Res.

Szerzői Táblázat

Total Headed by ATOMKI under name
of the author
Part of the author Part of the author & ATOMKI
Publications:200.3330
SCIPublications:0000
Cited publications:100.1670
Non-locally cited publications:100.1670
Cited SCIpublications:0000
Non-locally cited SCIpublications:0000
SCICited publications:100.1670
Non-locally SCIcited publications:100.1670
SCICited SCIpublications:0000
Non-locally SCIcited SCIpublications:0000
Citations:701.1670
Non-local citations:701.1670
SCICitations:701.1670
Non-local SCIcitations:701.1670
Impact~0:000.3330
Averaged impact:000.3330
SCIaveraged impact:0000
Citational effectivity:700.1670
Non-local citational effectivity:700.1670
SCIcitational effectivity:700.1670
Non-local SCIcitational effectivity:700.1670
Publications, n:5000
SCIPublications, n:0000
Cited publications, n:5000
Non-locally cited publications, n:5000
Cited SCIpublications, n:0000
Non-locally cited SCIpublications, n:0000
SCICited publications, n:5000
Non-locally SCIcited publications, n:5000
SCICited SCIpublications, n:0000
Non-locally SCIcited SCIpublications, n:0000
z-index:0000