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Awdankiewicz M., Szumowska M. (2014) Clastogenic lavas, spatter and scoria deposits: Evidence of Hawaiian to Strombolian-type eruptive activity at Męcinka (Lower Silesia, the Cenozoic Central European Volcanic Province). 4. Meeting of the Expert Volcanology Group of the Czech Geological Society 2014, 3-4.

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Year2014
Original EntryAwdankiewicz M., Szumowska M. (2014) Clastogenic lavas, spatter and scoria deposits: Evidence of Hawaiian to Strombolian-type eruptive activity at Męcinka (Lower Silesia, the Cenozoic Central European Volcanic Province). 4. Meeting of the Expert Volcanology Group of the Czech Geological Society 2014, 3-4.
Mindat Ref. ID16369513Long-form Identifiermindat:1:5:16369513:0
GUID0
Full ReferenceAwdankiewicz M., Szumowska M. (2014) Clastogenic lavas, spatter and scoria deposits: Evidence of Hawaiian to Strombolian-type eruptive activity at Męcinka (Lower Silesia, the Cenozoic Central European Volcanic Province). 4. Meeting of the Expert Volcanology Group of the Czech Geological Society 2014, 3-4.
Plain TextAwdankiewicz M., Szumowska M. (2014) Clastogenic lavas, spatter and scoria deposits: Evidence of Hawaiian to Strombolian-type eruptive activity at Męcinka (Lower Silesia, the Cenozoic Central European Volcanic Province). 4. Meeting of the Expert Volcanology Group of the Czech Geological Society 2014, 3-4.

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Męcinka basalt quarry, Męcinka, Gmina Męcinka, Jawor County, Lower Silesian Voivodeship, Poland

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Szumowska, M., Awdankiewicz, M., Christiansen, E.H. (2014) Conditions of formation and crystallization of the Ostrzyca Hill basanite (Lower Silesia) – preliminary constrains from . Mineralogia – Special Papers, 42, 108-109.
Szumowska M., Awdankiewicz M., Christiansen E. H., 2014. Conditions of formation and crystallization of the Ostrzyca Hill basanite (Lower Silesia) – preliminary constrains from geothermobarometry. Mineralogia – Special Papers, 42, 108-109.
Awdankiewicz, M. (2005) Reconstructing an eroded scoria cone: the Miocene Sośnica Hill volcano (Lower Silesia, SW Poland). Geological Quarterly (Kwartalnik Geologiczny) Vol 49, No 4 P.439–448 PIG Warszawa.
Sánchez, M. Carracedo, Sarrionandia, F., Ibarguchi, J. I. Gil (2014) Post-depositional intrusion and extrusion through a scoria and spatter cone of fountain-fed nephelinite lavas (Las Herrerías volcano, Calatrava, Spain). Bulletin of Volcanology, 76 (9). doi:10.1007/s00445-014-0860-4
AWDANKIEWICZ, Marek, AWDANKIEWICZ, Honorata, RAPPRICH, Vladislav, STÁRKOVÁ, Marcela (2014) A Permian andesitic tuff ring at Rožmitál (the Intra-Sudetic Basin, Czech Republic) – evolution from explosive to effusive and high-level intrusive activity. Geological Quarterly, 58 (4) doi:10.7306/gq.1184
Awdankiewicz, M. (2013) Targowica, quarry of basalt. Miocene, basaltic scoria cone (structure, deposits, petrology). Mineralogia Special Papers: XXth Anniversary Meeting of the Petrology Group of the Mineralogical Society of Poland "From the deep Earth to the human's environment", Niemcza, Poland, 17-20 October 2013. 41: 97-103.
Sottili, G., Palladino, D. M., & Zanon, V. (2004). Plinian activity during the early eruptive history of the Sabatini Volcanic District, Central Italy. Journal of Volcanology and Geothermal Research, 135(4), 361-379.
Gutmann, J.T. (2002) Strombolian and effusive activity as precursors to phreatomagmatism: eruptive sequence at maars of the Pinacate volcanic field, Sonora, Mexico. Journal of Volcanology and Geothermal Research, 113 (1) 345-356 doi:10.1016/s0377-0273(01)00265-7
Schwarzkopf, L. M., Tobschall, H. J. (1997) Železná Hůrka (Eisenbühl) — volcanology and geochemistry of a Quaternary scoria and lapilli cone in the Ohře (Eger) Rift. Journal of the Czech Geological Society, 42 (3) 73
Martin, Ulrike, Németh, Károly (2006) How Strombolian is a “Strombolian” scoria cone? Some irregularities in scoria cone architecture from the Transmexican Volcanic Belt, near Volcán Ceboruco, (Mexico) and Al Haruj (Libya) Journal of Volcanology and Geothermal Research, 155 (1) 104-118 doi:10.1016/j.jvolgeores.2006.02.012
Hałuszczak, A. (2000) Quaternary tectonic activity along foreland preexisting dislocation – some evidence from the Kleszczów Graben (south-central Poland) Journal of the Czech Geological Society, 45 (3-4)
 
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