Zobrazeno 1 - 7
of 7
pro vyhledávání: '"György Buda"'
Publikováno v:
Geologia Croatica, Vol 64, Iss 2, Pp 153-162 (2011)
Potassium feldspars from different granitoids and gneisses of Papuk Mt. (Slavonia, Croatia) have been investigated by X-ray powder diffraction. Diffraction patterns classically observed as well as patterns calculated by Rietveld refinement were compa
Externí odkaz:
https://doaj.org/article/437a0f03c7ad45148dee6e1f6b8b4003
Publikováno v:
Földtani Közlöny. 149:93-104
Nowadays zircon is the most common mineral of the geological U-Pb dating method. One of the main barriers of getting properly time-resolved and reliable zircon age data is just the internal heterogeneity of the zircon crystals themselves. For overcom
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::739d22b7a4c78aa2d7873bab3363ff52
https://doi.org/10.23928/foldt.kozl.2019.149.2.93
https://doi.org/10.23928/foldt.kozl.2019.149.2.93
Autor:
Domagoj Jamičić, György Buda, Christoph Hauzenberger, Eva Klötzli, Urs Klötzli, Marija Horvat
Publikováno v:
Geochronometria. 45:198-210
Detailed cathodoluminescence (CL) and back scattered electron (BSE) imaging of zircon crystals, coupled with in-situ U-Pb zircon dating by Laser Ablation Multi-Collector Inductively Coupled Plasma Mass Spectrometry (LA-MC-ICP-MS) were used to develop
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e5bb084d5f6ec88602b4eb2c1fca9488
https://doi.org/10.1515/geochr-2015-0099
https://doi.org/10.1515/geochr-2015-0099
Publikováno v:
Geologia Croatica, Vol 65, Iss 2, Pp 243-253 (2012)
Geologia Croatica
Volume 65
Issue 2
Geologia Croatica
Volume 65
Issue 2
Variscan granitoids occur in the southeastern part of the Tisza Mega Unit of Hungary. The presence of amphibole, calc-alkaline-type Mg-rich biotite in metaluminous basic enclaves, and muscovite and Fe-Al-biotite in peraluminous granitoids, suggests a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5502258a5d51b22327dec0722793c85f
http://www.geologia-croatica.hr/ojs/index.php/GC/article/view/550
http://www.geologia-croatica.hr/ojs/index.php/GC/article/view/550
Publikováno v:
Central European Geology. 53:165-180
The Mid-Hungarian (or Zagreb-Zemplin) Line of WSW-ENE strike divides the Pannonian basement into two mega-units, the Tisia Composite Terrane in the SE and the ALCAPA Composite Terrane in the NW. They became juxtaposed no earlier than the Middle Mioce
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c764b413595c81059083ff235887f5c3
https://doi.org/10.1556/ceugeol.53.2010.2-3.4
https://doi.org/10.1556/ceugeol.53.2010.2-3.4
Publikováno v:
Acta Geologica Hungarica. 47:117-138
Three major groups (A-C) of Central European Variscan granitoids can be distinguished based on petrologic and chemical data: A. Low-K, high-Na, calc-alkaline, alkali-calcic, met/peraluminous, I- and S-type, trondhjemitic (slightly granodioritic)-suit
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0e0a7f0fa5f7543759b414dc6e4a1377
https://doi.org/10.1556/ageol.47.2004.2-3.3
https://doi.org/10.1556/ageol.47.2004.2-3.3
Autor:
Gábor Dobosi, György Buda
Publikováno v:
Neues Jahrbuch für Mineralogie - Abhandlungen. 180:115-147
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::00b6cb7624e5aeb9e89ceceac4739fca
https://doi.org/10.1127/0077-7757/2004/0180-0115
https://doi.org/10.1127/0077-7757/2004/0180-0115