Petrographical characteristics of Ditró (Orotva) granites, Eastern Carpathians, Transylvania, Romania a preliminary description /
One of the most important rock groups outcropping in the NE part of the Ditró Massif, north of the Orotva (Nagyág) creek and from the Török creek to the crystalline schists is the group of the granitic rocks. On the basis of their modal composition and textural features, this rock group can be divid...
Elmentve itt :
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| Dokumentumtípus: | Cikk |
| Megjelent: |
University of Szeged, Department of Mineralogy, Geochemistry and Petrology
Szeged
1998
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| Sorozat: | Acta mineralogica-petrographica
39 |
| Kulcsszavak: | Kőzettan, Ásványtan, Földtan |
| Tárgyszavak: | |
| Online Access: | http://acta.bibl.u-szeged.hu/24868 |
| LEADER | 01980nab a2200229 i 4500 | ||
|---|---|---|---|
| 001 | acta24868 | ||
| 005 | 20220727142058.0 | ||
| 008 | 161017s1998 hu o 0|| eng d | ||
| 022 | |a 0365-8066 | ||
| 040 | |a SZTE Egyetemi Kiadványok Repozitórium |b hun | ||
| 041 | |a eng | ||
| 100 | 1 | |a Kovács Gábor | |
| 245 | 1 | 0 | |a Petrographical characteristics of Ditró (Orotva) granites, Eastern Carpathians, Transylvania, Romania |h [elektronikus dokumentum] : |b a preliminary description / |c Kovács Gábor |
| 260 | |a University of Szeged, Department of Mineralogy, Geochemistry and Petrology |b Szeged |c 1998 | ||
| 300 | |a 35-48 | ||
| 490 | 0 | |a Acta mineralogica-petrographica |v 39 | |
| 520 | 3 | |a One of the most important rock groups outcropping in the NE part of the Ditró Massif, north of the Orotva (Nagyág) creek and from the Török creek to the crystalline schists is the group of the granitic rocks. On the basis of their modal composition and textural features, this rock group can be divided into the following rock types: 1. syeno- and monzogranites with equigranular texture; with potassium feldspar megacrystalline texture, alkaline granites. 2. syenites, quartz syenites, alkaline syenites, foidic monzosyenites. 3. monzonites, quartz monzonites. 4. cataclasites. On the geological maps of 1:10.000 scale the granitoid formations were shown as a homogeneous body. Our studies have revealed that petrography of this area is much more complex than it was interpreted by the former studies. On the basis of the textural studies, it has been concluded that secondary textural patterns of the rock types are similar, and it can be attributed to endomagmatic effect, weathering processes and tectonic deformation. | |
| 650 | 4 | |a Természettudományok | |
| 650 | 4 | |a Föld- és kapcsolódó környezettudományok | |
| 695 | |a Kőzettan, Ásványtan, Földtan | ||
| 700 | 0 | 2 | |a Pál Molnár Elemér |e aut |
| 856 | 4 | 0 | |u http://acta.bibl.u-szeged.hu/24868/1/mineralogica_039_035-048.pdf |z Dokumentum-elérés |