Zobrazeno 1 - 10
of 37
pro vyhledávání: '"Jakob Pamić"'
Autor:
Jakob Pamić
Publikováno v:
Geologia Croatica, Vol 50, Iss 2, Pp 173-180 (2010)
Externí odkaz:
https://doaj.org/article/042865dd4f124fc382631d2806bfaa90
Publikováno v:
Geologia Croatica, Vol 47, Iss 2, Pp 149-155 (2010)
The palynological data suggest a Late Silurian to ?Early Carboniferous sedimentation age for the weakly metamorphosed rocks from the Mts. Psunj, Papuk and Krndija (Slavonija, North Croatia). Palynofacies and organo-petrographic data indicate that the
Externí odkaz:
https://doaj.org/article/e4fb0d902bca47cf8d672b530465ac05
Autor:
Jakob Pamić
Publikováno v:
Geologia Croatica, Vol 45, Iss 0, Pp 173-175 (2010)
Externí odkaz:
https://doaj.org/article/a0a6e0cbe6574741a2e8649ad436c582
Autor:
Jakob Pamić, Ivan Jurković
Publikováno v:
Rudarsko-geološko-naftni Zbornik, Vol 9, Iss 1, Pp 1-9 (1997)
In the paper are presented basic geological, petrologieca1, geochemi-cal and mineral deposit data for five main magmatic-metallogenic formations of the northwestern and central Dinarides: (l)The Permo Triassic rifting related andesite-diorite formati
Externí odkaz:
https://doaj.org/article/17dcdf5166da4b4a929c63cd2dae6433
Autor:
Jakob Pamić
Publikováno v:
Geologija, Vol 34, Pp 255-264 (1991)
Two different granitic-metamorphic complexes can be distinguished in Prošara Mt. The Hercynian complex consists mostly of cataclastic and phyllonitized gneissgranites and amphibolites. Rocks of the Alpine metamorphic complex are much more widespread
Externí odkaz:
https://doaj.org/article/ca090059732f4605a09732e50bc09c72
Autor:
Jakob Pamić, Marvin Lanphere
Publikováno v:
Geologija, Vol 34, Pp 81-253 (1991)
Hercynian crystalline complex of the Slavonian Mountains and surrounding basement of the Pannonian Basin comprises the following units: (1) anchimetamorphic and very low-grade metamorphic rocks with metabasic igneous rocks, (2)progressive metamorphic
Externí odkaz:
https://doaj.org/article/ea5a36a913174a2ebd9667a5469e69c2
Autor:
Hazim Hrvatović, Jakob Pamić
Publikováno v:
Acta Geologica Hungarica. 48:133-151
The Internal Dinarides include ten larger allochthonous pre-Alpine complexes, similar in many respects to those in the Eastern Alps, Carpathians and Rhodopes. The Dinaride Paleozoic complexes consist mainly of Devonian to Permian formations and are c
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1dabaf38f9e3c824308f011a4ec54d73
https://doi.org/10.1556/ageol.48.2005.2.4
https://doi.org/10.1556/ageol.48.2005.2.4
Autor:
Damir Slovenec, Jakob Pamić
Publikováno v:
Acta Geologica Hungarica. 48:205-224
The Dinaridic Alpine ophiolites can be divided into two groups: 1) those of the Jurassic Dinaride Ophiolite Zone (DOZ) and 2) those of the Cretaceous-Early Paleogene (1) Sava-Vardar Zone (SVZ). However geologically and petrologically they have so far
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::cfd82d7102d4a7af18980563d7a5c224
https://doi.org/10.1556/ageol.48.2005.2.7
https://doi.org/10.1556/ageol.48.2005.2.7
Autor:
Péter Horváth, Jakob Pamić, Gábor Dobosi, Péter Árkai, Dražen Balen, Darko Tibljaš, Katalin Judik, Bruno Tomljenović
Publikováno v:
Acta Geologica Hungarica. 47:151-176
New mineral paragenetic, illite Kübler index, chlorite "crystallinity", apparent crystallite thickness, lattice strain, and K-white mica geobarometric data proved that the Eoalpine (Paleozoic-Mesozoic) metamorphic complex was affected by medium-pres
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::fc32a87b5b5d875cfab31d239ddf2b2c
https://doi.org/10.1556/ageol.47.2004.2-3.5
https://doi.org/10.1556/ageol.47.2004.2-3.5
Publikováno v:
Mineralogy and Petrology. 82:65-79
K–Ar and Ar–Ar whole rock and mineral ages are presented for 25 samples of metamorphic rocks from the Mid-Bosnian Schist Mts., representing one of the largest allochthonous Palaeozoic terranes incorporated within the Internal Dinarides. Four main
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f0cff608d0690828faaa484ade4b1ab1
https://doi.org/10.1007/s00710-004-0041-9
https://doi.org/10.1007/s00710-004-0041-9