Zobrazeno 1 - 10
of 68
pro vyhledávání: '"Volker Jacobshagen"'
Autor:
Klaus-J. Reutter
Publikováno v:
Zeitschrift der Deutschen Geologischen Gesellschaft. 149:469-471
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1ee10c24122257d2f794130768d6d39b
https://doi.org/10.1127/zdgg/149/1999/469
https://doi.org/10.1127/zdgg/149/1999/469
Autor:
Sebastian U. Senger
Publikováno v:
Umweltwissenschaften und Schadstoff-Forschung. 14:163-163
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7605416f60eb0865b5766295e533a726
https://doi.org/10.1007/bf03038280
https://doi.org/10.1007/bf03038280
Autor:
Reutter, Klaus-J.
Publikováno v:
Zeitschrift der Deutschen Gesellschaft für Geowissenschaften; March 1999, Vol. 149 Issue: 4 p469-471, 3p
Autor:
MAURIZIO GAETANI, VOLKER JACOBSHAGEN, ALDA NICORA, GÜNTER KAUFFMANN, VASSILI TSELEPIDIS, NERINA FANTINI SESTINI, DOROTHEE MERTMANN, VANA SKOURTSIS-CORONEOU
Publikováno v:
Rivista Italiana di Paleontologia e Stratigrafia, Vol 98, Iss 2 (2017)
The sections of Marathovouno hillock in Chios (Greece), proposed by Assereto (1974) as stratotype for the base of the Anisian, have been revisited. An additional new section, Parthenis, near the town of Chios, was also considered. The ammonoid fauna
Externí odkaz:
https://doaj.org/article/a759ebad98aa4fb8a93f67aecf4998bf
Autor:
DOROTHEE MERTMANN, VOLKER JACOBSHAGEN
Publikováno v:
Rivista Italiana di Paleontologia e Stratigrafia, Vol 109, Iss 3 (2003)
On the Greek island of Chios, Lower Triassic sections bave delivered rich ammonoid faunas from red limestones of the Hallstatt facies. Here, we present a palaeontological description of Spathian ammonoids, which have been collected during two field c
Externí odkaz:
https://doaj.org/article/c22b6a4d262a4686ad7470db1b752c2c
Publikováno v:
Zeitschrift der Deutschen Geologischen Gesellschaft. 154:85-100
Summarization: The Plattenkalk area around the Samaria gorge,western Crete, has been investigated by structural analysis and studies of microfabrics. The study area is dominated by a large-scale anticline striking to the NNE. All fracture systems obs
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::48fe5498326b34eef513f48e71446068
https://doi.org/10.1127/zdgg/154/2003/85
https://doi.org/10.1127/zdgg/154/2003/85
Publikováno v:
Journal of South American Earth Sciences. 10:1-19
Summarization: The Eastern Cordillera of southern Bolivia is situated between the Altiplano high plateau in the west and the thin-skinned Subandean thrust belt in the east. It is mainly built of Ordovician anchimetamorphic sedimentary rocks with a di
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7612549940b789204703b90b10d4c5de
https://doi.org/10.1016/s0895-9811(97)00001-1
https://doi.org/10.1016/s0895-9811(97)00001-1
Publikováno v:
Zeitschrift der Deutschen Geologischen Gesellschaft. 144:396-405
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::22d905964f7aad09544c87c2aaf3410d
https://doi.org/10.1127/zdgg/144/1993/396
https://doi.org/10.1127/zdgg/144/1993/396
Autor:
Volker Jacobshagen
Publikováno v:
Geologische Rundschau. 81:185-197
Within the fracturai pattern of Morocco, 35–45° and 70–90° directions are predominant. Most of the faults originated already during the Upper Palaeozoic and were repeatedly reactivated, later on. Two of the large fracture systems are considered
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::73dbeef7a1e77be21fe288bba37970b8
https://doi.org/10.1007/bf01764548
https://doi.org/10.1007/bf01764548
Publikováno v:
Tectonics. 26
[1] Although the structural geometry of the Cenozoic Altiplano-Puna plateau in the central Andes is well defined, the temporal evolution of this contractile deformation is poorly constrained. To address this shortcoming, we used apatite fission track
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::23bce5492bead175a48bacd5ce48c683
https://doi.org/10.1029/2005tc001869
https://doi.org/10.1029/2005tc001869