Artigo Revisado por pares

The Balkanids as an Instance of Back-Arc Thrust Belt: Possible Relation with the Hellenids

1974; Geological Society of America; Volume: 85; Issue: 7 Linguagem: Inglês

10.1130/0016-7606(1974)85 2.0.co;2

ISSN

1943-2674

Autores

M. BOCCALEI, P. Manetti, Angelο Peccerillo,

Tópico(s)

earthquake and tectonic studies

Resumo

Research Article| July 01, 1974 The Balkanids as an Instance of Back-Arc Thrust Belt: Possible Relation with the Hellenids M. BOCCALEI; M. BOCCALEI 1Istituto di Geologia e Paleontologia dell'Università, Via Lamarmora 4- 50121 Firenze, Italy Search for other works by this author on: GSW Google Scholar P. MANETTI; P. MANETTI 2Institute di Mineralogia, Petrografia e Geochimica dell'Università, Via Lamartnora 4 - 50121 Firenze, Italy Search for other works by this author on: GSW Google Scholar A. PECCERILLO A. PECCERILLO 2Institute di Mineralogia, Petrografia e Geochimica dell'Università, Via Lamartnora 4 - 50121 Firenze, Italy Search for other works by this author on: GSW Google Scholar Author and Article Information M. BOCCALEI 1Istituto di Geologia e Paleontologia dell'Università, Via Lamarmora 4- 50121 Firenze, Italy P. MANETTI 2Institute di Mineralogia, Petrografia e Geochimica dell'Università, Via Lamartnora 4 - 50121 Firenze, Italy A. PECCERILLO 2Institute di Mineralogia, Petrografia e Geochimica dell'Università, Via Lamartnora 4 - 50121 Firenze, Italy Publisher: Geological Society of America First Online: 01 Jun 2017 Online ISSN: 1943-2674 Print ISSN: 0016-7606 Geological Society of America GSA Bulletin (1974) 85 (7): 1077–1084. https://doi.org/10.1130/0016-7606(1974)85 2.0.CO;2 Article history First Online: 01 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation M. BOCCALEI, P. MANETTI, A. PECCERILLO; The Balkanids as an Instance of Back-Arc Thrust Belt: Possible Relation with the Hellenids. GSA Bulletin 1974;; 85 (7): 1077–1084. doi: https://doi.org/10.1130/0016-7606(1974)85 2.0.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGSA Bulletin Search Advanced Search Abstract The Late Cretaceous calc-alkaline and Late Cretaceous–early Eocene alkaline (shoshonitic) magmatism of Srednogora in the Balkan chain of Bulgaria are interpreted as associated with an ancient active continental margin of Cordilleran (Andean) type.A tectonic evolution of back-arc thrust-belt type agrees, for the Balkanids, with the lack of large overthrust, ophiolite and radio-larite rock-type, eumiogeosyncline in this area.The distribution of magmatism from the Mesozoic to the Recent and the tectonic evolution of the Balkanic-Hellenic area suggest a discontinuous southward Tertiary migration of an arc-trench system away from the southwestern edge of the Rhodope massic to its present location in the eastern Mediterranean. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access.

Referência(s)