Title: Shear zones in the upper mantle: A case study in an Alpine Iherzolite massif
Abstract:Research Article| October 01, 1991 Shear zones in the upper mantle: A case study in an Alpine Iherzolite massif R.L.M. Vissers; R.L.M. Vissers 1Institute of Earth Sciences, P.O. Box 80.021, Utrecht, N...Research Article| October 01, 1991 Shear zones in the upper mantle: A case study in an Alpine Iherzolite massif R.L.M. Vissers; R.L.M. Vissers 1Institute of Earth Sciences, P.O. Box 80.021, Utrecht, Netherlands Search for other works by this author on: GSW Google Scholar M. R. Drury; M. R. Drury 1Institute of Earth Sciences, P.O. Box 80.021, Utrecht, Netherlands Search for other works by this author on: GSW Google Scholar E. H. Hoogerduijn Strating; E. H. Hoogerduijn Strating 1Institute of Earth Sciences, P.O. Box 80.021, Utrecht, Netherlands Search for other works by this author on: GSW Google Scholar D. van der Wal D. van der Wal 1Institute of Earth Sciences, P.O. Box 80.021, Utrecht, Netherlands Search for other works by this author on: GSW Google Scholar Geology (1991) 19 (10): 990–993. https://doi.org/10.1130/0091-7613(1991)019<0990:SZITUM>2.3.CO;2 Article history first online: 02 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share MailTo Twitter LinkedIn Tools Icon Tools Get Permissions Search Site Citation R.L.M. Vissers, M. R. Drury, E. H. Hoogerduijn Strating, D. van der Wal; Shear zones in the upper mantle: A case study in an Alpine Iherzolite massif. Geology 1991;; 19 (10): 990–993. doi: https://doi.org/10.1130/0091-7613(1991)019<0990:SZITUM>2.3.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 SocietyGeology Search Advanced Search Abstract The Erro-Tobbio upper-mantle lherzolite of northwest Italy, emplaced in the Alpine suture zone during collision of the European and Adriatic plates, has preserved a set of major shear zones formed at temperatures in the range 800-1040 °C during the period of Jurassic rifting and breakup and development of the Piemonte-Ligurian oceanic basin. These structures clearly demonstrate localization of the deformation in the Piemonte-Ligurian upper mantle during lithosphere stretching and breakup. 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.Read More
Publication Year: 1991
Publication Date: 1991-01-01
Language: en
Type: article
Indexed In: ['crossref']
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Cited By Count: 104
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