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Growth of pillow lobes—Evidence from pillow lavas of Hokkaido, Japan, and North Island, New Zealand
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1985
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Marine GeologyMorphotectonicsVolcanologyPillow LavasEngineeringPillow LobesVolcanismGeographyNew ZealandGeologyGeochronologyVolcanic ProcessOrogenyPillow Lobes—evidenceEarth ScienceRegional GeologyPyroclastic FlowTectonics
Research Article| July 01, 1985 Growth of pillow lobes—Evidence from pillow lavas of Hokkaido, Japan, and North Island, New Zealand Hiromitsu Yamagishi Hiromitsu Yamagishi 1Geological Survey of Hokkaido, Kitaku, Kita 18 Nishi 12, Sapporo 060 Japan Search for other works by this author on: GSW Google Scholar Geology (1985) 13 (7): 499–502. https://doi.org/10.1130/0091-7613(1985)13<499:GOPLFP>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 Hiromitsu Yamagishi; Growth of pillow lobes—Evidence from pillow lavas of Hokkaido, Japan, and North Island, New Zealand. Geology 1985;; 13 (7): 499–502. doi: https://doi.org/10.1130/0091-7613(1985)13<499:GOPLFP>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 SocietyGeology Search Advanced Search Abstract Pillow lavas of Cretaceous and Neogene age well exposed in Hokkaido, Japan, and those of Neogene age in North Island, New Zealand, provide evidence of their mode of growth. Some pillow lobes diverge by formation of longitudinal surface spreading cracks; the others grow by formation of transverse spreading cracks, leaving one or more crusts ending toward the front of the lobes and constrictions. Therefore, it is possible to determine the direction of growth of pillow lobes by tracing the crusts and/or constrictions. 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.