Tectonic Significance of the Kodiak-Bowie Seamount Chain, Northeastern Pacific
1974; Geological Society of America; Volume: 2; Issue: 3 Linguagem: Inglês
10.1130/0091-7613(1974)2 2.0.co;2
ISSN1943-2682
AutoresEli A. Silver, Roland von Huene, James K. Crouch,
Tópico(s)earthquake and tectonic studies
ResumoResearch Article| March 01, 1974 Tectonic Significance of the Kodiak-Bowie Seamount Chain, Northeastern Pacific Eli A. Silver; Eli A. Silver 1Board of Earth Sciences, University of California, Santa Cruz, Santa Cruz, California 95064, and U.S. Geological Survey, Menlo Park, California 94025 Search for other works by this author on: GSW Google Scholar Roland von Huene; Roland von Huene 2U.S. Geological Survey, Reston, Virginia 22092 Search for other works by this author on: GSW Google Scholar James K. Crouch James K. Crouch 3U.S. Geological Survey, Menlo Park, California 94025 Search for other works by this author on: GSW Google Scholar Author and Article Information Eli A. Silver 1Board of Earth Sciences, University of California, Santa Cruz, Santa Cruz, California 95064, and U.S. Geological Survey, Menlo Park, California 94025 Roland von Huene 2U.S. Geological Survey, Reston, Virginia 22092 James K. Crouch 3U.S. Geological Survey, Menlo Park, California 94025 Publisher: Geological Society of America First Online: 02 Jun 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 Geological Society of America Geology (1974) 2 (3): 147–150. https://doi.org/10.1130/0091-7613(1974)2 2.0.CO;2 Article history First Online: 02 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Eli A. Silver, Roland von Huene, James K. Crouch; Tectonic Significance of the Kodiak-Bowie Seamount Chain, Northeastern Pacific. Geology 1974;; 2 (3): 147–150. doi: https://doi.org/10.1130/0091-7613(1974)2 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 The hypothesis of a fixed melting spot reference frame (M) for relative plate motion is tested in the northeastern Pacific Ocean, where the Kodiak-Bowie seamount chain intersects the northern triple junction between the Pacific, American, and Juan de Fuca plates. Available age determinations on Kodiak and Giacomini Seamounts provide an estimated average rate of volcanic propagation along the chain of 6.5 cm per yr and allow estimates of plate movements relative to the melting spot. The inferred motion of the American plate relative to M is close to that observed along the Yellowstone-Snake River Plain volcanic trend and broadly supports the concept of a fixed melting spot reference frame. However, the convex northward curvature of the Kodiak-Bowie chain and of several chains to the south does not support the hypothesis. The lack of parallelism between these seamounts and the Hawaiian chain suggests slow relative movement between the Kodiak-Bowie and Hawaiian melting spots. 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.
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