Talk:Japan Trench
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Wiki Education Foundation-supported course assignment
[edit] This article is or was the subject of a Wiki Education Foundation-supported course assignment. Further details are available on the course page. Student editor(s): KAlder10.
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North American
[edit]Many tectonic maps, including two over at Plate tectonics, show the Japan trench as dividing the Pacific plate and the North American plate, not the Eurasian plate. A lot of off-site maps show the northern half of Japan (including Tokyo) as being on the North American plate. --75.58.54.17 17:20, 20 October 2007 (UTC)
Oceanic crust is contrasted to continental crust, even though certain shallow seas rest on continental crust. See oceanic crust. μηδείς (talk) 04:03, 12 March 2011 (UTC)
When was it found/named
[edit]When was the Japan Trench identified as a geographic feature and named? We might include who identified it also. I am assuming it was discovered in the mid 20th century. = Randall Bart Talk 05:04, 22 March 2011 (UTC)
External links modified
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External links modified
[edit]Hello fellow Wikipedians,
I have just modified one external link on Japan Trench. Please take a moment to review my edit. If you have any questions, or need the bot to ignore the links, or the page altogether, please visit this simple FaQ for additional information. I made the following changes:
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Microbial Activity
[edit]There are some articles on sediment samples collected from the Japan Trench indicating a change in microbial diversity within communities at the bottom of the trench. Phylogenetic analysis has shown that microbes within the sediment has shown a wide distribution of types within present bacteria. https://academic.oup.com/femsle/article/170/1/271/454601
References
[edit]Huene, Roland Von, et al. “A Summary of Cenozoic Tectonic History along the IPOD Japan Trench Transect.” GSA Bulletin, GeoScienceWorld, 1 Sept. 1982, pubs.geoscienceworld.org/gsa/gsabulletin/article-abstract/93/9/829/187884. • The Cretaceous to early Paleogene period of convergence within the Japan is shown by andesitic volcanism associated with a large syncline.
Kosuku, Heki, et al. “Silent Fault Slip Following an Interplate Thrust Earthquake at the Japan Trench.” Nature News, Nature Publishing Group, 10 Apr. 1997, www.nature.com/articles/386595a0. • A recorded earthquake during the Winter (December) of 1994 within the Japan Trench caused crustal movements and a fault slip to be observed.
Lallemand, Serge, and Xavier Le Pichon. “Coulomb Wedge Model Applied to the Subduction of Seamounts in the Japan Trench.” Geology, GeoScienceWorld, 1 Nov. 1987, pubs.geoscienceworld.org/gsa/geology/article-abstract/15/11/1065/204262. • Examples in the seamount chain junction between the Japan and Kuril trenches illustrate the stages of subduction.
Tanioka, Yuichiro, et al. “What Controls the Lateral Variation of Large Earthquake Occurrence along the Japan Trench?” Island Arc, Wiley/Blackwell (10.1111), 5 Apr. 2006, onlinelibrary.wiley.com/doi/abs/10.1111/j.1440-1738.1997.tb00176.x. • Large earthquake occurrence within the Japan Trench may be explained by the variation of surface roughness of the subducting plate.
Volkman, J.K., et al. “The Origin and Fate of Lipids in the Japan Trench.” Physics and Chemistry of the Earth, Pergamon, 26 Mar. 2003, www.sciencedirect.com/science/article/pii/0079194679901204. • Lipids found within sediment samples from the Japan Trench include compounds such as sterol ethers, and very long-chain unsaturated ketones that assist searches for the origin organisms and the relevant biochemical pathways involved.
Yanagibiyashi, Miki, et al. “Changes in the Microbial Community in Japan Trench Sediment from a Depth of 6292 m during Cultivation without Decompression.” FEMS Microbiology Letters, Oxford University Press, 1 Jan. 1999, academic.oup.com/femsle/article/170/1/271/454601. • Sediment samples from the Japan trench showed that the microbial diversity displayed a wide distribution of types in the domain Bacteria. — Preceding unsigned comment added by KAlder10 (talk • contribs) 03:44, 22 April 2018 (UTC)
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