Control of Volcanic Activity by Crustal Structure: Inference from the Izu‐Bonin‐Mariana and Northeast Japan Arcs

2019 ◽  
Vol 46 (22) ◽  
pp. 12968-12976
Author(s):  
Katsuya Kaneko ◽  
Kenta Mishiro ◽  
Yoshiyuki Tatsumi
Keyword(s):  
Crustal Structure ◽  
Volcanic Activity

scholarly journals Temporal changes of the crustal structure associated with the M6.1 earthquake on September 3, 1998, and the volcanic activity of Mount Iwate, Japan

2000 ◽  
Vol 27 (2) ◽  
pp. 269-272 ◽  
Author(s):  
Takeshi Nishimura ◽  
Naoki Uchida ◽  
Haruo Sato ◽  
Masakazu Ohtake ◽  
Satoru Tanaka ◽  
...  
Keyword(s):  
Crustal Structure ◽  
Volcanic Activity ◽  
Temporal Changes

Lunar mare volcanism: lateral heterogeneities in volcanic activity and relationship with crustal structure

2014 ◽  
Vol 401 (1) ◽  
pp. 127-138 ◽  
Author(s):  
Tomokatsu Morota ◽  
Yoshiaki Ishihara ◽  
Sho Sasaki ◽  
Sander Goossens ◽  
Koji Matsumoto ◽  
...  
Keyword(s):  
Crustal Structure ◽  
Volcanic Activity ◽  
Lunar Mare ◽  
Mare Volcanism ◽  
Lateral Heterogeneities

Seismicity and crustal structure related to the Miyake-jima volcanic activity in 2000

2002 ◽  
Vol 29 (19) ◽  
pp. 12-1-12-4 ◽  
Author(s):  
A. Nishizawa ◽  
T. Ono ◽  
Y. Otani
Keyword(s):  
Crustal Structure ◽  
Volcanic Activity

Stratigraphic position and localities of the Temlyan flora from the Anadyr river lower course basin

Palaeobotany ◽  
2015 ◽  
Vol 6 ◽  
pp. 48-67 ◽  
Author(s):  
L. B. Golovneva ◽  
A. A. Grabovskiy
Keyword(s):  
Volcanic Activity ◽  
City Area ◽  
Plant Fossils ◽  
Stratigraphic Position ◽  
Early Paleocene ◽  
First Time ◽  
Systematic Composition ◽  
Stratigraphic Range

Plant fossils from the volcano-clastic deposits of the lower part of the Tanyurer Formation and lower part of the Tavaivaam Unit in the Anadyr city area (Northeastrn Russia) are described for the first time. This assemblage was named as the Temlyan flora. It consists of 25 taxa and includes ferns, horsetails, lycophytes, ginkgoaleans, czekanowskialeans, cycadophytes, conifers and angiosperms. The Temlyan flora is similar in systematic composition to the Rarytkin flora from the upper part of the Rarytkin Formation which was dated as the late Maastrichtian-Danian. But it is distinguished from the latter by presence of the numerous relicts (Lokyma, Nilssonia, Encephalartopsis, Phoenicopsis and Ginkgo ex gr. sibirica). Probably the presence of relicts in the Temlyan flora is connected with influence of volcanic activity. Age of the Temlyan flora is determined as the late Maastrichtian-Danian on the basis of systematic similarity with the Rarytkin Flora. However this age may be slightly younger, possibly only early Paleocene, because the Tanyurer Formation superposes the Rarytkin Formation. Stratigraphic range of Lokyma, Nilssonia, Encephalartopsis, Phoenicopsis and Ginkgo ex gr. sibirica is extended from its previously known latest records in the early Campanian or middle Maastrichtian up to as late as the latest Maastrichtian or early Paleocene. It is very possible, that these typical Mesozoic taxa may have persisted into the Paleogene.

10 years of volcanic activity in Alaska; 1983 to 1992; a video

1995 ◽  
Author(s):  
Michael P. Doukas ◽  
Robert G. McGimsey ◽  
Joseph M. Dorava
Keyword(s):  
Volcanic Activity
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