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Fossil diatoms from the fine-grained tuffaceous sediment in Hakone Volcano
Haga, Masakazu +2 more
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“Kintoki-san-Makuyama Line” A Tektonik Line traversing Hakone Volcano
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Post-caldera geology of Gora Region in Hakone Volcano Group, Japan
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Calc alkali rocks derived from tholeiite magma in Hakone volcano
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Preliminary report on a Gravimetric Survey on Volcano Hakone, Japan
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Petrology of Hakone Volcano and the Adjacent Areas, Japan
Bulletin of the Geological Society of America, 1950Rocks of Hakone volcano and adjacent areas cover a wide range from basalt to dacite approximate to soda-rhyolite. They were erupted from various different centers during the period from older Miocene to Recent. Two different rock series are recognized, one characterized by the occurrence of monoclinic-pyroxene (a solid solution series from augite to ...
Hisashi Kuno
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Seismic Constraint on the Fluid-Bearing Systems Feeding Hakone Volcano, Central Japan
Journal of Geophysical Research: Solid Earth, 2020AbstractInvestigating heterogeneous structures beneath active volcanoes is important for better understanding of volcanic activity and improved mitigation of volcanic risk. In central Japan, Hakone volcano has recently shown shallow earthquake swarms and deep low‐frequency earthquakes (DLFEs), which are probably related to geothermal or deep magmatic ...
Ryou Honda +2 more
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The geothermal system of the Hakone volcano
Geothermics, 1970The isothermal map of the Hakone volcano at sea level shows that the geothermal area now 12 by 13 km in diameter is clearly related with the present volcanic activity in central cones. Four zones are recognized in the distribution of thermal waters.
Y Oki, T Hirano
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