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New volcano-tectonic morphostructure in case of a 42-km deep-sea calderoida at Detroit seamount rise (NW Pacific Ocean)

https://doi.org/10.7868/S0435428118030070

Abstract

The volcano-tectonic and tephrachronological analysis and available materials regarding the northern edge of the Emperor Seamount Chain allowed for the first time to detect the unknown circled volcano-tectonic 42-km deep-sea morphostructure known as calderoida (author's terminology) lying at –2900–2200 m depth. It is structurally complex and broken by faults into blocks of different sizes and shapes. It refers to the northern portion of the Detroit Seamount Rise (NW Pacific Ocean) and is a Pliocene horst that was formed in the Early Pleistocene at depths from –3000 to –2000 m. Its close analogues have not yet been found on Earth, but similar objects do probably exist on Venus.

About the Author

I. V. Melekestsev
Institute of Volcanology and Seismology FEB RAS, Petropavlovsk-Kamchatskiy
Russian Federation


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Review

For citations:


Melekestsev I.V. New volcano-tectonic morphostructure in case of a 42-km deep-sea calderoida at Detroit seamount rise (NW Pacific Ocean). Geomorfologiya. 2018;(3):82-92. (In Russ.) https://doi.org/10.7868/S0435428118030070

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