Volcanic Activity of the Venus Coronae

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Аннотация

This work presents the results of studying the topographic confi guration of the Venus coronae, spatially related to the manifestations of late episodes of volcanism — lobate plains. It has been established that coronae are relatively rarely associated with young volcanism. However, those that are spatially related to the lobate plains are long-lived complexes, and their volcanism is confi ned to the fi nal phases of activity.

Негізгі сөздер

Авторлар туралы

E. Guseva

Vernadsky Institute of Geochemistry and Analytical Chemistry, Russian Academy of Sciences

Email: guseva-evgeniya@yandex.ru
Moscow, Russia

M. Ivanov

Vernadsky Institute of Geochemistry and Analytical Chemistry, Russian Academy of Sciences

Email: mikhail_ivanov@brown.edu
Moscow, Russia

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