Исследование структуры и химического состава неглубокого ледяного керна вулкана Ушковский

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Аннотация

Камчатка – это второй по размеру в России район оледенения, который подходит для палеореконструкции по ледяным кернам. Различные факторы (вулканическая активность, низкая антропогенная нагрузка и т.д.) формируют уникальную, но в тоже время сложную для интерпретации химическую запись в местных ледниках. В работе определены основные источники химических маркеров и оценено влияние сезонного таяния на их миграцию.

Об авторах

М. А. Воробьев

Институт географии РАН

Автор, ответственный за переписку.
Email: m.vorobyev@igras.ru
Россия, Москва

С. С. Кутузов

Университет штата Огайо

Email: m.vorobyev@igras.ru

Школа наук о Земле

США, Колумбус

М. М. Виноградова

Институт географии РАН

Email: m.vorobyev@igras.ru
Россия, Москва

А. Г. Хайрединова

Институт географии РАН

Email: m.vorobyev@igras.ru
Россия, Москва

Ю. Н. Чижова

Институт географии РАН; Институт геологии рудных месторождений, петрологии, минералогии и геохимии (ИГЕМ) РАН

Email: m.vorobyev@igras.ru
Россия, Москва; Москва

В. Н. Михаленко

Институт географии РАН

Email: m.vorobyev@igras.ru
Россия, Москва

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