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Автор Kasameyer, Paul
Автор Wilt, Michael
Автор Daily, William
Автор Felske, Donald
Дата выпуска 1991
dc.description A time‐domain electromagnetic survey was conducted near the rhyolite dome Novarupta. We found a continuous (60 to 100 m thick) high‐resistivity surface layer, which represents the unsaturated or unaltered tephra and whose base is probably the water table. This layer is thinnest near fumaroles; the largest thin areas lie under the tephra ring surrounding Novarupta, where the altered zones extend to a depth of more than 100 m. A deeper conductive layer is associated with the top of the underlying sedimentary rocks and is inferred to indicate the depth to the pre‐eruptive surface.
Формат application.pdf
Копирайт Copyright 1991 by the American Geophysical Union.
Тема Katmai Scientific Drilling Project, Surface Phase
Тема Exploration Geophysics
Тема Exploration Geophysics: Magnetic and electrical methods
Тема Volcanology
Тема Volcanology: Eruption monitoring
Тема Volcanology: Ash deposits
Тема Volcanology: Hydrothermal systems
Тема Volcanology: Eruption mechanisms
Название Time‐domain electromagnetic soundings in the vicinity of Novarupta, Katmai National Park, Alaska
Тип article
DOI 10.1029/91GL01759
Electronic ISSN 1944-8007
Print ISSN 0094-8276
Журнал Geophysical Research Letters
Том 18
Первая страница 1525
Последняя страница 1528
Аффилиация Kasameyer, Paul; Lawrence Livermore National Laboratory
Аффилиация Wilt, Michael; Lawrence Livermore National Laboratory
Аффилиация Daily, William; Lawrence Livermore National Laboratory
Аффилиация Felske, Donald; Lawrence Livermore National Laboratory
Выпуск 8
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Библиографическая ссылка Keith, T.E.C, Argillic alteration in the Novarupta vent region, Katmai National Park, Alaska, this issue, 1991.
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