Форма представления | Статьи в зарубежных журналах и сборниках |
Год публикации | 2022 |
Язык | английский |
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Нургалиев Данис Карлович, автор
Огнев Игорь Николаевич, автор
Утемов Эдуард Валерьевич, автор
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Библиографическое описание на языке оригинала |
Ognev I. N., Utemov E. V., Nurgaliev D. K. THE USE OF «NATIVE» WAVELET TRANSFORM FOR DETERMINING LATERAL DENSITY VARIATION OF THE VOLGO-URALIAN SUBCRATON // SOCAR Proceedings. 2021. № 2 (Special Issue). p. 135–140. |
Аннотация |
In the last two decades in conjunction with the development of satellite
gravimetry, the techniques of regional-scale inverse and forward gravity
modeling started to be more actively incorporated in the construction of crustal and lithospheric scale models. Such regional models are usually built as a set of layers and bodies with constant densities. This approach often leads to a certain difference between the initially used measured gravity field and a gravity field that is produced by the model. One of the examples of this kind of models is a recent lithospheric model of the Volgo-Uralian subcraton. In the current study, we are applying the method of «native» wavelet transform to the residual gravity anomaly for defining the possible lateral density variations within the lithospheric layers of Volgo-Uralia. |
Ключевые слова |
Wavelet transform, Gravity field inversion, Forward gravity modeling, Volgo-Uralian subcraton, Satellite gravimetry. |
Название журнала |
SOCAR Proceedings
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https://repository.kpfu.ru/?p_id=263760 |
Файлы ресурса | |
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Полная запись метаданных |
Поле DC |
Значение |
Язык |
dc.contributor.author |
Нургалиев Данис Карлович |
ru_RU |
dc.contributor.author |
Огнев Игорь Николаевич |
ru_RU |
dc.contributor.author |
Утемов Эдуард Валерьевич |
ru_RU |
dc.date.accessioned |
2022-01-01T00:00:00Z |
ru_RU |
dc.date.available |
2022-01-01T00:00:00Z |
ru_RU |
dc.date.issued |
2022 |
ru_RU |
dc.identifier.citation |
Ognev I. N., Utemov E. V., Nurgaliev D. K. THE USE OF «NATIVE» WAVELET TRANSFORM FOR DETERMINING LATERAL DENSITY VARIATION OF THE VOLGO-URALIAN SUBCRATON // SOCAR Proceedings. 2021. № 2 (Special Issue). p. 135–140. |
ru_RU |
dc.identifier.uri |
https://repository.kpfu.ru/?p_id=263760 |
ru_RU |
dc.description.abstract |
SOCAR Proceedings |
ru_RU |
dc.description.abstract |
In the last two decades in conjunction with the development of satellite
gravimetry, the techniques of regional-scale inverse and forward gravity
modeling started to be more actively incorporated in the construction of crustal and lithospheric scale models. Such regional models are usually built as a set of layers and bodies with constant densities. This approach often leads to a certain difference between the initially used measured gravity field and a gravity field that is produced by the model. One of the examples of this kind of models is a recent lithospheric model of the Volgo-Uralian subcraton. In the current study, we are applying the method of «native» wavelet transform to the residual gravity anomaly for defining the possible lateral density variations within the lithospheric layers of Volgo-Uralia. |
ru_RU |
dc.language.iso |
ru |
ru_RU |
dc.subject |
Wavelet transform |
ru_RU |
dc.subject |
Gravity field inversion |
ru_RU |
dc.subject |
Forward gravity modeling |
ru_RU |
dc.subject |
Volgo-Uralian subcraton |
ru_RU |
dc.subject |
Satellite gravimetry. |
ru_RU |
dc.title |
THE USE OF «NATIVE» WAVELET TRANSFORM FOR DETERMINING LATERAL DENSITY VARIATION OF THE VOLGO-URALIAN SUBCRATON |
ru_RU |
dc.type |
Статьи в зарубежных журналах и сборниках |
ru_RU |
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