CRUST AND MANTLE OF THE BAIKAL RIFT ZONE FROM P- AND S-WAVE RECEIVER FUNCTIONS

We have obtained P-wave and S-wave receiver functions for 10 broadband seismograph stations in the Baikal rift zone (BRZ) and inverted them for seismic velocity models of the crust and upper mantle. The thinnest crust (30–35 km) is found in the Baikal basin, the thickest in the East Sayan uplift (45...

Полное описание

Библиографические подробности

Главные авторы:	L. P. Vinnik, S. I. Oreshin, L. R. Tsydypova, V. V. Mordvinova, M. M. Kobelev, M. A. Khritova, Ts. A. Tubanov
Формат:	Artigo
Язык:	Inglês
Опубликовано:	Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust 2017-12-01
Серии:	Геодинамика и тектонофизика
Предметы:	vp/vs ratio fluid-filled porosity mantle mantle plume lithosphere – asthenosphere boundary
Online-ссылка:	https://www.gt-crust.ru/jour/article/view/466
Метки:	Добавить метку Нет меток, Требуется 1-ая метка записи!