The structure of the Earth’s inner core is not well known between depths of ∼100–200 km beneath the inner core boundary. This is a result of the PKP core phase triplication and the existence of strong precursors to PKP phases, which hinder the measurement of inner core compressional PKIKP waves at epicentral distances between roughly 143 and 148◦. Consequently, interpretation of…

Tahun Terbit

1997

Edisi

1

Deskripsi Fisik

xxxii, 852p: ill: 26 cm

Judul Seri

Jil 2

No. Panggil

R.2X1.3 HAM 1Jil.2