Slab interactions in the Taiwan region based on the P- and S-velocity distributions in the upper mantle

• P- and S-velocity anomalies in the mantle beneath Taiwan are presented. • Seismic tomography clearly reveals two slabs beneath Taiwan. • The origin of Taiwan is due to collision of two oppositely oriented subduction zones.

Gespeichert in:
Autor*in:

Koulakov, Ivan [verfasserIn]

Wu, Yih-Min

Huang, Hsin-Hua

Dobretsov, Nikolay

Jakovlev, Andrey

Zabelina, Irina

Jaxybulatov, Kairly

Chervov, Viktor

Format:

E-Artikel

Sprache:

Englisch

Erschienen:

2014

Schlagwörter:

Ryukyu arc

Taiwan

Seismic tomography

Collision

Luzon arc

Subduction

Umfang:

12

Übergeordnetes Werk:

Enthalten in: Comparison of the prevalence and changing resistance to nalidixic acid and ciprofloxacin of Shigella between Europe–America and Asia–Africa from 1998 to 2009 - 2012transfer abstract, Amsterdam [u.a.]

Übergeordnetes Werk:

volume:79 ; year:2014 ; day:5 ; month:01 ; pages:53-64 ; extent:12

Links:

Volltext

DOI / URN:

10.1016/j.jseaes.2013.09.026

Katalog-ID:

ELV033648441

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