In:
Journal of Geophysical Research: Solid Earth, American Geophysical Union (AGU), Vol. 121, No. 10 ( 2016-10), p. 7514-7546
Abstract:
Three seismic refraction profiles constrain the crustal structure along the Kermadec arc The north Kermadec fore‐arc hosts the Eocene Tonga arc. Back‐arc crustal thickness is 4 km thinner south of the Central Kermadec Discontinuity Along‐strike transitions in crustal structure are inherited and reflect the Cenozoic evolution of the Tonga‐Kermadec margin
Type of Medium:
Online Resource
ISSN:
2169-9313
,
2169-9356
DOI:
10.1002/jgrb.v121.10
DOI:
10.1002/2016JB013194
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2016
detail.hit.zdb_id:
2016813-5
detail.hit.zdb_id:
161666-3
detail.hit.zdb_id:
3094197-0
SSG:
16,13
Permalink