In:
Tectonics, American Geophysical Union (AGU), Vol. 36, No. 7 ( 2017-07), p. 1352-1375
Abstract:
Pyrenean foreland basin sediment sources progressively evolved from east to west in response to diachronous uplift across the Pyrenees Sediment from nonorogenic sources are present throughout the Eocene deposits, from either first cycle or recycled from early foreland deposits Fluctuation of U‐Pb and (U‐Th)/He spectra indicates high‐frequency provenance changes superimposed over primary trends
Type of Medium:
Online Resource
ISSN:
0278-7407
,
1944-9194
DOI:
10.1002/2017TC004504
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2017
detail.hit.zdb_id:
2013221-9
detail.hit.zdb_id:
780264-X
SSG:
16,13
SSG:
13
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