In:
Geochemistry, Geophysics, Geosystems, American Geophysical Union (AGU), Vol. 23, No. 3 ( 2022-03)
Abstract:
Multi‐phase intercontinental collision is identified in western Anatolia by sedimentary basin changes Sedimentary provenance change indicate collision was at 76 Ma, but significant thick‐skinned deformation was delayed until 54 Ma The 20 Myr duration of initial collision can be explained by three multi‐stage mechanisms involving changes in plate coupling
Type of Medium:
Online Resource
ISSN:
1525-2027
,
1525-2027
DOI:
10.1029/2021GC010232
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2022
detail.hit.zdb_id:
2027201-7
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