In:
Journal of Geophysical Research: Solid Earth, American Geophysical Union (AGU), Vol. 124, No. 11 ( 2019-11), p. 12077-12098
Abstract:
Mesozoic strike‐slip motion along the Altyn Tagh Fault (ATF) shearing zone controlled the formation of transtensional basins Change in the direction of regional stress field occurred during the Late Jurassic‐Early Cretaceous The Qilian Shan and the Qaidam Basin were completely inverted under a N‐S or NE‐SW oriented compression during the Early Cenozoic
Type of Medium:
Online Resource
ISSN:
2169-9313
,
2169-9356
DOI:
10.1029/2019JB018086
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2019
detail.hit.zdb_id:
2016813-5
detail.hit.zdb_id:
161666-3
detail.hit.zdb_id:
3094197-0
SSG:
16,13
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