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Back-arc heterogeneity and final closure of the Hegenshan-Nenjiang Ocean: constraints from Paleozoic successions of the Xing’an accretionary terrane, NE China

delete2026-03-28
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OA
AI
Z
Zhiwei Song
C
Chenyue Liang *
F
Franz Neubauer
C
Christoph von Hagke
Y
Yongjiang Liu
J
Jianbo Zhou
C
Changqing Zheng
X
Xianghe Jia
G
Guochun Zhao
DOI：10.1016/j.gsf.2026.102311delete
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Abstract

Abstract

En 中文
• “Ordovician” strata were deposited in the Late Silurian and Early Carboniferous. • A Paleozoic back-arc extensional system exists in the Xing’an Accretionary Terrane. • Along-strike heterogeneity characterizes the back-arc basins of the HNO. • The final closure of the HNO is constrained to the Carboniferous (ca. 330–310 Ma).
Keywords:
Structural analysis
Zircon U-Pb dating
Provenance analysis
Xing’an Accretionary Terrane
Central Asian Orogenic Belt
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Journal

Geoscience Frontiers cover
Geoscience Frontiers
IF:
8.9
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1.9K
Citations:
1.2W

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