Reconstructing Ocean‐Plate Stratigraphy (OPS) to Understand Accretionary Style and Mélange Fabric: Insights From the Bangong‐Nujiang Suture (Tibet, China)-Reference-Cited by-同舟云学术

Reconstructing Ocean‐Plate Stratigraphy (OPS) to Understand Accretionary Style and Mélange Fabric: Insights From the Bangong‐Nujiang Suture (Tibet, China)

Published:2021-09-23 Issue:18 Volume:48 Page:
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophysical Research Letters

Author:

Zeng Min¹²³^ORCID,Zhang Ruisi¹⁴,Chen Si²,Liu Xinyu²,Li Chenwei²^ORCID,Ettensohn Frank R.⁵,Bie Lidong⁶

Affiliation:

1. School of Earth Sciences Yunnan University Kunming China

2. College of Earth Sciences Chengdu University of Technology Chengdu China

3. Key Laboratory of Sanjiang Metallogeny, Resources Exploration & Utilization Ministry of Natural Resources Kunming China

4. College of Geophysics Chengdu University of Technology Chengdu China

5. Department of Earth & Environmental Sciences University of Kentucky Lexington KY USA

6. Geophysical Institute (GPI), Karlsruhe Institute of Technology Karlsruhe Germany

Funder

National Natural Science Foundation of China

Chengdu University of Technology

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021GL094457

Reference68 articles.

1. Detrital zircon ages from the Chugach terrane, southern Alaska, reveal multiple episodes of accretion and erosion in a subduction complex

2. Deformation of a seamount subducting beneath an accretionary prism: Constraints from numerical simulation

3. Seamount subduction erosion in the Nankai Trough and its potential impact on the seismogenic zone

4. The western Durkan Complex (Makran Accretionary Prism, SE Iran): A Late Cretaceous tectonically disrupted seamounts chain and its role in controlling deformation style

5. Three-dimensional velocity structure of the northern Hikurangi margin, Raukumara, New Zealand: Implications for the growth of continental crust by subduction erosion and tectonic underplating

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