EconPapers    
Economics at your fingertips  
 

Lower-crustal earthquakes in southern Tibet are linked to eclogitization of dry metastable granulite

Feng Shi, Yanbin Wang (), Tony Yu, Lupei Zhu, Junfeng Zhang, Jianguo Wen, Julien Gasc, Sarah Incel, Alexandre Schubnel, Ziyu Li, Tao Chen, Wenlong Liu, Vitali Prakapenka and Zhenmin Jin
Additional contact information
Feng Shi: China University of Geosciences
Yanbin Wang: The University of Chicago
Tony Yu: The University of Chicago
Lupei Zhu: Saint Louis University
Junfeng Zhang: China University of Geosciences
Jianguo Wen: Argonne National Laboratory
Julien Gasc: École Normale Supérieure PSL Research University
Sarah Incel: École Normale Supérieure PSL Research University
Alexandre Schubnel: École Normale Supérieure PSL Research University
Ziyu Li: Saint Louis University
Tao Chen: China University of Geosciences
Wenlong Liu: China University of Geosciences
Vitali Prakapenka: The University of Chicago
Zhenmin Jin: China University of Geosciences

Nature Communications, 2018, vol. 9, issue 1, 1-13

Abstract: Abstract Southern Tibet is the most active orogenic region on Earth where the Indian Plate thrusts under Eurasia, pushing the seismic discontinuity between the crust and the mantle to an unusual depth of ~80 km. Numerous earthquakes occur in the lower portion of this thickened continental crust, but the triggering mechanisms remain enigmatic. Here we show that dry granulite rocks, the dominant constituent of the subducted Indian crust, become brittle when deformed under conditions corresponding to the eclogite stability field. Microfractures propagate dynamically, producing acoustic emission, a laboratory analog of earthquakes, leading to macroscopic faults. Failed specimens are characterized by weak reaction bands consisting of nanometric products of the metamorphic reaction. Assisted by brittle intra-granular ruptures, the reaction bands develop into shear bands which self-organize to form macroscopic Riedel-like fault zones. These results provide a viable mechanism for deep seismicity with additional constraints on orogenic processes in Tibet.

Date: 2018
References: Add references at CitEc
Citations:

Downloads: (external link)
https://www.nature.com/articles/s41467-018-05964-1 Abstract (text/html)

Related works:
This item may be available elsewhere in EconPapers: Search for items with the same title.

Export reference: BibTeX RIS (EndNote, ProCite, RefMan) HTML/Text

Persistent link: https://EconPapers.repec.org/RePEc:nat:natcom:v:9:y:2018:i:1:d:10.1038_s41467-018-05964-1

Ordering information: This journal article can be ordered from
https://www.nature.com/ncomms/

DOI: 10.1038/s41467-018-05964-1

Access Statistics for this article

Nature Communications is currently edited by Nathalie Le Bot, Enda Bergin and Fiona Gillespie

More articles in Nature Communications from Nature
Bibliographic data for series maintained by Sonal Shukla () and Springer Nature Abstracting and Indexing ().

 
Page updated 2025-03-19
Handle: RePEc:nat:natcom:v:9:y:2018:i:1:d:10.1038_s41467-018-05964-1